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第 6 卷第 1 期 

古生物学文摘 ( 网络版 ) 

目 

录 

2010 年 3 月 

古生物学 

综论 ………………………(1) 

遗迹化石 …………………(8) 

分子古生物学 ……………(10) 

古生态学 …………………(14) 

微体古生物学 

综论 ………………………(20) 

孢粉 ………………………(21) 

牙形石 ……………………(31) 

小壳化石 …………………(34) 

古植物学 

综论 ………………………(35) 

藻类 ………………………(37) 

真菌 ………………………(41) 

蕨类植物 ( 广义 )………(42) 

早期种子植物 ……………(43) 

裸子植物 …………………(43) 

被子植物 …………………(44) 

古无脊椎动物学 

原生动物 …………………(45) 

古杯、多孔及腔肠动物 …(52) 

苔藓动物 …………………(55) 

腕足动物 …………………(59) 

软体动物 …………………(70) 

节肢动物 …………………(86) 

棘皮动物 …………………(119) 

分类位置不明 ……………(121) 

古脊椎动物学 

综论 ………………………(123) 

鱼类 ………………………(124) 

两栖类 ……………………(128) 

爬行类 ……………………(128) 

鸟类 ………………………(134) 

哺乳类 ……………………(136) 

古人类学 

古人类学 …………………(145) 

历史地质学、地层学 

综论 ………………………(146) 

古地理学、古气候学 ……(150) 

前古生界 …………………(153) 

古生界 ……………………(158) 

中生界 ……………………(169) 

新生界 ……………………(180)

第 6 卷第 1 期 

古生物学文摘 ( 网络版 ) 

2010 年 3 月 

古生物学 

综论 

2010010001 

回复 : 碳酸盐岩中记录的后生动物支 

系早新元古代起源的证据 = Early 

Neoproterozoic origin of the metazoan 

clade recorded in carbonate rock texture: 

REPLY. ( 英文 ). Neuweiler F; Turner E 

C; Burdige D J. Geology, 2009, 37(9): 

E196-E196 

2010010002 

安第斯中部晚中新世海侵高潮的同位 

素、古生物和遗迹学证据 = Isotopic, 

paleontologic, and ichnologic evidence 

for late Miocene pulses of marine incursions 

in the central Andes. ( 英文 ). Uba 

C E; Hasler C A; Buatois L A; Schmitt 

A K; Plessen B. Geology, 2009, 37(9): 

827-830 

Recognition of an inferred Miocene 

marine incursion affecting areas from 

Colombia through Peru and Bolivia and 

into Argentina is essential to delineate 

the South American Seaway. In Bolivia, 

corresponding strata of inferred marine 

origin have been assigned to the late 

Miocene Yecua Formation. We carried 

out high-resolution delta C-13 and delta 

O-18 isotopic studies on 135 in situ carbonates 

from 3 outcrops, combined with 

detailed sedimentologic, paleontologic, 

and ichnologic analysis. Four less negative 

delta C-13 excursion levels were 

recorded that coincide well with beds 

containing marine body (barnacle) and 

trace (Ophiomorpha) fossils. These 

strata are interbedded with red-green 

beds containing mudcracks, plant roots, 

gypsum, and trace fossils of the continental 

Scoyenia ichnofacies. Our data 

are significant in that they show for the 

first time four possible short-lived marine 

incursions in the Bolivian central 

Andes during the late Miocene. The result 

is constrained by a new U-Pb date 

of 7.17 +/- 0.34 Ma at the top of Yecua 

strata. 

2010010003 

两侧对称动物的崛起 = The rise of bilaterians. 

( 英文 ). Freeman G. Historical 

Biology, 2009, 21(1 & 2): 99-114 

Recently Shen et al. have argued that 

the Ediacaran faunas from Avalon- 

Charnwood [580-560 million years ago 

(MA)], the White Sea-Flinders Range 

(560-550 MA) and Namibia (550- 

543 MA) occupied the same morphospace 

even though these faunas differed 

in species composition, ecology, biogeography 

and age. The traits they used 

to characterise these faunas could not 

distinguish between important promorphological 

features such as radial vs. bilaterian 

and unitary vs. colonial animals. 

Their inappropriate assignment of symmetry 

properties led to the homogenisation 

of morphospace in these different 

faunas. Another way to examine shifts in 

morphospace involves sorting out radial 

vs. bilaterian and unitary vs. colonial 

genera in terms of their time of first appearance 

in the fossil record. While genera 

with both kinds of symmetry properties 

and unitary and colonial animals 

were present during the early Ediacaran, 

there was a large proportional increase 

in new bilaterian genera and a decrease 

1

in colonial genera beginning between 

560-550 MA. The increase in bilaterians 

may have been associated with the ability 

to exploit food sources in and on the 

substrate of shallow water environments. 

2010010004 

来自过去的声音 : 关于古生代与中生 

代动物声音的综述 = Voices of the past: 

a review of Paleozoic and Mesozoic 

animal sounds. ( 英文 ). Senter P. Historical 

Biology, 2008, 20(4): 255-287 

Here, I present a review and synthesis 

of fossil and neontological evidence to 

find major trends in the pre-Cenozoic 

evolution of animal acoustic behaviour. 

Anatomical, ecological and phylogenetic 

data support the following scenario. 

Stridulating insects, including crickets, 

performed the first terrestrial twilight 

choruses during the Triassic. The twilight 

chorus was joined by water boatmen 

in the Lower Jurassic, anurans in 

the Upper Jurassic, geckoes and birds in 

the Lower Cretaceous, and cicadas and 

crocodilians in the Upper Cretaceous. 

Parallel evolution of defensive stridulation 

took place multiple times within 

Malacostraca, Arachnida and Coleoptera. 

Parallel evolution of defensive and 

courtship-related sound production took 

place in Actinopterygii, possibly as early 

as the Devonian. Defensive vocalisations 

by tetrapods probably did not appear 

until their predators acquired tympanic 

ears in the Permian. Tympanic 

ears appeared independently in Diadectomorpha, 

Seymouriamorpha, Parareptilia, 

Diapsida and derived Synapsida. 

Crocodilians and birds acquired vocal 

organs independently, and there is no 

anatomical evidence for vocal ability in 

bird-line archosaurs basal to the avian 

clade Ornithothoraces. Acoustic displays 

by non-avian dinosaurs were therefore 

probably non-vocal. Other aspects of the 

evolution of acoustic behaviour in these 

and other lineages are also discussed. 

2010010005 

宾夕法尼亚州 Buckhorn Asphalt 

Quarry 沉积相分析与动物群 : 一个 

以文石保存的重要的古生代化石库的 

回顾与新资料 = Facies and fauna of the 

Pennsylvanian Buckhorn Asphalt 

Quarry deposit: a review and new data 

on an important Palaeozoic fossil Lagerstätte 

with aragonite preservation. ( 英 

文 ). Seuß B; Nützel A; Mapes R H; 

Yancey T E. Facies, 2009, 55(4): 609- 

645 

The Pennsylvanian Buckhorn Asphalt 

Quarry contains the best-preserved Palaeozoic 

mollusc fauna in the world. 

Early impregnation of mixed siliciclastic–carbonate 

rocks (mudstones, pack to 

grainstones, shell beds, and conglomerates) 

with hydrocarbons prevented aragonite 

destruction (“Impregnation Fossil 

Lagerstätte”). The exceptional preservation 

comprises shell microstructures, 

microornaments and early ontogenetic 

shells. Most gastropods had planktotrophic 

larval development indicating a 

high primary production although the 

remains of phytoplankton are very rare 

in this and other Late Palaeozoic deposits. 

Deposition occurred close to a shallow-water 

coastal area. Mass flow processes 

(density currents) triggered by 

storms were involved in the transport 

mechanisms of some units. Shells of 

benthic molluscs yield the most diverse 

known Palaeozoic microboring assemblage, 

indicating at least partly euphotic 

conditions. The invertebrate fauna comprises 

about 160 species and is dominated 

by molluscs, which is unusual for 

a Palaeozoic deposit, suggesting that 

aragonite dissolution produces a major 

bias in the fossil record. However, most 

mollusc genera in the Buckhorn deposit 

are also known from other Pennsylvanian 

occurrences as recrystallised shells. 

This shows that preservation bias via 

preferential aragonite dissolution may be 

overestimated. 

2

2010010006 

过去或现今生命的遗迹 : 是生物信号 

和潜在的生命指示者吗 ? = Traces of 

past or present life: Bio-signatures and 

potential life indicators?. ( 英文 ). Gargaud 

M; Mustin C; Reisse J. Comptes 

Rendus Palevol, 2009, 8(7): 593-603 

Historical sciences are based on archives. 

What is true for human history is 

also true for the history of life. In human 

history, archives are easily identified; 

they are manuscripts, paintings, buildings, 

sculptures, artefacts. As soon as we 

go further into the past, the situation becomes 

different. A carefully polished 

stone with a symmetrical shape is, without 

any possible doubt, an archive but 

what about a stone with some edges 

which could as well be man-made as 

shaped by natural processes? Anthropologists 

reach sometimes an agreement, 

but in other cases, the question remains 

unanswered. Even if it is an agreement 

about the fact that the stone is indeed a 

human artefact, dating an object is not 

obvious at all. The dating is necessarily 

an indirect process, based on observations, 

which do not concern the object 

itself but the context in which it was discovered. 

2010010007 

在矿物中寻找生命的痕迹 = Looking 

for traces of life in minerals. ( 英文 ). 

Benzerara K; Menguy N. Comptes Rendus 

Palevol, 2009, 8(7): 617-628 

Traces of life have been extensively 

looked for in minerals. It is indeed 

thought that a wide diversity of living 

organisms can control the formation of 

mineral phases and thus may leave imprints 

of their activity in the morphology, 

chemistry and crystallographic structure 

of the mineral end-product. Here, we 

illustrate the bases and limits of this approach 

by reviewing some studies on 

biogenic magnetites and carbonates. 

More than an exhaustive review, we 

give a personal view on the limitations 

provided by an empirical approach 

based on defining so-called biosignatures 

and suggest developing a more 

comprehensive mechanistic understanding 

of how life controls mineral nucleation 

and growth and induces potential 

specific features 

2010010008 

仿生类型的化学合成 = Chemical synthesis 

of biomimetic forms. ( 英文 ). 

Livage J. Comptes Rendus Palevol, 2009, 

8(7): 629-636 

The biogenic origin of the first traces 

of life is often based on the morphological 

analysis of microfossils. However 

life-like forms can also be obtained via 

chemical synthesis from purely inorganic 

precursors. Many examples can be 

found in literature that are mainly based 

on aqueous solution chemistry. Osmotic 

growth of gelatinous precipitates is observed 

during the formation of “chemical 

gardens”. Point defects in surfactant 

mesophases lead to mesoporous silica 

with curved shapes. The oriented attachment 

of nanocrystals via hydrophilic 

polymers leads to mesocrystals that exhibit 

a large variety of unusual shapes. 

2010010009 

西澳大利亚皮尔巴拉克拉通和南非巴 

伯顿绿岩带钻孔太古代水热成因岩和 

沉积岩中的生命早期痕迹和调查研究 

= Early traces of life investigations in 

drilling Archean hydrothermal and 

sedimentary rocks of the Pilbara Craton, 

Western Australia and Barberton Greenstone 

Belt, South Africa. ( 英文 ). Philippot 

P; Van Kranendonk M; Van Zuilen 

M; Lepot K. Comptes Rendus 

Palevol, 2009, 8(7): 649-663 

The Pilbara Craton of Western Australia 

and the Barberton Greenstone Belt 

of the Kaapvaal Craton, South Africa, 

contain some of the oldest and best preserved 

Archaean rocks and microfossils 

in the world. Two stratigraphic horizons 

in the Pilbara Craton were drilled as part 

3

of a collaborative effort between France 

and Australia (the Pilbara Drilling Project) 

during August 2004, including the 

3481 Ma Dresser Formation (Warrawoona 

Group) and 2724 Ma Tumbiana 

Formation (Fortescue Group). A new 

diamond drill hole was cored in August 

2008 through part of the 3250 Ma Fig 

Tree Group in the Barberton Greenstone 

Belt as part of a joint project between 

France and South Africa. These pristine 

diamond drill cores present a unique opportunity 

to constrain the chemistry of 

the earliest ocean, the composition of the 

atmosphere, and the settings and types 

of microbial ecosystems spanning the 

Archean Eon. These drill core samples 

can also provide new clues on the earliest 

metabolic pathways 

2010010010 

在地面模拟环境中天体生物学技术和 

仪器操作的有效性 = Validation of 

astrobiology technologies and instrument 

operations in terrestrial analogue 

environments. ( 英文 ). Léveillé R. 

Comptes Rendus Palevol, 2009, 8(7): 

637-648 

Terrestrial analogue environments are 

places on Earth that present geological 

or environmental conditions that are 

similar to those found on an extraterrestrial 

body. Analogue environments serve 

four functions: (1) learn about planetary 

processes on Earth and elsewhere; (2) 

test technologies, methodologies, and 

protocols; (3) train highly-qualified personnel, 

as well as science and operations 

teams; (4) engage the public, space 

agencies, media, and educators. Analogue 

studies also enable the development 

and validation of biosignatures and 

detection techniques. Analogue programs 

include the Canadian Space 

Agency's Canadian Analogue Research 

Network, NASA's Astrobiology Science 

and Technology for Exploring Planets, 

and NASA's Analog Missions. Examples 

of technology and instrument testing 

and validation in analogue environments 

include the Haughton-Mars Project 

Research Station, the Arctic Mars 

Analog Svalbard Expedition (AMASE), 

the Rio Tinto basin, and NASA's Field 

Integrated Design and Operations 

(FIDO). 

2010010011 

生物活性和地球表面的演化 : 从岩石 

记录中观察碳 , 硫 , 氮和铁的稳定同 

位素的变化 = Biologi-cal activity and 

the Earth's surface evolution: Insights 

from carbon, sulfur, nitro-gen and iron 

stable isotopes in the rock record. ( 英文 ). 

Thomazo C; Pinti D L; Busigny V; Ader 

M; Hashizume K; Philippot P. Comptes 

Ren-dus Palevol, 2009, 8(7): 665-678 

The search for early Earth biological 

activity is hindered by the scarcity of the 

rock record. The very few exposed 

sedimentary rocks have all been affected 

by secondary processes such as metamorphism 

and weathering, which might 

have distorted morphological microfossils 

and biogenic minerals beyond recognition 

and have altered organic matter 

to kerogen. The search for biological 

activity in such rocks therefore relies 

entirely on chemical, molecular or isotopic 

indicators. A powerful tool used 

for this purpose is the stable isotope signature 

of elements related to life (C, N, 

S, Fe). It provides key informations not 

only on the metabolic pathways operating 

at the time of the sediment deposition, 

but more globally on the biogeochemical 

cycling of these elements and 

thus on the Earth's surface evolution. 

Here, we review the basis of stable isotope 

biogeochemistry for these isotopic 

systems. Rather than an exhaustive approach, 

we address some examples to 

illustrate how they can be used as 

biosignatures of early life and as proxies 

for its environment, while keeping in 

mind what their limitations are. We then 

focus on the covariations among these 

isotopic systems during the Archean 

time period to show that they convey 

important information both on the evolu- 

4

tion of the redox state of the terrestrial 

surface reservoirs and on co-occurring 

ecosystems in the Archean. 

2010010012 

使用光谱指纹法确定可居住太阳系外 

行星的特征 = Characterizing habitable 

extrasolar planets using spectral fingerprints. 

( 英文 ). Kalteneggera L; Selsis F. 

Comptes Rendus Palevol, 2009, 8(7): 

679-691 

The detection and characterization of 

an Earth-like planet is approaching rapidly 

thanks to radial velocity (RV) surveys 

(e.g. HARPS) and transit searches 

(Corot, Kepler). A rough characterization 

of these planets will be already 

achievable in 2014 with the James Webb 

Space Telescope, and more detailed 

spectral studies will be obtained by future 

large ground based telescopes (ELT, 

TNT, GMT), and dedicated space-based 

missions like Darwin, Terrestrial Planet 

Finder, New World Observer. In this article 

we discuss how we can read a 

planet's spectrum to assess its habitability 

and search for the signatures of a 

biosphere. Identifying signs of life implies 

understanding how the observed 

atmosphere physically and chemically 

works, and thus gathering information 

on the planet in addition to observing its 

spectral fingerprint. 

2010010013 

华北地台中元古代碳酸盐中的微生物 

席及其生成油气的潜力 = Microbial 

Mats in the Mesoproterozoic Carbonates 

of the North China Platform and Their 

Potential for Hydrocarbon Generation. 

( 英文 ). Shi Xiaoying; Zhang Chuanheng; 

Jiang Ganqing; Liu Juan; Wang Yi; Liu 

Dianbo. Journal of China university of 

geosciences, 2008, 19(5): 549-566 

The well-preserved Mesoproterozoic 

succession in the North China platform 

consists mainly of three lithological associations 

including peritidal quartz 

sandstone, shallow marine and lagoonal 

dark to black shales, and shallow epeiric 

carbonates, with a total thickness of up 

to 8 000 m. In addition to welldocumented 

microplants, macroalgae, 

and microbial buildups, abundant microbially 

induced sedimentary structures 

(MISS) and mat-related sediments have 

been recognized in these rocks. Intensive 

microbial mat layers and MISS are 

especially well preserved in the carbonates 

of the upper Gaoyuzhuang (ca. 1.5 

Ga) and lower Wumishan (ca. 1.45 Ga) 

formations, indicating diversified microbial 

activities and a high organic production. 

In these petrified biomats, putative 

microbial fossils (both coccoidal 

and filamentous) and framboidal pyrites 

have been identified. The abundance of 

authigenic carbonate minerals in the host 

rocks, such as, acicular aragonites, rosette 

barites, radial siderites, ankerites, 

and botryoidal carbonate cements, suggests 

authigenic carbonate precipitation 

from anaerobic oxidation of methane 

(AOM) under anoxic/euxinic conditions. 

Warm climate and anoxic/euxinic conditions 

in the Mesoproterozoic oceans may 

have facilitated high microbial productivity 

and organic burial in sediments. 

Although authigenic carbonate cements 

may record carbonate precipitation from 

anaerobic methane oxidation, gas blister 

(or dome) structures may indicate gas 

release from active methanogenesis during 

shallow burial. Bituminous fragments 

in mat-related carbonates also 

provide evidence for hydrocarbon generation. 

Under proper conditions, the 

Mesoproterozoic mat-rich carbonates 

will have the potential for hydrocarbon 

generation and serve as source rocks. On 

the basis of petrified biomats, a rough 

estimation suggests that the Mesoproterozoic 

carbonates of the North China 

platform might have a hydrocarbon production 

potential in the order of 10 × 10 8 

t. 

5

2010010014 

波罗的古陆 : 中奥陶世生物多样性的 

一个热点 = Baltica: A mid Ordovician 

diversity hotspot. ( 英文 ). Rasmussen C 

M Ø; Hansen J; Harper D A T. Historical 

Biology, 2007, 19(3): 255-261 

A detailed bed-by-bed study of late 

Early—early Mid Ordovician Eastern 

Baltic brachiopods has been used to 

construct an -diversity curve through 

the upper Billingen—Kunda regional 

stages (Arenig-early Llanvirn). Surprisingly 

the main peak in diversity does not 

occur until the Volkhov-Kunda boundary, 

whereas global data indicate a peak 

in the mid Volkhov. On Baltica especially 

the orthidines show a time lag 

compared with the global data. This 

study is based more than 30 000 specimens 

collected from argillaceous limestones 

with interfingering marls at eight 

different localities in the East Baltic area. 

2010010015 

伊比利亚半岛上白垩统独特的新发 

现 : 西班牙 Cuenca 地区 “Lo Hueco” 

的古生物遗址 = New and exceptional 

discovery in the Upper Cretaceous of the 

Iberian Peninsula: the palaeontological 

site of “Lo Hueco”, Cuenca, Spain. ( 英 

文 ). Barroso-Barcenilla F; Cambra-Moo 

O; Escaso F; Ortega F; Pascual A; 

Perez-Garcia A; Rodriguez-Lazaro J; 

Sanz J L; Segura M & Torices A. Cretaceous 

Research, 2009, 30(5): 1268- 

1278 2 图版 . 

The palaeontological site of “Lo 

Hueco” was discovered in Cuenca, 

Spain, in 2007. It includes a stratigraphic 

interval in “Garumn” facies belonging 

to the upper part of the Villalba 

de la Sierra Formation. A succession of 

versicolor marly mudstone levels (V, G1, 

R1, G2, R2 and M) can be observed at 

the site studied. This succession is partially 

modified by a sandy channel structure 

(C) and by a sulphated interval (S). 

The C structure and the G1, G2 and R2 

(lower part) levels have an extremely 

rich and varied fossil concentration and 

have provided to date more than 8500 

macroremains. These are mainly from 

vertebrates, but also from plants and invertebrates. 

In general, vertebrates are 

represented by mineralized bones with 

an early infilling of gypsum, a ferruginous 

crust, and a secondary precipitation 

of gypsum; invertebrates by internal 

moulds; and plants by carbonized remains. 

Among the vertebrates, titanosaur 

dinosaurs (some of them with partially 

articulated skeletons) are by far the 

most common representatives, although 

lepisosteid fishes, bothremydid turtles, 

squamate lizards, eusuchian crocodiles, 

and ornithischian and theropod dinosaurs 

are also well represented. The relative 

stratigraphic position and the palaeontological 

content of this site allow to 

attribute it to the upper Campanianlower 

Maastrichtian. Interpretation of its 

materials suggests a near coast muddy 

flood plain crossed by distributary sandy 

channels environment, exposed to brackish 

to fresh water aquatic influence. 

2010010016 

俄勒冈州 John Day 组 ( 龟背湾及金 

伯利段 ) 的年代地层学和生物地层学 

修订兼论北美阿里卡里阶陆生哺乳动 

物的年龄校正 = Revised chronostratigraphy 

and biostratigraphy of the John 

Day Formation (Turtle Cove and Kimberly 

Members), Oregon, with implications 

for updated calibration of the Arikareean 

North American land mammal 

age. ( 英文 ). Albright L B; Woodburne 

M O; Fremd T J; Swisher C C; MacFadden 

B J; Scott G R. Journal of Geology, 

2008, 116(3): 211-237 

Although the Arikareean North 

American land mammal age was first 

typified in the Great Plains, the succession 

there contains significant unconformities, 

a generally poor magnetic record, 

relatively sparse radioisotopic 

calibration, and a major faunal hiatus. In 

the John Day Valley of central Oregon, 

6

however, is a thick, remarkably complete 

sequence of Oligocene through 

early Miocene strata ( the John Day 

Formation) potentially amenable to addressing 

these shortcomings and long 

known to harbor one of the richest records 

of mid-Tertiary mammals in North 

America. Since Prothero and Rensberger's 

first magnetostratigraphic study of 

the John Day Formation in 1985, new 

advances in geochronology, together 

with a more comprehensive suite of paleomagnetic 

sections keyed to new radioisotopic 

and biostratigraphic data, 

have greatly enhanced chronostratigraphic 

precision. In our attempt to refine 

John Day chronostratigraphy, we 

sampled nearly 300 sites for magnetostratigraphy 

over a 500-m-thick interval 

and used several radioisotopically dated 

volcanic tuffs for our correlation with 

the geomagnetic polarity timescale. 

Many of the rocks analyzed showed unusual 

magnetic behavior, possibly due to 

the known zeolitization in this region, 

thereby precluding an abundance of 

class 1 polarity determinations. Nevertheless, 

preliminary results indicate that 

the Turtle Cove Member stratigraphically 

upward through the lower Kimberly 

Member extends from late chron 

C12n through C7n. 1r, or from about 

30.6 to 24.1 Ma. Intensive radioisotopic 

and magnetostratigraphic characterization 

of these strata provides a framework 

by which the associated biostratigraphy 

is assessed for biochronological significance 

relative to fossiliferous successions 

of the Great Plains, in turn resulting 

in reassessment of Arikareean subbiochron 

(Ar1-Ar4) boundaries. We present 

a revision of those boundaries that 

differs from their traditional timing as a 

hypothesis for testing in other locations. 

2010010017 

热障和坡栖动物群的毁灭 = Thermal 

barriers and the fate of perched faunas. 

( 英文 ). Stanley S M. Geology, 2010, 

38(1): 31-34 

Thermal barriers provide an explanation 

for the geologically sudden extinction 

of benthic faunas of epeiric seas 

when these seas disappeared by contracting 

to the open ocean. Biotic interactions 

could not have caused the sudden extinctions, 

and neither could reduction of 

the regional area of seafloor because 

substantial areas of shallow seafloor remained 

along neighboring continental 

shelves when epeiric seas drained. Instead, 

temperature contrasts must have 

been responsible. Epeiric seas had 

strongly seasonal climates, and when 

some receded to continental margins, 

many of their species would have encountered 

waters that failed to provide 

the maximum or minimum temperature 

required for reproduction. When epeiric 

seas receded poleward, equatorward, or 

into Coriolis-driven currents, many species 

faced lethal temperatures. The history 

of the Jurassic Sundance Sea provides 

a striking example of the fate of a 

warm-adapted fauna driven westward 

into an area dominated by a cool, Coriolis-driven 

current. 

2010010018 

加拿大纽芬兰 5.65 亿年的错点组中埃 

迪卡拉生物群自主移动的首个证据 = 

First evidence for locomotion in the 

Ediacara biota from the 565 Ma Mistaken 

Point Formation, Newfoundland. 

( 英文 ). Liu A G; Mcllroy D; Brasier M 

D. Geology, 2010, 38(2): 123-126 

Evidence for locomotion in the Precambrian 

fossil record is scant. Reliable 

Ediacaran trace fossils are all younger 

than 560 Ma, and consist of relatively 

simple horizontal burrows and trails 

from shallow-water deposits. Here we 

describe an assemblage of macroscopic 

locomotory traces from deep-water environments 

at Mistaken Point, southeastern 

Newfoundland, Canada, dated to ca. 

565 Ma. These trails extend the record 

of complex trace fossils back into the 

earliest Avalonian biota. Our new evidence 

for large motile organisms on the 

7

seafloor at this time suggests that at least 

some of these early Ediacaran organisms, 

whose biological affinities are 

widely debated, could have been muscular 

and of metazoan grade 

2010010019 

2008 年莫斯科自然探险者协会中的古 

生物部 = Section of paleontology of the 

Moscow Society of Nature Explorers in 

2008. ( 英文 ). Amitrov O V. Paleontological 

Journal, 2009, 43(5): 594-597 

2010010020 

回溯俄罗斯古生物学史 = From the 

history of Russian paleontology. ( 英文 ). 

Lobacheva S V. Paleontological Journal, 

2010, 44(1): 99-103 

2010010021 

系统发生与演化生物学 = Phylogeny 

and evolutionary biology. ( 英文 ). 

Tatarinov L P. Paleontological Journal, 

2010, 44(2): 117-119 

The phylogenetic system of Hennig, 

which was designed for classification of 

synchronous organisms, has only been 

adapted secondarily to total reconstruction 

of phylogeny. All fields of fundamental 

biology are related to the development 

of evolutionary theory. A better 

understanding of the origin of life requires 

new concepts of the historical geology 

of prebiological environment and 

new concepts of molecular genetics and 

biochemistry concerning ribonucleic acids 

as the initial units for the origin of 

life. 

2010010022 

再读多样性曲线 = Diversity curves revisited. 

( 英文 ). Ponomarenko A G; 

Dmitriev V Yu. Paleontological Journal, 

2009, 43(2): 226-229 

遗迹化石 

2010010023 

四川自贡地区晚侏罗世剑龙类皮肤印 

痕化石新观察 = Stegosaurian skin impressions 

from the Upper Jurassic 

Shangshaximiao Formation, Zigong, Sichuan, 

China. ( 中文 ). 邢立达 ; 彭光照 ; 

舒纯康 . 地质通报 , 2008, 27(7): 1049- 

1053 

重新观察了四川自贡晚侏罗世上沙 

溪庙组巨棘龙皮肤印痕化石。化石材 

料清楚地显示了巨棘龙体被鳞片。这 

些鳞片总体镶嵌排列成网状。大多数 

鳞片呈五边形 , 少数呈四边形或六边 

形。鳞片之间以沟缝相接。小鳞片中 

散布有少量五边形或六边形的大鳞 

片 , 每枚大鳞片被 13~14 枚鳞片所 

环绕。鳞片表面粗糙 , 不存在 “ 瘤状 

小突 ”, 有条索状隆突。条索状隆突 

可降低环境光线造成的眩光 , 降低鳞 

片表面整体亮度水平。据原始埋藏的 

位置和鳞片的分布推测 , 四川巨棘龙 

皮肤印痕化石的身体位置可能为前肢 

的肘关节及其邻近的上臂、体侧的皮 

肤 . 

2010010024 

冰室 , 冷水型碳酸盐斜坡 : 以西西里 

岛上新世 Capodarso 组上部为例 : 遗 

迹化石在前积楔状体成长期重建中的 

作用 = Icehouse, cool-water carbonate 

ramps: the case of the Upper Pliocene 

Capodarso Fm (Sicily): role of trace fossils 

in the reconstruction of growth 

stages of prograding wedges. ( 英文 ). 

Massari F; Alessandro A D. Facies, 

2010, 56(1): 47-58 

An integrated approach, based on the 

use of trace fossils combined with 

analysis of physical and biogenic structures, 

identification of key surfaces, and 

reconstruction of stratigraphic architecture, 

proved to be of critical value in defining 

the depositional environments, 

elucidating the dynamics of progradation, 

and characterizing the various systems 

tracts of Upper Pliocene progradational 

wedges (Capodarso area, Sicily) 

generated by cool-water carbonate 

8

amps. The studied succession consists 

of a stack of six cycles, consisting of terrigenous 

mudstones passing upwards 

into biocalcarenite wedges with distinct 

clinoforms. The prograding biocalcarenite 

bodies show seaward-increasing 

height and steepness of the clinoformed 

front as a result of development into increasingly 

deeper water, and may be regarded 

as the record of distally steepened 

ramps, dominated by storminduced 

downwelling flows. Evidence of 

forced-regressive progradation is provided 

by stratal geometries, physical 

structures, and trace fossil assemblages 

existing at the top of the bodies, which 

attest to a gradual increase in energy 

level at the top of the ramp, concurrently 

with the progression of seaward outbuilding 

of the bodies. Three trace-fossil 

suites (Thalassinoides / Piscichnus, 

Scolicia, Dactyloidites) are shown to be 

linked with the successive growth stages 

of individual prograding wedges, 

whereas abandonment stages, characterized 

by starvation of sediment input, are 

marked by the Ophiomorpha suite. The 

Capodarso ramps, like other Plio- 

Pleistocene equivalents of the Mediterranean 

area, are small, high-gradient 

ramps, with stratigraphical architecture 

controlled by high-amplitude, orbitally 

driven glacio-eustatic changes. An ecologically 

and bathymetrically based subdivision 

of the ramps into inner, mid and 

outer ramp environments is hardly applicable, 

as most of the wedge progradation 

occurs in highly dynamic conditions, 

dominated by physical processes of 

transport and resedimentation of skeletal 

material, which result in faunal composition 

dominated by allochthonous material. 

The use of trace fossils is of critical 

value in this context, due to the scarcity 

of ecological information provided by 

faunal elements. 

2010010025 

重新评价晚二叠世一巨齿龙遗迹 

Pachypes = A re-evaluation of 

Pachypes, a pareiasaurian track from the 

Late Permian. ( 英文 ). Valentini M; 

Nicosia U; Conti M A. Neues Jahrbuch 

fur Geologie u. Palaontologie / Abhandlungen, 

2009, 251(1): 71-94 

The ichnotaxon Pachypes dolomiticus 

Leonardi et al., 1975 from the Upper 

Permian Arenaria di Val Gardena 

(Northern Italy) was erected on the bosis 

of an isolated pes and assigned to pareiasaurs. 

Over the last three decades several 

other footprints haqve been found, 

including partial trackways, allowing 

here to refine the P. dolomiticus features 

and variability and to confirm the biotaxon 

correlation with pareiasaurs. Recently, 

two large reptilian ichnotaxa hve 

been uncovered from the Upper Tatarian 

of Russia. 

2010010026 

美国弗吉尼亚下志留统作为行为古生 

态证据的 Atthrophycus alleghaniensis 

的集群和形态变异 = Clustering and 

morphologic variation in Arthrophycus 

alleghaniensis (Lower Silurian of Virginia, 

USA) as evidence of behavioral 

paleoecology. ( 英文 ). Miller W III; 

Webb F Jr; Raymond L A. Neues Jahrbuch 

fur Geologie u. Palaontologie / 

Abhandlungen, 2009, 251(1): 109-117 

Based on depositional setting, the spatial 

patterns of burrows and their 

morpnhologie variations, the trace producer 

was likely a powerful burrower 

capable of penetrating a thick tidal sand 

blanket, locating food-rich patches 

within a buried mud layer, of mining 

lthe patches (while simultaneouly avoiding 

adjacent burrowers in manycases), 

and backfilling its burrow system as it 

either shifted position for more mining 

activity or withdrew from the area. The 

pattern does not necessarily record the 

activities of hundreds of endobenthic 

animals in a small space, but instead 

could reflect a burst of activity by a 

small population exploiting the food- 

9

ich mud before subsequent deposition 

but the resource out of reach. 

2010010027 

摩洛哥 Iouaridene 向斜上侏罗统行迹 

中的巨形兽足类足迹 = Gigantic theropod 

footprints from Upper Jurassic 

trackways (Iouaridene syncline, Morocco). 

( 其他 ). Boutakiout M; Hadri M; 

Nouri J; Diaz-Martinez I; Perez-Lorente 

F. Revista Espanola de paleontologia, 

2009, 24(1): 31-46 

Gigantic theropod footprints from 

Upper Jurassic trackways (Iouaridene 

syncline, Morocco). The dinosaur ichnological 

research provide data of interest. 

One of them includes the discovery 

of gigantic digitigrade theropod footprints, 

with a not described size. The exposures 

of ichnitic levels are continuous 

in the zone and the continuity of stratigraphic 

beds permits the good correlation. 

All sites are directly linked, except 

one of them that are separated by a 

cover of quaternary glacis sediments. 

After a comparative study it is proposed 

that two of the three gigantic theropod 

trackways and the digitigrade footprints 

described in this paper, are the largest 

dicovered yet in the world. 

2010010028 

西班亚 Cameros 盆地 Los Cayos 恐龙 

产地的龟和翼龙足迹 : 追踪下白垩统 

的生物多样性 = Turtle and pterosaur 

tracks from the Los Cayos dinosaur 

tracksite, Cameros Basin (Cornago, La 

Rioja, Spain): tracking the Lower Cretaceous 

bio-diversity.. ( 英文 ). Moratalla J 

J; Hernan J. Revista Espanola de paleontologia, 

2009, 24(1): 59-77 

The turtle tracks are formed by parallel 

isolated digit impressions. Digits 

show acuminate distal ends and relatively 

blunt proximal margins. Most of 

the tracks show three digits, and only 

two of them are pentadactyl. No trackways 

can be observed but only different 

track alignments suggesting some kind 

of direction of movement. Two trackbearing 

layers have yielded 5 pterosaur 

manus prints. No pes footprints or 

trackways have been discovered at these 

outcrops yet. These prints are tridactyl, 

with digit I, the shortest, and III, the 

longest. The angles between the digits 

are variable: angle I-II is significantly 

bigger than between II-III. These tracks 

from Los Cayos were the first discovery 

of pterosaur tracks in the Enciso Group 

分子古生物学 

2010010029 

分子化石揭示在白垩纪泉水坑中的流 

体组分和流量强度 = Molecular fossils 

reveal fluid composition and flow intensity 

at a Cretaceous seep. ( 英文 ). Peckmann 

J; Birgel D; Kiel S. Geology, 2009, 

37(9): 847-850 

An isolated Hauterivian marine limestone 

from the Crimean Peninsula containing 

masses of articulated specimens 

of the dimerelloid brachiopod Peregrinella 

has previously been interpreted 

to represent a hydrocarbon-seep deposit. 

In order to constrain the intensity of 

seepage and the composition of fl uids, 

we investigated the lipid biomarker inventory 

of this seep limestone. The 

dominant biomarkers are C-13-depleted 

isoprenoids including tail-to-tail linked 

pentamethylicosane (delta C-13 value: - 

108 parts per thousand), representing 

molecular fossils of methanotrophic archaea. 

This observation reveals that the 

seepage fl uids contained methane. Because 

the seep carbonates have been 

found to be only moderately C-13- 

depleted (delta C-13 values as low as - 

14 parts per thousand), a signifi cant 

contribution from a less C-13-depleted 

carbon source than methane, probably 

marine carbonate, is apparent. Such a 

degree of admixture of marine carbonate 

is typical for seep limestones resulting 

from low fl ow rates. The observed biomarker 

pattern with the prominent occurrence 

of biphytanes, but lacking crocetane, 

reveals that the methanotrophic 

10

archaea at the Hauterivian seep site were 

similar to archaea of the ANME-1 cluster. 

Archaea of this cluster are known to 

be able to cope with lower methane concentrations 

than ANME-2 archaea; 

therefore ANME-1 archaea are better 

adapted to low seepage rates and diffusive 

fl ow. The Peregrinella limestone 

contains only a small amount of early 

diagenetic cement. Based on a comparison 

with biomarker patterns of other ancient 

seep deposits, it is apparent that 

diffusive seepage typically results in 

limestones with little cement, whereas 

advective, more intense seepage appears 

to favor cement precipitation. If applied 

with caution, this supposed relationship 

can be used as a fi rst approximation of 

seepage intensity. 

2010010030 

Transvaal 超群中发现的晚太古代分 

子化石记录了微生物多样性和好氧生 

活的痕迹 = Late Archean molecular 

fossils from the Transvaal Supergroup 

record the antiquity of microbial diversity 

and aerobiosis. ( 英文 ). Waldbauer J 

R; Sherman L S; Sumner D Y; Summons 

R E. Precambrian Research, 2009, 

169(1-4): 28-47 

Cores recovered during the Agouron 

Griqualand Drilling Project contain over 

2500 m of well-preserved late Archean 

Transvaal Supergroup sediments, dating 

from ca. 2.67 to 2.46 Ga. Bitumen extracts 

of these strata were obtained using 

clean drilling, sampling and analysis 

protocols that avoided overprinting syngenetic 

molecular fossil signatures with 

contaminant hydrocarbons. Comparisons 

of biomarker contents in stratigraphically 

correlated intervals from diverse 

lithofacies in two boreholes separated by 

24 km, as well as across a 2 Gyr unconformity, 

provide compelling support for 

their syngenetic nature. The suite of molecular 

fossils identified in the late Archean 

bitumens includes hopanes attributable 

to bacteria, potentially including 

cyanobacteria and methanotrophs, and 

steranes of eukaryotic origin. This molecular 

fossil record supports an origin 

in the Archean Eon of the three Domains 

of cellular life, as well as of oxygenic 

photosynthesis and the anabolic use of 

O 2 . 

2010010031 

川东北上寺剖面中的生物地球化学记 

录 : 二叠纪古生产力的证据 = Biogeochemical 

Records at Shangsi Section, 

Northeast Sichuan in China: The Permian 

Paleoproductivity Proxies. ( 英文 ). 

Ma Zhongwu; Hu Chaoyong; Yan Jiaxin; 

Xie Xinong. Journal of China university 

of geosciences, 2008, 19(5): 461-470 

The marine primary producers assimilate 

the atmospheric CO 2 to form the organic 

carbon in surface water. The organic 

carbon then settles down through 

the water column and is removed from 

the oceans by final preservation in sediments 

in the form of petroleum or nature 

gases. The reconstruction of paleoproductivity 

will thus improve our understanding 

of the biological processes in 

the formation of fossil energy resource 

and help to locate new sites for future 

exploration. In this study, biorelated 

elements P, Cd, Al, Ba, as well as redox 

sensitive element Mo, were analyzed in 

the 448 rock samples collected from 

Permian strata at the Shangsi Section, 

Guangyuan, Northeast Sichuan in China. 

On the basis of the Ti content, the nondetrital 

contents of P, Ca, and Al, denoted 

as P xs , Cd xs , and Al xs , were calculated 

and found to coincide with the 

TOC content throughout the whole section, 

with some enrichment intervals being 

found in the middle part of Chihsia 

Formation, topmost Maokou Formation, 

and Dalong Formation. This suggests 

that the biorelated elements could be 

used as proxies for the paleoproductivity 

here in this section. Ba xs , a paleoproductivity 

indicator widely used in the paleoceanography, 

shows insignificant correlation 

with TOC, P xs , Cd xs , and Al xs , 

probably arising from the loss of bio- 

11

logical barium in anoxic conditions. 

Compiled with the data of TOC content 

and P xs , Cd xs , and Al xs , three episodes of 

enhanced paleoproductivity were identified 

in Permian strata including the middle 

part of Chihsia Formation, topmost 

Maokou Formation, and Dalong Formation. 

2010010032 

川东北晚二叠世地层中初级生产者和 

沉积环境条件的分子记录 = Molecular 

Records of Primary Producers and 

Sedimentary Environmental Conditions 

of Late Permian Rocks in Northeast Sichuan, 

China. ( 英文 ). Ruan Xiaoyan; 

Luo Genming; Hu Shouzhi; Chen Feng; 

Sun Si; Wu Wenjun; Guo Qiaozhen; Liu 

Guoquan. Journal of China university of 

geosciences, 2008, 19(5): 471-480 

A series of biomarkers were identified 

in the aliphatic and aromatic fractions of 

the extracts from Late Permian Dalong 

and Wujiaping formations in Shangsi 

Section, Northeast Sichuan, South China, 

on the basis of the analysis of gas chromatography-mass 

spectrometry (GC- 

MC). The dominance of lowermolecular-weight 

n-alkanes throughout 

the profile suggests the dominant contribution 

of algae and bacteria to the organics 

preserved in the marine section. 

Wujiaping Formation is characterized by 

the elevated contribution from algae as 

well as other photoautotrophs such as 

photosynthetic bacteria as shown by the 

molecular ratios of hopanes to steranes 

or tricyclic terpanes as well as the ratio 

of pristane (Pr) and phytane (Ph) to C 17 

and C 18 n-alkanes. This is in accord with 

the data from the microscopic measurement 

on the calcareous algae. In contrast, 

Dalong Formation is featured by enhanced 

contribution from bacteria and 

probably terrestrial organics indicated 

by the enhanced C 24 tetracyclic terpanes 

relative to tricyclic terpanes. The two 

formations also show a distinct discrimination 

in sedimentary environmental 

conditions including redox condition 

and salinity. The anoxic condition 

was only found in the middle of the 

Dalong Formation as shown by the ratios 

of Pr/Ph and dibenzothiophene to 

phenanthrene, consistent with the reported 

data of Mo and U. An enhanced 

salinity indicated by the homohopane 

index is observed at the shallow Wujiaping 

Formation. On the basis of the composition 

of primary productivity and the 

redox condition, Dalong Formation is 

proposed, herein, to be potential hydrocarbon 

source rocks in the study site. It 

is notable that the topmost end-Permian 

is characterized by a large perturbance 

in both the redox condition and salinity, 

with oxic conditions being frequently 

interrupted by short-term anoxia, likely 

showing a causal relationship with the 

episodic biotic crisis across the Permian—Triassic 

boundary. 

2010010033 

川东北广元一条二叠系剖面中有机物 

丰度的主要控制因素 = Main Controlling 

Factors of Organic Matter Richness 

in a Permian Section of Guangyuan, 

Northeast Sichuan. ( 英文 ). Xie Xinong; 

Li Hongjing; Xiong Xiang; Huang Junhua; 

Yan Jiaxin; Qin Jianzhong; Tenger; 

Li Wu. Journal of China university of 

geosciences, 2008, 19(5): 507-517 

A complete Permian section in Guangyuan, 

Northeast Sichuan, has been investigated, 

to explore the variation in 

organic matter richness and its main 

controlling factors. The research results 

of the detailed lithological description 

and organic/inorganic geochemical 

analysis of about 325 samples indicate 

that a high content of total organic carbon 

(TOC) occurs in calcareous mudstones 

and laminated marls or thinbedded 

limestones. In carbonate rocks, 

the TOC content is negatively related to 

the thickness of the massive beds; the 

thinner the bed is, the higher the TOC 

content is. Marine organic matter is enriched 

in the outer shelf and relatively 

shallow basin floor environments with 

12

the maximum TOC contents of 5.07% 

and 14.6%, respectively. The main factors 

that affect the quantity and quality 

of marine organic matter include primary 

productivity, depositional processes, 

and redox conditions during deposition 

and the early diagenesis stage. 

Three intervals of marine good quality 

source rocks are identified in this section; 

they are lower Chihsia Formation, topmost 

Maokou Formation, and the middle 

segment of the Dalong Formation. They 

are formed in anoxic environments, in 

association with high primary productivity. 

Among these, high productivity in 

the lower Chihsia interval may originate 

from an upwelling flow area, whereas, 

in the rest of the intervals, it is inferred 

to be related to hot fluid activity due to 

volcanic eruption. The results of this 

study suggest that good quality marine 

source rocks in the Permian strata offer 

significant hydrocarbon potential. 

2010010034 

四川华蓥山地区穿越 P\T 界线的钙质 

微生物岩中有机物质的出现 = Occurrence 

of Organic Matter in Calcimicrobialites 

across Permian–Triassic Boundary 

in Huayingshan Region, Sichuan, 

South China. ( 英文 ). Yang Hao; Wang 

Yongbiao; Chen Lin. Journal of China 

university of geosciences, 2008, 19(5): 

518-525 

Calcimicrobialites across the Permian-Triassic 

boundary in Huayingshan 

region were investigated using the fluorescence 

microscopic measurements to 

understand the occurrence of organic 

matter. The microbialites are composed 

of micrite matrix and coarse spar cement. 

Abundant rhombic or magnetic needlelike 

carbonate minerals were observed 

adrift within the cement. The fluorescence 

microscopic measurement indicates 

the micrite matrix in microbialites 

shows the most abundant organic matter, 

with the rhombic or magnetic needlelike 

carbonate minerals and coarse spar 

cement coming to the 2nd and the 3rd, 

respectively. Organic matter is mainly 

preserved in the space between the 

grains of the micrite minerals but almost 

evenly distributed in the rhombic or 

magnetic needle-like carbonate minerals. 

As one of the common diagenesis types, 

dolomitization is observed to occur in 

the microbialites in Huayingshan. However, 

the carbonate cement in microbialites 

still has high content of element Sr 

as shown by the microprobe analysis, 

reflecting that the dolomitization might 

have happened in a restricted environment. 

Observation under the fluorescence 

microscope shows that dolomitization 

just led to the redistribution of 

organic matter in the grain space of 

dolomite minerals, inferring that the 

diagenesis has a slight effect on the 

preservation, and thus on the content of 

organic matter in the microbialites. 

2010010035 

华北轩隆凹陷中元古代初级生产力和 

古环境条件的分子证据 = Molecular 

Evidence for Primary Producers and Paleo-environmental 

Conditions in Mesoproterozoic 

in the Xuanlong Depression 

in North China. ( 英文 ). Luo Genming; 

Xie Shucheng; Wu Wenjun; Sun Si; 

Huang Junhua; Shi Xiaoying. Journal of 

China university of geosciences, 2008, 

19(5): 567-576 

The molecular organic compounds 

have been identified by gas chromatography 

(GC) and GC-mass spectrometry 

(GC-MS) from Mesoproterozoic rocks 

in the Xuanlong depression in North 

China. The main saturated compounds 

are n-alkanes, monomethylalkanes, n- 

alkylcyclohexanes, acyclic isoprenoids, 

and hopanes. The dominant lowermolecular-weight 

n-alkanes are indicative 

of the main contribution of microorganisms, 

in particular, the chemosynthetic 

bacteria. The presence of abundant 

monomethylalkanes (mid- and endbranched) 

and the long chained (>C 20 ) 

acyclic isoprenoids indicates the existence 

of abundant bacteria and/or ar- 

13

chaea in ancient oceans. The low abundance 

of pristane and phytane is suggestive 

of the relatively low abundance of 

photosynthetic autotrophs in comparison 

with chemosynthetic bacteria in the 

Mesoproterozoic oceans in North China. 

The sedimentary environmental condition 

is suboxic/anoxic, as indicated by 

the low value of the Pr/Ph ratio as well 

as the presence of abundant sulfurbearing 

organic compounds, consistent 

with the other geochemical data in North 

China and elsewhere in the world. Both 

the composition of the primary producers 

and the sedimentary environmental 

conditions are favorable for the formation 

of hydrocarbon source rocks. 

古生态学 

2010010036 

古新世 - 始新世热最大值对深海微体底 

栖群落结构的影响 : 利用峰值顺序曲 

线确定古生态反应 = Impact of the Paleocene-Eocene 

thermal maximum on 

deep-ocean microbenthic community 

structure: Using rank-abundance curves 

to quantify paleoecological response. 

( 英文 ). Webb A E; Leighton L R; Schellenberg 

S A; Landau E A; Thomas E. 

Geology, 2009, 37(9): 783-786 

Global climate change has often resulted 

in extinction events that can be 

quantitatively measured by taxonomic 

loss but are more difficult to assess in 

terms of ecological restructuring. We 

use a commonly applied ecological tool, 

rank-abundance curves (RACs), to 

evaluate the ecological response of benthic 

foraminiferal and ostracode communities 

to the Paleocene-Eocene thermal 

maximum, which may be seen as an 

analog for current and future global 

warming. RACs are proxies for community 

structure, and therefore changes in 

the shape of RACs allow inferences to 

be drawn about and quantification of 

ecological responses. Benthic foraminiferal 

communities became increasingly 

stressed during the Paleocene-Eocene 

thermal maximum, and community reorganization 

occurred before the taxonomically 

defined extinction horizon. In 

contrast, ostracode communities became 

less stressed during the same interval, 

reinforcing the idea that different groups 

of organisms respond differently to extinction 

events and global warming. The 

decoupling of ecologic impact from 

taxonomic impact during the Paleocene- 

Eocene thermal maximum reaffirms the 

fact that future climate change could 

have far-reaching effects on taxa and 

ecosystems and proves the importance 

of examining both the taxonomic and 

ecologic responses of communities during 

extinction events. Abundance 

2010010037 

显生宙底栖碳酸盐相 : 以俄罗斯地台 

石炭系为例并评述 = Benthic carbonate 

facies of the Phanerozoic: Review and 

example from the carboniferous of the 

Russian platform. ( 英文 ). Kabanov P B. 

Stratigraphy and Geological Correlation, 

2009, 17(5): 493-509 

General classifications of Phanerozoic 

carbonate facies and controlling them 

factors are reviewed. Three principal 

carbonate factories distinguished by W. 

Schlager (2000, 2003) are the tropical 

shallow-water, the cool-water, and the 

mudmound factories. The general term 

for facies associations in the first factory 

is photozoan carbonates. The cool-water 

factory encompasses environments producing 

heterozoan carbonate facies. The 

mudmound factory is a non-actualistic 

sedimentary system producing moundshape 

buildups of non-skeletal microbial 

micrites (also termed automicrites). The 

benthic carbonate production is controlled 

by light, bottom temperature, eutrophication, 

siliciclastic influx, and the 

evolution of marine ecosystems. The cyclic 

alternation of skeletal associations 

(“biofacies”) formed under the control 

of high-amplitude sea level changes is 

exemplified by the Moscovian (Carboniferous) 

epeiric carbonates of the East 

14

European Craton. Three principal biofacies 

associations in this example are 

bryonoderm extended (heterozoan), staffellid-syphonean 

(photozoan). and 

Meekella-Ortonella (intertidal flat to 

stagnant lagoon). 

2010010038 

初龙类中两种新疾病的发现及其对未 

来化石病理学研究的意义 = The discovery 

of two novel archosaur diseases 

with implications for future paleopathological 

exploration. ( 英文 ). Wolff E 

D S. Historical Biology, 2008, 20(3): 

185-189 

Two novel bone diseases from the archosaur 

record were noted during the 

course of a survey of archosaur oral pathology. 

These abnormalities, pertaining 

to abnormal suturing of the crocodilian 

palate and ventral mandibular muscle 

scarring in tyrannosaurs, are classified 

within this paper according to a new 

classification system for ancient bone 

pathology. Standardization of this type 

is suggested for future disease exploration. 

2010010039 

澳大利亚新生代腕足类壳上的钻孔 = 

Drill holes in Australian Cainozoic 

brachiopods. ( 英文 ). Tuura M; Baumiller 

T K; McNamara K J. Historical Biology, 

2008, 20(3): 203-212 

The fossil record of drill holes in marine 

invertebrates has received a considerable 

amount of interest from paleontologists, 

primarily due to its importance 

for reconstructing the history of interactions 

between drilling predators and 

their prey. Such drill holes have been 

described in numerous studies of Paleozoic 

brachiopods but rarely in those focusing 

on brachiopods of the post- 

Paleozoic, a striking pattern given that in 

the late Mesozoic and Cainozoic drilling 

gastropods diversified and frequencies 

of drilled molluscs increased dramatically. 

During the past several years, 

however, drilled brachiopods were reported 

in several studies of the Mesozoic 

and Cainozoic, suggesting that this phenomenon 

may be more common than 

has been previously assumed. Here we 

report on 10 genera of brachiopods from 

four Cainozoic basins in Australia of 

which 7 shows evidence of having been 

drilled by predators. Of 298 specimens 

examined, 38 contain a single complete 

hole. Drilled specimens were identified 

in all 4 basins and in all stratigraphic 

units. When considered in the context of 

recent reports of drilled Cainozoic 

brachiopods, these Australian brachiopods 

further imply that drilling predation 

on these invertebrates was geographically, 

taxonomically and temporally 

widespread. 

2010010040 

化石病理学的研究对象是生物特征及 

其与环境的相互作用 , 而非生物对其 

自身的作用 = Paleopathologies are features 

of an organism and its interaction 

with the environment and should not be 

treated like organisms unto themselves. 

( 英文 ). Beatty B L; Rothschild B M. 

Historical Biology, 2009, 21(3 & 4): 

229-233 

Though the history of disease has an 

evolutionary history in itself, this history 

of pathologies, which are physical manifestations 

of immune responses to disease 

processes, has a history that is intimately 

linked to the history of the host 

organisms themselves. But many of 

these physical manifestations of an organism's 

response to disease are related 

to aspects of the immune system that are 

rooted so deeply in the phylogeny of 

vertebrates, or at least amniotes, that one 

must exercise caution when interpreting 

a pathology as novel. Here, we argue 

that the interpretation of paleopathologies 

must be founded on the basis of 

disease manifestations which relate to 

phylogeny, but recognise that much of 

this relationship is so deeply rooted that 

novel paleopathologies would be rare. 

15

The former presents an interesting 

speculation, but does not allow for 

placement of findings within an ecological 

and chronological context. Likewise, 

the assignment of specimens as paleopathological 

holotypes defeats this purpose 

in attempting to narrowly define the 

physical manifestation of the immune 

response to disease, doing nothing more 

than a photographic library of paleopathologies 

could do, but not conveying 

the true nature of paleopathologies and 

could lead to artificial classification 

schemes that would cause more confusion 

than clarity. 

2010010041 

化石病理学中同源现象的局限性 = 

The limitations of homology in vertebrate 

paleopathology. ( 英文 ). Wolff E D 

S. Historical Biology, 2009, 21(3 & 4): 

235-238 

2010010042 

川东北二叠纪化石群落和生境类型的 

再划分 = Subdivision of Permian Fossil 

Communities and Habitat Types in 

Northeast Sichuan, South China. ( 英文 ). 

Yan Jiaxin; Ma Zhixin; Xie Xinong; 

Xue Wuqiang; Li Bo; Liu Dongqin. 

Journal of China university of geosciences, 

2008, 19(5): 441-450 

Recent achievement in hydrocarbon 

exploration in Northeast Sichuan demonstrated 

that Permian calcareous and 

argillaceous deposits are the major contributing 

source rocks. Reevaluation on 

the hydrocarbon potential of the Permian 

strata over the whole Yangtze region is 

thus to be desired. A comprehensive corroboration 

was carried out at the Shangsi 

Section, Guangyuan, Northeast Sichuan, 

which is believed to be another promising 

area in South China. This article 

deals with the ecological and depositional 

conditions of the Permian strata in 

the section, including the Chihsia, Maokou, 

Wujiaping, and Dalong formations, 

which share some similarities with 

those occurring in the broad Yangtze 

carbonate platforms. Five fossil communities 

of Mizzia-Permocalculus, Hayasakaia, 

Inozoan, Ostracod, and Crinoid 

were identified in the Yangtze region 

and described in detail including 

their components and occurrence. On 

the basis of the fossil communities and 

depositional features, 23 habitat types, 

mainly occurring from inner to outer 

shelves, were recognized at the Shangsi 

Section in order to reconstruct the depositional 

conditions and accordingly to 

evaluate the paleoproductivity. In addition, 

the subdivision of Chihsia Formation 

in the section was revised, which 

would be of significance for the reconstruction 

of the Chihsian paleogeography 

in the study area. 

2010010043 

通过 TOC 和生境类型初步估算古生 

产力 : 哪种方法更可靠 -- 以华南上扬 

子台地奥陶纪 - 志留纪过渡期黑色页岩 

为例 = Preliminary Estimation of Paleoproductivity 

via TOC and Habitat 

Types: Which Method Is More Reliable? 

—A Case Study on the Ordovician– 

Silurian Transitional Black Shales of the 

Upper Yangtze Platform, South China. 

( 英文 ). Su Wenbo; Wang Yongbiao; 

Bradley D Cramer; Axel Munnecke; Li 

Zhiming; Fu Lipu. Journal of China 


534-548 

New total organic carbon (TOC) data 

from the two Ordovician–Silurian transitional 

graptolite-bearing black shale intervals, 

the Wufeng Formation and the 

Longmaxi Formation in Central 

Guizhou and West Hubei, respectively, 

as well as previously reported TOC data 

from the same intervals in other places 

on the Yangtze platform of South China, 

have been used to produce an initial estimate 

of the primary paleoproductivity 

via a conventional inverse method (i.e., 

R pp-inverse ). The values of the R pp-inverse are 

estimated to be 32 (43–21) gC/(m 2·a) 

16

(Wufeng Formation) and 21 (27–16) 

gC/(m 2·a) (Longmaxi Formation). Also, 

simultaneously, the habitat types (i.e., 

HT; cf., BA: benthic assemblage) and 

their temporal and spatial changes have 

been documented from the same succession, 

and an initial estimate of the primary 

paleoproductivity has been produced 

using a forward method (i.e., R ppforward). 

Being bounded mainly by the 

peritidal to inner-shelf environment 

shelly-facies or mixed-facies successions 

with BA1 to BA3 faunas both at 

the top and the base, which indicates the 

habitat types from HT II 1 to HT III 2 , the 

biohabitat type of the two graptolitebearing 

black shale intervals can be limited 

to HT III to HT IV, corresponding 

to the inner shelf to the outer shelf, with 

depths from roughly 60 m to 200—300 

m. Based on the current data from the 

South China Sea and the southern part of 

the East China Sea, values of R pp-forward 

should be about 100 to 400 gC/(m 2·a). 

The difference in the results via the two 

methods suggests that paleoproductivity 

estimates from the geological strata need 

to be made cautiously, with particular 

attention paid to the paleogeographic 

setting, oxic-anoxic conditions, as also 

the preservation factor of organic carbon. 

2010010044 

通过对 Donzére (Drôme, France) 

Chauve-Souris 洞穴中的微体脊椎动 

物应用定量方法恢复古环境 : 方法定 

义与应用的探索 = La grotte de la 

Chauve-Souris à Donzère (Drôme, 

France.) L’environnement holocène par 

la méthode quantitative appliquée aux 

microvertébrés. Essai de définition et 

application. ( 法文 ). Jeannet M; Vital J. 

Revue de Paleobiologie, 2009, 28(1): 

139-173 

L’étude de la microfaune de la grotte 

de la Chauve-Souris (Donzère, Drôme) 

couvre largement la seconde moitié de 

l’Holocène et principalement les 

époques du Néolithique final et du 

Bronze final. Les espèces rencontrées 

sont relativement banales hormis le 

Campagnol ibérique (Microtus cabrerae 

Thomas, 1906) devenu strictement 

ibérique et le Rhinolophe de Roumanie 

(Rhinolophus mehelyi matschie, 1901) 

disparu récemment de France ou en voie 

de disparition. La Souris grise (Mus 

musculus L., 1758) fait une apparition 

fugace au Néolithique final et semble 

s’implanter durablement durant le 

Bronze final. La position médiorhodanienne 

du site enregistre les fluctuations 

animales autant que les migrations 

humaines imprimées dans les 

styles de céramiques. Mais la faune en 

plus, par sa sensibilité, transcrit 

l’influence humaine sur l’environnement 

(ex. : la déforestation), les changements 

climatiques, et même, si l’on en croit la 

coïncidence de quelques accidents de la 

courbe thermique, avec les variations du 

taux de 14C résiduel atmosphérique. Les 

données biométriques utilisées pour la 

détermination des Chiroptères sont ajoutées 

en annexe. 

2010010045 

突尼斯东北部的 Barremo-Aptian 缺 

氧事件 «OAE 1a» : 关于有孔虫 = 

L’événement anoxique « OAE 1a » Barrémo-Aptien 

en Tunisie nord-orientale : 

Intérêt des foraminifères. ( 法文 ). Elkhazri 

A; Razgallah S; Abdallah H; Ben 

Haj Ali N. Revue de Paleobiologie, 

2009, 28(1): 93-130 

En Tunisie nord-orientale le Barrémo- 

Aptien est caractérisé par une sédimentation 

continue de bassin débutant par 

deux barres carbonatées à intercalations 

marneuses riches en foraminifères benthiques 

à structures complexes qui sont 

dominants par rapport aux formes planctoniques 

dont la forme des loges est 

globuleuse; il s’agit du‘faciès barrémien'. 

L’Aptien inférieur débute par des 

couches argileuses grises à microfaciès 

laminé contenant de la matière organique 

associée à des grains phosphatés 

et de la glauconie. Ces couches à 

17

matière organique comprennent des foraminifères 

planctoniques à loges radialement 

allongées (Lilliputianella, Leupoldina) 

adaptées à la déficience en 

oxygène. La première occurrence (FAD) 

de Leupoldina cabri fait suite aux 

couches grises laminées. Cette apparition 

indique la partie moyenne du 

Bédoulien supérieur et l’espèce définit 

une zone à extension totale. La distribution 

des foraminifères benthiques enregistre 

des variations verticales ; ainsi au 

cours du Barrémien et la base de 

l’Aptien inférieur prédominent des associations 

à tests calcaires (Nodosariidae) ; 

par contre dans la partie supérieure de 

l’Aptien inférieur (niveau à matière organique) 

prédominent des associations à 

tests agglutinés, principalement les genres 

Ammodiscus et Textularia. L’Aptien 

moyen et supérieur sont caractérisés par 

une sédimentation essentiellement argileuse 

avec des passées marno-calcaires 

contenant des foraminifères benthiques 

fréquemment à tests calcaires, accompagnés 

par d’abondants foraminifères 

planctoniques à loges globuleuses. 

L’objectif de ce travail est la localisation 

et la description des niveaux à matière 

organique « Black shales » de l’Aptien 

inférieur ainsi que leur influence sur la 

distribution des foraminifères planctoniques 

et benthiques. L’analyse est 

basée sur l’étude quantitative de ces foraminifères, 

notamment leur distribution 

de part et d’autre des niveaux à matière 

organique. Une analyse sédimentologique 

est également réalisée dans le 

but de reconstruire les paléoenvironnements 

au cours du Barrémo-Aptien. 

L’événement anoxique OAE 1a est circonscrit 

à l’échelle de la Tunisie nordorientale. 

2010010046 

寻找多变量分析所需的最小样本量 

(MSR): 古生态学启示 = Finding 

the Minimum Sample Richness (MSR) 

for multivariate analyses: implications 

for palaeoecology. ( 英文 ). Travouillon 

K J; Archer M; Legendre S; Hand S J. 

Historical Biology, 2007, 19(4): 315- 

320 

Many techniques have been developed 

to estimate species richness and 

beta diversity. Those techniques, dependent 

on sampling, require abundance 

or presence/absence data. Palaeontological 

data is by nature incomplete, and 

presence/absence data is often the only 

type of data that can be used to provide 

an estimate of ancient biodiversity. We 

used a simulation approach to investigate 

the behaviour of commonly used 

similarity indices, and the reliability of 

classifications derived from these indices, 

when working with incomplete data. 

We drew samples, of varying number 

and richness, from artificial species lists, 

which represented original life assemblages, 

and calculated error rates for 

classifications of the parent lists and 

samples. Using these results, we estimated 

the Minimum Sample Richness 

(MSR) needed to achieve 95% classification 

accuracy. Results were compared 

for classifications derived from several 

commonly used similarity indexes (Dice, 

Jaccard, Simpson and Raup-Crick). 

MSR was similar for the Dice, Jaccard 

and Simpson indices. MSR for the 

Raup-Crick index was often much lower, 

suggesting that it is preferable for classifying 

patchy data, however the performance 

of this index was less stable than 

the other three in the simulations, which 

required an even lower MSR. MSR can 

be found for all presence/absence data 

from the contour graphs and equations 

as long as the absolute species richness 

and the beta diversity can be estimated. 

2010010047 

英国怀特岛渐新统双犬齿鳄化石中一 

例可能的坏死性皮炎 = A possible case 

of necrotizing dermatitis in the crocodylian 

Diplocynodon, from the Oligocene 

of the Isle of Wight, United Kingdom. 

( 英文 ). Wolff E D S; Fowler D W; 

18

Bonde J W. Historical Biology, 2007, 

19(2): 203-207 

Here we describe a pathological osteoderm 

from the crocodylomorph Diplocynodon 

hantoniensis (Bouldnor Formation, 

earliest Oligocene, Isle of Wight, 

United Kingdom). The specimen bears a 

porous, erosive branching channel that 

distorts the surface ornamentation and 

periosteum over 60% of the preserved 

dorsal surface area. We diagnose this 

condition as necrotizing dermatitis: a 

surficial bacterial or fungal infection that 

can penetrate the dermal layers to affect 

the underlaying penosteum of osteoderms. 

This condition has been previously 

reported for an extant tortoise 

and caiman; however, this is the first reported 

occurrence in the fossil record. 

2010010048 

晚白垩世 Arkhangelskiella 群的生物 

统计 : 由营养流控制的生态表型 = 

Biometry of the Late Cretaceous Arkhangelskiella 

group: ecophenotypes controlled 

by nutrient flux. ( 英文 ). Linnert 

C; Mutterlose J. Cretaceous Research, 

2009, 30(5): 1193-1204 1 图版 . 

This study focuses on the morphometry 

and taxonomy of the Late Cretaceous 

coccolith genus Arkhangelskiella. Sixty 

samples from the Campanian– 

Maastrichtian interval of DSDP Hole 

390A (Blake Nose) were investigated 

for their contents of Arkhangelskiella 

spp. In each sample one hundred specimens 

of Arkhangelskiella spp. were examined 

by measuring the coccolith 

length and width, as well as the length 

and width of the central area. In the 

samples investigated the Arkhangelskiella 

group exhibits a large size variation, 

specimens length varies from 

4.95 μm to 14.52 μm. Former taxonomic 

concepts, based on morphometry, subdivided 

the Arkhangelskiella group into 

three species: Arkhangelskiella maastrichtiana, 

Arkhangelskiella confusa and 

Arkhangelskiella cymbiformis. Our data 

show a large variability of the morphometric 

data (coccolith length, width 

of the outer rim). There is no indication 

for three independant species; two of the 

quoted taxa (1. thick outer 

rim = Arkhangelskiella maastrichtiana; 

2. very thin outer 

rim = Arkkhangelskiella cymbiformis) 

seem to be extreme forms of a continuous 

morphometric lineage. The lower 

part of the investigated succession 

(139.92–133.42 mbsf) is dominated by 

small specimens with an average length 

of 6.8 μm whereas the upper part 

(132.86–126.15 mbsf) is characterized 

by larger specimens (mean 8.7 μm). In 

DSDP Hole 390A the size increase appears 

to be very abrupt, within two samples 

(samples 133.42 mbsf, 132.86 mbsf) 

the mean size increases by 1.51 μm. 

Previous morphometric studies of Arkhangelskiella 

indicate a more continuous 

size increase throughout the late Campanian–Maastrichtian. 

The abrupt size 

increase observed here hints toward a 

minor hiatus in DSDP Hole 390A separating 

upper Campanian from lower 

Maastrichtian sediments. It seems likely 

that the size increase of Arkhangelskiella 

reflects changes of various environmental 

factors like nutrient supply and 

sea water chemistry (Mg/Ca ratio; Ca 

concentration). A comparison of morphometric 

results with previous palaeoecological 

studies documents a nutrient 

control for the growth of Arkhangelskiella. 

Small specimens can be 

related to more mesotrophic conditions 

whereas large specimens are linked to 

oligotrophic surface waters. 

2010010049 

保存在古代叶甲虫中的原始结构颜色 

= Original structural color preserved in 

an ancient leaf beetle. ( 英文 ). Tanaka G; 

Taniguchi H; Maeda H; Nomura S. Geology, 

2010, 38(2): 127-130 

Greenish-blue metallic colored fossil 

elytra of the leaf beetle (Plateumaris sp.) 

have been discovered in the peat sediment 

of the middle Pleistocene (ca. 600 

19

ka) Hirabaru Formation, Kyushu, Japan. 

Scanning and transmission electron microscopy 

revealed the smooth outer surface 

of the fossil elytra and five alternating 

electron-dense and electron-lucent 

layers in the epicuticle. By applying the 

matrix method to the epicuticle, three 

reflective peaks of wavelengths 388 nm, 

544 nm, and 656 nm were computed. 

These peaks correspond to the reflective 

color observed under white light. Thus, 

the coloration of the fossils was caused 

by multilayer reflectors of the epicuticle 

of the elytra. Pyrolysis–gas chromatography–mass 

spectrometric analysis 

revealed that the fossil elytra have preserved 

some of their original macromolecules 

(chitin, protein, and amino 

acids), which are similar to those of a 

related Holocene species. The highporosity 

matrix of the peat contains 

many fragments of diatoms, indicating 

the high productivity of the water column 

but a reducing bottom environment. 

Slight acidity of the interstitial water 

also seems to contribute to the preservation 

of some original macromolecules of 

fossil insects through geologic time. 

2010010050 

脊椎动物陆地扩张过程中生境空间形 

成的机制 = On the dynamics of the 

formation of the niche space during the 

exploration of land by vertebrates. ( 英 

文 ). Sennikov A G. Paleontological 

Journal, 2009, 43(5): 478-482 

The dynamics of the formation and 

filling the niche space during the exploration 

of land by vertebrates and probable 

relationships of the packing density 

and structural pattern of the niche space 

with ecological crises (mass extinctions) 

in the geological past are considered. 

2010010051 

文德期和早古生代海洋群落营养结构 

的发展 = Development of the trophic 

structure of Vendian and Early Paleozoic 

marine communities. ( 英文 ). 

Rozhnov S V. Paleontological Journal, 

2009, 43(11): 1364-1377 4 图版 . 

Major trophic links are reconstructed 

for the Vendian and Early Paleozoic. A 

hypothesis of the predominant development 

of extracorporeal or skin digestion 

in Vendian multicellular consumers is 

substantiated. The main food sources 

were algal-bacterial films, finely dispersed 

debris falling from the photic 

zone in cold shallow seas lacking a 

thermocline and debris on the surface of 

the sediment. Symbiosis with phototrophic 

and chemotrophic bacteria was 

widespread. Pelagic filtration and filtration 

of the near-bottom finely dispersed 

organic matter (including bacteria), and 

debris-feeding appeared when internal 

digestion became widespread in the 

Cambrian. These were supplemented in 

the Ordovician by feeding on the live 

phyto- and zooplankton in the water 

column one meter above the bottom. Before 

the Ordovician, feeding on live 

plankton and more so active predation 

on larger multicellular animals was the 

exception rather than the rule. The role 

of active predators in the biota did not 

become more important until the end of 

the Silurian. Mass morphogenesis 

among occurred multicellular animals as 

the amount and diversity of nutritional 

and/or spatial resources rapidly increased, 

while before that the lack of 

these was a limiting factor. 

微体古生物学 

综论 

2010010052 

西南印度洋中脊热液羽状流中微生物 

化石的发现及意义 = Discovery of microbial 

fossils in hydrothermal plume of 

the southwest Indian ridge and its significance. 

( 中文 ). 雷吉江 ; 初凤友 ; 李小 

虎 ; 于晓果 ; 韩喜球 ; 陶春辉 ; 杨克红 . 微 

体古生物学报 , 2009, 26(1): 39-47 4 图 

版 . 

20

深海热液微生物因其生存于海底极 

端环境 , 能够提供深部生物圈和生物地 

球化学信息而成为当今海洋科学领域 

关心的热点问题之一。本文以西南印 

度洋中脊热液羽状流水体中悬浮颗粒 

物为研究对象 , 选取典型的 3 个 CTD 

采水站位 , 对离底 42 —500m 的不同水 

层悬浮体过滤的滤膜进行扫描电镜观 

察和 X 射线能谱面扫描分析。结果表 

明 , 热液羽状流颗粒物中含有大量的微 

生物化石 , 包括丝状、球状、杆状和簇 

状等 4 种形态。对不同形态微生 

物化石能谱分析表明 Si、O、Ca 、Fe 

和 Zn 等元素在微生物化石中都有高 

值出现 , 其中丝状体中具有 Ti 和 Mn 

的高值出现 , 球状体中 Ba 具有高值 , 说 

明微生物化石化过程中不同类型的微 

生物体对金属元素的选择性吸收 , 钙化 

和铁硅酸盐岩化是微生物化石化的主 

要机制。微生物化石在羽状流中的分 

布状况能够提供活动热液喷口的空间 

信息 , 为我们寻找喷口提供帮助。 

孢粉 

2010010053 

徐州王庄煤矿山西组孢粉植物群及其 

地层意义 = Palynofloras of the Shanxi 

Formation from the Wangzhuang coal 

mine of Xuzhou, Jiangsu and their 

stratigraphical significance. ( 中文 ). 黄 

嫔 ; 朱怀诚 ; 王阿云 . 微体古生物学 

报 , 2002, 19(1): 33-52 6 图版 . 

徐州王庄煤矿山西组中、下部产有 

丰富的孢粉化石 , 保存完好 , 共计 55 属 

132 种 ( 包括 3 新种 ) 2 个未定型孢子及 

1 个疑源类未定类型。根据孢粉属种 

组成及其含量的变化 , 自下而上分为两 

套组合 :Cyclogranisporites- 

Gulisporites- Laevigatosporites- Florinites 

组合 ( 简称组合 1) 和 Calamospora- 

Gulisporites- Vesiculatisporites- 

Florinites 组合 ( 简称组合 2 )。 

根据组合内一些重要分子的地质时限 

讨论及其与相关组合的对比 , 将组合 1 

的地质时代归为早二叠世早期 , 组合 2 

的时代归为早二叠世晚期。文中描述 

孢子 3 新种 , 图示孢子花粉 91 种。 

2010010054 

玻利维亚北部潘多拉 X-1 号钻孔的宾 

夕法尼亚阶孢粉植物群 = The Pennsylvanian 

palynoflora of the Pando X-1 

Borehole, northern Bolivia. ( 英文 ). 

Pasquo M. Review of Palaeobotany and 

Palynology, 2009, 157(3-4): 266-284 5 

图版 . 

Palynological analysis of ten core 

samples obtained from 867–729 m depth 

in the Pando X-1 Borehole (11° 36′07″ S, 

67° 56′45″ W), northern Bolivia, is presented. 

Palynomorphs are fairly wellpreserved 

although many contain abundant 

pyrite. The whole assemblage is 

composed of 48 species of which six are 

spores. Among the pollen grains, 21 are 

monosaccate and 19 bisaccate (11 striate 

species). Scarce scolecodonts, microforaminifera 

and algae are also present. 

Two assemblages are recognized on the 

basis of the stratigraphic distribution of 

species, mainly of the striate pollen 

grains. The lower assemblage (A1) is 

dominated by amorphous organic matter 

and scarce monosaccate pollen grains, 

trilete spores and microforaminifera. 

The upper assemblage (A2) is dominated 

by tracheids and brown and black 

phytoclasts and characterized by more 

diverse palynomorphs, mainly striate 

and non-striate pollen grains. The geographical 

and stratigraphic distribution 

of taxa reveals that many species are recorded 

from Pennsylvanian and Permian 

palynofloras elsewhere in Gondwana 

and Euramerica. The presence of Lahirites 

segmentatus, Limitisporites scitulus, 

Lunatisporites onerosus and Vittatina 

species, common with Brazilian palynofloras, 

supports a Moscovian age for 

the assemblage 2. This age is also supported 

by calcareous microfossils previously 

found in the same interval of this 

borehole. Twenty two species are first 

records in the Pennsylvanian of Bolivia 

21

(e.g., Florinites eremus, Protohaploxypinus 

varius, Striatopodocarpites antiquus, 

S. gondwanensis, S. solitus, Vittatina 

sp.). Palynofacies features of both 

assemblages are indicative of a shallow 

marine palaeoenvironment. Qualitative 

changes on the floral composition between 

A1 and A2 may reflect broadly 

local palaeoclimatical changes. The 

dominance of Cordaitales and Coniferales 

in A1 indicates a relatively more 

humid local condition than during A2 

time, which is characterized by the appearance 

of abundant and diverse striate 

pollen grains related to new groups of 

Pteridosperms. These features are in 

agreement with a lower humidity or seasonally 

arid conditions prevailing in the 

terrestrial landscape near to the Copacabana 

marine palaeoenvironment. 

2010010055 

安徽天马国家自然保护区早春植物的 

花粉形态与其生态因子 = Study on 

pollen morphology and ecological factors 

of flowering plants in early spring in 

tianma national natural reservation region 

of Anhui Province. ( 中文 ). 许仁鑫 ; 

周忠泽 ; 陈延松 . 微体古生物学报 , 2009, 

26(1): 65-76 2 图版 . 

应用光学显微镜对安徽省天马国家 

级自然保护区早春开花的 13 科 19 属 

20 种 ( 其中 1 亚种 ,2 变种 ) 植物的花粉 

形态进行了观察和研究。结果表明花 

粉粒扁球形至长球形 ,P/ E 值最大的为 

杏 ( A rmeniaca uul glaris Lam. ) , 

大小为 1. 32 (1. 17 - 1. 60)μm , 最小的 

为旌节花 ( S tachy urus chinensis 

Franch. ) , 大小为 0. 86 (0. 83 - 0. 

89)μm; 花粉最大的为北京忍冬 (L 

onicera el isae Franch. ) , 大小为 85. 5 

(75. 0 - 97. 0) ×73. 75 (63. 75 - 82. 5)μm; 

最小的为鄂西清风藤 [ S abia campanulate 

Wall. ex Roxb. subsp . ri tchieae 

(Rehd. et Wils. ) Y. F. Wu ] , 大小为 17. 

62 (15. 32 -19. 68) ×14. 3 (12. 51 - 16. 

44)μm。萌发孔主要有 3 - 4 沟 (20 

%) 、多沟 (5 %) 、3 - 4 孔沟 (65 %) 、 

散孔 (10 %) 等类型。外壁纹饰主要有 

刺状 (5 %) 、细网状 (85 %) 、粗网状 

(10 %) 等类型。同时研究了这些花粉 

的形态特征、地理分 

布及其生态因子。根据这些植物在该 

地区赖以生存的生态因子 , 包括地理位 

置、海拔高度、年降水量、年积温、 

生境 , 以及开花期间的最低温度、最高 

温度和月积温 , 得出这些植物分布区的 

主要生态因子 , 为利用地层中相应化石 

花粉重建大别山区古气候、古环境及 

气候变迁提供了现代孢粉学资料和依 

据。 

2010010056 

江淮丘陵区早春开花植物的花粉形态 

与其生态因子 = Study on pollen morphology 

and ecological factors in the 

region of Jianghuai hill. ( 中文 ). 岳春 ; 周 

忠泽 ; 余涛 . 微体古生物学报 , 2009, 

26(1): 77-91 3 图版 . 

应用光学显微镜对安徽省枞阳县和 

安徽大学校园内春季开花的 22 科 30 

属 40 种植物的花粉形态进行了观察 

和研究。结果表明花粉粒扁球形至长 

球形 ,P/ E 值最大的花粉见于贴梗海棠 

[ Chaenomeles s peciosa (Sweet) Nakai 

] , 为 1. 41 (1. 23 —1. 79) ,P/ E 值最 

小的花粉见于枫杨 ( Pterocary a stenoptera 

C. DC. ) , 为 0. 78 (0. 71 —0. 83) ; 

体积最大的花粉见于金银花 (L onicera 

j aponica Thunb) , 直径为 60. 8 (57. 5 - 

65. 0)μm , 体积最小的花粉见于菱叶绣 

线菊 (A risaema j acquemont i i Blume) , 

为 11. 5 (10. 0 - 12. 5) ×9. 8 (8. 0 - 12. 

0)μm。萌发孔主要有 3 沟 (20. 5 %) 、 

3 孔沟 (61. 5 %) 、散孔 (15. 4 %) 、六 

孔 (2. 6 %) 等类型。外壁纹饰主要有 

条纹 2 穿孔 (22. 5 %) 、细网状 (27. 5 

%) 、粗网状 (25. 0 %) 、条纹状 (50 %) 

和颗粒状 (12. 5 %) 等类型。同时调查 

了其生态因子 , 包括地理位置、海拔高 

度、年降水量、年积温及生境等 , 得出 

了这些植物分布区的主要生态因子。 

22

该花粉组合信息可用以重建古植被、 

古气候及古环境的变化。 

2010010057 

全新世泥炭中花粉百分比与稳定碳同 

位素之间相似的变化趋势 -- 古气候研 

究的可能诠释 = Analogous trends in 

pollen percentages and carbon stable 

isotope composition of Holocene peat — 

Possible interpretation for palaeoclimate 

studies. ( 英文 ). Skrzypek G; 

Baranowska-Kącka A; Keller-Sikora A; 

Jędrysek M. Review of Palaeobotany 

and Palynology, 2009, 156(3-4): 507- 

518 

Pollen and spore analysis and analysis 

of carbon stable isotope composition in 

a peat core from Hala Izerska (SW Poland) 

were used for palaeoclimate studies 

of the Holocene over the last ~ 8.5 ka. 

The results of these two methods have 

been compared and variations of the 

δ 13 C value show a clear relationship 

with the pollen percentages of tree taxa, 

such as Carpinus, Fagus, Picea, and 

Pinus as well as with spores of Sphagnum 

and akinetes of Cyanophyta. However, 

lags of up to ~ 200 years of pollen 

maxima and minima versus δ 13 C were 

observed. The δ 13 C value in the peat 

core varied between − 23.47 and 

− 27.58‰ and is interpreted here as reflecting 

temperature control of the carbon 

isotope composition of the peat. According 

to this interpretation and pollen 

analysis of the study area, the following 

climatic periods for the Holocene can be 

described: Atlantic–beginning warm 

(8.50–7.90 ka cal. BP) followed by 

moderated cold (7.90–5.75 ka cal. BP), 

Subboreal–beginning moderated cold 

(5.75–5.40 ka cal. BP) then warm (5.40– 

2.55 ka cal. BP), Subatlantic–beginning 

warm (2.55–2.20 ka cal. BP) then cold 

and moderate cold (2.20 ka–0.40 ka cal. 

BP) with a climatic minimum ~ 1.60 ka 

cal. BP. The highest relative difference 

between growing season temperatures 

was about 3.6 °C, which has been observed 

between the Subboreal temperature 

maximum (5.00 ka cal. BP) and the 

Subatlantic temperature minimum 

(1.60 ka cal. BP). 

2010010058 

中寒武世至早泥盆世孢型壁的纹层 = 

Laminae in palynomorph walls from the 

Middle Cambrian–Early Devonian. ( 英 

文 ). Taylor W A. Review of Palaeobotany 

and Palynology, 2009, 

156(1-2): 7-13 2 图版 . 

This study was undertaken to examine 

the wall ultrastructure of widely dispersed, 

mainly lower Paleozoic palynomorphs/cryptospores. 

Many of these palynomorphs 

have walls that are at least 

partially composed of laminae. The 

walls and their constituent laminae are 

variable in their construction, but show 

certain similarities to one another and to 

some extant land plants (e.g., sphaerocarpalean 

liverworts). Careful examination 

with transmission electron microscopy 

reveals that: 1) Cambrian–Early 

Devonian laminate palynomorphs have 

laminae that are fairly uniform in their 

thickness, 2) most contemporaneous 

acritarchs have walls that are thicker 

than individual laminae in these putatively 

land-derived palynomorphs and 

cryptospores, 3) extant algae have lamellae, 

not laminae, in their cyst walls, 

and in smaller numbers than the laminae 

in these palynomorphs/cryptospores, and 

4) extant liverworts have laminae whose 

thickness overlaps that of these palynomorphs/cryptospores, 

but also have 

some laminae that are much thicker. The 

antiquity of these palynomorphs clearly 

establishes the plesiomorphic state of 

laminate wall construction among land 

plants. While it is not possible to assign 

the producers of these palynomorphs to 

any specific group of organisms based 

on the ultrastructure of the wall, they 

clearly produced spores with thicker, 

more complex walls than any fossil or 

extant alga known to date. 

23

2010010059 

波兰北部中泥盆世分散大孢子及似种 

子大孢子的外壁结构 = Wall ultrastructure 

in some dispersed megaspores and 

seed-megaspores from the Middle Devonian 

of northern Poland. ( 英文 ). Turnau 

E; Zavialova N; Prejbisz A. Review 

of Palaeobotany and Palynology, 2009, 

156(1-2): 14-33 10 图版 . 

A detailed investigation using light 

microscopy (LM), scanning electron microscopy 

(SEM) and transmission electron 

microscopy (TEM) has been undertaken 

on three dispersed megaspore taxa 

recovered from Givetian deposits of 

northern Poland. Morphology of Contagisporites 

optivus is the same as that 

of megaspores reported from sporangia 

of Archaeopteris, but the producers of 

the seed-megaspores Granditetraspora 

zharkovae and of Biharisporites? capillatus 

are unknown. The affinity of the 

former is of special interest as monomegaspory 

is one of the botanical innovations 

that characterizes the seed plants 

(though it also occurs in other heterosporous 

plants). Comparisons at ultrastructural 

level with megaspores and 

large spores of plant groups believed to 

have attained, in the Middle Devonian, 

some level of heterospory are discussed. 

It is suggested that the alveolate outer 

wall of the seed-megaspores studied, 

consisting of granular units, is similar to 

that of archaeopteridalean megaspores. 

Specimens of G. zharkovae bear also 

some morphological resemblance to anisodiametric 

tetrads from the Devonian 

and Carboniferous ovules of presumed 

or certain pteridosperms in being enclosed 

in resistant meshy membranes 

(mesh-sack). Wall thickness of aborted 

versus functional megaspores of G. 

zharkovae, and the lack of indication 

that the mature functional megaspore 

wall was stretched, point to a nonlycopsid 

origin of G. zharkovae. It is 

suggested that the anisodiametric tetrads 

discussed may have been produced by a 

plant related to archaeopteridaleans. 

2010010060 

美国伊利诺伊盆地中宾夕法尼亚期早 

期大孢子外壁构造的研究 = An ultrastructural 

investigation of early Middle 

Pennsylvanian megaspores from the Illinois 

Basin, USA. ( 英文 ). Glasspool I J; 

Collinson M E; Scott A C; Brain A P R; 

Plotnick R E; Kenig F. Review of Palaeobotany 


156(1-2): 62-78 7 图版 . 

Four megaspore genera: Cystosporites, 

Rotatisporites, Zonalessporites, and 

Valvisisporites were isolated from palaeokarst 

fill deposits of early Middle 

Pennsylvanian age, hosted within Ordovician 

limestones at Central Quarry in 

Central, Kendall County, Illinois, U.S.A. 

Five uncompacted megaspore species 

were identified and studied using scanning 

and transmission electron microscopy 

(SEM and TEM). The species 

Valvisisporites sculptus Bhardwaj is 

emended based on improved morphological 

and new ultrastructural data. The 

genus Pseudovalvisisporites Lachkar is 

recognized as a junior synonym of 

Valvisisporites. The ontogenetic development 

of aborted and functional Cystosporites 

diabolicus megaspores is investigated 

and the timing of sporopollenin 

deposition in both the exine and massa is 

reported. In Carboniferous megaspores, 

the importance of detailed investigation 

of the periapertural region is emphasized 

by the discovery of fusiform lamellate 

thickenings in Valvisisporites and Rotatisporites. 

The taxonomic and systematic 

importance of these features are considered 

in light of the otherwise highly conserved 

ultrastructure that is recognized 

in many lycopsid megaspores of this age. 

2010010061 

俄罗斯二叠纪裸子植物花粉中出现类 

似被子植物花粉外壁结构 = Occurrence 

of angiosperm-like ultrastructural 

features in gymnosperm pollen from the 

Permian of Russia. ( 英文 ). Zavialova N 

E; Gomankov A V. Review of Pa- 

24

laeobotany and Palynology, 2009, 

156(1-2): 79-89 4 图版 . 

The morphology and ultrastructure of 

some dispersed pollen grains from the 

Permian of the Russian Platform were 

studied using light microscopy (LM), 

scanning electron microscopy (SEM) 

and transmission electron microscopy 

(TEM). Although being morphologically 

similar in LM (more or less circular in 

polar view with reticulate structure), 

these pollen grains demonstrate strong 

differences when studied under SEM 

and TEM, showing that they correspond 

to two different pollen taxa. The first 

one exhibits under SEM a coarser reticulum 

over the poles of the pollen grain 

and a finer peripheral reticulum. The ectexine 

includes a perforated tectum, 

spongy infratectum with rather regular 

short partitions, and a supposed foot 

layer. The thick inner layer (supposed 

endexine) appears nearly homogeneous, 

but in places lamellate structures are distinguishable 

suggesting that this layer 

was originally lamellate. Such pollen 

grains may be identified as Reticulatina 

microreticulata. The second pool of 

specimens was assigned to 

Samoilovitchisaccites turboreticulatus. 

The pollen grains of S. turboreticulatus 

demonstrate a continuous tectum completely 

covering the underlying exinal 

layers; under SEM these pollen grains 

appear nearly smooth. Differing in ectexine 

ultrastructure, they are similar to 

Reticulatina in the ultrastructure of the 

innermost layer. Although both taxa are 

of gymnospermous (pinopsid) affinity, 

the similarity between the surface of Reticulatina 

exine and that of Cretaceous 

angiosperm pollen is fascinating. 

2010010062 

三叠纪苏铁 Delemaya spinulosa 的花 

粉及其在苏铁演化上的意义 = Pollen 

of the Triassic cycad Delemaya spinulosa 

and implications on cycad evolution. 

( 英文 ). Schwendemann A B; Taylor T N; 

Taylor E L. Review of Palaeobotany and 

Palynology, 2009, 156(1-2): 98-103 1 图 

版 . 

The Cycadales are an order of gymnosperms 

that represent one of the oldest 

lineages of seed plants. Cycads are 

thought to have originated in the Carboniferous, 

and subsequently diversified 

and geographically expanded throughout 

the Mesozoic. Despite the geologic diversity 

of the group, the evolutionary 

history of cycads remains unresolved. 

To a large degree this is because the 

leaves of cycads and various other fossil 

groups (e.g., pteridosperms and Bennettitales) 

are morphologically similar. 

To date there are relatively few fossil 

cycad reproductive structures. Several 

are known from the Permian of China, 

but these compression specimens provide 

little detailed information useful in 

tracing the evolution of cycad cone 

morphology and anatomy. A permineralized 

cycad pollen cone from the Triassic 

of Antarctica, Delemaya spinulosa, contains 

in situ pollen. The objective of the 

current study is to further elaborate the 

structure of the pollen grains in this species, 

with particular emphasis directed at 

the structure and organization of the pollen 

wall. The elliptical shape, monosulcate 

aperture, and small size of the pollen 

grains are like those of extant Cycadales. 

The exine, although originally 

described as homogenous, appears to 

possess an alveolar organization. Pollen 

and cone features are compared to those 

in extant Cycadales. 

2010010063 

木贼的系统发生及演化 : 来自孢子外 

壁结构的证据 = Phylogeny and evolution 

of the horsetails: Evidence from 

spore wall ultrastructure. ( 英文 ). Grauvogel-Stamm 

L; Lugardon B. Review of 

Palaeobotany and Palynology, 2009, 

156(1-2): 116-129 4 图版 . 

A new comparative TEM study of the 

ultrastructure of the spores of the Carboniferous 

genus Calamites with those 

25

of Triassic Equisetites sp. and 

Schizoneura paradoxa, Jurassic Equisetum 

columnare and living Equisetum has 

allowed the recognition of an evolutionary 

series confirming that Calamites and 

Equisetum are closely related and belong 

to the same lineage. Such a relationship 

was previously proposed by Good 

[Good, C.W., 1975. Pennsylvanian-age 

calamitean cones, elater-bearing spores, 

and associated vegetative organs. Palaeontogr. 

Abt. B 153, 28–99.] on the basis 

of morphological and anatomical similarities. 

Indeed, this study clearly shows 

that the ultrastructure of the spores of 

Triassic and Jurassic Equisetales is intermediate 

between that of Carboniferous 

Calamites and modern Equisetum, 

demonstrating that Equisetum evolved 

from Calamites. The present study illustrates 

how Calamites spores of the 

Calamospora type progressively 

evolved into the quite different spores of 

living Equisetum. Indeed, it would not 

have been possible to understand how 

such a transition occurred without this 

TEM study. Similarly, it underscores the 

proclivity of the Equisetales to develop 

unusual structures in both their spores 

and their reproductive organs. Moreover, 

it demonstrates that the ultrastructural 

features of equisetalean spores changed 

greatly during their long evolutionary 

history, whereas those of other Pteridophytes 

groups, such as ferns and lycopsids, 

remained unchanged. However, the 

most striking outcome of this comparative 

TEM study is the demonstration that 

spores of the Triassic horsetails show 

many ultrastructural similarities with 

spores of the Ophioglossaceae, a living 

family of primitive ferns. According to 

Lugardon and Brousmiche Delcambre 

[Lugardon, B., Brousmiche-Delcambre, 

C., 1994. Exospore ultrastructure in 

Carboniferous sphenopsids. In: Kurmann, 

M.H., Doyle, J.A. (Eds.), Ultrastructure 

of fossil spores and pollen, pp. 

53–66, Royal Botanic Gardens, Kew.], 

who made the same observations for the 

spores of Calamites, these similarities 

indicate that horsetails and ferns are 

closely related and have a common origin. 

These results are in agreement with 

those of a recent DNA analysis which 

shows that the horsetails and the ferns 

form a monophyletic group of plants. 

Moreover, they support and are in 

agreement with the phylogenetic analysis 

using cladistic principles of Stein et 

al. [Stein, W.E., Wight, D.C., Beck, 

C.B., 1984. Possible alternatives for the 

origin of Sphenopsida. Syst. Bot. 9 (1), 

102–118.] which suggests that the 

sphenophytes and the ferns as a whole 

are descended from a common ancestor, 

the Devonian complex Cladoxylopsida 

including the Hyeniales. The fact that 

the Hyeniales combine sphenophyte and 

fern-like features would explain why the 

spores of the ferns and those of the ancient 

sphenophytes have the same ultrastructural 

features. Moreover, this study 

indicates that spore ultrastructure retains 

ancestral features for a longer time than 

the other parts of the plants which 

evolve and thus change more rapidly. 

This study provides a further demonstration 

that spore ultrastructure, particularly 

of those preserved in situ, is of great 

value in researching the evolutionary 

and phylogenetic relationships of plants. 

2010010064 

现生和化石买麻藤孢子外壁超微结构 

和形态的对比 = Comparative pollen 

morphology and ultrastructure of modern 

and fossil gnetophytes. ( 英文 ). Tekleva 

M V; Krassilov V A. Review of Palaeobotany 


156(1-2): 130-138 2 图版 . 

A considerable disparity of pollen 

characters in the modern Gnetales (including 

the inaperturate and monosulcate 

germination types, the psilate, polyplicate 

and spinulose sculptural types) 

stands in sharp contrast with their ultrastructural 

uniformity. In all of the ultrustructurally 

studied living species of 

Ephedra, Welwitschia and Gnetum, the 

26

infratectum is granular, mostly consisting 

of small granules, while the 

endexine is uniformly thick and lamellate. 

The recently discovered fossil 

gnetophytes are a diverse group, recognized 

primarily on the basis of their ovulate 

cupules, but heterogeneous in respect 

to their pollen organs and pollen 

morphology. The pollen grains are 

mostly asaccate or, rarely, bisaccate 

(Preflosella, Dinophyton), with small 

ruguloid sacci (Baisianthus) or vestigial 

protosaccate structures (Cryptosacciferites). 

The germination types are inaperturate, 

cryptoporate, monosulcate 

and trisulcate. In the majority of forms 

the infratectum is granular, consisting of 

small granules, large granules, combinations 

of various granules, or even columella-like 

elements; rarely, the infratectum 

is alveolar. The endexine varies 

from distinctly lamellate to homogeneous. 

Our analysis of pollen grain morphology 

and ultrastructure of extant 

gnetophytes lends support to phylogenetic 

relatedness of extinct forms. Palaeobotanical 

data show a striking parallelism 

of morphological variations between 

gnetophytes and angiosperms. 

2010010065 

Osmunda regalis L. 孢子与相似孢子 

在形态、发育及外壁结构上的对比 = 

Morphological, developmental and ultrastructural 

comparison of Osmunda 

regalis L. spores with spore mimics. ( 英 

文 ). Moore S E M; Gabarayeva N; 

Hemsley A R. Review of Palaeobotany 


184 3 图版 . 

A comparison of spores from Osmunda 

regalis L. and polystyrene-based 

spore mimics has been undertaken in 

order to provide insights into the development 

and formation of relatively 

primitive fern spores. In recent years, 

self-assembly experiments have provided 

different perspectives on the processes 

involved in pollen and spore wall 

pattern formation. The spore mimics obtained 

from the latest experiments 

closely resemble extant spore types and 

permit comparison with both immature 

and mature spores. 

2010010066 

Trevesia burckii( 五加科 ) 四分体期 

孢壁的发育 II: 自集合作用的更多证 

据 = Sporoderm development in Trevesia 

burckii (Araliaceae): II. Post-tetrad 

period: Further evidence for the participation 

of self-assembly processes. ( 英 

文 ). Gabarayeva N; Grigorjeva V; Rowley 

J R; Hemsley A R. Review of Palaeobotany 


156(1-2): 233-247 6 图版 . 

The developmental events in the periplasmic 

space, the cytoplasm of microspores 

and in the tapetum of Trevesia 

burckii have been traced in detail during 

microspore ontogeny from the late tetrad 

stage, through the post-tetrad period, to 

intine formation (following on from our 

study of the tetrad period also published 

herein). The data obtained give further 

support to our previously proposed hypothesis 

regarding self-assembly of a 

number of colloidal micellar systems 

during exine (and possibly intine) development. 

The main structures of the mature 

exine are columellae, granules and 

tripartite lamellae with central white 

lines which evidently form on a base of 

cylindrical, spherical and lamellar transitive 

micelle mesophases after sporopollenin 

accumulation. Further information 

provides evidence for the importance of 

physico-chemical regularities in pollen 

wall development. 

2010010067 

通过扫描透射 X 射线显微镜 

(STXM) 研究现代和化石孢壁的外 

壁结构及化学成分 = Ultrastructural 

and chemical study of modern and fossil 

sporoderms by Scanning Transmission 

X-ray Microscopy (STXM). ( 英文 ). 

Bernard S; Benzerara K; Beyssac O; 

27

Brown Jr. G E; Stamm L G; Duringer P. 

Review of Palaeobotany and Palynology, 

2009, 156(1-2): 248-261 5 图版 . 

Diverse microscopy techniques have 

been extensively used in the past to 

study the ultrastructure of modern and 

fossil sporoderms for various purposes 

such as taxonomic identification or 

study of sporoderm formation and its 

evolution in different groups of plants. 

Optical microscopy and Scanning and 

Transmission Electron Microscopies 

(SEM and TEM) have been particularly 

useful in providing structural information 

at the μm- and nm-scales. In parallel, 

chemical analyses have been conducted 

on bulk samples to document 

variations in sporopollenin composition 

between major groups and compositional 

evolution/preservation during 

coalification processes. Here, we describe 

a microscopy tool, Scanning 

Transmission X-ray Microscopy 

(STXM), which offers valuable capabilities 

for palynological studies as demonstrated 

by applications of this technique 

to fossil spores over the past decade. 

This microscopy technique, which uses 

soft X-rays produced by synchrotron radiation 

sources, provides 25-nm spatial 

resolution element-based image contrast, 

and K or L near-edge X-ray absorption 

fine structure (NEXAFS) spectra at each 

25-nm x 25-nm pixel in a STXM image 

for a number of key elements (e.g., K- 

edges of C, N, O, F, Na, Mg, Al, and Si 

and L-edges of K, Ca, Ti-Zn, Ga, Ge, As, 

Se, Rb, and Sr). STXM can be performed 

in situ on thin samples with no 

need for prior chemical extraction or 

staining. Comparison with conventional 

imaging techniques such as optical microscopy 

and TEM shows that STXM is 

an ideal complement to these microscopies. 

We present new STXM data 

obtained on modern Lilium longiflorum 

Thunb. pollen grains and on wellpreserved 

lycopsid spores, identified as 

Annalepis zeilleri (Fliche) Grauvogel- 

Stamm and Duringer, collected from the 

Lettenkohle Formation of the Wasselonne 

Quarry (NE France). Using this 

technique, different biochemical compounds 

such as sporopollenin or cellulose 

can be specifically imaged at the 

25-nm scale. Additionally, NEXAFS 

spectra can provide information on elemental 

speciation, i.e. the types of C- 

containing functional groups (e.g., aromatic, 

aliphatic, carboxylic, alcoholic…) 

and the redox state of iron and manganese. 

Based on these analyses, it is possible 

to document the chemical preservation 

of fossil spores that experienced 

diagenesis and possibly metamorphism. 

2010010068 

晚更新世以来浙江余姚地区植被变化 

及人类活动 = Vegetation and human 

activity in Yuyao ( Zhejiang province) 

inferred from the sporo-pollen record 

since the Late Pleistocene. ( 中文 ). 李春 

海 ; 唐领余 ; 万和文 ; 王苏民 ; 姚书春 ; 张殿 

发 . 微体古生物学报 , 2009, 26(1): 48- 

56 

浙江余姚河姆渡镇 7 m 钻孔的孢粉 

记录提供了晚更新世以来的植被变化 

及其反映的气候变化和人类活动的历 

史。在全新世海侵之前 , 研究区发育常 

绿落叶阔叶混交林。全新世早中期 , 海 

侵发生 , 植被由亚热带针阔叶混交林发 

展为常绿落叶阔叶混交林 , 碳屑和禾本 

科 ( ≥35μm) 花粉的增高说明 , 可能在河 

姆渡文化之前 , 研究区已经有人类活 

动。7 cal. kyr BP 之后 , 高含量的禾本 

科 ( ≥35μm) 花粉表明钻孔点的临近地 

区有水稻种植。亚热带与温带乔木花 

粉的比值 ( sub/ tem) 显示 , 在 8 cal. kyr 

BP 之前的海侵期间 , 浙江余姚地区气 

候最温暖湿润 ;7. 5 —5. 86 cal. kyr BP 

期间 , 温度低于海侵期但是仍然属于全 

新世暖期 , 温度高于现在 ;5. 86 cal. kyr 

BP 之后 , 温度下降 ;4 cal. kyr BP 之后 

温度进一步下降 , 接近现在。 

28

2010010069 

西鄂尔多斯六种强旱生植物的花粉形 

态及其生态因子 = Study on pollen 

morphology and its ecological factors of 

Xerophil in western Erdos.. ( 中文 ). 韩 

雪 ; 智颖飙 ; 周忠泽 ; 杨持 ; 安树青 ; 宿志安 ; 

王强 . 微体古生物学报 , 2009, 26(1): 

57-64 1 图版 . 

为了探讨特殊生境条件下强旱生植 

物的花粉形态与生态因子的相关性 , 应 

用光学显微镜对西鄂尔多斯地区 5 月 

份开花的 2 科 5 属 6 种强旱生灌木刺 

柄叶棘豆 (Oxytropis aciphylla Ledeb) 

、沙冬青 [ Ammopiptanthus mongolic 

(Maxim) Cheng f . ] 、狭叶锦鸡 

儿 (Caragana stenophylla Pojark) 、四合 

木 (Tet raena mongolica Maxim) 、霸王 

(Zygophyllum xanthoxylon Maxim) 和 

柠条锦鸡儿 (Caragana korshinskiiKom) 

的花粉形态进行了观察和研究 . 结果表 

明 : 花粉粒近球形至长球形 , 萌发孔主 

要是 3 孔沟 , 沟狭。外壁纹饰主要是细 

网状纹饰。同时研究了采样点生态因 

子 , 包括地理位置、海拔高度、年降水 

量、年积温及生境等 , 特别提供了 5 月 

份的气候因子 , 得出这些花粉分布区的 

主要生态因子。 

2010010070 

蒙古东戈壁盆地万利特凹陷特 1 井早 

白垩世孢粉组合 = Early Cretaceous 

sporopollen assemblages from well Te 1 

in the Wanlite depression,eastern Gobi 

basin,Mongolia. ( 中文 ). 魏文艳 ; 贺振建 ; 

边雪梅 ; 齐玉民 ; 王香婷 ; 陈书伟 ; 吴金宝 . 

微体古生物学报 , 2009, 26(2): 164- 

172 3 图版 . 

将东戈壁盆地万利特凹陷特 1 井划 

分为三个孢粉组合 :1. Cicatricosis 

porites-Classopollis-Piceaepollenites 

Piceites 组合 , 2. Perinopollenites- 

Cycadopites-Pinaceae-Walchiites 组合 ; 

3. Laevigatosporites-Lygodiaceae- 

Perinopollenites 组合 , 根据孢粉组合特 

征推测第一个孢粉组合倾向于早白垩 

世最早期 Berriasian 期 , 但也不排除属 

于晚侏罗世的可能 , 第二个组合为早 

白垩世 Berriasian —Valanginian 期 , 第 

三个孢粉组合为早白垩世 Hauterivian 

—Barremian 期 . 

2010010071 

日本海南部全新世的栎属的花粉粒的 

纹饰 = Sculpture of pollen grains of 

Quercus L. from the holocene of the 

south of the Sea of Japan. ( 英文 ). 

Naryshkina N N; Evstigneeva T A. Paleontological 

Journal, 2009, 43(10): 

1309-1315 2 图版 . 

Fossil pollen grains of Quercus L. 

were studied with application of an EVO 

40 scanning electron microscope. The 

material came from Holocene core samples 

from deep water zone of the south 

of the Sea of Japan and shelf zone of 

East Korea Bay. The pollen grains were 

obtained from three radiocarbon-dated 

palynological assemblages. Six types of 

fossil pollen grains were revealed: four 

of them were assigned to deciduous oaks 

and two were assigned to evergreen oaks. 

2010010072 

藏南古近系柳区砾岩孢粉化石的发现 

及初步研究 = Discovery and preliminary 

study on palynofossils from the Paleogene 

Liuqu conglomerates in southern 

Xizang (Tibet). ( 中文 ). 韦利杰 ; 刘小 

汉 ; 严富华 ; 麦学舜 ; 周学君 ; 李广伟 ; 刘小 

兵 . 微体古生物学报 , 2009, 26(3): 249- 

260 1 图版 . 

作者首次对柳区砾岩夹层中的泥岩 

和泥质粉砂岩进行了孢粉学研究 , 共 

鉴定出 52 个形态属。其孢粉组合特 

征是 : 以被子植物花粉占优势 (62. 77 

% —83. 19 %), 其次是裸子植物花粉 

(11. 95 % —32. 31 %), 蕨类植物孢子 

最少 (4. 80 % —10. 38 %) 。被子植物 

花粉以具孔类为主 , 三孔沟或三沟类 

花粉在组合中有一定含量。裸子植物 

花粉以具双气囊类居多。孢粉植物群 

的总体特征表明其时代可能为古近纪 

29

晚期。当时的古植被为落叶阔叶林或 

针阔混交林 , 气候较温暖湿润 , 主要为 

暖温带的环境。 

2010010073 

山东聊城地区阿城镇煤田二叠纪孢粉 

组合 = Permian sporo-pollen assemblages 

of the Echeng town coalfield,Liaocheng,Shandong 

Province. ( 中 

文 ). 宋香锁 ; 王奎峰 ; 王明镇 ; 贾强 . 微体 

古生物学报 , 2009, 26(3): 271-282 

对山东聊城阿城镇煤田 A1926 、 

A2026 、L104 钻孔岩石样品进行了分 

析 , 发现从太原组中上部到上石盒子 

组地层中均有大量孢粉化石保存 , 经 

分析鉴定和统计 , 共有孢粉化石 53 个 

属 168 种及部分未定种。根据孢粉属 

种的纵向分布情况及含量的变化 , 在 

本区二叠系建立了 4 个孢粉组合 , 自 

上而下为 : IV. Triquitrites microgranifer-Macrotorispora 

media 组合带 ; 

III. Limitisporites rhombicorpus- 

Patellisporites meishanensis 组合带 ; II. 

Gulisporites 

cochlearius- 

Sinulatisporites sinensis 组合带 ; I. 

Thymospora pseudothiessenii- 

Laevogatisporites vulgaris 组合带。通 

过与邻区及华北部分地区对比 , 确定 

本区孢粉组合所在的地质时代应为 : 

太原组中上部 , 早二叠世早 ( 组合 Ⅰ); 

山西组 , 早二叠世中期 ( 组合 Ⅱ ); 下石 

盒子组 , 早二叠世晚期 ( 组合 Ⅲ ); 上石 

盒子组 , 晚二叠世早期 ( 组合 Ⅳ ). 

2010010074 

瑞典南部三叠纪 - 侏罗纪过渡层孢粉地 

层学 = Palynostratigraphy of the Triassic-Jurassic 

transition in southern Sweden. 

( 英文 ). Larsson L M. GFF, 2009, 

131(1-2): 147-163 12 图版 . 

Palynological samples from Upper 

Triassic and Lower Jurassic exposures 

and borehole sections of the Hoganas 

and Rya formations (Fm), NW Skane 

(Sweden), exhibit diverse and generally 

well-preserved palynomorph assemblages 

that can be divided into four miospore 

zones (from bottom to top): (1) the 

informal "Topmost upper Rhaetian" 

zone of Lund; (2) the TSI assemblage 

zone which spans the Triassic-Jurassic 

(T-J) boundary; (3) the Hettangian 

Pinuspollenites-Trachysporites Zone and 

(4) the Sinemurian Cerebropollenites 

macroverrucosus Zone. Uppermost 

Rhaetian and T-J boundary strata have 

previously been considered to be absent 

in Skane, but are identified palynologically 

in all but one (Kulla-Gunnarstorp) 

section in this study. The palynological 

assemblages characterise continental 

deposition with intermittent marine influences. 

The presence of well-preserved 

miospores in nearly all assemblages indicates 

minimal transport during dispersal 

and deposition. The T-J transition is 

characterised by a spore-spike, not previously 

recognised in T-J assemblages 

of Skane. However, the upper Hettangian 

and Sinemurian assemblages of this 

study are similar in composition to coeval 

palynofloras derived from sediments 

deposited in paralic environments elsewhere 

in Skane and Denmark. 

2010010075 

瑞典斯韦阿兰东南部乌普兰地区石器 

时代的植被 = Stone age vegetation in 

Uppland, Southeastern Svealand, Sweden. 

( 英文 ). Karlsson S. GFF, 2007, 

129(4): 295-305 

A compilation has been done of 12 

pollen diagrams from the county of Uppland, 

southeastern Sweden, in order to 

describe the earliest vegetational history 

in the Uppland archipelago. All diagrams 

cover the Middle and the Late 

Neolithic (3300-2300 BC), while nine of 

them date back to the Early Neolithic 

(3900-3300 BC) and four to the Late 

Mesolithic (5500-3900 BC). The main 

part of the sites has been investigated in 

connection with archaeological projects. 

The pollen studies carried out so far are 

not detailed enough to trace the farming 

history in Uppland, but some important 

30

esults are obtained: (i) One site indicates 

weak signs of clearance and cultivation 

from the Late Mesolithic. (ii) 

From the Early Neolithic possible traces 

of cattle breeding occur at one site. (iii) 

More obvious but sparse finds of human 

indicators start during the Middle and 

the Late Neolithic, with possible cattle 

breeding from five sites and cultivation 

from four sites. Cattle breeding seems 

not to have been applied in the archipelago 

during the Stone Age, but was initiated 

when the sites were connected with 

the mainland. (iv) Palynological indications 

may verify that the maritime deciduous 

forest zone in the Stockholm 

archipelago is of natural origin. (v) The 

elm decline can be traced in more than 

50% of the diagrams and occur c. 2500 

BC. (vi) In seven diagrams from the 

Early Neolithic and 10 from the Middle 

and Late Neolithic, pollen of Picea occur 

in the sediments, indicating either limited 

spruce stands in the vicinity or 

windblown pollen, possibly from the 

eastern coast of the Baltic. 

2010010076 

北高加索西部晚三叠世孢粉植物群 = 

Late Triassic palynological flora from 

western Ciscaucasia. ( 英文 ). 

Yaroshenko O P. Paleontological Journal, 

2007, 41(11): 1190-1197 3 图版 . 

A palynological flora from Pre- 

Cretaceous deposits of western Ciscaucasia 

is studied. Although these deposits 

were previously referred to the Paleozoic, 

comparison with the palynological 

floras of other regions has dated them to 

the Late Triassic. A hypothesis is proposed 

that during the Late Triassic time 

western Ciscaucasia constituted an 

ecotone with a temperate warm climate. 

2010010077 

季曼北部晚泥盆世 ( 弗拉斯阶 ) 沉积 

中含孢子的孢子囊植物化石 = Fossil 

plants with spores in the sporangia from 

the Upper Devonian (Frasnian) deposits 

of northern Timan. ( 英文 ). Snigirevsky 

S M; Tschibrikova E V; Olli V A. Paleontological 

Journal, 2007, 41(4): 461- 

468 2 图版 . 

Fossil plants from the Upper Devonian 

(Frasnian) of northern Timan are 

studied. The sporangia contain wellpreserved 

spores, which were studied in 

transmitted light using a scanning electron 

microscope. The genus Gutzeitia S. 

Snigirevsky, gen. nov. is established. 

Macroremains and in situ spores of G. 

timanica (Petros.) S. Snig., comb. nov. 

and ?Cephalopteris mirabilis (Nath.) 

Nath. are described. Microspores in 

Dimeripteris gracilis Schmalh. are identified, 

and microspores and megaspores 

in ?Cephalopteris mirabilis are studied 

for the first time. 

牙形石 

2010010078 

四川盐边稗子田志留系牙形刺生物地 

层的再研究 = Restudy on the Silurian 

conodont biostratigraphy of the baizitian 

section in Yanbian County, Sichuan. ( 中 

文 ). 王成源 ; 王平 ; 杨光华 ; 谢伟 . 地层学 

杂志 , 2009, 33(3): 303-317 2 图版 . 

首次在稗子田剖面发现 

Caudicriodus woschmi dti 并确认 

Pteros pathodus eopennatus 带的存在 ; 

以前报道的本剖面的 Oz arkodina cris 

pa 和 Oz arkodina eosteinhornensis 经 

4 次样品分析 , 仍得不到确认。稗子田 

剖面的普里道利统 ( Pridoli) 的沉积可 

能不全 , 不宜建阶。志留系与泥盆系之 

间可能为假整合。进一步讨论了牙形 

刺分带以及志留系内部统间的界线。 

认为金淳泰等 (2005) 依据稗子田剖面 

命名的 6 个新阶名 , 不宜使用 

2010010079 

依据牙形刺确定的蒙古国塔琳波格德 

组 (Taliin Bogd Formation) 的时代 = 

Age of the Taliin bogd Formation of 

Mongolia based on conodonts. ( 中文 ). 

王成源 ;Dorjsuren Byambadash; 郎嘉 

31

斌 ;Yadamjav Dagva-Ochir;Horloo 

Yadamjav;Bujinlkham Boijir. 微体古生 

物学报 , 2009, 26(1): 31-38 1 图版 . 

在蒙古南部波尔海尔汗乌尔 (Bor 

hairhanuul) 剖面的塔琳波格德组下部 

的 6 个样品中发现了牙形刺 , 通过研究 

清楚地表明含牙形刺动物群的塔琳波 

格德组下部的时代是中洛霍考夫阶 ( 早 

泥盆世 ) 到中艾菲尔阶 ( 中泥盆世 ) 。 

塔琳波格德组的牙形刺动物群更接近 

于北美同时期的动物群 , 而与洲同期 

动物群相远。这一动物群可能属于冷 

水动物群。作者在文中描写了一个新 

种 : S teptotax is mongol ianus sp . nov. 

Wang 

2010010080 

塔里木中央隆起区上奥陶统的牙形刺 

= Upper Ordovician conodonts from the 

central high,Tarim block,NW China. ( 中 

文 ). 王志浩 ; 李越 ; 王建坡 ; 马俊业 ; 姚小 

刚 ; 黄智斌 ; 张园园 . 微体古生物学 

报 , 2009, 26(2): 97-116 3 图版 . 

塔里木板块中央隆起区的上奥陶统 , 

即巴楚露头剖面吐木休克组和良里塔 

格组以及塔克拉玛干沙漠腹地塔中油 

田井下良里塔格组皆为灰岩相。作者 

对前人报道的牙形刺带作了修改 , 首次 

系统描述牙形刺动物群全貌 , 共计 14 

属 21 种。在曾归入 Pygodusserra 带 

和 P. anserinus 带的吐木休克组底部 

和下部发现 

Yangtzeplacognathus jianyeensis , 故应 

改为 Yangtzeplacognathus jianyeensis 

带 ; 吐木休克组中部因发现 

Baltoniodus alobatus 和 B . variabils 共 

生 , 应属 B. alobatus 带。在 Yangt zeplacognathus 

jianyeensis 带和 

Baltoniodus alobat us 带之间尚未发现 

可靠的 B. variabilis , 因此是否存在 B. 

variabilis 带尚存疑问。巴楚露头区上 

奥陶统的牙形刺序列由下而上应为 

Yangtzeplacognathus jianyeensis 带 , 

Baltoniodus variabilis 带 ?, B. alobatus 

带和 Belodina confluens 带。塔中的良 

里塔格组则可识别出 B. confluens 带 

和 Yaoxianognathus yaoxianensis 带。 

将中央隆起区牙形刺动物群组合与其 

相邻的柯坪地块进行对比 , 说明晚奥陶 

世因两个地理区水深的差异导致牙形 

刺带完整性的差异 

2010010081 

早至中奥陶世牙形类的生物多样性 : 

中国东部安徽紫台 (Zitai) 组的一个实 

例研究 = Biodiversification of Early to 

Middle Ordovician conodonts: a case 

study from the Zitai Formation of Anhui 

Province, eastern China. ( 英文 ). Wu 

Rongchang; Percival I G; Zhan Renbin. 

Alcheringa, 2010, 34(1): 75 - 86 

The Lower-Middle Ordovician Zitai 

Formation of the South China palaeoplate 

consists of a succession of purple 

red, nodular argillaceous limestones. Palaeogeographically, 

it is distributed 

along the southeastern margin of the 

Yangtze Platform, and is of late Floian 

to Dapingian age, correlative with the 

Dawan Formation of the Middle and 

Lower Yangtze Platform. In Shitai 

County, Anhui Province, East China, the 

Zitai Formation is rich in conodonts, 

enabling the recognition of four biozones 

based on first appearance data. 

Detailed palaeontological and biostratigraphical 

study of these conodonts reveals 

that the Ordovician conodont radiation 

in the Lower Yangtze Platform 

attained its first diversity peak low in the 

Oepikodus evae Biozone. This diversification 

is generally consistent with macroevolutionary 

trends of brachiopods of 

South China and graptolites of the Upper 

Yangtze Platform, but was earlier 

than that of trilobites and acritarchs of 

the same palaeoplate. Correlation with 

the sea-level curve for South China suggests 

that conodont diversity change 

during the Ordovician radiation was 

mainly controlled by regional sea-level 

fluctuations 

32

2010010082 

哈萨克斯坦南部法门阶牙形石新属 

Barskovella 和 Bizignathus = New 

genera Barskovella and Bizignathus 

(Conodonts) from the Famennian of 

southern Kazakhstan. ( 英文 ). Gatovsky 

Yu A. Paleontological Journal, 2009, 

43(5): 550-557 5 图版 . 

New genera Barskovella gen. nov. 

and Bizignathus gen. nov. are described 

from the Famennian deep-sea carbonate 

deposits of the Bolshoi Karatau Mountain 

Range (southern Kazakhstan). 

2010010083 

哈萨克斯坦中部晚奥陶世硅质岩中的 

牙形石 = Conodonts from the upper Ordovician 

siliceous rocks of Central Kazakhstan. 

( 英文 ). Tolmacheva T Yu; 

Degtyarev K E; Ryazantsev A V; Nikitina 

O I. Paleontological Journal, 2009, 

43(11): 1498-1512 6 图版 . 

Several conodont localities of the upper 

Sandbian Stage are known in siliceous 

deposits of Central Kazakhstan. 

All of them produced similar assemblages 

overwhelmingly dominated by 

Periodon grandis with insignificant admixture 

of Scabbardella altipes, Hamarodus 

europaeus, Pygodus anserinus, 

Protopanderodus sp., and Drepanodus 

sp. The main feature of this fauna is in 

the co-occurrence of H. europaeus and P. 

grandis, forms characteristic for deepwater 

facies at shelf or microcontinents 

margins of temperate and warm-water 

paleobiogeographic provinces. The Ordovician 

paleo-oceanic basin of Kazakhstan 

and southern Urals were parts of the 

uniform biogeographic area as indicated 

by similarity of Ordovician conodont 

assemblages in siliceous deposits of 

these regions. 

2010010084 

沃罗涅什台背斜 ( 苏联地台中心区 

域 )Evlanovian 和 Livnian 亚阶 ( 晚泥 

盆世 )Polygnathus 属牙形石新发现 = 

New conodonts of the genus Polygnathus 

from the Evlanovian and Livnian 

(Upper Devonian) of the Voronezh Anteclise 

(central Devonian Field). ( 英文 ). 

Kirilishina E M; Kononova L I. Paleontological 

Journal, 2010, 44(1): 68-78 4 

图版 . 

New conodont species of the genus 

Polygnathus (P. krutoensis sp. nov., P. 

makhlinae sp. nov., P. menneri sp. nov., 

P. obruchevae sp. nov.) are described 

from the Evlanovian-Livnian (Upper 

Devonian) deposits of the Voronezh Anteclise 

(central regions of the Rassian 

platform). The ontogenetic series of the 

new species are presented. 

2010010085 

塔吉克斯坦中部 Palmatolepis 属弗拉 

斯阶牙形石新发现 = New Frasnian 

conodonts of the genus Palmatolepis 

from the Central Tajikistan. ( 英文 ). 

Bardashev I A. Paleontological Journal, 

2009, 43(3): 300-305 3 图版 . 

New Lower-Middle Frasnian conodonts 

of the genus Palmatolepis Ulrich 

et Bassler, 1926 are described from the 

Kalagach and Kulyali formations of the 

Sishkat key section of Central Tajikistan. 

Palmatolepis manzuri sp. nov. descends 

from Pa. punctata (Hinde) and is an ancestor 

of P. kireevae Ovnatanova, Pa. 

salibaevi sp. nov., and also of the P. 

rhenana Bischoff branch. 

2010010086 

俄罗斯地台东部弗拉斯阶牙形石 = 

Frasnian conodonts from the eastern 

Russian Platform. ( 英文 ). Ovnatanova N 

S; Kononova L I. Paleontological Journal, 

2008, 42(10): 997-1166 49 图版 . 

The Frasnian conodonts of the eastern 

Russian Platform from the Timan in the 

north to the Orenburg Region in the 

south are characterized in detail both paleontologically 

and stratigraphically. 

This paper is a continuation of a previously 

published monograph (Ovnatanova 

and Kononova, 2001) on the 

Frasnian conodonts of the shallow-water 

33

strata of the central Russian Platform, 

where polygnathids prevail. The conodont 

assemblages from the shallowwater 

and basinal sections of the Volga- 

Ural province and Southern Timan are 

analyzed. Problems and difficulties associated 

with the correlation of the shallow-water 

and deep-water Frasnian sections 

of the eastern Russian Platform 

and their correlation with the existing 

zonal conodont scales are discussed. The 

correlation between the deep-water 

Mendym deposits and the shallow-water 

Rechitza and Voronezh strata of the 

Volga-Ural province with the Vetlasyan 

and Sirachoi deposits of the Southern 

Timan is substantiated. The stratotype of 

the Semiluki Regional Stage of the Central 

Devonian Field contains equivalents 

of the lowermost beds of the Domanik 

Formation (unit 1), based entirely on polygnathids. 

Phylogenetic reconstructions 

for Palmatolepis and Polygnathus are 

suggested based on the ontogenetic series 

for some species of these two genera 

and the presence of transitional forms 

between some of the species. Based on 

these phylogenetic reconstructions, 

conodont zonal scales for the shallowwater 

and deep-water sections of the 

Frasnian Stage of the Russian Platform 

are proposed and their correlation with 

the existing conodont zonal scales is 

also adduced. Some aspects of biofacies 

control are considered based on the distribution 

of conodonts in the sections 

studied. In Systematic Paleontology, 91 

conodont species of the genera Ancyrodella, 

Mesotaxis, Palmatolepis, and 

Polygnathus are described, including the 

new species Palmatolepis menneri, P. 

kaledai, P. acutangularis, and Polygnathus 

reitlingerae. 

2010010087 

哈萨克斯坦南部法门阶沉积中的 

Antognathus 新种 ( 牙形石 ) = New 

species of Antognathus (Conodonts) 

from the Famennian deposits of southern 

Kazakhstan. ( 英文 ). Gatovsky Yu A. 

Paleontological Journal, 2008, 42(2): 

176-180 4 图版 . 

A new conodont species, Antognathus 

vjatsheslavi sp. nov., is described from 

the Famennian shallow-water carbonate 

deposits of the Bolshoi (Greater) 

Karatau Range in southern Kazakhstan. 

2010010088 

晚古生代牙形石分子和器官的形态功 

能分析 = Morphofunctional analysis of 

Late Paleozoic conodont elements and 

apparatuses. ( 英文 ). Zhuravlev A V. Paleontological 

Journal, 2007, 41(5): 549- 

557 8 图版 . 

Five functional types are recognized 

among Late Paleozoic conodont elements; 

they are distinguished by morphological 

and histological characteristics: 

grasping-holding, filtering, cutting, 

crushing, and grinding. Combinations of 

functional types of elements form functional 

types of conodont apparatuses, the 

main of which are filtering, graspingcutting, 

grasping-pressing, graspingcutting-grinding, 

and grasping-cuttingcrushing 

apparatuses. 

小壳化石 

2010010089 

似软舌螺类化石 ( 寒武纪疑难生物 ) 

形态学和分类学新数据 = New data on 

the morphology and systematics of hyolithelminthes 

(Cambrian problematic 

organisms). ( 英文 ). Novozhilova N V. 


120-124 2 图版 . 

Phosphatic structures are discovered 

in the tube interior of the hyolithelminth 

species Hyolithellus vitricus from the 

Lower Cambrian of the Siberian Platform. 

Anatomic interpretation of these 

structures suggests that these small-sized 

shelly fossils represent the earliest 

worm-shaped organisms probably 

closely related to modern Nemathelminthes. 

34

2010010090 

陕南早寒武世早期管柱状生物化石新 

发现 = Discovery on the column-like 

fossils from the early Early Cambrian of 

south Shaanxi. ( 中文 ). 刘云焕 ; 邵铁全 ; 

房启飞 ; 冯健雪 ; 郑曦 . 微体古生物学 

报 , 2009, 26(3): 291-296 1 图版 . 

繁殖是生物体产生子代的现象 , 是 

生物体最基本的特征之一。最近作者 

在陕南宁强宽川铺地区早寒武世最早 

期的宽川铺生物群中发现了数十枚管 

柱状生物化石 , 首次发现这些管柱状 

生物化石具可能的 “ 断裂生殖 ” 特征。 

在部分管柱状生物化石上可清晰分辨 

出 “ 收缢带 ”、“ 收缢纹 ” 和 “ 新生单节 ” 

等断裂生殖特征 , 据此建立可能的管 

柱状生物 “ 断裂生殖 ” 生殖发育序列。 

2010010091 

陕南早寒武世早期磷酸盐化 

Punctatus 发育模式研究 = Study on 

the developmental model of phosphatized 

Punctatus from the earliest 

Cambrian of south Shaanxi. ( 中文 ). 刘 

云焕 ; 邵铁全 ; 韩健 ; 房启飞 ; 冯健雪 ; 郑曦 . 

微体古生物学报 , 2009, 26(3): 243- 

248 1 图版 . 

在陕南宁强宽川铺地区早寒武世早 

期灯影组宽川铺段地层中发现了数十 

枚呈三维立体精美保存的磷酸盐化 

Punctatus 动物化石 , 包括花冠状口部 , 

5 辐射锥体及不同发育阶段的胚胎化 

石标本和 2 枚罕见的完整 Punctatus 

化石。研究表明 , 这些胚胎标本中的 

部分类型与 Punctatus 有关 , 通过对这 

些 Punctatus 及与 Punctatus 有关的胚 

胎化石认真观察 , 对 Punctatus 的生长 

方式和发育模式进行了研究 , 提出两 

极生长发育模式。腔肠动物的出现标 

志着真后生动物的开始 , 所以腔肠动 

物一直在生物起源与演化研究方面占 

据显要地位 , 上述研究为 “ 化石胚胎学 ” 

这一新的研究领域增添了新内容。 

古植物学 

综论 

2010010092 

北太平洋框架植物群发展的 Koryak 

阶段 = The Koryak phase of the Flora 

development in the Northern Pacific 

frame. ( 英文 ). Moiseeva M G. Paleontological 

Journal, 2009, 43(6): 702- 

710 6 图版 . 

The Koryak phase of the floristic development 

in the Northern Pacific frame 

is discussed. Newly obtained data on the 

Koryak Flora from the Amaam Lagoon 

area (Northeastern Russia) and Paleocene 

floras of the Northern Alaska have 

extended geographic and temporal 

ranges of the phase. Interregional 

statuses of the Koryak phase and phytostratigraphic 

horizon based on this phase, 

which is traced over the entire Northern 

Pacific frame and not just the Anadyr- 

Koryak region as was earlier supposed, 

are substantiated. The upper boundary of 

this horizon is defined; the age ranges 

from the Late Maastrichtian-Danian to 

Early Selandian. 

2010010093 

俄罗斯滨海边疆区南部早白垩世 

Lipovtsy 煤田针脂煤的成煤植物 = 

The coal-forming plants of rhabdopissites 

in the Lipovtsy coal field (Lower 

Cretaceous of Southern Primorye). ( 英 

文 ). Bugdaeva E V; Markevich V S. Paleontological 

Journal, 2009, 43(10): 

1217-1229 7 图版 . 

The plants that produced unique resinous 

coals (rhabdopissites) of the 

Lipovtsy coal field are revealed. They 

belong mainly to the group Miroviaceae 

(Oswaldheeria). Pseudotorellia (Ginkgoales) 

played an important role in the 

formation of humic coals of this Early 

Cretaceous coal field. The coal-forming 

plants comprise also cyatheaceous and 

gleicheniaceous ferns. A leafy shoot of 

Pseudotorellia has been found in this 

locality for the first time. It is assigned 

to the new species Pseudotorellia krassilovii 

Bugdaeva sp. nov. 

35

2010010094 

中生代买麻藤类和早期被子植物的多 

样性 = Diversity of Mesozoic gnetophytes 

and the first angiosperms. ( 英文 ). 

Krassilov V A. Paleontological Journal, 

2009, 43(10): 1272-1280 1 图版 . 

A provisionary system of gnetophytes 

is proposed, including recently discovered 

Mesozoic members. The following 

principal characters are used, in descending 

order of significance: strobilar 

structure of ovulate organs (eugnetophytes) 

as opposed to flowerlike cupules 

and their aggregates (anthognetophytes), 

radial vs. bilateral symmetry of seed cupules, 

and morphological distinctions in 

the pollen organs, pollen micromorphology 

and exine ultrastructure. The fossil 

members show mosaic associations of 

morphological traits, which attests to 

different evolution rates of their ovulate 

and pollinate structures. The system includes 

two superorders and eight orders, 

several of which are new. A dichotomous 

key is provided to differentiate between 

genera of fossil gnetophytes based 

on ovulate structures. Two stages in evolution 

of gnetophyte morphological diversity 

are recognized: first in the Triassic 

and then in the Early Cretaceous, the 

latter was associated with the origin of 

new type herbaceous wetland communities. 

Angiosperms or some of them 

might have originated as elements of 

gnetophyte diversity in such communities. 

2010010095 

阿拉斯加半岛北部的晚古新世植物 

群 : 植物通过白令陆桥的迁移及环境 

变化的影响 = Late paleocene flora of 

the northern Alaska Peninsula: the role 

of transberingian plant migrations and 

climatic change. ( 英文 ). Moiseeva M G; 

Herman A B; Spicer R A. Paleontological 

Journal, 2009, 43(10): 1298-1308 6 

图版 . 

For the first time, the Late Sagwon 

Flora is described from the upper beds 

of the Prince Creek Formation (Upper 

Paleocene) at the Sagavanirktok River 

(northern Alaska Peninsula). The flora is 

dominated by the angiosperm Tiliaephyllum 

brooksense Moiseeva et Herman 

sp. nov. and conifer Metasequoia 

occidentalis (Newb.) Chaney. The Late 

Sagwon Flora is most similar to the 

Danian or Danian-Selandian flora from 

the middle part of the Upper Tsagayan 

Subformation (Amur Region) and lower 

part of the Wuyun Formation (Heilongjiang 

Province, China). This similarity 

allows us to hypothesize that the genus 

Tiliaephyllum, which dominated in the 

Late Tsagayan Flora, migrated via the 

Bering Land Bridge from southern paleolatitudes 

of the Far East to high latitudes 

of the Arctic Pacific, due to the 

progressively warming climate of the 

Paleocene. Additional new angiosperm 

species are described from the Late 

Sagwon Flora: Archeampelos mullii 

Moiseeva et Herman sp. nov., Tiliaephyllum 

brooksense Moiseeva et Herman 

sp. nov., and Dicotylophyllum sagwonicum 

Moiseeva et Herman sp. nov. 

2010010096 

Valdai 高地南部晚更新世果实种子化 

石组合 = Upper pleistocene carpological 

assemblages from the south of the 

Valdai Upland. ( 英文 ). Zyuganova I S. 


1351-1362 4 图版 . 

Paleocarpological study was accomplished 

at four Upper Pleistocene sections 

of the Central Forest State Nature 

Biosphere Reserve (southern of Valdai 

Uplands). Sixty-five taxa of higher 

plants were found in the fossil flora of 

the region. Two carpological assemblages 

were distinguished reflecting different 

ecological and climatic conditions. 

The earlier assemblage is typical of Mikulino 

(Eemian) Interglacial, and the 

later corresponds to interglacial/glacial 

transition and the beginning of Early 

36

Valdai (Early Weischelian) glacial epoch. 

The obtained paleocarpological results 

were considered in light of palynological 

data. 

2010010097 

新西兰侏罗纪的植物和气候 = Vegetation 

and climate of the New Zealand Jurassic. 

( 英文 ). Pole M. GFF, 2009, 

131(1-2): 105-111 

New Zealand's Jurassic plant fossils 

are known from non-marine settings in 

two terranes: the Murihiku forearc basin 

and from a small area on the Rakaia Terrane, 

an accretionary prism. These terranes 

lay in relatively high latitudes 

along the Gondwana margin but their 

precise location, latitude and position 

with respect to each other is unclear. 

The flora was dominated by conifers, 

ferns, bennettitaleans, pentoxylaleans 

and locally equisetaleans, but it is relatively 

depauperate, perhaps reflecting a 

high latitude position. Most climate indicators 

suggest a warm temperate climate 

with rainfall that was not especially 

high and that might have been 

seasonal at times. Revision of the New 

Zealand Jurassic flora is overdue, and 

while new genera may be discovered, 

species numbers may well decrease. 

藻类 

2010010098 

再访意大利 Umbria–Marche: 对西 

特提斯渐新世沟鞭藻孢囊事件的精细 

磁性地层校准 = Umbria–Marche revisited: 

A refined magnetostratigraphic 

calibration of dinoflagellate cyst events 

for the Oligocene of the Western Tethys. 

( 英文 ). Prossa J; Houbenb A J P; Simaeysc 

S V; Williamsd G L; Kotthoffa 

U; Coccionie R; Wilpshaarf M; Brinkhuisb 

H. Review of Palaeobotany and 

Palynology, 2010, 158(3-4): 213-235 4 

图版 . 

In order to contribute to the improvement 

of biostratigraphic age control for 

the Oligocene of the Western Tethys, we 

have carried out a high-resolution study 

of dinoflagellate cysts from three outcrop 

sections in the Umbria–Marche Basin 

of Central Italy. All three sections 

investigated (Contessa Barbetti Road, 

Monte Cagnero and Pieve d'Accinelli) 

have magnetostratigraphic age control, 

thus allowing us to firmly tie the identified 

dinoflagellate cyst bioevents to the 

global geomagnetic polarity timescale. 

The Oligocene succession of the 

Umbria–Marche Basin is marked by recurrent 

acmes of Chiropteridium spp., 

Lingulodinium machaerophorum and 

Deflandrea spp. that can be correlated 

between the sections studied. These 

acmes originate from long-distance 

transport from near-shore environments 

into the pelagic setting represented by 

the sections studied, probably triggered 

by eustatic sea-level variations. Four 

formal dinoflagellate cyst zones of 

Wilpshaar et al. (1996; Journal of the 

Geological Society, London 153, 553- 

561), viz the Hpu, Clo, Dbi, and Ebu 

zones are revised. Furthermore we propose 

two new subzones for the Dbi zone. 

The new taxon Oligokolpoma galeottii is 

formally described. 

2010010099 

南极洲东部三叠纪的一种分类不明的 

非海相似叶状体生物 = An enigmatic 

non-marine thalloid organism from the 

Triassic of East Antarctica. ( 英文 ). 

Bomfleur B; Krings M; Kaštovský J; 

Kerp H. Review of Palaeobotany and 

Palynology, 2009, 157(3-4): 317-325 4 

图版 . 

An enigmatic thallophyte (Litothallus 

ganovex gen. et sp. nov.) occurs in the 

form of compressions with cellular preservation 

and associated sheets of complete 

cells in non-marine Triassic deposits 

in the Transantarctic Mountains, Antarctica. 

A combination of microscopic 

techniques (i.e. bright field and epifluorescence 

microscopy, SEM) was used to 

document details of this organism. The 

thalli are flat and appear to be composed 

37

of one to several congruently superimposed 

cell sheets that together form a 

plectenchyma or pseudoparenchyma. 

This discovery represents the youngest 

record of sheets of fossil cells, which 

have heretofore exclusively been reported 

from the Proterozoic and Palaeozoic, 

and is one of the few examples of 

cell sheets that can be attributed to macroscopic 

remains with confidence. We 

interpret the thalloid organism from 

Antarctica as the remains of a crustose 

freshwater macroalga based on its occurrence 

in overbank deposits of a braided 

fluvial environment and its morphological 

similarity to thalli of extant freshwater 

representatives of the red algal order 

Hildenbrandiales. 

2010010100 

波兰中部 Holy Cross 山脉下法门阶的 

浮游植物 = Lower Famennian phytoplankton 

from the Holy Cross Mountains, 

Central Poland. ( 英文 ). Filipiak P. 

Review of Palaeobotany and Palynology, 

2009, 157(3-4): 326-338 4 图版 . 

A rich phytoplankton assemblage and 

low diversity miospore microflora is described 

from the Lower Famennian deposits 

of the Kowala Quarry, Holy Cross 

Mountains, Central Poland. This assemblage 

is assigned to the Pw acritarcha 

zone, which is correlated with the late 

triangularis–crepida standard conodont 

zones based on appearance of the acritarch 

Puteoscortum williereae. Comparison 

of the present palynological results 

with well-documented data from 

Belgium clearly indicates differences in 

marine microflora composition in both 

regions. The important taxa Visbysphaera 

(?) occultata, Ephelopalla media, 

and Palacanthus tripus in Belgium are 

absent in the samples from the Holy 

Cross Mountains and by contrast, the 

phytoplankton frequent in Poland (Lophosphaeridium, 

Dictyotidium or Cymatiosphaera) 

are rare in Belgium. The 

taxonomical difference between the 

Holy Cross Mountains and Belgium palynoflora 

may probably reflect environmental 

differences: offshore and more 

proximal environmental conditions respectively. 

Three new species (Leiofusa 

turnauae sp. nov., Lophosphaeridium 

irregularis sp. nov. and Veryhachium? 

kowalae sp. nov.) have been formally 

instituted and two new taxa (Centrasphaeridium 

sp. A and Centrasphaeridium 

sp. B) are left in open nomenclature. 

2010010101 

新疆巴楚晚奥陶世礁丘中的蓝菌群落 

= Cyanobacterial community from the 

reef mound of the Lianglitag Formation 

(Upper Ordovician),Bachu,Xinjiang,NW 

China. ( 中文 ). 王建坡 ; 李越 ; 张园园 ; 杨 

海军 ; 黄智斌 . 微体古生物学报 , 2009, 

26(2): 139-147 

新疆巴楚上奥陶统良里塔格组 “ 中 

红灰岩 ” 中见蓝菌 - 绿藻形成的礁丘 , 常 

见 3 类蓝菌类化石 : Gi rvanel 

la ,Renalcid 和 Ortonella , 其中 

Renalcid 包括 Renalcis 和 Izhella 。蓝 

菌群落所形成的微生物岩构造包括钙 

化的微生物膜和微生物席、叠层石和 

凝块石 , 对礁灰岩的建造作用主要体现 

在作为灰泥物源、粘结颗粒和形成格 

架 

2010010102 

地中海东部颗石藻锶 / 钙比值 : 生产与 

输出过程 = Coccolith Sr/Ca ratios in 

the eastern Mediterranean: Production 

versus export processes. ( 英文 ). Auliaherliaty 

L; Stoll H M; Ziveri P; Malinverno 

E; Triantaphyllou M; Stravrakakis 

S; Lykousis V. Marine Micropaleontology, 

2009, 73(3-4): 196-206 

Samples collected by two sediment 

traps located southwest of Crete in the 

eastern Mediterranean (EMED) [48A 

(1953 m) and 48B (950 m)] from June 

2005 to May 2006 were used to study 

fluxes of organic carbon, carbonate and 

coccolithophores in combination with 

the variations of Sr/Ca ratios in different 

individually picked coccolith species. 

38

Considering the complexity of the 

EMED, we validate the use of Sr/Ca ratios 

as productivity proxy and unravel 

the varied processes which may influence 

it. We examined the relationship 

between the seasonal peaks in export 

fluxes and the Sr/Ca ratio in coccoliths 

of three upper photic zone coccolithophores 

species collected in the traps, 

Calcidiscus leptoporus, Helicosphaera 

carteri and Emiliania huxleyi. We aimed 

at testing whether high export fluxes are 

correlated with high Sr/Ca ratios, suggestive 

of higher nutrient-stimulated 

production, or Sr/Ca ratios are unchanged 

during high export periods, 

suggestive of increased export efficiency 

or scavenging. Periods of enhanced trap 

fluxes in March and June result from 

surface water blooms recognized in satellite 

imagery. An additional peak flux 

was found in January, but this peak 

represents re-suspended or recycled material 

in the water column. 

The amplitude of seasonal variations 

in the Sr/Ca ratios of the three investigated 

species is small in both traps. In 

the shallow trap, a decrease in the Sr/Ca 

ratio of C. leptoporus occurred synchronously 

with minimal fluxes. The other 

two species were not measured for this 

period. In the deep trap, no such decrease 

in Sr/Ca was observed during 

minimal fluxes, in either C. leptoporus 

or H. carteri, probably due to a long 

residence of coccoliths in the water column, 

recycling and low export efficiency. 

Absolute Sr/Ca ratios for all species 

are lower than in other more productive 

environments like the Bay of 

Bengal, Arabian Sea, or Sargasso Sea. 

We conclude that Sr/Ca ratios in coccoliths 

of surface sediments in the EMED 

reflect mainly spring–summer bloom 

conditions averaged over hundreds to 

thousands of years. 

In addition, the origin of varying calcite 

thickness in H. carteri was investigated. 

The similarity of average Sr/Ca 

ratios in differently-calcified specimens 

confirms that coccolith thickness variations 

in this species result from primary 

biomineralization processes and not 

from variable overgrowth by (low Sr) 

abiogenic calcite in the water column or 

the sediments. 

2010010103 

横贯阿尔泰山戈壁沙漠 ( 蒙古 ) 晚古 

新世轮藻 = Charophytes from the Upper 

Paleocene of the Trans-Altai Gobi 

Desert (Mongolia). ( 英文 ). Gereltsetseg 

L. Paleontological Journal, 2009, 43(6): 

699-701 1 图版 . 

Charophyte assemblage is described 

from the Naran Member of the Tsagaan 

sair section (Upper Paleocene). A new 

species, Mesochara cornuta, is described. 

2010010104 

西伯利亚二叠三叠纪暗色玄武岩地层 

中的细菌化石 = Fossil bacteria from 

the Permotriassic Trappean strata of Siberia. 

( 英文 ). Astafieva M M; Rozanov 

A Yu; Sadovnikov G N; Sapova E V. 


896-904 6 图版 . 

The strata of the Permotriassic Trappean 

Complex of Siberia (Ilimpeya 

River and Kapchan locality) are studied. 

The water-lava and water-tuff boundaries 

are shown to be promising for bacterial 

paleontological studies. The analysis 

of fossilized microbial communities 

shows that they vary depending on 

sedimentation conditions. This example 

is important for a better understanding 

of the prospects for the study of similar 

situations in the Archean and Proterozoic. 

2010010105 

卡累利阿太古代的细菌古生物学研究 

= Bacterial Paleontological study of Archaean 

of Karelia. ( 英文 ). Astafieva M 

M; Rozanov A Yu. Paleontological 

Journal, 2009, 43(8): 905-910 8 图版 . 

39

Newly found biomorphic microstructures 

from the Upper Archaean (Lopian) 

rocks from Northern Karelia are described. 

Various microorganisms of a 

bacterial nature and even cyanobacteria 

(and possibly eukaryotic forms) are recognized. 

The importance of electron microscopy, 

along with traditional methods, 

for the study of the earliest manifestations 

of life in the Archaean and Early 

Proterozoic is emphasized. 

2010010106 

嗜盐的藻细菌和蓝细菌群落及在碳酸 

盐沉积中所起的作用 = Halophilic algal-bacterial 

and cyanobacterial communities 

and their role in carbonate precipitation. 

( 英文 ). Gerasimenko L M; 

Mikhodyuk O S. Paleontological Journal, 

2009, 43(8): 940-957 14 图版 . 

This work studies the diversity of 

cyanobacterial and algal-bacterial communities 

of saline water bodies in the 

Crimean Peninsula and Altai Region. 

Plant-bacterial communities are described 

for the first time. The dependence 

of the production and destruction 

on the season and salinity of the water 

body is shown. The development of 

planktonic cyanobacteria is related to the 

presence of zooplankton, the development 

of which is controlled by hydrogen 

sulfide. The high hydrogen sulfide tolerance 

of benthic cyanobacteria secures 

the integrity of cyanobacterial communities. 

Observations in nature and laboratory 

modeling show that the formation 

of mineral layers is restricted to conditions 

of supersaturation with mineral 

components. Carbonate precipitation can 

take place in cyanobacterial communities 

under conditions of mixing sea water 

enriched with Ca and Mg with continental 

water enriched with sodium carbonate. 

Cyanobacteria are able to form 

and transform various Ca-Mgcarbonates. 

Dolomite formation is a derived 

process that occurs in cyanobacterial 

mats in the presence of sulfatereducing 

bacteria. Carbonatization of 

cyanobacterial cells is considered using 

the example of the unicellular halophilic-alkaliphilic 

cyanobacterium Euhalothece 

sp. The accomplished study is 

of certain interest for interpretation of 

geological and paleontological data in 

the context of the supposed analogy between 

cyanobacterial mats and ancient 

stromatolites. 

2010010107 

马斯特里赫特阶钙质超微化石 Micula 

murus 的纬度迁移 : 对全球气候变化 

的意义 = Latitudinal migration of calcareous 

nannofossil Micula murus in the 

Maastrichtian: Implications for global 

climate change. ( 英文 ). Thibault N; 

Gardin S; Galbrun B. Geology, 2010, 

38(3): 203-206 

Micula murus is one of the main calcareous 

nannofossil biostratigrapic 

markers of Tethyan and Intermediate 

provinces in the upper Maastrichtian 

(uppermost Cretaceous). A review of its 

first occurrence at 14 deep-sea sites and 

sections shows that it is time transgressive 

from the Tropical Realm of the Atlantic 

and Pacific Oceans to the intermediate 

latitudes of the North Atlantic, 

South Atlantic, Indian Ocean, and the 

northern Tethys. M. murus remained 

confined to the Tropical Realm for 1.2 

m.y. in the early–late Maastrichtian, thus 

supporting high-latitudinal thermal gradients. 

It subsequently spread out in the 

late Maastrichtian to temperate latitudes 

and to the Tethys in coincidence with 

the onset of a thermohaline circulation 

change ca. 67.5 Ma, suggesting a major 

change in surface-water circulation and 

interocean communications 

2010010108 

塔里木板块塔中上奥陶统良里塔格组 

的核形石 = Oncolites from the Lianglitag 

Formation ( Kaitian,Upper Ordovician),Tazhong,Tarim 

block,NW China. 

( 中文 ). 张园园 ; 杨海军 ; 王建坡 ; 黄智斌 ; 

40

李越 . 微体古生物学报 , 2009, 26(3): 

234-242 2 图版 . 

核形石包壳特征是分类的重要依据 , 

包壳形态在一定程度取决于其生长环 

境中的水流能量因素。塔中油田 3 口 

井上奥陶统凯迪阶良里塔格组礁滩相 

所显示的生态指标具有差异性 , 其中 

核形石形态学与其产出层位沉积时的 

能量条件具有很大程度的协同。全包 

裹型圆形或椭圆形核形石多见于颗粒 

灰岩和泥粒状灰岩 , 代表中 — 高能沉 

积环境 ; 正常核形石在高能环境出现频 

率较大 ; 薄皮型核形石多为中等能量的 

产物 ; 半包裹型核形石多见于灰泥基 

质的粒泥状灰岩 — 泥粒状灰岩 , 指示水 

流能量偏低的环境 , 复合型核形石具 

备半包裹型和全包裹型核形石特征 , 代 

表水动力条件相对较强、中高等能量 

相互交替的环境。 

2010010109 

横贯阿尔泰山戈壁沙漠 ( 蒙古 ) 古新 

世晚期轮藻门 = Charophytes from the 

Upper Paleocene of the Trans-Altai 

Gobi Desert (Mongolia). ( 英文 ). Gereltsetseg 

L. Paleontological Journal, 2008, 

42(6): 699-701 1 图版 . 

Charophyte assemblage is described 

from the Naran Member of the Tsagaan 

sair section (Upper Paleocene). A new 

species, Mesochara cornuta, is described. 

2010010110 

巴拿马东太平洋海岸作为碳酸盐生产 

者和生境提供者的珊瑚藻 : 初步估评 

= Coralline algae as carbonate producers 

and habitat providers on the Eastern Pacific 

coast of Panama: preliminary assessment. 

( 英文 ). Fortunato H; Schafer 

P. Neues Jahrbuch fur Geologie u. 

Palaontologie / Abhandlungen, 2009, 

253(1): 145-161 

Preliminary results show that maerl 

and rhodoliths are important components 

of the shelf contributing significantly 

to the total carbonate production, 

which is much higher in the Gulf of 

Chiriqui. Silty and sandy-mud bottoms 

predominate in the Gulf of Panama, 

while a mixture of maerl, ehodoliths and 

coral is commonly found in the Gulf of 

Chiriqui. Carallines support multilayered 

communities, with a low trophic 

diversity, few predators, abundant sessile 

forms, thick-shelled grzers and detritus 

feeders. Material is highly bioeroded 

and incrustated. soft sedimen 

communities are dominated by thinshelled, 

well preserved filter feeders and 

vagile predators. 

2010010111 

Kola 半岛元古代早期的绿藻纲 ( 绿 

藻 ) = Prasinophyceae (Green Algae) 

from the Lower Proterozoic of the Kola 

Peninsula. ( 英文 ). Rozanov A Yu; Astafieva 

M M. Paleontological Journal, 

2008, 42(4): 425-430 2 图版 . 

Eukaryotic organisms discovered 

from the earliest Lower Proterozoic 

phosphorites (2.04 Ga) of the Kola Peninsula 

are described. These are fossil 

forms Pechengia melezhiki gen. et sp. 

nov., which are tentatively assigned to 

green algae of the class Prasinophyceae. 

真菌 

2010010112 

法国中部上维宪阶 ( 密西西比系 ) 的 

微体真菌类 : 壶菌门和亲缘关系仍然 

不明的似壶菌状化石 = Microfungi 

from the upper Visean (Mississippian) 

of central France: Chytridiomycota and 

chytrid-like remains of uncertain affinity. 

( 英文 ). Krings M; Dotzler N; Galtier J; 

Taylor T N. Review of Palaeobotany 


328 4 图版 . 

A diverse assemblage of eucarpic and 

apparently holocarpic chytrids, and chytrid-like 

remains of uncertain affinity is 

preserved in late Visean (Mississippian; 

~ 330 Ma) cherts from Combres 

(Roanne area) and Esnost in central 

France. The evidence is primarily com- 

41

posed of various types of (resting) 

spores, as well as epibiotic and endobiotic 

(putative) zoosporangia that occur 

in/on solitary unicells, peronosporomycetous 

oogonia, (degrading) vascular 

plant tissues (i.e. xylem, periderm, cortical 

parenchyma), and various plant and 

fungal spores. Vegetative parts such as 

tenuous filaments or rhizomycelia in organic 

connection are rarely preserved. 

Host responses possibly linked to chytrid 

infection occur in the form of two 

different types of callosities, some with 

a distinct penetration canal, in lycophyte 

xylem and periderm, as well as in fungal 

spores. We suggest that the majority of 

chytrids and chytrid-like remains preserved 

in the Visean cherts belonged to a 

community of saprotrophic microorganisms 

that functioned in the decomposition 

of organic matter. Only a few forms 

appear to have been parasites. The 

Visean cherts from France provide a rare 

opportunity to examine the diversity of 

Chytridiomycota in a Carboniferous 

ecosystem. 

2010010113 

前寒武纪微体化石 Arctacellularia 和 

Glomovertella 特征 = On the nature of 

the Precambrian microfossils Arctacellularia 

and Glomovertella. ( 英文 ). 

Hermann T N; Podkovyrov V N. Paleontological 

Journal, 2008, 42(6): 655- 

664 3 图版 . 

Possible phylogenetic relationships 

between the organic-walled microfossils 

of the form genus Arctacellularia 

Hermann, 1976, representing chainlike 

aggregates of cells, and the filaments of 

the genus Glomovertella Reitlinger, 

1948, which comprises variously coiled 

filaments, are discussed. The possible 

relationship of these microfossils with 

different morphologies to lower ascomycetes 

is discussed. The chains of Arctacellularia 

are interpreted as exogenously 

produced spores, and the filaments 

that are associated with them are 

treated as vegetative hyphae that have a 

characteristic coiling during their transition 

phase, perhaps before the formation 

of sporophores. An emended diagnosis 

of the genus Arctacellularia and 

emended descriptions of the species A. 

ellipsoidea Hermann, 1976, A. kelleri 

Hermann et Jankauskas, 1989 are provided; 

and a new species, Glomovertella 

miroedikhia sp. nov., is described. 

蕨类植物 ( 广义 ) 

2010010114 

沃罗涅什地区 ( 西俄 ) 泥盆纪的新属 

种 Istchenkophyton filiciforme, 具厚 

角质层的小型维管植物 = Istchenkophyton 

filiciforme gen. et sp. nov., a 

new small vascular plant with thick cuticle 

from the Devonian of Voronezh Region 

(European Russia). ( 英文 ). 

Broushkin A V; Gordenko N V. Paleontological 

Journal, 2009, 43(10): 1202- 

1216 9 图版 . 

Remains of a new small vascular 

plant, Istchenkophyton filiciforme gen. et 

sp. nov., are described from the Upper 

Givetian strata of Pavlovsk vicinity (Voronezh 

Region). The plant is characterized 

by a very thick cuticle (up to 300 

μm), complex branching pattern, similar 

to that of a frond rachis, anomocytic 

stomata, and a well-developed vascular 

bundle with a central elongated in transversal 

section protoxylem strand and 

massive metaxylem composed chiefly of 

scalariform bordered-pitted tracheids. A 

reconstruction of the new plant is proposed; 

its ecology and systematic position 

are considered. In the light of new 

data relationships of problematic Devonian 

plants with thick cuticle are discussed. 

2010010115 

中泥盆世石松类植物 

Protolepidodendron scharianum 的研 

究历史及其正模标本的描述 = Middle 

Devonian lycophyte Protolepidodendron 

scharianum: History of study and description 

of the holotype. ( 英文 ). Jurina 

42

A L. Paleontological Journal, 2009, 

43(10): 1253-1261 3 图版 . 

The authorship of Protolepidodendron 

and its type species P. scharianum 

is discussed in accordance with the International 

Code of Botanical Nomenclature. 

The age and locality of the holotype 

are traced. For the first time, the 

morphology of the holotype and other 

specimens kept at the National Museum 

in Prague is described in detail as well 

as new materials collected in the Barrandien 

localities (Czech Republic). 

2010010116 

俄罗斯诺夫哥罗德区域早石炭世一种 

新的具有小孢子囊的器官 = A new 

microsporangiate organ from the Lower 

Carboniferous of the Novgorod Region, 

Russia. ( 英文 ). Orlova O A; Meyer- 

Melikian N R; Zavialova N E. Paleontological 

Journal, 2009, 43(10): 1316- 

1329 9 图版 . 

A new species of the genus Telangiopsis, 

T. nonnae O. Orlova et Zavialova, 

was described on the basis of a microsporangiate 

organ from the Lower 

Carboniferous deposits of the Novgorod 

Region. The morphology of branching 

fertile axes, synangia, and sporangia was 

thoroughly studied. The threedimensional 

system of fertile axes 

branches monopodially; ultimate axes 

bear numerous connivent bunches of synangia, 

which consist of three to six basally 

fused elongated ovate sporangia. 

The morphology and ultrastructure of 

prepollen grains were studied, which 

were extracted from the rock matrix surrounding 

the sporangia. The two-layered 

exine includes a well-developed 

endexine and an alveolate ectexine, with 

one-three rows of large thin-walled alveolae. 

The new species was compared 

with other Early Carboniferous microsporangiate 

organs. 

早期种子植物 

2010010117 

阿尔汉格尔斯克地区下石炭统 ( 皱羊 

齿类 ?) 木化石新发现 = A new fossil 

wood (Lyginopteridophyta?) from the 

Lower Carboniferous of the Arkhangelsk 

Region. ( 英文 ). Orlova O A. 


584-588 2 图版 . 

A new Early Carboniferous wood of 

pycnoxylic type is described from Lake 

Tovskoe locality in the Arkhangelsk Region. 

Tovoxylon alekseevii gen. et sp. 

nov. is characterized by short uniseriate 

rays and narrow tracheids with uniseriate 

pitting on their radial and tangential 

walls. The wood under description is 

compared with the most similar anatomically 

preserved woods from different 

Lower Carboniferous localities of 

the world. 

2010010118 

莫斯科台坳二叠纪三叠纪界线沉积中 

的一新属 Navipelt( 盾籽目 , 种子蕨 

类 ) = A new genus Navipelta (Peltaspermales, 

Pteridospermae) from the 

Permian/Triassic boundary deposits of 

the Moscow syneclise. ( 英文 ). Karasev 

E V. Paleontological Journal, 2009, 

43(10): 1262-1271 6 图版 . 

A new genus of peltaspermalean ovuliferous 

organs Navipelta gen. nov. is 

described from the terrestrial deposits of 

the Nedubrovo locality (village of 

Nedubrovo, Vologda Region, Russia), 

belonging to the base of Vetlugian 

Group (Upper Permian-Lower Triassic). 

Data on the anatomy of the peltate bilateral 

ovuliferous organs are obtained for 

the first time. Vascular strands in the 

peltoid depart from that of a stalk and 

branch up to three times distally. Transfusion 

tissue around the vascular strands 

is well developed. The new genus had a 

system of radially arranged resin canals, 

broaden into large secretory cavities. 

裸子植物 

2010010119 

43

堪察加半岛西北部白垩纪和古近纪的 

松科 Piceoxylon 属新种 = New species 

of Piceoxylon Gothan (Pinaceae) from 

the Cretaceous and Paleogene of the 

northwestern Kamchatka Peninsula. ( 英 

文 ). Blokhina N I; Afonin M A. Paleontological 

Journal, 2009, 43(10): 1190- 

1201 2 图版 . 

New fossil species of Piceoxylon 

(Pinaceae), P. talovskiense sp. nov. and 

P. kamtschatkiense sp. nov., are described 

on the basis of wood anatomy 

from the Cretaceous and Paleogene (respectively) 

of the Talovka River basin in 

the northwestern Kamchatka Peninsula. 

The Late Cretaceous P. talovskiense sp. 

nov. shows wood characters of modern 

Picea. The wood anatomy of the Paleogene 

Piceoxylon kamtschatkiense sp. 

nov. is somewhat similar to those of 

modern Picea sitchensis and P. jezoensis. 

Fossil woods of Piceoxylon have been 

found in the Kamchatka Peninsula for 

the first time. 

2010010120 

科达属和早期松柏类的花粉演化 = 

Pollen evolution in cordaites and early 

conifers. ( 英文 ). Gomankov A V. Paleontological 

Journal, 2009, 43(10): 

1217-1229 7 图版 . 

The plants that produced unique resinous 

coals (rhabdopissites) of the 

Lipovtsy coal field are revealed. They 

belong mainly to the group Miroviaceae 

(Oswaldheeria). Pseudotorellia (Ginkgoales) 

played an important role in the 

formation of humic coals of this Early 

Cretaceous coal field. The coal-forming 

plants comprise also cyatheaceous and 

gleicheniaceous ferns. A leafy shoot of 

Pseudotorellia has been found in this 

locality for the first time. It is assigned 

to the new species Pseudotorellia krassilovii 

Bugdaeva sp. nov. 

2010010121 

俄罗斯滨海边疆区 Alchan 洼地的白 

垩纪裸子植物的多样性 = Diversity of 

cretaceous gymnosperms in the Alchan 

Depression of Primorye. ( 英文 ). 

Volynets E B. Paleontological Journal, 

2009, 43(10): 1339-1350 4 图版 . 

The diversity of Cretaceous gymnosperms 

from the Alchan Depression in 

northwestern Primorye is discussed. The 

pike of gymnosperm diversity is restricted 

to the middle of the Late Albian, 

and a sharp decline took place in the 

terminal Albian. A new species, Dictyozamites 

serafimae sp. nov., is described. 

被子植物 

2010010122 

亚洲北部白垩纪和早古近纪的 

Liriodendrites 属 = Genus Liriodendrites 

in Cretaceous and early Paleogene 

floras of Northern Asia. ( 英文 ). Alekseev 

P I. Paleontological Journal, 2009, 

43(10): 1181-1189 7 图版 . 

Leaves of Liriodendrites Johnson 

were found in the Gyliakian (Santonian) 

and Boshnyakovo (Danian) floras of 

Sakhalin Island, Rarytkin, Koryak, and 

Kakanaut (Maastrichtian) floras of the 

Koryak Upland, and Antibes (Coniacian) 

flora of western Siberia. The study of 

new finds and revision of earlier collections 

resulted in the erection of a new 

species, L. occidentalis P. Alekseev, sp. 

nov., and creation of two new combinations, 

L. sachalinensis (Krysht.) P. 

Alekseev, comb. nov. and L. aeternus 

(Golovn.) P. Alekseev, comb. nov. The 

geographical and stratigraphic ranges of 

Liriodendrites in the Northern Hemisphere 

were reviewed. 

2010010123 

北亚晚白垩世植物群中悬铃木科 

Pseudoprotophyllum 属的形态、分类 

和分布 = The morphology, taxonomy, 

and occurrence of the genus Pseudoprotophyllum 

Hollick (Platanaceae) in Late 

Cretaceous floras of Northern Asia. ( 英 

文 ). Golovneva L B. Paleontological 

44

Journal, 2009, 43(10): 1230-1244 9 图 

版 . 

An extended generic diagnosis of 

Pseudoprotophyllum is given on the basis 

of new data from Late Cretaceous 

floras of Northern Asia. Both peltate and 

apeltate morphological types are included 

in the genus. The morphological 

diversity is described in the type species 

P. boreale (Dawson) Hollick from the 

Cenomanian-Turonian of North America 

and four North Asiatic species: P. minimum 

I. Lebed. , P. sibiricum I. Lebed., P. 

hatangaense Abramova, and P. giganteum 

Sveshn. et Budants. The geographical 

and stratigraphic analyses 

show that Pseudoprotophyllum evolved 

in Northern Asia since the Cenomanian 

until Campanian and was restricted to 

the Siberian-Canadian floristic region 

with a warm-temperate humid climate. 

2010010124 

哈萨克斯坦西部森诺曼阶 - 土仑阶的新 

属 Sarbaicarpa( 金缕梅目 ) = New 

genus Sarbaicarpa gen. nov. (Hamamelidales) 

from the Cenomanian- 

Turonian of Western Kazakhstan. ( 英文 ). 

Maslova N P. Paleontological Journal, 

2009, 43(10): 1281-1297 8 图版 . 

Anatomically preserved infructescences 

of Sarbaicarpa shilinii gen. et sp. 

nov. are described from the Cenomanian-Turonian 

of Kazakhstan and assigned 

to the Hamamelidales on the basis 

of their microstructure. The infructescence 

consists of about 30 free 

broadly cuneate fruits. The fruits are 

monocarpellate, without stylode, and 

basally with hairs. The seed is solitary 

and anatropic. Two types of sterile elements 

are present: (1) semispherical 

structures that are comparable in size to 

the fruits and densely covered with 

rounded trichomes and (2) narrow linear 

structures reaching more than a half of 

the fruit length. The new genus is characterized 

by a mosaic of platanaceous 

and hamamelidaceous characters. The 

plant remains are found associating with 

fossil leaves of the typically Platanus 

aspect. 

2010010125 

鄂霍次克海北海岸线土仑阶 - 科尼亚克 

阶 Pseudoprotophyllum 属 ( 悬铃木 

科 ) 叶的形态多样性 = Morphological 

diversity of leaves of Pseudoprotophyllum 

(Platanaceae) from the Turonian- 

Coniacian of the northern coast of the 

Sea of Okhotsk. ( 英文 ). Shczepetov S V; 

Golovneva L B. Paleontological Journal, 

2009, 43(10): 1330-1338 4 图版 . 

Fossil plants of the Chingandzha flora 

were studied from volcanogenic sediments 

of the Chingandzha and Rond 

formations on the northern coast of the 

Sea of Okhotsk. It was concluded that 

all platanaceous leaves earlier described 

in this flora as different taxa belong to 

one highly variable species, Pseudoprotophyllum 

cordatum Samyl. emend. 

Shczepetov et Golovneva. 

古无脊椎动物学 

原生动物 

2010010126 

贵州省紫云县宗地剖面早石炭世大塘 

期 — 早二叠世栖霞期的蜓类动物群 = 

Fusulinid faunas from the Datangian to 

Chihsian strata of the Zongdi section in 

Ziyun County,Guizhou Province. ( 中文 ). 

史宇坤 ; 刘家润 ; 杨湘宁 ; 朱李鸣 . 微体古 

生物学报 , 2009, 26(1): 1-30 4 图版 . 

贵州省紫云县宗地剖面产出早石炭 

世大塘期至早二叠世栖霞期连续的类 

化石序列。研究结果显示 : 该段地层中 

共产出类 36 属 453 种 ( 包括 14 个新 

种、14 个亚种、47 个相似种、18 个 

变种以及 30 个未定种 ) 。依据化石 

组合特征 , 可以识别出 13 个蜓类化石 

带 , 从老至新为 Eostaffella Eostaff ellina 

富集带 , Pseudostaffella 富集 

带 ,Profusulinella depati 延限带 , Profusulinella 

chaohuensis P. fenghuangshanensis 

间隔带 , Fusulina Fusulinella 

45

富集带 , Protriticites ziyunensis sp. nov. 

富集带 , Triticites hobblensis 延限带 , 

Triticites panteleevi 富集带 , 

Sphaeroschw agerina subrotunda 延限 

带 , Eoparafusulina ovata 富集带 , Stafella 

– Pseudoendothyra 组合带 , 

Misellina termieri 富集带 , Misellina 

pamirensis – Misellina ovalis 共存延限 

带。依据各带中的蜓类属种分布 , 宗地 

剖面的蜓类化石带序列可以很好地与 

中国华南、北美得克萨斯、日本中部 

和俄罗斯等地区同期的蜓类化石序列 

对比。 

2010010127 

滇东石林地区早 — 中二叠世 

Globivalvulina 有孔虫动物群 = Earlymiddle 

Permian globivalvulina ( Foraminifera) 

fauna from the stone forest 

area,eastern Yunnan Province. ( 中文 ). 

施贵军 ; 董丽萍 ; 刘庆国 ; 王超 . 微体古生 

物学报 , 2009, 26(2): 148-157 2 图版 . 

对云南石林地区早 — 中二叠世地 

层剖面中的 Globivalvulina( 球瓣虫属 ) 

化石系统研究结果表明 , 栖霞组含 16 

种 , 茅口组含有 13 种 , 两组中物种相似 

度可达 92 %。种级分异度变化显示 , 

栖霞组的种以增加趋势为主 , 茅口组则 

以减少为趋势。总体上这一时期 

Globivalvulina 动物群物种上升高峰仅 

有一次 , 出现在栖霞组中上部 ; 而下降 

高潮有两次 , 第一次出现于栖霞组上部 

与茅口组底部界线附近 , 第二次是茅口 

组顶部。后一次下降幅度远大于前者 , 

可能与中二叠世末期有孔虫动物群演 

化事件有关。 

2010010128 

东海陆架泥质沉积区全新世有孔虫和 

介形虫及其古环境应用 = Holocene 

benthic foraminifera and ostracoda from 

the shelf mud area of the East China Sea 

and their paleoenvironmental implications. 

( 中文 ). 赵泉鸿 ; 翦知湣 ; 张在秀 ; 

成鑫荣 ; 王可 ; 郑洪波 . 微体古生物学 

报 , 2009, 26(2): 117-128 1 图版 . 

浙江岸外东海内陆架 MD0623040 

柱状样完整保存有 10. 6 cal. kaPB 以 

来的全新世沉积记录 , 采取 257 个沉积 

物样品进行了有孔虫和介形虫定量分 

析。依据丰度上的优势成分和特征种 

的分布 , 识别出 6 个底栖有孔虫组合和 

4 个介形虫组合。应用属种组合和不 

同生态 ( 表生 / 内生、内陆架 / 中 — 内陆 

架、暖水 ) 种的丰度 , 探讨了研究区全 

新世以来的古环境变迁。分析结果揭 

示了研究区全新世早期海面快速上升 , 

沉积环境由滨岸内陆架 (10. 6 —9. 8cal. 

kaBP) 、内陆架外缘 (9. 8 —7. 8 cal. 

kaBP) 转变至中陆架内侧并达全新世 

最高海面 (7. 8 —3. 4 cal. kaBP) 。台湾 

暖流在 8. 0 cal. kaBP 起开始发育 , 并在 

5. 7 —2. 8 和 0. 7 —0 cal. kaBP 二个时 

期派生出明显的上升流。台湾暖流及 

其所派生的上升流是造成东海陆架泥 

质快速沉积的最主要原因。依据浮游 

有孔虫 Globi gerina bul loi des 的丰度 

变化 , 推测浙闽沿岸流在 4. 9 —3. 2 cal. 

kaBP 时期最为强盛 

2010010129 

有孔虫 Hantkenina 属演化中的缺失 

的环节和下 - 中始新统界线的问题 = 

The missing link in the evolutionary origin 

of the foraminiferal genus Hantkenina 

and the problem of the lower-middle 

Eocene boundary. ( 英文 ). Rögl F; Egger 

H. Geology, 2010, 38(1): 23-26 

The initial appearance of the planktonic 

foraminiferal genus Hantkenina 

has been used for about fifty years to 

recognize the base of the Lutetian and 

middle Eocene. However, probably as a 

result of incomplete stratigraphic records, 

discrepant ranges of Hantkenina 

have been reported by various investigators 

at many Eocene sections. Here we 

report the first complete evolutionary 

transition from Clavigerinella to Hantkenina, 

from the northwestern Tethyan 

46

deep-water section at Holzhäusl (Salzburg, 

Austria). A newly discovered species, 

Hantkenina nov. sp., is the link between 

Clavigerinella caucasica and 

Hantkenina mexicana. This finding unequivocally 

heralds the initial entry of 

Hantkenina, which is correlated to the 

upper part of calcareous nannoplankton 

Subzone NP15b (Sullivania gigas Subzone), 

to be defined. This indicates a 

mismatch of 4.5 m.y. between the base 

of the Lutetian at the type locality, which 

has been placed within Subzone NP14b, 

and the first appearance datum of Hantkenina. 

Consequently, the first occurrence 

of Hantkenina can no longer be 

used as a marker for the base of the middle 

Eocene. 

2010010130 

白垩纪放射虫 Afens Riedel et Sanfilippo 

属新种 = New cretaceous radiolarian 

species of the genus Afens Riedel 

et Sanfilippo. ( 英文 ). Bragina L G. Paleontological 

Journal, 2010, 44(1): 11- 

15 2 图版 . 

Diverse radiolarians from the Upper 

Cretaceous Perapedhi and Moni formations 

(southern Cyprus) are studied. 

Many representatives of the genus Afens 

Riedel et Sanfilippo, 1974 are recognized. 

The diagnosis of the genus Afens 

is emended and three new species of this 

genus, Afens perapediensis sp. nov., Afens 

moniensis sp. nov., and Afens concinnus 

sp. nov., are described. In addition, 

the species Afens liriodes Riedel et 

Sanfilippo, 1974 is redescribed. 

2010010131 

有孔虫 Fusulinoida Fursenko 超目的 

系统分类位置 = Taxonomic position of 

the superorder Fusulinoida Fursenko in 

the Foraminifera system. ( 英文 ). Mikhalevich 

V I. Paleontological Journal, 

2009, 43(2): 117-128 5 图版 . 

Comparative morphological analysis 

of the test and apertural structures in 

lower and higher members of the superorder 

Fusulinoida and class Miliolata 

has shown that they are similar in test, 

developmental trends from primitive 

forms with a tubular chamber to complex 

supermultichamber tests of the 

fusulinoid shape. As series of sections 

were compared, supplementary inner 

deposits at the bottom of chambers of 

endothyrids (tubercles, rostra, chomata) 

showed homology with the teeth of 

Miliolata. The high magnesium composition 

of the test wall and some ultrastructural 

features shared by the two 

groups support their affinity and suggest 

the assignment of the superorder Fusulinoida 

to the class Miliolata as an early 

phylogenetic lineage. 

2010010132 

乌拉尔山北部晚维宪期 endothyrid 类 

有孔虫新种 = New endothyrids (Foraminifera) 

from the Upper Visean of 

the northern Ural Mountains. ( 英文 ). 

Ponomarjova G Yu. Paleontological 

Journal, 2009, 43(2): 129-133 2 图版 . 

New endothyrids from the Upper 

Visean of the western slope of the northern 

Ural Mountains are described and 

assigned to the new species Eoendothyranopsis 

(Ninella) extremus and E. (N.) 

poststaffelliformis. 

2010010133 

罗斯托夫地区上白垩统有孔虫 

Pseudosiderolites Smout 的首次发现 

= The first find of Pseudosiderolites 

Smout (Foraminifera) in the Upper Cretaceous 

of the Rostov Region. ( 英文 ). 

Zakrevskaya E Yu. Paleontological 

Journal, 2009, 43(1): 19-33 6 图版 . 

A taxonomic description of larger foraminifers 

of the genus Pseudosiderolites, 

from Upper Cretaceous beds in the 

Rostov Region that were previously assigned 

to the Paleogene, is provided for 

the first time. The beds with these foraminifers 

are dated as Maastrichtian. 

Species criteria and the taxonomic posi- 

47

tion of the genus Pseudosiderolites are 

discussed. 

2010010134 

乌拉尔山南部泥盆纪放射虫新发现 : 

2. 中 - 晚泥盆世 = New radiolarians from 

the Devonian of the southern Ural 

Mountains: 2. Middle-Late Devonian. 

( 英文 ). Afanasieva M S; Amon E O. Paleontological 

Journal, 2009, 43(1): 34- 

49 6 图版 . 

Middle-Late Devonian Radiolarians 

are recorded for the first time in the 

southern Ural Mountains in Bashkortostan, 

in a section of Kariukmas Mountain 

(Upper Eifelian) and on the southern 

slope of Argagan Mountain (Middle 

Frasnian). The new Late Eifelian assemblage 

is composed of 17 species of 11 

genera, and Middle Frasnian radiolarians 

comprise 13 species of 7 genera of 

spherical, discoidal, pylomate, and spiny 

radiolarians. A new species, Primaritripus 

kariukmasensis, sp. nov., is described. 

The prevalence of discoidal 

forms in the oryctocenosis suggests shallow 

marine conditions in the Late 

Eifelian and Middle Frasnian basins. 

Two new biostratons, the Upper Eifelian 

beds with Primaritripus kariukmasensis 

and Middle Frasnian beds with Primaritripus 

chuvashovi, are established based 

on radiolarians. 

2010010135 

放射虫 Adamas Afanasieva, 2000 和 

Wonella Afanasieva, 2000 属新名 = 

New replacement names for the genera 

Adamas Afanasieva, 2000 and Wonella 

Afanasieva, 2000 (Radiolaria). ( 英文 ). 

Afanasieva M S. Paleontological Journal, 

2009, 43(1): 115 

2010010136 

乌拉尔山南部泥盆纪放射虫新发现 : 

1. 早 - 中泥盆世 ( 埃姆斯期晚期 — 艾菲 

尔期早期 ) = New radiolarians from 

the Devonian of the southern Ural 

Mountains: 1. Early-Middle Devonian 

(Late Emsian-Early Eifelian). ( 英文 ). 

Afanasieva M S; Amon E O. Paleontological 

Journal, 2008, 42(5): 451- 

467 5 图版 . 

Late Emsian-Early Eifelian radiolarians 

from the southern Ural Mountains 

are recorded and described for the first 

time. They come from the Kamennaya 

Gora section on the Tanalyk River near 

the town of Buribay, Bashkiria. The new 

Late Emsian-Early Eifelian radiolarian 

assemblage consists of 20 species of 11 

genera of spherical, discoidal, spindleshaped, 

pylomate, and spiny radiolarians. 

Four new species, i.e., Entactinia rostriformis 

sp. nov., Palaeodiscaleksus tumefactus 

sp. nov., Primaritripus buribayensis 

sp. nov., and P. chuvashovi sp. 

nov., are described. The diagnosis of the 

genus Primaritripus Afanasieva, 2000 is 

amended. The fact that the oryctocenosis 

is dominated by discoidal radiolarians 

suggests that, in the Late Emsian-Early 

Eifelian, the area under study was occupied 

by a relatively shallow marine basin. 

Based on radiolarians, a new Upper 

Emsian-Lower Eifelian biostraton, beds 

with Primaritripus buribayensis- 

Entactinia rostriformis, is established. 

The history of the study of Early Devonian 

radiolarians is considered. 

2010010137 

古生代放射虫 Entactinia Foreman, 

1963 和 Stigmosphaerostylus Rüst, 

1892 属的分类位置 = Taxonomic status 

of the genera Entactinia Foreman, 1963 

and Stigmosphaerostylus Rüst, 1892 

(Radiolaria of the Paleozoic). ( 英文 ). 


Journal, 2008, 42(4): 343- 

349 1 图版 . 

The genera Entactinia Foreman, 1963 

and Stigmosphaerostylus Rüst, 1892 are 

revised. The major differences between 

the two genera are manifested in the 

structure of the outer shell, internal spicule, 

and the number of the main spines; 

this suggests that they should be as- 

48

signed to different families (Entactiniidae 

and Haplentactiniidae) of different 

classes (Sphaerellaria and Spumellaria). 

2010010138 

放射虫 Palaeodiscus Afanasieva, 2000 

属和 Palaeodiscidae Afanasieva, 2000 

科新名 = New replacement names for 

the genus Palaeodiscus Afanasieva, 

2000 and the family Palaeodiscidae 

Afanasieva, 2000 (Radiolaria). ( 英文 ). 

Afanasieva M S. Paleontological Journal, 

2008, 42(4): 440 

2010010139 

新西伯利亚群岛 Kotel’ny 岛晚三叠世 

nodosariid 类有孔虫一新属 —— 

Dagysina = Dagysina —A new 

nodosariid genus (foraminifera) from the 

Upper Triassic of Kotel’ny Island, New 

Siberian Islands. ( 英文 ). Yadrenkin A V. 


221-226 4 图版 . 

A new nodosariid genus Dagysina 

gen. nov. with the type species Dagysina 

novosibirica sp. nov. is described from 

the Norian deposits of Kotel’ny Island, 

New Siberian Islands. A close phylogenetic 

relationship between Dagysina and 

the Early Liassic Frondiculinita is revealed 

based on morphological resemblance 

and an identical geographic range. 

2010010140 

塞浦路斯南部 Perapedhi 组土仑阶 - 桑 

托阶放射虫 Neosciadiocapsidae 科 = 

Radiolarians of the family Neosciadiocapsidae 

from the Turonian-Santonian 

of the Perapedhi Formation, southern 

Cyprus. ( 英文 ). Bragina L G. Paleontological 

Journal, 2008, 42(2): 127- 

138 4 图版 . 

Abundant radiolarians of the family 

Neosciadiocapsidae Pessagno (order 

Nassellaria) are examined, 11 new species, 

including Coniforma quasiantiochensis 

sp. nov., Lipmanium? ovalum sp. 

nov., Microsciadiocapsa devalvensa sp. 

nov., M. macropora sp. nov., M. mambrini 

sp. nov., M. mangaleniensis sp. 

nov., M. quasisutterensis sp. nov., M. 

tethyensis sp. nov., M.? elegantissima sp. 

nov., Neosciadiocapsa urquharti sp. 

nov., and Sciadiocapsa? rugosa sp. nov. 

are described. Diagnoses of two genera 

and one species, Coniforma Pessagno, 

1969, Microsciadiocapsa Pessagno, 

1969, and Sciadiocapsa? rumseyensis 

Pessagno, 1969 are emended. These 

species are members of the richest Late 

Cretaceous radiolarian assemblages 

from the metalbearing deposits of the 

Perapedhi Formation of southern Cyprus 

(Turonian-Santonian). 

2010010141 

塞浦路斯南部晚三叠世放射虫 = Late 

Triassic radiolarians of southern Cyprus. 

( 英文 ). N Yu Bragin. Paleontological 

Journal, 2007, 41(10): 951-1029 25 图 

版 . 

Radiolarians from the Upper Triassic 

of the allochthonous Mamonia Assemblage 

of southern Cyprus are considered. 

The Phasoula Formation, composed of 

basic volcanics, with lenses and interbeds 

of micritic limestones and cherts, 

contains (1) a Lower Norian assemblage 

with Capnodoce crystallina-Trialatus 

robustus, which also includes Capnodoce 

anapetes De Wever, Capnuchosphaera 

deweveri Kozur et Mostler, 

C. theloides De Wever, Deflandrecyrtium 

curvatum Kozur et Mostler, Icrioma 

cruciformis Tekin, Kahlerosphaera 

norica Kozur et Mock, Kinyrosphaera 

helicata Bragin, Mostlericyrtium 

sitepesiformis Tekin, Palaeosaturnalis 

latiannulatus Kozur et Mostler, 

Spongostylus tortilis Kozur et Mostler, 

Xiphotheca rugosa Bragin, and Zhamojdasphaera 

proceruspinosa Lahm; (2) a 

Middle Norian assemblage with Capnodoce 

sarisa accompanied by Loffa 

mulleri Pessagno, Nabolella trispinosa 

Bragin, and Praexehasaturnalis 

tenuispinosus (Donofrio et Mostler); and 

(3) an Upper Norian assemblage with 

Livarella densiporata-Lysemelas olbia 

49

accompanied by Pentactinocarpus sevaticus 

Kozur et Mostler, Praemesosaturnalis 

multidentatus (Kozur et Mostler), 

and others. This assemblage also occurs 

in clastic turbidites of the Vlambouros 

Formation. In the sections of southern 

Cyprus, radiolarian zones are recognized 

that correspond to the zones previously 

established in the Far East of Russia, 

which include Capnodoce crystallina 

(Lower and Middle Norian) and Lysemelas 

olbia (lower part of the Upper Norian). 

Radiolarians belonging to three 

orders, 24 families, 59 genera, and 101 

species are described; of them 2 genera, 

9 species, and 1 subspecies were previously 

described by the author; 14 new 

species and 1 new subspecies are established. 

The diagnoses of many genera 

and species are emended, the stratigraphic 

and geographical ranges of the 

majority of taxa are substantially expanded. 

2010010142 

白垩纪放射虫 Multastrum Vishnevskaya 

属新种及其古生物地理分布 

= New species of Cretaceous radiolarians 

of the genus Multastrum Vishnevskaya 

and their paleobiogeographical 

distribution. ( 英文 ). Bragina L G; Vishnevskaya 

V S. Paleontological Journal, 

2007, 41(6): 589-595 2 图版 . 

The study of the Upper Cretaceous 

beds of southern Cyprus (Tethyan Superrealm) 

revealed rich radiolarian assemblages, 

including six-eight-rayed 

stauraxonic morphotypes, which rarely 

occur in the Mesozoic. The diagnosis of 

the genus Multastrum Vishnevskaya, 

1991 is emended and four new species, 

Multastrum cypricum sp. nov., M. mangaleniense 

sp. nov., M. robustum sp. 

nov., and M. ? perapediense sp. nov., 

are described. The description of M. regale 

Vishnevskaya is emended. It is established 

that the genus Multastrum existed 

in the Coniacian-Campanian in 

both high and low latitude regions. 

2010010143 

伏尔加河地区上白垩统放射虫 

Pseudoaulophacidae Riedel 科新种 = 

New radiolarian species of the family 

Pseudoaulophacidae Riedel from the 

Upper Cretaceous of the Volga Region. 

( 英文 ). Vishnevskaya V S. Paleontological 

Journal, 2007, 41(5): 489- 

500 4 图版 . 

New radiolarians from the Upper Cretaceous 

(Coniacian-Santonian) siliceous 

beds outcropping northwest of Saratov, 

at the villages of Mezino-Lapshinovka 

and Vishnevoe are described. Three new 

species, Alievium olferievi sp. nov., A. 

rozanovi sp. nov., and Pseudoaulophacus 

alekseevi sp., are established. 

They are distinguished by the pseudoaulophacoid 

star-shaped structure of the 

shell wall. The terminology and taxonomic 

characteristics used in the description 

of new taxa are discussed. Radiolarian 

species are of great importance 

for stratification and correlation of Cretaceous 

deposits. 

2010010144 

北乌拉尔山脉东坡上白垩统 - 下古近系 

放射虫新种 = New radiolarian species 

from the Upper Cretaceous-Lower Paleogene 

of the eastern slope of the 

northern Ural Mountains. ( 英文 ). Sarkisova 

E V. Paleontological Journal, 

2007, 41(5): 501-505 1 图版 . 

Five new radiolarian species, Dictyophimus? 

orbiculiporosus sp. nov., Spongomelissa 

imperceptusa sp. nov., Theocoronium 

puncticulatum sp. nov., Pterocyrtidium 

porrectum sp. nov., and Tripodiscinus 

corona sp. nov., from the 

Campanian-Danian diatomites of the 

Leplinskaya Formation of the northern 

Ural Mountains are described. They are 

useful for stratification and correlation 

of the Upper Cretaceous and Lower Paleogene 

beds of the Ural Region of 

Western Siberia. 

50

2010010145 

西西伯利亚侏罗纪和石炭纪有孔虫 

Ammosiphonia He, 1977 属的代表分 

子 = Representatives of the genus 

Ammosiphonia He, 1977 (Foraminifera) 

from the Jurassic and Carboniferous of 

Western Siberia. ( 英文 ). Marinov V A. 


490-499 2 图版 . 

The wide distribution of the genus 

Ammosiphonia in the Upper Jurassic and 

Carboniferous of Western Siberia is established 

for the first time. Six haplophragmoidid 

species of Western Siberia 

are assigned to this genus. The diagnosis 

of the genus is emended; the taxonomic 

positions and scopes of the species 

Ammosiphonia nonioninoides (Reuss), A. 

beresoviensis (Bulatova), and A. sibirica 

(Zaspelova) are revised; two new species, 

A. suprajurassica sp. nov. and A. 

valanginica sp. nov., are described. 

2010010146 

显生宙放射虫演化中的生物危机和阶 

段 = Biotic crises and stages of radiolarian 

evolution in the Phanerozoic. ( 英文 ). 


Journal, 2006, 40(4): S453- 

S467 3 图版 . 

The questions of ecology and taphonomy 

of radiolarians are reviewed and 

reexamined. In Recent oceans and seas, 

the major part of the “radiolarian rain” 

(dead individuals) comes from the layer 

of the water column which is not deeper 

than 500 m; therefore, the bottom radiolarian 

thanatocenoses and taphocenoses 

are formed in all oceanic zones, including 

the coastal and central oligotrophic 

regions of oceans. However, radiolarians 

should not be regarded as indicators of 

exclusively deepwater oceanic conditions. 

The crucial moments in the evolution 

of radiolarians at the major Phanerozoic 

boundaries are recognized. A 

dynamic model of cyclic development of 

radiolarians in the Phanerozoic is proposed 

and four phases and nine stages in 

their evolution are recognized. The absence 

of an outburst of radiolarian biodiversity 

in the Holocene is shown. 

Many great extinctions of radiolarians 

occurred at the boundaries between seasons 

of galactic years. 

2010010147 

西特提斯晚白垩世 rotaliid 类有孔虫 

= Late Cretaceous rotaliids (Foraminiferida) 

from the Western Tethys. 

( 英文 ). Boix C; Villalonga R; Caus E; 

Hottiger L. Neues Jahrbuch fur Geologie 

u. Palaontologie / Abhandlungen, 

2009, 253(2-3): 197-227 

During the global community maturation 

cycle starting at the Cenomanian- 

Turonian boundary and ending with the 

events at the K-T boundary, the rotallid 

foraminifera produce for the first time in 

Earth History a considerable diversity of 

K-strategists that exhibit large shell sizes, 

complex umbilical structures and an 

imprtant dimorphism of generations. In 

the Late Cretaceous Pyrenean Gulf four 

groups are distinguished. 

2010010148 

放射虫 Heliodiscidae Haeckel 科新种 

= New species of the family Heliodiscidae 

Haeckel (radiolaria). ( 英文 ). Vishnevskaya 

V S. Paleontological Journal, 

2006, 40(2): 134-142 4 图版 . 

The family Heliodiscidae Haeckel, 

1881, which includes five genera, is reviewed. 

New methods of investigation 

are applied to the inner structure of Cretaceous 

spherical radiolarian skeletons, 

which reveal numerous taxa with an eccentric 

microsphere. Three new species, 

Astrophacus marinae sp. nov., Excentrosphaerella 

kovalenkovi sp. nov., and 

Excentrosphaerella kurilovi sp. nov., are 

described. The eccentric position of the 

microsphere suggests that these forms 

are nontypical Mesozoic radiolarians or 

new representatives of the family Heliodiscidae 

Haeckel, 1881, which was previously 

recorded in the Cenozoic. 

51

2010010149 

天山山脉中部早奥陶世钙质有孔虫新 

种 = New early Ordovician calcareous 

foraminifers of the middle Tien Shan. 

( 英文 ). Sabirov A A; Gushchin S B. Paleontological 

Journal, 2006, 40(1): 11- 

19 2 图版 . 

Twelve new species of calcareous foraminifers 

of the genera Parathurammina, 

Parathuramminites, Bisphaera, 

Archaesphaera, and Vicinesphaera from 

the Lower Ordovician of the Middle 

Tien Shan are described. 

古杯、多孔及腔肠动物 

2010010150 

Conulariina Miller and Gurley, 1896 

亚目 ( 刺胞动物门 , 钵水母纲 ; Vendian– 

三叠系 ) 的分支分析 = Cladistic analysis 

of the Suborder Conulariina Miller 

and Gurley, 1896 (Cnidaria, Scyphozoa; 

Vendian–Triassic). ( 英文 ). Leme J; 

Simões M G; Marques A C; Van Iten H. 

Palaeontology, 2008, 51(3): 649-662 

Results of a cladistic analysis of the 

suborder Conulariina Miller and Gurley, 

1896, a major extinct (Vendian–Triassic) 

group of scyphozoan cnidarians, are presented. 

The analysis sought to test 

whether the three conulariid subfamilies 

(Conulariinae Walcott, 1886, Paraconulariinae 

Sinclair, 1952 and Ctenoconulariinae 

Sinclair, 1952) recognized in the 

Treatise on Invertebrate Paleontology 

(TIP) are monophyletic. A total of 17 

morphological characters were scored 

for 16 ingroup taxa, namely the genera 

Archaeoconularia, Baccaconularia, Climacoconus, 

Conularia, Conulariella, 

Conularina, Ctenoconularia, Eoconularia, 

Glyptoconularia, Metaconularia, Notoconularia, 

Paraconularia, Pseudoconularia, 

Reticulaconularia, Teresconularia 

and Vendoconularia. The extant medusozoan 

taxa Cubozoa, Stauromedusae, 

Coronatae and Semaeostomeae served 

as outgroups. Unweighted analysisof the 

data matrix yielded 1057 trees, and successive 

weighting analysis resulted in 

one of the 1057 original trees. The ingroup 

is monophyletic with two autapomorphies: 

(1) the quadrate geometry 

of the oral region; and (2) the presence 

of a mineralized (phosphatic) periderm. 

Within the ingroup, the clade (Vendoconularia, 

Teresconularia, Conularina, 

Eoconularia) is supported by the sinusoidal 

longitudinal geometry of the 

transverse ridges, and the much larger 

clade (Baccaconularia, Glyptoconularia, 

Metaconularia, Pseudoconularia, Conularia, 

Ctenoconularia, Archaeoconularia, 

Notoconularia, Climacoconus, Paraconularia, 

Reticulaconularia) is supported 

by the presence of external tubercles, 

which, however, were lost in the 

clade (Notoconularia, Climacoconus, 

Paraconularia, Reticulaconularia). As 

proposed by Van Iten et al. (2000), the 

clade (Notoconularia, Climacoconus, 

Paraconularia, Reticulaconularia) is 

supported by the termination and alternation 

of the transverse ribs in the corner 

sulcus. The previously recognized subfamilies 

Conulariinae, Paraconulariinae 

and Ctenoconulariinae were not recovered 

from this analysis. The diagnostic 

features of Conulariinae (continuation of 

the transverse ornament across the corner 

sulcus and lack of carinae) and 

Ctenoconulariinae (presence of carinae) 

are symplesiomorphic or homoplastic, 

and Paraconulariinae is polyphyletic. 

The families Conulariellidae Kiderlen, 

1937 and Conulariopsidae Sugiyama, 

1942, also recognized in the TIP, are 

monogeneric, and since they provide no 

additional phylogenetic information, 

should be abandoned. 

2010010151 

蒙古奥陶纪 - 志留纪珊瑚分类学多样性 

演化 = Evolution of the taxonomic diversity 

of Mongolian Ordovician- 

Silurian corals. ( 英文 ). Ulitina L M; 

Bondarenko O B; Minjin Ch. Paleontological 

Journal, 2009, 43(5): 499- 

505 4 图版 . 

52

Changes in the taxonomic diversity of 

Mongolian Ordovician-Silurian corals 

(Tabulatoidea, Heliolitoidea, Cyrtophyllida, 

Rugosa) are analyzed. Evolution of 

the taxonomic diversity is analyzed in 

two aspects: quantitative and qualitative 

changes. Changes in the diversity of 

Mongolian corals are caused by (1) evolutional 

developmental stage of the 

group and its adaptational possibilities 

(internal reason) and (2) changes in the 

environmental parameters, which reproduce 

regional and general global events 

(external reason). 

2010010152 

西伯利亚和蒙古盆地的奥陶纪珊瑚 : 

分类学多样性 , 形态发生和出现 = 

Ordovician corals of the Siberian and 

Mongolian basins: Taxonomic diversity, 

morphogenesis, and occurrence. ( 英文 ). 

Bondarenko O B; Ulitina L M. Paleontological 

Journal, 2009, 43(11): 1439- 

1457 4 图版 . 

Taxonomic diversity, structural peculiarities, 

and occurrence of the Ordovician 

corals Tabulatoidea, Heliolitoidea, 

Rugosa, and Cyrtophyllida from the Siberian 

and Mongolian basins are analyzed. 

The corals settled in the Siberian 

basin almost for 1.5 million of years earlier 

than in the Mongolian basin. First 

corals in the Siberian basin were found 

in the lowermost Muktei Horizon (Llanvirn, 

i.e. Darriwilian Stage) while first 

corals in the Mongolian basin are known 

from the lower part of the Bairim Horizon 

(Late Caradoc, i.e. lower part of the 

Katian Stage). First corals in both basins 

belonged to the subclass Tabulatoidea. 

2010010153 

海绵 (Cliona orientalis Thiele , 

1900) 的生物侵蚀率 : 超短距离的空 

间变化 = Bioerosion rates of the sponge 

Cliona orientalis Thiele, 1900: spatial 

variation over short distances. ( 英文 ). 

Holmes G; Ortiz J; Schönberg C H L. 

Facies, 2009, 55(2): 203-211 

We studied bioerosion rates and tissue 

growth of the sponge Cliona orientalis 

Thiele, 1900. Experimental blocks 

grafted with sponge tissue were deployed 

at three sites in Moreton Bay, 

QLD, Australia, which have different 

environmental conditions. Bioerosion 

rates varied between 4, 5, and 10 kg m −2 

year −1 when related to final tissue area 

and between 4, 7, and 16 kg m −2 year −1 

when related to initial tissue area of the 

graft, which supports findings of earlier 

studies. Comparing results between the 

sites, eutrophication appeared to have 

the most stimulating effect and is most 

likely to have caused the measured differences. 

However, slight differences 

between shading and current speeds may 

also have played a role. Variation may 

have masked spatial differences of 

sponge growth, which were insignificant 

between study sites. Growth and bioerosion 

nevertheless followed the same 

trend and were weakly correlated. Habitat 

quality itself had no influence. Overall, 

the twofold difference in sponge 

bioerosion over a distance as short as 10 

km suggests that when estimating bioerosion 

rates, subsamples should be 

tested at different locations. 

2010010154 

从底栖生物化石再释贵州独山泥盆系 

龙洞水段的时代 = Age Re-assessment 

Of The Longdongshui Member (Middle 

Devonian) In Southern Guizhou On The 

Basis Benthic Fossils. ( 中文 ). 廖卫华 ; 

邓占球 . 古生物学报 , 2009, 48(4): 637- 

645 

贵州独山的猴儿山组龙洞水段是一 

套浅海相碳酸盐沉积 , 盛产底栖生物化 

石。通过对该段地层中所含四射珊 

瑚、床板珊瑚和腕足类等化石属种的 

详尽分析 , 再次证实龙洞水段的地质时 

代仍应属中泥盆世早期 (Eife-lian)。而 

不是像某些根据痕迹化石或层序地层 

学的研究那样将它置于下泥盆统。 

53

2010010155 

贵州剑河寒武纪凯里生物群中拟轮盘 

水母钵 (Pararotadiscus) 和腕足类共存 

现象的初步研究 = A Preliminary Study 

Of The Medusiform Fossils (Pararotadiscus) 

Associations With Brachiopods 

From The Cambrian Kaili Biota,Jianhe,Guizhou. 

( 中文 ). 程心 ; 傅晓 

平 ; 赵元龙 . 古生物学报 , 2009, 48(4): 

672-680 

贵州剑河革东寒武纪凯里生物群中 

水母状化石属种单调 , 仅发现 1 属 1 种 

贵州拟轮盘水母钵 Pararotadiscus 

guizhouensis(Zhao et Zhu,1994), 但却 

有丰富的生态现象。近 40% 的标本与 

腕足类、三叶虫、金臂虫、棘皮动物 

或遗迹化石 Gardia 共存 , 是目前全球水 

母状化石中罕见的丰富生态现象。其 

中 65 件贵州拟轮盘水母钵盘体上、 

下或周围出现了背、腹壳分散保存的 

腕足类 , 说明腕足类与贵州拟轮盘水母 

钵共同埋藏 ;1 块标本的丛状触手中还 

包裹有腕足类 , 说明丛状触手不是类似 

于植物根系的固着器。这种现象还证 

实贵州拟轮盘水母钵不是固着而是浮 

游生活的 , 其与腕足类壳瓣共存 , 主要 

是浮游的贵州拟轮盘水母钵死亡后沉 

落海底与腕足类壳瓣重叠的结果。 

2010010156 

库兹涅茨克盆地下法门阶层孔虫目的 

发现 = Discovery of Lower Famennian 

Stromatoporoidea in the Kuznetsk Basin. 

( 英文 ). Khromykh V G. Paleontological 

Journal, 2008, 42(3): 227-231 2 图版 . 

Stromatoporoidea recorded for the 

first time from the Lower Famennian of 

the Kuznetsk Basin are described. The 

assemblage studied includes three new 

species, Actinostroma quasifenestratum 

sp. nov., Kyklopora tomiensis sp. nov., 

and Coenostroma rarum sp. nov., and 

three previously known species of different 

genera. 

2010010157 

乌拉尔近极地区晚奥陶世和志留纪的 

层孔虫目新种 = New species of stromatoporoidea 

from the Upper Ordovician 

and Silurian of the Subpolar Urals. 

( 英文 ). Antropova E V. Paleontological 

Journal, 2007, 41(6): 596-599 1 图版 . 

Stromatoporoidea are widespread in 

the Upper Ordovician and Silurian beds 

of the Kozhim River (western slope of 

the Subpolar Urals). Five new species 

Cystostroma prodigiosum sp. nov., Stylostroma 

flabellatum sp. nov., Labechiina 

arguta sp. nov., Ecclimadictyon 

faveolatum sp. nov., and Araneosustroma 

astroplexum sp. nov. are described. 

2010010158 

乌拉尔山脉近极地地区艾菲尔期沉积 

中 syringoporids 的新种 = New species 

of syringoporids from Eifelian deposits 

of the Subpolar Ural Mountains. 

( 英文 ). Lukin V Yu. Paleontological 

Journal, 2006, 40(4): 369-374 3 图版 . 

A high diversity of tabulate corals in 

Eifelian deposits of the Syv“yu River 

basin (Subpolar Urals) is reported for 

the first time. Most of the corals are represented 

by colonies of syringoporids. 

Five new species Syringopora parva sp. 

nov., S. insueta sp. nov., S. indecora sp. 

nov., Tetraporinus syvjuensis sp. nov., 

and Armalites serotinus sp. nov. are described. 

2010010159 

陕南早寒武世早期 Quadrapyrgites 再 

研究 = New Data On Quadrapyrgites 

From The Earliest Cambrian Of South 

Shaanxi. ( 中文 ). 刘云焕 ; 李勇 ; 弓虎军 ; 

张志刚 ; 马秋红 ; 吕晓强 ; 陈金 ; 闫亭廷 . 

古生物学报 , 2009, 48(4): 688-694 

处于 " 寒武纪生命大爆发 " 序幕阶段 

的梅树村期 , 生物类群大规模辐射、身 

体构型快速革新 , 与前寒武纪生物群面 

貌明显不同。最近在陕南宁强宽川铺 

地区梅树村期地层中发现了大量五辐 

射 Punctatus 及部分四辐射四方塔形 

54

壳属 Quadrapyrgites, 其中包括 1 个新 

种 Quadrapyrgites undulatuscostalis 

sp.nov. 。在此基础上对 

Quadrapyrgites 进行了属征补充。双 

胚层腔肠动物的出现标志着地球生命 

史的真后生动物演化开端 , 在生物起源 

演化历程上占据着关键的位置。本文 

为研究真后生动物起源演化、生物辐 

射、体型构建提供了重要实证。 

苔藓动物 

2010010160 

苔藓虫 Minussina Morozova, 1961 属 

的生物地理分布和演化 = Biogeography 

and evolution of bryozoans of the 

genus Minussina Morozova, 1961. ( 英 

文 ). Tolokonnikova Z A. Paleontological 

Journal, 2009, 43(4): 391-400 11 图 

版 . 

The spatial variations of bryozoans of 

the Devonian genus Minussina throughout 

its existence are discussed. The areal 

distribution of Minussina is shown to be 

restricted mainly to the Altai-Sayan region. 

The variability of seven morphological 

characters of Minussina species 

is analyzed. The variations in the number 

of acanthozooecia and in the thickness 

of walls are attributed to evolutionary 

change; variations in the measurements 

of apertures and heterozooecia are 

explained by geographical variation. The 

narrow stratigraphic range of Minussina 

species makes it possible to use them for 

correlation of Devonian deposits. 

2010010161 

蒙古中部 Tsagaan-Del 剖面晚奥陶世 

苔藓虫新种 = New Late Ordovician 

bryozoans from the Tsagaan-Del section 

of central Mongolia. ( 英文 ). Ariunchimeg 

Y. Paleontological Journal, 

2009, 43(4): 401-407 3 图版 . 

The Upper Ordovician rocks of Mongolia 

have yielded bryozoans of the order Rhabdomesida 

for the first time. These belong to two 

new species of the genera Ulrichostylus 

Bassler, 1952 and Nematopora Ulrich, 1888. 

The same rocks have yielded a new species of 

the genus Chasmatopora Eichwald, 1855 of 

the order Phylloporinida. The distribution of 

these genera is discussed and the descriptions 

of U. aculeatus sp. nov., N. galinae sp. nov. 

and Ch. spatiosa sp. nov. are presented. 

2010010162 

俄罗斯萨拉托夫州和莫斯科州侏罗纪 

窄唇苔虫新种 = New species of stenolaemate 

bryozoans from the Jurassic of 

the Moscow and Saratov Regions (Russia). 

( 英文 ). Viskova L A. Paleontological 

Journal, 2009, 43(4): 408-417 5 图 

版 . 

Three new species of the Middle Jurassic 

stenolaemate bryozoans of the 

genera Reptomultisparsa d’Orbigny and 

Microeciella Taylor et Sequeiros are described: 

R. saratovensis sp. nov. and M. 

seltseri sp. nov. from the Lower Bathonian 

and the Upper Callovian of the 

Saratov Region, respectively, and R. 

stupachenkoi sp. nov. from the Middle 

Callovian of the Moscow Region. Some 

specific features of their astogeny and 

colonial morphology are discussed. 

2010010163 

中石炭世苔藓虫 Rhombopora aleksandrae 

(Schulga-Nesterenko) 的群体 

发育和分类位置 = Astogeny and taxonomic 

position of the Middle Carboniferous 

bryozoans Rhombopora aleksandrae 

(Schulga-Nesterenko). ( 英文 ). Gorjunova 

R V. Paleontological Journal, 

2009, 43(5): 537-542 3 图版 . 

Based on the study of the astogeny of Nikiforovella 

aleksandrae Schulga-Nesterenko, 

1955, the internal morphology of this species 

is shown to be inconsistent with the diagnosis 

of the genus Nikiforovella. The placement of 

this species into the genus Rhombopora Meek, 

1872 is substantiated and the description of Rh. 

aleksandrae (Schulga-Nesterenko, 1955) is 

revised using modern terms. 

2010010164 

55

蒙古晚奥陶世苔藓虫地层和古地理分 

布 = Stratigraphic and paleogeographic 

distribution of the Upper Ordovician 

bryozoans of Mongolia. ( 英文 ). Ariunchimeg 

Ya. Paleontological Journal, 

2009, 43(11): 1432-1438 1 图版 . 

The taxonomic diversity and distribution 

of the Upper Ordovician bryozoans 

of Mongolia are analyzed. Five heterochronous 

assemblages of bryozoans are 

established: Chigertei and Tsagaan del 

in the Sandbian Stage and Bairim Ovoo, 

Uuregnur, and Sairin in the Katian Stage. 

The bryozoans are shown to be important 

for solving complex problems of 

stratigraphy of the Ordovician of Mongolia 

and for paleogeographic reconstructions. 

2010010165 

俄罗斯 Gorny Altai 地区泥盆纪苔藓 

虫新种 = New bryozoans from the Devonian 

of Gorny Altai (Russia). ( 英文 ). 

Tolokonnikova Z A. Paleontological 

Journal, 2010, 44(2): 151-156 3 图版 . 

New bryozoans Saffordotaxis altaicus 

sp. nov. from the Givetian Stage (Middle 

Devonian) and Cyphotrypa olgae sp. 

nov. and Crustopora aliena sp. nov. 

from the Famennian Stage (Upper Devonian) 

are described from the Devonian 

of Gorny Altai. 

2010010166 

列宁格勒州下奥陶统苔藓虫 

Esthoniopora lessnikowae 种的新记录 

及其群体变异 = New records of bryozoans 

from the Lower Ordovician of the 

Leningrad Region and intercolonial 

variability in Esthoniopora lessnikowae 

(Modzalevskaya). ( 英文 ). Koromyslova 

A V; Fedorov P V; Ershova V B. Paleontological 

Journal, 2009, 43(2): 153- 

161 6 图版 . 

The structure of vesicular tissue in 

bryozoans Esthoniopora lessnikowae 

(Modzalevskaya, 1953) from the Latorp 

Horizon (Lower Ordovician) of the Leningrad 

Region is studied for the first 

time. The intercolonial variability of this 

species, which is expressed in the variations 

in the thickness of the walls of 

autozooecia, shape of apertures, and the 

structure of vesicular tissue, is thoroughly 

studied. New data are used to 

supplement the description of the species 

E. lessnikowae (Modzalevskaya, 

1953) and the diagnosis of the genus 

Esthoniopora Bassler, 1911. 

2010010167 

俄罗斯布良斯克州中侏罗世苔藓虫新 

种群内变异 = Intracolonial variability 

in new bryozoans from the Middle Jurassic 

of the Bryansk Region (Russia). 


Journal, 2009, 43(2): 162-169 4 图版 . 

Two new species of encrusting bryozoans 

(Stenolaemata, Tubuliporida) 

from the Middle Callovian (Middle Jurassic) 

deposits of the Bryansk Region, 

Oncousoecia guzhovi sp. nov. and Microeciella 

fokinensis sp. nov., are described. 

Their intracolonial variability, 

which is due to differences in astogenetic 

stages and to external factors, is 

discussed. 

2010010168 

东欧地台上石炭统苔藓虫新科 

Medvedkellidae 的形态发生、起源和 

古生态 = Morphogenesis, origin, and 

paleoecology of the bryozoans of the 

family Medvedkellidae fam. nov. (Upper 

Carboniferous, East European Platform). 

( 英文 ). Gorjunova R V. Paleontological 

Journal, 2009, 43(1): 69-77 4 

图版 . 

A new family of the order Rhabdomesida, 

Medvedkellidae fam. nov., is described. 

This family consists of a new 

genus, Medvedkella gen. nov., comprising 

three species transferred from the 

genus Rhombopora Meek, 1872: the 

type species M. riasanensis (Schulga- 

Nesterenko, 1955), M. diaphragmata 

(Schulga-Nesterenko, 1955), and M. 

56

mariae (Dunaeva, 1961). The morphogenesis 

of the first two species is studied. 

For the first time axial zooecia are revealed 

in the suborder Golgdfussitrypina, 

which existed in parallel with the suborder 

Rhabdomesina of the order Rhabdomesida. 

A hypothesis that the new 

family evolved from the subfamily 

Nicklesoporinae Gorjunova, 1985 of the 

family Goldfussitrypidae, 1985 is proposed. 

Some questions of the ecological 

adaptation of these bryozoans in the 

Late Carboniferous marine basin of the 

East European Platform are discussed. 

2010010169 

阿仑尼克阶苔藓虫一新属 Lynnopora 

及其在 Revalotrypidae Gorjunova, 

1988 科中的系统分类位置 = A new 

genus of the Arenigian bryozoans, Lynnopora 

, and its systematic position in 

the family Revalotrypidae Gorjunova, 

1988. ( 英文 ). Gorjunova R V; Koromyslova 

A V. Paleontological Journal, 2008, 

42(5): 491-499 3 图版 . 

A new genus Lynnopora gen. nov. 

with the type species L. lunata sp. nov. 

and a new species Revalotrypa krestensis 

Koromyslova sp. nov. from the 

Arenigian Stage (Latorp and Volkhov 

horizons) of the Ordovician of the Leningrad 

Region are described. The positions 

of the genus Revalotrypa Bassler, 

1952 and the family Revalotrypidae 

Gorjunova, 1988 in the order 

Cystoporida are substantiated. The problems 

of biogeography and ecological 

adaptations of bryozoans of the family 

Revalotrypidae are discussed. 

2010010170 

上喀山亚阶层型剖面苔藓虫新种 = 

New bryozoan species from the stratotype 

section of the Upper Kazanian Sub. 

( 英文 ). Gorjunova R V; Sedaeva K M. 


350-362 6 图版 . 

Representatives of nine bryozoan 

genera of four orders are identified for 

the first time from the carbonate deposits 

of the stratotype section of the Upper 

Kazanian Substage of the Middle Permian. 

Among them four new species are 

established and described: Permopora 

volgensis sp. nov., Stellahexaformis burovi 

sp. nov., Alternifenestella esaulovae 

sp. nov., and Wjatkella definita sp. nov. 

A brief lithological characterization is 

provided of the carbonate deposits that 

contain the remains of these bryozoans 

and were formed under the conditions of 

transgression-regression cycles of the 

Late Kazanian marine basin. Some questions 

concerning the taphonomy, ecology, 

and morphology of the bryozoans 

studied are considered. 

2010010171 

俄罗斯欧洲部分中部 ( 莫斯科市、莫 

斯科州及科斯特罗马州 ) 侏罗纪窄唇 

纲苔藓虫新属种 = New Stenolaematous 

bryozoans from the Jurassic of central 

European Russia (Moscow city and 

the Moscow and Kostroma Regions). 


Journal, 2008, 42(2): 149-158 4 图版 . 

New bryozoans from the Middle 

Callovian (Middle Jurassic) of Moscow 

city (Reptomulticava pileola sp. nov.) 

and the Moscow Region (Spirodella radiolobata 

gen. et sp. nov.) and from the 

Middle Oxfordian (Upper Jurassic) of 

the Kostroma Region (Hyporosopora 

mittai sp. nov.) are described. All three 

bryozoans belong to the class Stenolaemata. 

Some features of their colonial 

organization and environmental conditions 

are discussed. 

2010010172 

外高加索上泥盆统新 cryptostomide 

类苔藓虫及 Cryptostomida 目演化的 

若干方面 = New cryptostomide bryozoans 

from the Upper Devonian of 

Transcaucasia and some aspects of the 

evolution of the order Cryptostomida. 

( 英文 ). Gorjunova R V. Paleontological 

Journal, 2007, 41(6): 600-613 6 图版 . 

57

New bryozoans of the suborder Ptilodictyina 

of the order Cryptostomida 

are described from the Upper Famennian 

of Transcaucasia: those of the family 

Worthenoporidae, i.e., a genus 

Geranopora gen. nov. comprising three 

species G. fabulosa sp. nov. (type species), 

G. fida sp. nov., and G. finitima sp. 

nov., and those of a new family Mysticellidae 

fam. nov., i.e., a genus Mysticella 

gen. nov. comprising four species 

M. labyrinthica sp. nov. (type species), 

M. laudativa sp. nov., M. sacrosancta sp. 

nov., and M. ortiva sp. nov. Thus, a Late 

Devonian part of the evolutionary line of 

ptilodictyines is revealed that shows 

their radiation at the levels of families, 

genera, and species. 

2010010173 

库兹涅茨克盆地上泥盆统 ( 下法门 

阶 ) 苔藓虫新种 = New bryozoans 

(Bryozoa) from the Upper Devonian 

(Lower Famennian) of the Kuznetsk Basin. 

( 英文 ). Tolokonnikova Z A. Paleontological 

Journal, 2007, 41(5): 537- 

541 4 图版 . 

New bryozoans from the Upper Devonian 

(Famennian) of the borderlands 

of the Kuznetsk Coal Basin are described: 

Orthopora tomensis sp. nov. 

and Minussina incrustata sp. nov. 

2010010174 

苔藓虫 (Trepostomida 目 )Orbipora 

Eichwald, 1856 属的形态发生、系统 

发育关系和分布 = Morphogenesis, 

phylogenetic relationships, and distribution 

of the bryozoans of the genus Orbipora 

Eichwald, 1856 (order Trepostomida). 

( 英文 ). Koromyslova A V. 


132-145 7 图版 . 

Five species of the genus Orbipora, 

including two new species, O. lynnensis 

sp. nov. and O. ukhakuensis sp. nov., are 

described from the Middle Ordovician 

of the Leningrad Region and Estonia. 

The colonies of the species O. acanthophora 

Bassler, 1911 and O. solida 

Bassler, 1911 are measured and figured 

for the first time. The stratigraphic range 

and geographic distribution of O. acanthophora 

are refined. A scheme of possible 

phylogenetic relationships and distribution 

maps of the species of the genus 

are presented. 

2010010175 

外高加索泥盆系 - 石炭系界线层苔藓虫 

新种 = New bryozoans from the Devonian-Carboniferous 

boundary beds of 

Transcaucasia. ( 英文 ). Gorjunova R V; 

Lavrentjeva V D. Paleontological Journal, 

2007, 41(2): 146-155 6 图版 . 

New species of Transcaucasian bryozoans 

are described: Primorela remota 

and Pseudoascopora subtilis (order 

Rhabdomesida) from the Upper Famennian 

and Anisotrypa hamata (order Trepostomida), 

Paranicklesopora stupenda, 

Euthyrhombopora barbara, Primorella 

testata, Ipmorella clara (order Rhabdomesida), 

and Taeniodictya vermiculata 

(order Cryptostomida) from the Tournaisian. 

2010010176 

莫斯科市和莫斯科州中侏罗世苔藓虫 

新种 ( 窄唇纲 ) = New bryozoans 

(Stenolaemata) from the Middle Jurassic 

of Moscow City and the Moscow Region. 


Journal, 2007, 41(1): 49-60 6 

图版 . 

Five new species of stenolaematous 

bryozoans are described from the Middle 

Callovian of Moscow City (Krasnopresnenskii 

Region) and the Moscow 

Region (Gzhel’ Railroad Station and the 

quarry between the small towns of Rechitsy 

and Troshkovo): Entalophora 

alexeevi sp. nov., Cellulipora retshitsiensis 

sp. nov., Diplosolen pravus sp. 

nov., Siphodictyum primarium sp. nov., 

and Ceata kamushkiensis sp. nov. The 

last four species belong to the genera 

that have never been recorded from de- 

58

posits older than the Lower Cretaceous. 

The presence of different types of heterozooecia 

in these bryozoans shows 

that the functional polymorphism of zooids 

developed considerably in the class 

Stenolaemata as early as the Middle Jurassic. 

2010010177 

阿富汗泥盆纪和伊朗石炭纪苔藓虫新 

类别 = New bryozoans from the Devonian 

of Afghanistan and the Carboniferous 

of Iran. ( 英文 ). Gorjunova R V. Paleontological 

Journal, 2006, 40(6): 626- 

635 5 图版 . 

A new family, Vidronovellidae, with 

a new genus, Vidronovella, and its type 

species V. fastigata sp. nov., and a new 

species, Europora gerirudensis, are described 

from the Famennian of Afghanistan, 

and the new species Primorella 

iranica, Heloclema magnificum, and 

Worthenopora elbursensis are described 

from the Viséan of Iran. 

2010010178 

波兰中部圣十字山泥盆纪和石炭纪苔 

藓虫新属种 = New Devonian and Carboniferous 

bryozoans of the Holy Cross 

Mountains (central Poland). ( 英文 ). 

Morozova I P; Weis O B; Racki G. Paleontological 

Journal, 2006, 40(5): 529- 

540 5 图版 . 

New bryozoans from the Middle- 

Upper Devonian (Eifelian-Frasnian) and 

the Lower Carboniferous (Tournaisian) 

of the Holy Cross Mountains in central 

Poland are described: Bigeyella sparsa 

gen. et sp. nov., B. separata gen. et sp. 

nov., Eridopora singula sp. nov., Leptotrypa 

pulchra sp. nov., Kysylschinipora 

klarae sp. nov., Coelotubulipora 

rara sp. nov., Alternifenestella genuina 

sp. nov., Exfenestella polonica sp. nov., 

and Rectifenestella localis sp. nov. Some 

paleogeographic and stratigraphic aspects 

of the Paleozoic deposits of this 

region are discussed and main bryozoan 

localities are described. 

2010010179 

莫斯科市和莫斯科州中侏罗世苔藓虫 

Stomatopora Bronn 属和 

Stoporatoma 新属 ( 窄唇纲 ) = Bryozoans 

of the genera Stomatopora Bronn 

and Stoporatoma gen. nov. (Stenolaemata) 

from the Middle Jurassic of Moscow 

City and the Moscow Region. ( 英 

文 ). Viskova L A. Paleontological 

Journal, 2006, 40(4): 425-430 2 图版 . 

Encrusting uniserial bryozoans are 

recorded from the Middle Callovian of 

Moscow city and the Moscow Region: 

Stoporatoma gerasimovi gen. et sp. nov. 

and three species of the genera 

Stomatopora Bronn; i.e., S. dichotoma 

(Lamouroux), S. waltoni Haime, and S. 

bajocensis (Orbigny). Some morphological 

characters and environmental 

conditions of these bryozoans are discussed. 

A new bryozoan that is characterized 

by a large size and distinctive 

circular reptozooecia is described. 

腕足动物 

2010010180 

托莫特壳类和腕足类的同源骨骼分泌 

物 = Homologous skeletal secretion in 

tommotiids and brachiopods. ( 英文 ). 

Balthasar U; Skovsted C B; Holmer L E; 

Brock G A. Geology, 2009, 37(12): 

1143-1146 

Tommotiids are distinctive components 

of the early Cambrian small shelly 

fauna, almost invariably represented by 

isolated phosphatic sclerites derived 

from a multielement protective cover 

(scleritome). The unusual range of tommotiid 

sclerite morphologies and unknown 

construction of the scleritome 

have severely hampered our understanding 

of their phylogenetic affinities. 

However, recent description of rare, articulated 

scleritome material belonging 

to the tommotiid genera Eccentrotheca 

and Paterimitra support the hypothesis 

that some tommotiids fall within the 

stem group of the lophophorate phyla 

59

Phoronida and Brachiopoda and that at 

least some tommotiid sclerites are homologous 

precursors of the shells of organophosphatic 

brachiopods. Here we 

show that the shell microstructure of Eccentrotheca 

and Paterimitra share substantial 

similarities with paterinid 

brachiopods. While paterinids possess an 

overall brachiopod morphology, their 

microstructure appears more similar to 

Eccentrotheca and Paterimitra than to 

nonpaterinate lingulids. These findings 

strongly support the existence of a 

brachiopod total group that is solidly 

rooted within tommotiids, and identify 

the organophosphatic skeletal composition 

as plesiomorphic with calcareous 

shells as derived. The microstructural 

changes of the proposed tommotiidbrachiopod 

transition probably reflect an 

adaptation to fluctuating food and phosphorous 

intake that came with the switch 

to a sessile life style at the base of the 

tommotiid clade. 

2010010181 

莫斯科州格舍尔阶地层中腕足类线纹 

长身贝科从中到晚石炭世的演化规律 

= Gzhelian brachiopods of the family 

Linoproductidae Stehli and regularities 

in their evolution in the Middle and Late 

Carboniferous of the Moscow Region. 

( 英文 ). Lazarev S S. Paleontological 

Journal, 2009, 43(4): 381-390 3 图版 . 

This paper completes the revision of 

the Middle and Late Carboniferous 

brachiopods of the family Linoproductidae 

from the Moscow Region. The species 

cannot be completely described according 

to the methods previously elaborated 

by the author because of the poor 

state of preservation of the material from 

Gzhelian deposits. Problems of the generic 

diagnostics of the Gzhelian linoproductids 

are discussed; a new species, 

Linispinus parvus, is described from the 

uppermost Kasimovian deposits that 

have been referred to the Gzhelian Stage. 

Regularities in the group evolution in 

the Moscovian, Kasimovian, and Gzhelian 

ages are analyzed. 

2010010182 

与过滤系统发育相关的古生代腕足类 

群落演变 = Changes in the communities 

of Paleozoic brachiopods due to 

their development of their filtering system. 

( 英文 ). Afanasjeva G A. Paleontological 

Journal, 2009, 43(11): 1378- 

1389 20 图版 . 

Onward changes in the communities 

of Paleozoic articulated brachiopods 

were mainly connected with the improvement 

of the function of their filter 

feeding system, which is responsible for 

the feeding of animals. Three major 

routes of improvement are known: (1) 

feeding using a primitive lophophore 

and specialized mantle (orders Strophomenida, 

Chonetida, and Productida); 

(2) increased complexity and enlargement 

of the spirolophe and the appearance 

of the spiral brachidium (orders 

Atrypida, Spiriferida, and Athyridida); 

(3) development of the protective structures 

preventing ingestible particles into 

the inner cavity of the shell (order 

Rhynchonellida). The most effective 

was the third variant that allowed rhynchonellids, 

which appeared in the Ordovician, 

to live up to recently and survive 

after two largest extinctions in the history 

of the group development: in the 

Late Devonian and at the Permian- 

Triassic boundary. 

2010010183 

现生或化石腕足类微形化原因分析 = 

Reasons of micromorphism in modern 

or fossil brachiopods. ( 英文 ). 

Pakhnevich A V. Paleontological Journal, 

2009, 43(11): 1458-1468 6 图版 . 

Mass samples of the micromorphic 

recent (Hemithyris psittacea, Eucalathis 

murrayi, Macandrevia cranium, 

Megathyris detruncate, Argyrotheca 

cuneata, Argyrotheca cordata) and fossil 

Silurian (Microsphaeridiorhynchus 

60

sp.) brachiopods were studied. New location 

of Eucalathis murrayi on the Kitovyi 

Ridge in the Atlantic Ocean is described. 

Rates of growth of shells were 

revealed by the study of the sizes and 

age of brachiopods. Reasons of dwarfism 

in brachiopods are discussed. Three 

strategies of growth of the micromorphic 

brachiopods are distinguished. Appearance 

of micromorphic brachiopods is 

connected with the changes in the rates 

of shell growth and life expectancy. 

2010010184 

列宁格勒地区中奥陶世似正形贝腕足 

类初始壳构造 = Structure of the firstformed 

shell of the Middle Ordovician 

orthid-like brachiopods from the Leningrad 

Region. ( 英文 ). Madison A A. Paleontological 

Journal, 2009, 43(11): 

1469-1476 5 图版 . 

Shell structure of the first-formed 

shell of the Middle Ordovician orthidlike 

brachiopods from the Leningrad 

Region is described. The 190-μm-wide 

first-formed shell is composed of finely 

granular layer while 700-μm-wide firstformed 

shell is fibrous. Thus the order 

Orthida in the Early Paleozoic included 

brachiopods with both planktotrophic 

and lecithotrophic larvae in the ontogeny. 

2010010185 

日本东北部北上山地南部中二叠世新 

属 Kanokurachonetes( 腕足类 , 戟贝 

类 ) = New Genus Kanokurachonetes 

(Brachiopoda, Chonetida) from the 

Middle Permian of the southern Kitakami 

Mountains, Northeast Japan. ( 英 

文 ). Afanasjeva G A; Tazawa Jun-ichi. 


16-20 3 图版 . 

A new chonetid genus and species, 

Kanokurachonetes kanokurensis (subfamily 

Rugosochonetinae, family 

Rugosochonetidae), from the Middle 

Permian (Wordian, Kanokura Formation) 

of the southern Kitakami Mountains 

(Northeast Japan) are described. 

2010010186 

Baltoscandia 地区奥陶纪 

Lycophoriidae 科 ( 腕足类 ) = Family 

Lycophoriidae (Brachiopoda) from the 

Ordovician of Baltoscandia. ( 英文 ). 

Madison A A; Rubel M. Paleontological 

Journal, 2010, 44(2): 129-139 6 图版 . 

The family Lycophoriidae from the 

Middle Ordovician of Baltoscandia with 

one monotypic genus and five species is 

revised. New inner structures were revealed 

and diagnoses of the family, genera, 

and species were specified in the 

study of cross sections and microstructure 

of the shell. The third prismatic 

layer, complex dental plates, and socket 

ridges with short pointed lateral outgrowths 

were recorded. The family Lycophoriidae 

cannot be assigned with 

confidence to any known brachiopod 

order. 

2010010187 

晚古生代腕足类 Linoproductidae 科 

的演化和系统分类学以及 Timan 北部 

早二叠世物种描述 = Evolution and 

systematics of the Late Paleozoic 

brachiopod family Linoproductidae with 

descriptions of species from the Lower 

Permian of the Northern Timan. ( 英文 ). 

Lazarev S S. Paleontological Journal, 

2010, 44(2): 140-150 2 图版 . 

The analysis of the morphological 

features of the genera of the family Linoproductidae 

in the Late Paleozoic substantiates 

its three subfamilies as three 

evolutionary trends beginning with the 

initial subfamily Coopericinae Lazarev, 

2004, which is known from the beginning 

of the Early Carboniferous and two 

its derivatives: subfamily Linipalinae 

subfam. nov., which appeared in the Podolskian 

Time (Upper Moscovian Age), 

and subfamily Linoproductinae Stehli, 

1954, which appeared in the Kasimovian 

Age. The problems and prospects of the 

further detailing of the system of these 

subfamilies are discussed. Three new 

61

species of the genus Sublinoproductus 

are described from the Lower Permian 

of Northern Timan. 

2010010188 

二叠纪腕足类 Productus djulfensis 

Stoyanow , 即 Sarytchevinella 

Waterhouse 属的正确命名者和发布 

日期 = Correct authorship and publication 

date of the Permian Brachiopod 

Productus djulfensis Stoyanow, the type 

species of Sarytchevinella Waterhouse. 

( 英文 ). Sone M. Paleontological Journal, 

2009, 43(3): 345-346 

2010010189 

晚二叠世 Beecheriidae Smirnova 科 

( 腕足门 ) 穿孔贝目个体发生学 = 

The ontogeny of the Late Permian terebratulids 

of the family Beecheriidae 

Smirnova (Brachiopoda). ( 英文 ). Smirnova 

T N. Paleontological Journal, 

2009, 43(2): 142-152 12 图版 . 

Based on the study of the ontogenetic 

changes of cardinalia and brachidium in 

the genera Beecheria Hall et Clarke, 

1893 and Calycelasma Smirnova, 2007 

(family Beecheriidae), a complex development 

of the brachidium, which corresponds 

to the angustothyridid type, and 

the formation of crural plates, which 

functioned as the outer hinge plates at 

the early developmental stages, are revealed. 

2010010190 

俄罗斯东北部埃姆斯期 ( 早泥盆世 ) 

Ambocoeliidae George 科腕足类 ( 石 

燕贝目 ) = Brachiopods from the family 

Ambocoeliidae George (Order 

Spiriferida) from the Emsian (Lower 

Devonian) of northeastern Russia. ( 英 

文 ). Baranov V V. Paleontological 

Journal, 2009, 43(1): 59-68 5 图版 . 

Brachiopods from the family Ambocoeliidae 

George from the Emsian 

(Lower Devonian) of northeastern Russia 

are described: Bisinocoelia despecta 

sp. nov.; Yakutospirifer gen. nov. with 

the type species Y. krivensis sp. nov.; 

Micospirifer gen. nov. with the type 

species M. simplex sp. nov.; Kolymospirifer 

gen. nov. with the type species 

K. optatus sp. nov. (subfamily Ambocoeliinae); 

Datnospirifer gen. nov. 

with the type species D. alius sp. nov.; 

Khalimospirifer gen. nov. with the type 

species Kh. microscopicus sp. nov.; 

Gerospirifer gen. nov. with the type 

species G. normalis sp. nov., and G. 

gerensis sp. nov.; Dogdospirifer gen. 

nov. with the type species D. yolkini sp. 

nov. (subfamily Rhynchospiriferinae). 

2010010191 

巴西塞尔希培地区白垩系舌形贝腕足 

类的首现 , 并重新研究巴塔哥尼亚南部 

的 'Lingula' bagualensi = The first occurrence 

of a lingulid brachiopod from 

the Cretaceous of Sergipe, Brazil, with a 

restudy of 'Lingula' bagualensis 

Wilckens, 1905 from southern Patagonia. 

( 英文 ). Holmer L E; Bengtson P. Palaeontologische 

Zeitschrift, 2009, 83(2): 

255-266 

The lingulid brachiopod Lingularia? 

notialis sp. nov. is described from the 

upper Turonian of the Sergipe Basin in 

northeastern Brazil. The rare but wellpreserved 

new material shows morphological 

characters such as muscle scars, 

mantle canals land a baculateshell structure. 

In a preliminary note L.? notialis 

was referred to Lingularia? bagualensis 

from the uppermost Cretaceous of 

southern Patagonia, a species restudied 

here and referred conditionally to 

Credolingula Smirnova in Smirnova and 

Ushatinskaya, 2001. 

2010010192 

Chaniella, 阿根廷西北部一新的下特 

马豆克阶腕足类及其在基部小嘴贝中 

的系统发育关系 = Chaniella, a new 

lower Tremadocian (Ordovician) 

brachiopod from northwestern Argentina 

and its phylogenetic relationships within 

62

asal rhynchonelliforms. ( 英文 ). 

Benedetto J L. Palaeontologische 

Zeitschrift, 2009, 83(2): 393-405 

The new rhynchonelliform brachiopod 

Chaniella pascuali n. gen. n. sp. is 

described. Cladistic analysis shows that 

Chaniella is closest to the billingsellides 

Protambonites and Korinevskia. The 

particular combination of features of the 

new genus, in particular the presence of 

narrow lateral deltidial plates instead of 

a complete pseudodeltidium, led to the 

designation of the new monotypic family 

Chaniellidae. Parsimony analysis 

supports the separation of clitambonitidines 

and billingsellidines as monophyletic 

clades within the order Billingsellida 

and places the protorthide 

Arctohedra and the orthides Jivinella 

and Bohemiella close to the ancestry of 

the billingsellides. 

2010010193 

贵州南部独山地区泥盆纪弗拉期的石 

燕贝类腕足动物 = Spiriferide Brachiopods 

From The Frasnian (Devonian) Of 

The Dushan AreaA,Southern 

Guizhou,China. ( 英文 ). 马学平 . 古生物 

学报 , 2009, 48(4): 611-627 

弗拉期是了解泥盆纪弗拉 - 法门灭绝 

事件之前古代生物多样性的一个关键 

阶段。贵州南部的独山地区因其所具 

有的完整层序及丰富的底栖生物化石 

成为我国主要泥盆系参考剖面之一。 

独山剖面弗拉期的石燕贝类腕足动物 

至少包括 5 种类型 , 其中 4 种在本文中 

为首次描述和图示。Conispirifer 之 

前只发现于欧洲及北美的弗拉期地层 

中 , 目前也首次在华南独山剖面的同期 

地层中发现。大多先前从贵州南部其 

他地区弗拉期地层中描述的多种 

Cyrtospirifer 可归于 Cyrtospirifer 

subextensoides 新种内。鉴于前人对 

Emanuella 的模式种 E.takwanensis 的 

内部构造描述的矛盾状况 , 本文暂把研 

究区具有抬离壳面的纤细铰窝、固着 

于壳面的主突起以及其前方下面为外 

铰板支撑的标本归于 

E.takwanensis。在华南弗拉期可初 

步识别出三个腕足动物群组合 

带 :Yocrarhynchus-Phlogoiderhynchus 

动物群以小嘴贝类 - 无洞贝类 - 双腔贝 

类腕足动物为特征 , 其时代大致从弗拉 

阶底部至 Pa.pun-ctata 带 ; 之后为 

Cyrtospirifer 动物群 , 以 

Cyrtospirifer 的存在为特征 , 又可分 

为早晚两部分 , 前者 ( 未命名 ) 以 

Conispiriferid 类的 Cyrtospirifer 和 

Pyramidaspirifer、弓石燕类无洞贝 

类等为特征 , 其时代大致为 Pa.“hass” 

带至下 Pa.rhenama 带 ; 后者为 

Hunanotoechia 动物群 , 以丰富的小 

嘴贝类 - 无洞贝类 - 弓石燕类腕足动物 

为特征 , 其时代大致为上 Pa.rhenama 

带至 Pa.linguiformis 带。 

2010010194 

最早的腕足类的起源和分布 = Origin 

and dispersal of the earliest brachiopods. 

( 英文 ). Ushatinskaya G T. Paleontological 

Journal, 2008, 42(8): 776- 

791 9 图版 . 

Brachiopods first appeared at the very 

beginning of the Phanerozoic together 

with the first skeletal organisms. Most 

brachiopod taxa that arose in the first 

half of the Cambrian had a short temporal 

range and became completely extinct 

by the middle of the Middle Cambrian. 

Rigid articulation of the valves of 

brachiopods was provided by various 

structures, which also appeared in the 

Early Cambrian. This fact points to the 

importance of this feature for the formation 

of the whole group and at the same 

time testifies to the high variability of 

rigid articulation at the early stages of 

brachiopod evolution. This is a typical 

manifestation of archaic diversity in this 

animal phylum, which appeared very 

early in the Phanerozoic. Another important 

property of the archaic diversity 

of the early brachiopods was the large 

number of centers of diversification. As 

63

for the majority of groups, climatic zonality 

was the main factor determining 

the distribution of brachiopods at the 

beginning of the Phanerozoic. The main 

ecological types of brachiopods also appeared 

in the Early Cambrian. 

2010010195 

腕足类目级以上分类系统 = Supraordinal 

brachiopod classification. ( 英文 ). 

Afanasjeva G A. Paleontological Journal, 

2008, 42(8): 792-802 

Three controversial problems of 

brachiopod supraordinal classification 

are discussed: the position of brachiopods 

in the classification of Metazoa, 

their classification at phylum and class 

level, and the classification of the articulate 

brachiopods. The position of 

brachiopods in the system of Metazoa 

remains uncertain. There are no strong 

reasons for changing the traditional division 

of the phylum Brachiopoda into the 

classes Inarticulata and Articulata. The 

class Articulata is divided into the subclasses 

Orthata, Strophomenata, Spiriferata, 

and Terebratulata. 

2010010196 

腕足类的系统发生学研究 = Lines of 

phylogenetic studies of brachiopods. ( 英 

文 ). Afanasjeva G A. Paleontological 

Journal, 2008, 42(8): 803-804 

The main techniques used in phylogenetic 

studies of brachiopods are reviewed, 

onto-phylogenetic and morphobiological. 

The advantages and shortcomings 

of each method are discussed. 

2010010197 

穿孔贝目腕足类个体 - 系统发育学研究 

= Ontophylogenetic studies of the 

brachiopods of the order Terebratulida. 

( 英文 ). Smirnova T N. Paleontological 

Journal, 2008, 42(8): 805-824 21 图版 . 

The patterns of ontophylogenetic 

change of the brachidium in Late Paleozoic, 

Mesozoic, and Cenozoic terebratulids 

are analyzed. The work of Russian 

specialists in establishing new evolutionary 

trends and working out terebratulid 

taxonomy on the basis of ontophylogenetic 

studies is discussed. 

2010010198 

腕足类戟贝目形态生物学研究 = Morphobiological 

study of the brachiopods 

of the Order Chonetida. ( 英文 ). Afanasjeva 

G A. Paleontological Journal, 2008, 

42(8): 825-829 6 图版 . 

A comparative morphological study 

of the brachiopods of the order Chonetida 

revealed a key part of the development 

of the shell structures connected 

with the feeding and respiration organs, 

such as the lophophore, musculature, 

and mantle, in the morphological evolution 

of the group. The general trends revealed 

in the development are adaptive 

and were restored based on morphofunctional 

analysis. Against the background 

of these trends, the correlative changes 

of the shell shape and its external ornamentation 

led to the repeated appearance 

of homeomorphs, whose similarity cannot 

be explained by adaptation. The phylogeny 

of the superfamily Anoplioidea is 

described as an example. 

2010010199 

近代腕足类生物地理学 = Biogeography 

of the recent brachiopods. ( 英文 ). 

Zezina O N. Paleontological Journal, 

2008, 42(8): 830-858 12 图版 . 

The vertical, latitudinal, and circumcontinental 

zonality of the distribution of 

the species, genera, and families of recent 

brachiopods is considered. The distortions 

of the latitudinal and meridional 

symmetry of the biogeographic structure 

of the ocean are analyzed in view of the 

patterns of the global circulation of the 

surface and intermediate waters. Thus 

ancient faunas may be reconstructed 

based on data on the structural characteristics 

of the taxocene of recent 

brachiopods. The features of the paedomorphic 

evolution of brachiopods from 

64

the different families in extreme habitats 

(interstitial, underwater caverns, submarine 

rises, abyssal depths, hydrothermal 

areas, and margins of habitats) are discussed. 

The biogeographic structure of 

bottom dwellers is shown to simplify 

with depth as well as with simplification 

of the hydrological structure of the 

ocean. The important role of the bathyal 

oceanic zone (slopes of continents, islands, 

submarine mountains, ridges, and 

rises) in the preservation of faunal relicts 

is shown. The historical change from 

brachiopods to bivalves that occurred 

from the Paleozoic to the Mesozoic and 

Cenozoic is shown to have resulted not 

from competitive exclusion, but from 

complex and global changes in the 

plankton composition, which were unfavorable 

for articulate brachiopods, 

which had already developed specialized 

feeding habits, feeding on food that led 

to the production of almost no metabolic 

waste products; they had even partly lost 

their alimentary canal. The development 

of shelly plankton and, especially, of 

diatoms hampered the post-Paleozoic 

revival of large assemblages of articulate 

brachiopods in shallow-water habitats. 

The unfilled ecological niches were 

colonized by bivalves, which were 

widely adapted to feeding on live phytoand 

zooplankton. Recent articulate 

brachiopods, which are adapted to feeding 

on the products of decay of dead 

plankton, form a belt of densely populated 

settlements of the organic biofilter 

outside the photic zone on the seaward 

edge of shelves and on the upper parts of 

the slopes of continents, islands, and 

submarine rises throughout the world. 

2010010200 

加拿大 Rocky 山脉早寒武世 Mural 

组腕足类 Eoobolus = The brachiopod 

Eoobolus from the Early Cambrian Mural 

Formation (Canadian Rocky Mountains). 

( 英文 ). Balthasar U. Palaeontologische 

Zeitschrift, 2009, 83(2): 404- 

418 

Eoobolus is one of the first representatives 

of the superfamily, Linguloidea, 

the defining characteristics of which include 

the classical morphology of oval 

shells and a pedicle that emerges from 

between the two valves. The material 

described here from the Mural Formation 

provides well-preserved muscle 

scars and larval shells that allow a discussion 

of the muscle system and the 

larval morphology of Eoobolus. The 

dorsal larval shell exhibits a morphology 

similar to other Cambrian linguloids, but 

also to paterinids, Mickwitzia muralensis, 

and some rhynchonelliforms. This 

suggests that there was a lesser degree of 

disparity among brachiopod larvae in the 

Cambrian than there is today. 

2010010201 

Kutorgina Billings( 腕足类 , 古脱贝 

目 ) 的壳体构造 = Shell structure of 

Kutorgina Billings (Brachiopoda, Kutorginida). 

( 英文 ). Malakhovskaya Ya E. 


479-490 8 图版 . 

Shell structure in members of the genus 

Kutorgina, Lower Cambrian 

brachiopods with calcareous shells and 

primitive articulation, is described for 

the first time. This type of shell structure 

resembles that of the Lower Cambrian 

mollusks and hyoliths rather than of 

brachiopods. 

2010010202 

俄罗斯东北部早中泥盆世腕足类正形 

贝 = Orthid brachiopods from the Lower 

and Middle Devonian of northeastern 

Russia. ( 英文 ). Baranov V V. Paleontological 

Journal, 2008, 42(4): 363- 

372 5 图版 . 

Brachiopods of the order Orthida 

from the Lower and Middle Devonian of 

northeastern Russia: Skenidium diversus 

Baranov (family Skenidiidae); Datnia 

gen. nov., with the type species D. asiatica 

sp. nov. (subfamily Prokopiinae); 

Janzhinshinia gen. nov., with the type 

65

species J. datnensis sp. nov. (subfamily 

Isorthinae); Cortezorthis chobotchalensis 

(Alekseeva) (subfamily Cortezorthinae); 

Elenia gen. nov., with the type 

species E. gerensis sp. nov. (family Dicoelosiidae); 

Seimtchania communis 

(family Seimtchaniidae); Simakovia gen. 

nov., with the type species S. rara sp. 

nov. (family Draboviidae); Schizophoria 

distenta sp. nov., S. grande Baranov, S. 

striatula (Schlotheim) (family Schizophoriinae); 

and Hypsomionia sinsera 

Baranov (family Hypsomioniidae) are 

described. 

2010010203 

莫斯科 Syneclise 地区早石炭世 

Unispirifer Campbell 属 ( 腕足类 , 石 

燕贝目 ) = The genus Unispirifer 

Campbell (Brachiopoda, Spiriferida) in 

the Early Carboniferous of the Moscow 

Syneclise. ( 英文 ). Afanasjeva G A. Paleontological 

Journal, 2008, 42(4): 373- 

377 1 图版 . 

Two new species of the genus 

Unispirifer Campbell, U. semicircularis 

and U. parvus, are established as a result 

of a revision of Early Carboniferous 

spiriferids from the Moscow Syneclise. 

These forms have previously been described 

under Spirifer tornacensis 

Koninck, 1883 and S. taidonensis Tolmatschow, 

1924. 

2010010204 

莫斯科州卡西莫夫阶 

Linoproductidae 科腕足类 = Brachiopods 

of the family Linoproductidae from 

the Kasimovian Stage of the Moscow 

Region. ( 英文 ). Lazarev S S. Paleontological 

Journal, 2008, 42(4): 378- 

388 2 图版 . 

Brachiopods from the Kasimovian 

Stage of the Moscow Region that for 

more than 70 years were referred to the 

genus Linoproductus (family Linoproductidae) 

are revised and redescribed. 

New characters connected with the ornamentation 

and inner structure of the 

dorsal valve are used for the first time in 

the analysis of the taxonomic structure 

of the group. Six species from three 

genera are described; four of them are 

new: one species of Linispinus Lazarev, 

2006, three species of Linipalus Lazarev, 

2007, and two species of Sublinoproductus 

gen. nov. The new genus is considered 

to be transitional between the genera 

Linispinus and Linoproductus. 

2010010205 

莫斯科 Syneclise 地区中石炭世 

Neotornquistia 属 ( 腕足类 , 戟贝 

类 ) = New Middle Carboniferous genus 

Neotornquistia (Brachiopoda, Chonetida) 

from the Moscow Syneclise. ( 英 

文 ). Afanasjeva G A. Paleontological 

Journal, 2008, 42(3): 260-264 1 图版 . 

A new Middle Carboniferous 

brachiopod genus, Neotornquistia, with 

the type species Paeckelmannia aljutovica 

E. Ivanova, 1952 (order Chonetida, 

superfamily Anoplioidea, family 

Anopliidae, subfamily Tornquistiinae) is 

described from the Alyutovo Formation 

of the Vereyan Horizon of the 

Moscovian Stage of the Moscow Syneclise. 

2010010206 

蒙古东北部二叠纪 ( 腕足类 ) 一新命 

名属 :Mongousia = Mongousia: A 

new productid genus (Brachiopoda) 

from the Permian of northeastern Mongolia. 

( 英文 ). Manankov I N. Paleontological 

Journal, 2008, 42(3): 265- 

268 1 图版 . 

A new linoproductid genus is described 

from the provincial Terrakea 

arguta Zone (lower part of the Upper 

Kazanian Substage) of the key section of 

the Tsagan-Temete Horizon (Kazanian 

Stage-Lower Tatarian Substage) of 

northeastern Mongolia. The type species 

of the new genus was found in the middle 

layers of the Lower Uldza Subformation, 

which contains numerous di- 

66

verse productids from the genus Terrakea. 

2010010207 

Agyrek 山 ( 哈萨克斯坦中心偏东北 

地区 ) 晚寒武世舌形贝 ( 腕足类 ) = 

New Upper Cambrian Lingulata 

(Brachiopoda) from the Agyrek mountains 

(northeastern central Kazakhstan). 

( 英文 ). Koneva S P; Ushatinskaya G T. 


139-148 5 图版 . 

Two new genera, Repkinella and 

Aristotreta, and five new species from 

the class Lingulata (Brachiopoda) are 

described from the Upper Cambrian 

olistolith limestone enclosed in the Upper 

Ordovician olistostrome from the 

Agyrek mountains (northeastern Kazakhstan). 

The family Curticiidae Walcott 

et Schuchert is referred to the order 

Lingulida, not order Acrotretida, where 

it was previously placed. 

2010010208 

俄罗斯西北部圣彼德堡地区晚奥陶世 

特有腕足类和棘皮动物属 = New endemic 

brachiopod and echinoderm genera 

from the Upper Ordovician of the St. 

Petersburg region, northwestern Russia. 

( 英文 ). Zuykov M A; Terentiev S S; 

Harper D A T. GFF, 2008, 130(2): 87- 

93 

A new brachiopod and a rhombiferan 

cystoid are described from the Gryazno 

and Schundorovo formations (Upper 

Ordovician; middle Sandbian), Idavere 

Regional Stage, of the St. Petersburg 

Region (northwestern Russia). The fossils 

are part of an abundant, wellpreserved 

benthic fauna. The rhynchonelliformean 

brachiopod Madiorthis 

alsami gen. et sp. nov. belongs to the 

family Plaesiomyidae (subfamily Plaesiomyinae); 

the dichoporite echinoderm 

Fusicystis magnificus gen. et sp. nov. is 

assigned to the family Echinoencrinitidae 

(subfamily Scoliocystinae). These 

new taxa have not been found outside 

the type locality. 

2010010209 

瑞典东约特兰省 Borenshult 地区赫南 

特亚阶地层 ( 奥陶系最顶部 ) 已知最 

早的 Stegerhynchus( 小嘴贝目 , 腕 

足动物门 ) = The earliest known 

Stegerhynchus (Rhynchonellida, 

Brachiopoda) from the Hirnantian strata 

(uppermost Ordovician) at Borenshult, 

Ostergotland, Sweden. ( 英文 ). Rong J Y; 

Jin J S; Zhan R B; Bergstrom J. 

GFF, 2008, 130(1): 21-30 

Stegerhynchus eoborealis sp. nov. 

from the Dalmanitina Beds (Hirnantian, 

uppermost Ordovician), Borenshult, Ostergotland, 

Sweden, is described in this 

study as the earliest known species of 

Stegerhynchus, within the family Rhynchotrematidae. 

This implies that Stegerhynchus 

originated during the latest Ordovician 

mass extinction event, and radiated 

in the Silurian Period to become 

one of most common rhynchonellide 

brachiopod genera in shallow tropical 

seas. In the early evolutionary stage of 

the genus, Stegerhynchus eoborealis already 

exhibited a notable reduction in 

the size of septalium compared to the 

closely related genus Rhynchotrema. 

Compared to its Silurian counterparts 

(e.g. Stegerhynchus borealis and S. 

peneborealis), Stegerhynchus eoborealis 

has some variable characters within single 

populations, particularly in the number 

of costae in the sulcus and on the 

fold, implying a morphological plasticity 

during the early evolutionary stage of 

the genus. During the Hirnantian mass 

extinction events, five rhynchonellide 

families were represented by small taxonomic 

groups, but only the Rhynchotrematidae 

and Trigonirhynchiidae diversified 

into many highly successful clades 

of rhynchonellides during the Silurian 

and Devonian. However, the Ancistrorhynchidae, 

Orthorhynchulidae, and 

Sphenotretidae largely disappeared by 

67

the end of the Ordovician, with a few 

species (such as Plectothyrella sp.) surviving 

into the earliest Silurian but 

shortly becoming extinct. 

2010010210 

欧亚大陆二叠纪穿孔贝属 : 形态学 , 

系统学和系统发生学 = Permian terebratulids 

of Eurasia: Morphology, systematics, 

and phylogeny. ( 英文 ). Smirnova 

T N. Paleontological Journal, 

2007, 41(11): 707-813 85 图版 . 

The Permian terebratulids of Eurasia 

are revised. The taxonomic composition 

of the Permian terebratulids of the Russian 

Platform, Northern Caucasus, Transcaucasia, 

northern and southeastern 

Pamirs, and northern China (Inner Mongolia) 

is elucidated. Fifty-one species 

(13 described here as new), 21 genera (3 

described here as new), 7 families, and 6 

superfamilies are described. During the 

progress of the study, the author (Smirnova, 

2004a, 2004b, 2006a, 2006b) and 

Smirnova and Grunt (2002, 2003a, 

2003b) described for the first time 19 

species, nine genera, two families, and 

one superfamily. Morphofunctional 

analysis reveals a great diversity of internal 

structures, of the time of their appearance 

in the ontogeny, and of their 

taxonomic significance. Ontogenetic 

study reveals phylogenetic relationships 

between the Permian and Meso- 

Cenozoic terebratulids, the presence of 

the superfamilies Terebratuloidea and 

Loboidothyroidea in the Permian, and a 

new type of brachidium ontogeny characterizing 

the superfamily Compositelasmatoidea. 

This book is intended for 

paleontologists and biologists interested 

in problems of taxonomy and phylogeny, 

and includes 5 plates, 80 figures, and 75 

bibliographic references. 

2010010211 

腕足类触手腕构造 = Structure of the 

brachiopod lophophore. ( 英文 ). Kuzmina 

T V; Malakhov V V. Paleontological 

Journal, 2007, 41(5): 520- 

536 13 图版 . 

Data on the development, structure, 

and functional morphology of the 

brachiopod lophophore are analyzed. 

The common origin of the tentacle apparatus 

in Lophophorata from the postoral 

ciliary band of the larva is shown. The 

brachiopod lophophore is based on the 

brachial axis consisting of the brachial 

fold running along the row of tentacles. 

The brachial axis may be attached to the 

brachial (dorsal) mantle lobe (trocholophe, 

schizolophe, and ptycholophe lophophores) 

or extend freely into the 

mantle cavity to form coiling brachia 

(spirolophe, zygolophe, and plectolophe 

lophophores). The circulation of water 

flows through the mantle cavity in the 

brachiopods with attached and free lophophores 

is described. A new hypothesis 

on the sorting of particles suspended 

in water during filtration is proposed. 

2010010212 

Novaya Zemlya 地区法门阶 

Camarotoechia radiata Nalivkin( 腕 

足类 , 小嘴贝目 ) 修订 = Revision of 

Camarotoechia radiata Nalivkin 

(Brachiopoda, Rhynchonellida) from the 

Famennian of Novaya Zemlya. ( 英文 ). 

Cherkesova S V. Paleontological Journal, 

2007, 41(4): 407-414 5 图版 . 

The shell interior of the rhynchonellid 

brachiopod Sinotectirostrum radiatum 

(Nalivkin) is studied for the first time. 

The description of this species is 

emended. The internal and external features 

of three species are analyzed to 

confirm their validity: S. radiatum, S. 

banffense (Warren), and S. arcticum 

Yudina. A new subspecies, S. banffense 

rachmanovense subsp. nov., and a new 

species, S. hayminense, are described. 

The genus Pseudosinotectirostrum 

Yudina, 1991 is treated as a subgenus of 

Sinotectirostrum Sartenaer, 1961. 

68

2010010213 

日本东北部北上山地南部中二叠世大 

戟贝类 ( 腕足类 ) 一新属一新种 = A 

new large chonetid (Brachiopoda) from 

the Middle Permian of the southern Kitakami 

Mountains, northeast Japan. ( 英 

文 ). Afanasjeva G A; Tazawa J. Paleontological 

Journal, 2007, 41(4): 424- 

428 3 图版 . 

A new chonetid genus and species, 

Kitakamichonetes multicapillatus gen. et 

sp. nov. (subfamily Chalimochonetinae, 

family Rugosochonetidae), from the 

Middle Permian (Wordian-Capitanian, 

Kanokura Formation) of the southern 

Kitakami Mountains (northeast Japan) is 

described. 

2010010214 

普斯科夫州奥陶纪 craniids 幼壳首次 

发现 = First finds of larval shells of Ordovician 

craniids in the Pskov Region. 

( 英文 ). Madison A A. Paleontological 

Journal, 2007, 41(3): 248-251 2 图版 . 

The inner surface of the dorsal valve 

at the early developmental stages and 

the larval shells lacking adult shell are 

described for the first time for the Ordovician 

craniids. The presence of a larval 

calcareous shell in the Early Paleozoic 

craniids is proposed. 

2010010215 

俄罗斯东北部泥盆纪腕足类新发现 = 

New Devonian brachiopods from northeastern 

Russia. ( 英文 ). Baranov V V. 


252-259 5 图版 . 

Brachiopods from the Devonian of 

northeastern Russia are described: Eoprokopia 

gen. nov., with the type species 

E. aequalis sp. nov. (subfamily Prokopiinae, 

order Orthida); Davoustia settedabanica 

sp. nov. and D. verkhojanica sp. 

nov. (family Anopliidae, order Chonetida); 

and Alkhovikovia gen. nov. with 

the type species A. libera sp. nov. and A. 

importuna sp. nov. and Tikhyspirifer gen. 

nov. with the type species T. globosus sp. 

nov. (subfamily Rhynchospiriferinae, 

order Spiriferida). 

2010010216 

俄罗斯东北部早 - 中泥盆世 

Delthyridina Ivanova 亚目 ( 石燕贝 

目 ) = Brachiopods of the suborder 

Delthyridina Ivanova (Order Spiriferida) 


northeastern Russia. ( 英文 ). Baranov V 

V; Al’khovik T S. Paleontological 

Journal, 2007, 41(1): 39-48 9 图版 . 

New brachiopods of the suborder 

Delthyridina Ivanova (order Spiriferida) 


northeastern Russia, Ivanothyris costatus 

sp. nov. (subfamily Delthyridinae), 

Eoreticularia lata sp. nov., Yania gen. 

nov. with the type species Y. tumida sp. 

nov. (subfamily Eoreticulariinae), Reticulariopsis 

equitans Modzalevskaya, 

and R. (?) borealis sp. nov. (subfamily 

Reticulariopsinae) are described. 

2010010217 

东欧泥盆纪和石炭纪石燕类 ( 腕足动 

物 ) 新种 = New species of spiriferids 

(Brachiopoda) from the Devonian and 

Carboniferous of Eastern Europe. ( 英文 ). 

Poletaev V I. Paleontological Journal, 

2006, 40(5): 507-517 4 图版 . 

In a revision of previously published 

materials, two new spiriferid species 

from the Late Tournaisian, Unispirifer 

subtornacensis sp. nov. and Mesochorispira 

ussuilensis sp. nov., and Atylephorus 

nalivkini sp. nov. from the Lytva 

Horizon of the Upper Devonian of 

Bashkiria are described. Based on the 

original collection, a new Serpukhovian 

subspecies, Podtsheremia duplicicosta 

triplicicosta, from the southern Ural 

Mountains and a new Late Carboniferous 

species, Purdonella kalashnikovi, 

from the polar Ural Mountains and adjacent 

islands are established. 

69

2010010218 

莫斯科地区中石炭世莫斯科阶下部腕 

足动物线纹长身贝科 

( Linoproductidae stehli ) = The 

brachiopod family Linoproductidae 

stehli from the lower Moscovian of the 

Middle Carboniferous of the Moscow 

Region. ( 英文 ). Lazarev S S. Paleontological 

Journal, 2006, 40(5): 518- 

528 2 图版 . 

The phylogeny and taxonomy of the 

brachiopod family Linoproductidae are 

revised. The change in the distributional 

pattern of spines and distinctive structure 

of the median lobe of the cardinal 

process are shown to be the main apomorphies 

in the family evolution. A new 

subfamily, Linispininae, and the included 

new genera, Linispinella and 

Linispinus, are described. In the nominotypical 

subfamily Linoproductinae, a 

new genus Linoproductoides and two 

new species included in this genus are 

described from the Vereiskian deposits 

of the Moscow Region. The new species 

Linispinus riparius (Trautschold), L. 

longus sp. nov., and L. staricensis 

(Ivanov) are described from the Kashirskian 

deposits. Another new species is 

tentatively described as “Linoproductus” 

kabanovi. 

2010010219 

俄罗斯板块中 - 晚泥盆世角锥状石燕类 

( 腕足动物门 ): 形态学 , 系统学和 

壳壁构造 = Pyramidal spiriferids 

(brachiopods) from the Middle and Upper 

Devonian of the Russian Plate: Morphology, 

systematics, and shell wall 

structure. ( 英文 ). Oleneva N V. Paleontological 

Journal, 2006, 40(4): 415- 

424 6 图版 . 

The pyramidal spiriferids Thomasaria 

Stainbrook, 1945 and Pyramina 

Ljaschenko, 1969 from the collection of 

brachiopods of Ljaschenko are examined. 

New data on the shell microornamentation 

and inner structure support 

the validity of the genus Piramina and 

its type species P. oskolensis Ljaschenko. 

A new species of the genus Thomasaria, 

T. rotunda is described. 

软体动物 

2010010220 

早寒武世腹足类开放松旋型初始壳 

( 胎壳 ) 形态学及研究意义 = Morphology 

of the openly coiled initial whorls 

( protoconchs) of the Early Cambrian 

gastropods with its implication. ( 中文 ). 

冯伟民 ; 钱逸 ; 冯曼 . 微体古生物学 

报 , 2009, 26(2): 158-163 1 图版 . 

对中国早寒武世软体动物腹足类标 

本的再研究表明 , 早期腹足类 

Archaeospiriids , Auriculaspiriids 和 

Xinjispiriids 无一例外都以开放松旋型 

初始壳 ( 胎壳 ) 为特征 , 但这些腹足类的 

胎壳与后续螺壳的分界各具标志。这 

种胎壳是古生代腹足类特有的特征。 

研究结果证明 , 以开放松旋型初始壳为 

特征的腹足类胎壳可以追溯到早寒武 

世的梅树村期。这种开放松旋型胎壳 

的特征使一直以来颇受争议的 

Archaeospiriids Auriculaspiriids 是否归 

属于腹足类得到了肯定。梅树村期的 

Archaeospiriids 胎壳直径在 200 - 

250μm 之间 , 表明其幼体是一种非漂浮 

营养型的生活模式 , 而沧浪铺期的 

Auriculaspiriids 和 Xinjispiriids 胎壳直 

径均小于 130μm , 其幼体可能是一种 

漂浮营养型的生活模式。因此 , 早期腹 

足类首先选择的是非漂浮营养型的幼 

体生活模式 , 而从发育非漂浮营养型的 

幼体生活模式到发育漂浮营养型的幼 

体生活模式 , 这种多样性的变化可能在 

寒武纪大爆发主幕阶段就已呈现。实 

现腹足类幼体生活模式多样化的因素 

除了捕食作用产生的生物竞争压力所 

诱导的逃逸本能外 , 动荡的水动力环境 

和由此引起的营养悬浮物进一步增加 

可能是促使早期腹足类幼体生活模式 

发生根本性变化的重要因素。 

70

2010010221 

白垩纪海洋营养物质、温室碳酸盐和 

锥螺类腹足动物的丰度 = Cretaceous 

marine nutrients, greenhouse carbonates, 

and the abundance of turritelline gastropods. 

( 英文 ). Allmon W D. Journal of 

Geology, 2007, 115(5): 509-523 

Modern marine carbonate sediments 

accumulate where carbonate-producing 

organisms are abundant and siliciclastic 

input is low. Such accumulations occur 

today in two main environments and 

may be characterized as warm, lownutrient 

(WLN; also known as tropical or 

chlorozoan) carbonates or cool, highnutrient 

(CHN; also known as coolwater, 

temperate, nontropical, foramol, or heterozoan) 

carbonates. Few carbonates 

form today in warm, high-nutrient 

(WHN) conditions because such environments 

are very rare. Modern WLN 

environments occur mainly in low latitudes, 

where nutrients from upwelling or 

terrestrial runoff are low. Modern CHN 

environments occur mainly in middle to 

high latitudes, where nutrients, mostly 

from upwelling, are abundant. However, 

WHN depositional environments may 

have been widespread during the Cretaceous 

and Paleogene. During these times, 

upwelled nutrientrich waters would, in 

general, have been warmer than they are 

today. Nutrients in these waters supported 

diverse carbonate-producing biotas 

that are not equivalent to either modern 

chlorozoan or heterozoan biotas. 

These conclusions derive from analysis 

of a growing data set of more than 40 

turritelline gastropod-dominated fossil 

assemblages (TDAs), a term herein redefined, 

ranging in age from Lower Cretaceous 

to Pleistocene. Today TDAs occur 

mainly in CHN conditions. They 

were widespread in both carbonate and 

siliciclastic facies in the Cretaceous and 

Paleogene but (with only a single known 

exception in the Pliocene of Chile) occur 

in the Neogene only in siliciclastic 

sediments. This change in environmental 

distribution can be explained by positing 

changes in (1) modal environmental 

preferences of turritellines, from WHN 

to CHN, and (2) carbonate depositional 

environments, from to WLN + WHN 

WLN +. Both changes were roughly coincident 

with the global change from " 

greenhouse" to " icehouse" conditions in 

CHN the Oligocene. 

2010010222 

浅水海洋环境的碳酸盐保存 : 热带硅 

质碎屑的意外作用 = Carbonate preservation 

in shallow marine environments: 

Unexpected role of tropical siliciclastics. 

( 英文 ). Best M M R; Ku T C W; 

Kidwell S M; Walter L M. Journal of 

Geology, 2007, 115(4): 437-456 

Coordinated taphonomic, geochronologic, 

and geochemical studies of bivalve 

death assemblages and their sedimentary 

environments of San Blas, Caribbean 

Panama, permit us to identify the 

major factors controlling skeletal degradation 

in mixed carbonate-siliciclastic 

tropical shelf sediments. Ten sites were 

studied along environmental gradients 

including water nutrients, grain size, and 

sediment chemistry (carbonate, organic 

carbon, and reactive iron contents). Taphonomic 

data were derived from naturally 

occurring bivalve death assemblages 

and experimentally deployed 

specimens of Mytilus edulis and Mercenaria 

mercenaria to determine environmental 

controls on types and intensities 

of postmortem damage to skeletal hardparts 

and to quantify short-term rates of 

damage accrual. Death assemblage 

shells were dated using C-14 and amino 

acid racemization techniques to examine 

shell persistence, scales of time averaging, 

and long-term rates of damage accrual, 

including correlations between 

shell damage and shell age. Pore water 

and sediment geochemical analyses 

were used to determine the pathways 

and extent of early diagenetic change in 

the different sediment-pore water environments. 

We found that carbonate shell 

preservation is enhanced in dominantly 

71

siliciclastic sediments compared to 

dominantly carbonate sediments. The 

most important factors limiting the 

postmortem persistence of shell material 

are (1) exposure above the sedimentwater 

interface, which is enhanced in 

coarser-grained carbonate sediments and 

permits attack by bioeroders and encrusters; 

(2) the availability of abundant 

reactive iron mineral phases in the sediments, 

which promotes supersaturated 

pore waters and limits acid production; 

and (3) shell microstructure (rather than 

mineralogy), particularly organic content 

that is the focus of intense microbial 

attack. Thus, there is significant potential 

for enhanced carbonate shell preservation 

in areas receiving ferric-rich 

tropical weathering products, which are 

common in much of the tropics today 

and are associated with subduction systems 

in the geologic past. This suggests 

that paleodiversity estimates from carbonate 

tropical settings are minima and 

that siliciclastic settings are probably 

underestimated regions for carbon burial, 

given the large proportion of tropical 

shelf area characterized by such conditions 

and the relatively high proportional 

capture there of local carbonate production 

2010010223 

泰国东部中二叠统瓜德鲁普世稀有的 

似蜓螺型腹足类 Magnicapitatus 属一 

新种 = A new species of the rare neritopsid 

gastropod Magnicapitatus from 

the Guadalupian (Middle Permian) of 

East Thailand (the Indochina Terrane). 

( 英文 ). Sone M. Alcheringa, 2010, 34(1): 

1 - 6 

A new species of the rare neritopsid 

gastropod genus Magnicapitatus is 

documented from a fusulinoid-rich limestone 

of the Khao Taa Ngog Formation 

(Capitanian, Middle Permian) at Khao 

Makha in East Thailand near the Cambodian 

border (in the Indochina Terrane). 

This represents the first record of this 

Permo-Triassic genus outside South 

China and from the Capitanian. Magnicapitatus 

is one of the typical molluscan 

Lazarus taxa that apparently disappeared 

at the end of the Permian but reappeared 

after the Early Triassic. 

2010010224 

腹足类证据不支持早三叠世小型化效 

应假说 = Gastropod evidence against 

the Early Triassic Lilliput effect. ( 英文 ). 

Brayard A; Nützel A; Stephen D; Bylund 

K G; Jenks J; Bucher H. Geology, 

2010, 38(2): 147-150 

Size reduction in the aftermath of the 

Permian-Triassic mass extinction event 

has repeatedly been described for various 

marine organisms, including gastropods 

(the Lilliput effect). A Smithian 

gastropod assemblage from Utah, USA, 

reveals numerous large-sized specimens 

of different genera as high as 70 mm, the 

largest ever reported from the Early Triassic. 

Other gastropods reported from 

Serbia and Italy are also as large as 35 

mm. Size frequency distributions of the 

studied assemblages indicate that they 

were not unusually small when compared 

with later Mesozoic and modern 

faunas. The occurrence of large-sized 

gastropods less than 2 Ma after the Permian-Triassic 

mass extinction refutes the 

Lilliput hypothesis in this clade, at least 

for the last 75% of the Early Triassic 

2010010225 

伏尔加河中下游地区由 P.A. Gerasimov 

采集的早白垩世腹足类 = Early 

Cretaceous gastropods of the Middle- 

Lower Volga river region from P.A. 

Gerasimov’s collection. ( 英文 ). Golovinova 

M A; Guzhov A V. Paleontological 

Journal, 2009, 43(5): 506-513 2 图 

版 . 

Based on the studying of gastropods 

collected by P.A. Gerasimov from the 

Cretaceous beds of the Volga region, 

four new species are established: Avellana 

hauteriviensis sp. nov. from the 

Upper Hauterivian of the Ulyanovsk re- 

72

gion, “Palaeorissoina” sokolovensis sp. 

nov., O. sinzowi sp. nov., and Nerineopsis 

turritum sp. nov. from Lower Aptian 

of the Saratov region. The Upper Hauterivian 

for the first time yielded representatives 

of the genera Pseudomelania 

s. l., Ampullina, and Sulcoactaeon. The 

specimens of Cirsocerithium subspinosum 

Deshayes, 1842, Ringinella obtusa 

(Nackij, 1916), and Crispotrochus humilis 

(Trautschold, 1865) found in the 

Lower Aptian of the Volga region are 

figured for the first time. 

2010010226 

乌拉尔古盆地古生代菊石的生态结构 

和生态进化阶段 = Ecological structure 

and stage of ecogenesis of Paleozoic 

ammonoids in the Uralian paleobasin. 

( 英文 ). Boiko M S; Konovalova V A. 


519-526 2 图版 . 

The ecological structure of Paleozoic 

ammonoid assemblages of the Uralian 

paleobasin is discussed. Life forms (nektobenthic, 

planktonic, and benthopelagic) 

are used as ecological units. Four stages 

in evolution of the communities, with 

distinct structure and evolutionary pathways, 

are recognized. 

2010010227 

早白垩世 Ancyloceratina 亚目菊石异 

形和单形的演化 = The evolution of the 

heteromorph and monomorph Early Cretaceous 

ammonites of the suborder 

Ancyloceratina Wiedmann. ( 英文 ). 

Mikhailova I A; Baraboshkin E Yu. Paleontological 

Journal, 2009, 43(5): 527- 

536 6 图版 . 

The relationship between the appearances 

of heteromorph and monomorph 

ammonoids and changes in the abiotic 

environment was studied. The correlation 

of these processes was examined for 

different intervals in the Early Cretaceous. 

The phylogeny of the superfamily 

Ancyloceratoidea Gill from the time of 

appearance of early heteromorphs (due 

to changes in ecological specialization) 

and the reversal process of the return to 

monomorph shells is examined for four 

superfamilies. The origin of monomorph 

ammonites of the superfamilies Theodoritoidea 

Baraboshkin et I. Michailova, 

superfam. nov., Douvilleiceratoidea 

Parona et Bonarelli, Parahoplitoidea 

Spath et Deshayesitoidea Stoyanow 

from heteromorph ancestral families 

Crioceratitidae Gill, Ancyloceratidae 

Gill, Hemihoplitidae Spath, and Heteroceratidae 

Spath in the superfamily Ancyloceratoidea 

Gill is suggested. 

2010010228 

Volgian 阶的菊石新种 Craspedites 

schulginae sp. nov. = Craspedites 

schulginae sp. nov., a new ammonite 

species from the Volgian Stage. ( 英文 ). 

Alifirov A S. Paleontological Journal, 

2009, 43(6): 612-614 1 图版 . 

Revision of the Siberian Middle- and 

Upper Volgian ammonites, which were 

previously identified as Craspedites 

mosquensis Geras. allow their reidentification 

as a new species C. schulginae 

sp. nov. 

2010010229 

俄罗斯地台 Ryazanian 阶特提斯型菊 

石属 Subalpinites Mazenot = Ammonites 

of Tethyan origin from the Ryazanian 

of the Russian platform: Genus 

Subalpinites Mazenot. ( 英文 ). Mitta V 

V. Paleontological Journal, 2009, 43(5): 

615-625 6 图版 . 

The ammonite genus Subalpinites is 

known from the Berriasian of southern 

and central Europe, North Africa, Mangyshlak, 

and Ryazanian Stage of Central 

Russia. New species are described: S. 

gruendeli sp. nov., S. faurieformis sp. 

nov., S. remaneiformis sp. nov. These 

species and also S. krischtafowitschi 

Mitta characterize the lower subzone of 

the Riasanites rjasanensis Zone in the 

Moscow Region. The upper subzone of 

this zone in the Ryazan Region con- 

73

tained members of Subalpinites identified 

in open nomenclature. 

2010010230 

Ulyanovsk Povolzhye 地区早阿普特期 

的菊石新种 Cheloniceras natarius sp. 

nov. = Cheloniceras natarius sp. nov. 

(Ammonoidea) from the Lower Aptian 

of Ulyanovsk Povolzhye. ( 英文 ). Mikhailova 

I A. Paleontological Journal, 

2009, 43(6): 626-630 3 图版 . 

A new species Cheloniceras natarius 

sp. nov. (Ammonoidea, Douvilleiceratidae) 

is described from the Lower Aptian 

of Ulyanovsk Povolzhye. 

2010010231 

Primorye 南部早三叠世菊石 

Euflemingites 的一个新种 = A new 

species of Euflemingites Spath (Ammonoidea) 

from the Lower Triassic of 

Southern Primorye. ( 英文 ). Smyshlyaeva 

O P. Paleontological Journal, 

2010, 44(2): 125-128 2 图版 . 

A new species, Euflemingites artyomensis 

sp. nov., is described from the 

Olenekian of the vicinity of the town of 

Artyom (Southern Primorye). Geographical 

differentiation of the genus 

Euflemingites is discussed. 

2010010232 

巴伐利亚中新世 Sandelzhausen 化石 

产地的陆生软体动物及其古生态价值 

= Continental molluscs of the fossil site 

Sandelzhausen (Miocene; Upper Freshwater 

Molasse from Bavaria) and atheir 

value for palaeoecological assessment. 

( 英文 ). Mosser M; Niederhofer H-J; 

Falkner G. Palaeontologische 

Zeitschrift, 2009, 83(1): 25-54 

The continental mollusc fauna of 

Sandelzhausen is presented and shown 

to consist 66 snail and 3 bivalve taxa. 

Previous ecological interpretations were 

partly based on poorly preserved material 

and are shown to be erroneous. 

Within a series of quantitative samples, 

ecologically four mollusc communities 

can be distinguished (two each for terrestrial 

and freshwater molluscs), highly 

indicative of ecological conditions and 

changes in the landscape surrounding 

the fossil site as well as the locality itself. 

2010010233 

新西伯利亚群岛弗拉期菊石 = On 

Frasnian ammonoids of the New Siberian 

Islands. ( 英文 ). Nikolaeva S V; 

Kuzmichev A B; Aristov V A. Paleontological 

Journal, 2009, 43(2): 134- 

141 5 图版 . 

Ammonoids from the basal beds of 

the Nerpalakh Formation (Lower Frasnian) 

of Belkovsky Island (New Siberian 

Archipelago) are systematically studied. 

Taxonomically, the assemblage studied 

(Manticoceras insulare sp. nov., Tornoceras 

typum (Sandberger, 1851), and 

T. contractum Glenister, 1958) is similar 

to the Early Frasnian ammonoid assemblage 

of South Timan, from which its is 

distinguished by the absence of the genera 

Timanites and Komioceras. The 

same beds contain conodonts of the 

Palmatolepis transitans Zone (= MN 4 

Zone of the Montagne Noire standard 

succession), which allow the correlation 

of the beds studied with the Timanites 

keyserlingi and Komioceras stuckenbergi 

ammonoid zones of South Timan. 

The Early Frasnian ammonoids could 

supposedly have entered the region of 

the New Siberian Archipelago from the 

southwest at the time of a major transgression, 

which facilitated the distribution 

of the genera Manticoceras and 

Tornoceras. A new species of the genus 

Manticoceras is described. 

2010010234 

双壳类分类系统和系统分类原则 = 

Principles of systematics and the system 

of bivalves. ( 英文 ). Nevesskaja L A. Paleontological 

Journal, 2009, 43(1): 1-11 

The systems of the class Bivalvia accepted 

in recent manuals are discussed. 

The system proposed by L.A. Ne- 

74

vesskaja, O.A. Skarlato, Ya.I. Starobogatov, 

and A.G. Eberzin (1971) is 

substantiated and updated. Morphological 

characters important for the establishment 

of taxa of different ranks are 

listed. Three superorders and 17 orders 

are established; two orders, which are 

restricted to the Cambrian and the beginning 

of the Ordovician, are placed 

outside the accepted superorders. 

2010010235 

亚北方带侏罗纪卡洛夫期早期 

Eckhardites 

Mitta 

( Cardioceratidae , 菊石亚纲 ) = 

Genus Eckhardites Mitta (Cardioceratidae, 

Ammonoidea) from the Lower 

Callovian of the subboreal Jurassic. ( 英 

文 ). Mitta V V. Paleontological Journal, 

2009, 43(1): 50-58 3 图版 . 

The genus Eckhardites Mitta 1999, 

with the type species Macrocephalites 

pavlowi Smorodina, 1928 is discussed 

and its diagnosis and assignment to the 

family Cardioceratidae are substantiated. 

Eckhardites is compared to the genus 

Macrocephalites Zittel (family Sphaeroceratidae), 

to which some workers presently 

assign the type species of Eckhardites. 

Three species of Eckhardites 

are recorded from the basal Callovian 

elatmae Zone of the Russian Platform, 

one of which (E. menzeli (Mönnig)) was 

originally described from the synchronous 

beds in Germany. A new species E. 

dietli sp. nov. is described. 

2010010236 

新疆寒武纪早期单壳类软体动物化石 

分类学与生物地层学 = Taxonomy and 

biostratigraphy of the Early Cambrian 

Univalved mollusc fossils from Xinjiang. 

( 中文 ). 钱逸 ; 冯伟民 ; 李国祥 ; 杨爱华 ; 冯 

曼 ; 赵鑫 ; 肖兵 . 微体古生物学报 , 2009, 

26(3): 193-210 2 图版 . 

作者系统描述了新疆阿克苏 — 乌什 

地区下寒武统玉尔吐斯组中上部单壳 

类软体动物化石 10 属 10 种 , 其中包括 

3 个新种、3 个老种和 4 个未定种 , 它 

们是 Shabaktiella multiformis sp. 

nov. , Ilsanella acuta sp. 

nov. ,Xianfengella yuertusiensis sp. 

nov. , Parcaconus xinjiangensis , Protostenotheca 

xinjiangensis , Aldanella 

attleborensis , Obtusoconus sp . , 

Yochelcionella sp. , Bemella sp. 和 

Mellopegma sp. 。上述 10 个属种基本 

上代表了玉尔吐斯组单壳类软体动物 

的面貌特征。文中介绍了本研究区 10 

个属和属级以上分类系统在国际学术 

界的意见分歧后 , 重申了以壳的对称性 

和有无肌痕确定纲级界线的最佳分类 

原则 , 提出了应用壳型划分目级分类单 

元和口缘形状、壳顶与口缘的相对位 

置划分科级分类单元的可行性和有效 

性 , 但是不能接受把所有单板状软体动 

物化石通常被归入单板纲的做法 , 因为 

寒武纪早期一些单板状软体动物化石 

不一定符合单板纲的真实含义。文中 

还回顾了近二十年来建立的始单板纲 

( Eomonoplacophora) (Missarzhevsky , 

1989) , 太阳女神螺纲 ( Helcionelloida) , 

背壳肌纲 ( Tergomya) ( Peel , 1991a ,b) 

和似腹足纲 ( Paragast ropoda) (Linsley 

& Kier , 1984) 等纲级的新概念。还有 

一些早期软体动物专家将许多单板状 

( 包括帽状和螺旋状 ) 化石归入单板纲 

(Runnegar et al . ,1976 , 1985) , 而另有 

一些中青年软体动物专家继承传统理 

念 , 将它们归入了腹足纲 ( Parkhaev in 

Alexander et al . , 2001) 。钱逸和本格 

森将早期单壳类软体动物化石分成了 

五大形态类别 , 未确定科级以上分类单 

元名称 (Qian & Bengt son , 1989) 。总 

之 , 目前纲级分类单元界线不清 , 目级 

以下分类单元十分混乱 , 在没有全面清 

理早期单壳类软体动物百余个属和属 

级以上分类单元之前 , 是难以统一本文 

研究的早期单壳类软体动物 10 个属 

和属级以上分类系统。我们认为在确 

定属级以上分类系统及其与之密切相 

关的演化谱系关系时 , 不是利用理论前 

提 , 而是在不间断的剖面上对单壳类软 

75

体动物化石进行逐层采集并对其构造 

要素的详细研究 , 才能使得出的结论和 

提出的新分类系统发生错误的几率最 

小。文中还归纳和总结了本研究区玉 

尔吐斯组中上部单壳类软体动物群面 

貌的六大特点 , 其中二点最重要 :1) 该 

动物群与梅树村期微软体动物群的面 

貌有明显的差别 , 它缺失了梅树村期微 

软体动物群中最原始、最特征、最丰 

富的类群 , 如笠帽状的马哈螺类化石 

Maikhanella , Purella 等和螺旋状的始 

旋螺类化石 Archaeospira 等。但是该 

动物群面貌却与邻区的哈萨克斯坦 

Atdabanian 期的微软体动物和我国峡 

区西蒿坪动物群面貌接近 , 出现了许多 

相同或相似的属种 , 如 Shabaktiella , 

Mellopegma , Aldanella , Yochelcionella 

等。2) 该动物群共生有全球分布的相 

当于筇竹寺期的标准化石 , 如原牙形类 

Gapparodus , Amphigeisina , 

Hagionella 等 , 有口唇并有背腹分异和 

复杂口盖的软舌螺类 Microconus , 

Pachytheca 等 , 具有肉茎孔和铰合面的 

有铰腕足类和像 Obolus 那样的原始 

无铰腕足类 , 有各种形态类型的金臂虫 

Dabashanella , Liangshanella 等 , 还有 

可疑的三叶虫颊刺等。上述信息足以 

说明玉尔吐斯组中上部地层时代应属 

筇竹寺期而非梅树村期 , 从而解决了长 

期以来有关玉尔吐斯组时代归属的争 

议。玉尔吐斯组单壳类软体动物群的 

研究 , 再次证实了寒武纪生命大爆发期 

间 , 早期单壳类软体动物与小壳动物群 

一起经历了三次大发展和三次大绝灭 

事件。这在早期单壳类软体动物化石 

分类学、生物地层学和早期演化史上 

均有较高的科学价值。 

2010010237 

中东土耳其 Taurus 山 Pojetaia runnegari 

和 Fordilla 的首次记录及寒武 

纪双壳类评论 = First record of Pojetaia 

runnegari Jell, 1980 and Fordilla Barrande, 

1881 from the Middle East (Taurus 

Mountains, Turkey) and critical review 

of Cambrian bivalves. ( 英文 ). 

Elicki O; Gursu S. Palaeontologische 

Zeitschrift, 2009, 83(2): 267-291 

Cambrian bivalves from the Middle 

East are reported here for the first time. 

The majority of the new findings consists 

of Pojetaia runnegari Jell, 1980, 

but a few specimens of Fordilla sp. represent 

the first report of this genus from 

"Middle Cambrian" strata. Based on a 

compilation of the hitherto reported, but 

mostly revised Cambrian bivalves, the 

today widely accepted taxa are discussed. 

The genera Pojetaia Jell, 1980 and Fordilla 

Bassande, 1881 are critically 

evaluated, and three valid species are 

icluded in Pojetaia: P. runnegari Jell, P. 

sarhroensis Geyer and Streng, 1998, and 

-- with limitations -- P. ostseensis Hinz- 

Schallreuter, 1995. Fordilla also includes 

three species: F. troyensis, F. sibirica, 

and F. germanica. 

2010010238 

德国西北部下萨克森地区上白垩统赛 

诺曼阶上部箭石 Praeactinocamax 

plenus 及其在欧洲的分布模式 = The 

Upper Cretaceous belemnite Praeactinocamas 

plenus (Blainville, 1827) from 

Lower Saxony (Upper Cenomanian, 

northwest Germany) and its distribution 

pattern in Europe. ( 英文 ). Wiese F; 

Kostak M; Wood C J. Palaeontologische 

Zeitschrift, 2009, 83(2): 309-321 

Occurrences of Praeactinocamas plenus 

are documented and described for 

the first time on the basis of two in situ 

finds. The find horizon and its surrounding 

beds are re-evaluated in a sequence 

stratigraphical context. The distribution 

pattern of P. plenus suggests a preference 

for nearshore settings and a demersal 

mode of life. 

2010010239 

印度西北部卡奇地区渐新世和早中新 

世腹足类证实一次从西特提斯至印度 - 

太平洋的早期生物地理转移 = Oligocene 

and Early Miocene gastropods 

76

from Kutch (NW India) document an 

early biogeographic switch from Western 

Tethys to Indo-Pacific. ( 英文 ). 

Harzhauser M; Reuter M; Piller W E; 

Berning B; Kroh A; Mandic O. Palaeontologische 

Zeitschrift, 2009, 83(2): 333- 

372 

Shallow marine gastropod assemblages 

from Chattia, Aquitanian and 

Burdigalian sections in the Indian Kutch 

Basin are described. They provide insight 

into the composition and biogeographic 

relations of the gastropod 

assemblages at this junction between the 

Western Tethys and Proto-Indo-Pacific 

Ocean. For the fist time, an improved 

biostratigraphy allows a clear separation 

of the assemblages, especially for the 

hitherto undifferentiated Early Miocene 

faunas. In contrast, the Burdigalian assemblages 

witness a minor reappearance 

of Western Tethys taxa, 

suggesting the re-establishment of rather 

ineffective migration pathways prior to 

the final closure of the Tethyan Seaway. 

Cerithium bermotiense and Lyria (Indolyria) 

maniyaraensis are introduced as 

new species. 

2010010240 

论类三角蚌类 —— 兼论藏东的景星动 

物群 = Non-Marine Cretaceous Bivalvia 

Trigonioidoidea,With A Note On The 

Jingxing Fauna From Eastern Tibet,China. 

( 中文 ). 陈金华 . 古生物学 

报 , 2009, 48(4): 589-610 

论述亚洲白垩纪广泛分布的非海相 

双壳类类三角蚌类的分类、演化和起 

源 , 并讨论景星动物群的时代及 TPN 动 

物群的组合划分。认为类三角蚌类分 

5 个科 , 各科有独立的、相互平行的演 

化系列 ; 该类群最早形成于特提斯东部 

边缘地区的边缘隔离体环境 , 根据有关 

内部构造研究 , 其起源可能与海相三角 

蛤类有关。类三角蚌类经历过 3 个演 

化阶段 : 早期阶段 , 即爆发性成种阶段 , 

以景星动物群为代表 ; 藏东的生物地层 

研究表明 , 景星动物群时代是 

Tithonian—Berriasian 期 ; 中期阶段 , 即 

辐射阶段 , 以 TPN 动物群为代表 , 时代为 

Hauterivian—Turonian 期 , 或 

Valanginian—Turonioan 期 , 此阶段还可 

再分出 5 个组合 , 可用于地层划分和对 

比 ; 晚期阶段 , 即衰退阶段 , 以 

Pseudohyria 动物群为代表 , 时代为晚 

白垩世中 — 晚期。 

2010010241 

古生代海洋生态系统的头足类 = 

Cephalopods in the marine ecosystems 

of the Paleozoic. ( 英文 ). Barskov I S; 

Boiko M S; Konovalova V A; Leonova 

T B; Nikolaeva S V. Paleontological 

Journal, 2008, 42(11): 1167-1284 97 图 

版 . 

2010010242 

乌克兰上始新统 Mandrikovka 层腹足 

类研究现状以及 Conorbis 属一新种 

的描述 = The current state of study of 

the gastropods of the Mandrikovka Beds 

(Upper Eocene of Ukraine), with the description 

of a new species of Conorbis. 

( 英文 ). Amitrov O V. Paleontological 

Journal, 2008, 42(6): 581-584 2 图版 . 

Gastropod assemblages from the 

Mandrikovka Beds of two main localities 

(village of Mandrikovka and Chapli 

granite quarry) are compared. The 

Chapli Assemblage is much more diverse 

in the number of species, which 

are mostly small-sized, collected by 

washing in sieves; the use of this technique 

is the main reason for the apparently 

higher diversity of this assemblage. 

However, some large-sized species occur 

in one locality and are absent from 

the other. In particular, the new species 

Conorbis veselovi sp. nov. is only recorded 

in the Chapli quarry; it is here 

described and evidence for its assignment 

to the genus Conorbis is presented. 

2010010243 

77

二叠纪 Metalegoceratidae 科 ( 棱角菊 

石目 , 菊石亚纲 ) 的系统发生学 = 

Phylogeny of the Permian family 

Metalegoceratidae (Goniatitida, Ammonoidea). 

( 英文 ). Boiko M S; Leonova 

T B; Lin Mu. Paleontological Journal, 

2008, 42(6): 585-595 5 图版 . 

The paper discusses the evolution of 

the Permian ammonoid family Metalegoceratidae, 

and a new phylogenetic reconstruction 

is proposed. Three subfamilies 

are recognized in this family: 

Metalegoceratinae Plummer et Scott, 

1937; Pericycloceratinae Zhao et Zheng, 

1977; and Eothinitinae Ruzhencev, 1956. 

The genus Metalegoceras Schindewolf, 

1931 is subdivided into three subgenera: 

Metalegoceras s. str., Mesometalegoceras 

subgen. nov., and Artimetalegoceras 

subgen. nov. Five species of the 

endemic South Chinese metalegoceratids 

are described: Pseudometalegoceras 

shangraoense (Zhao et Zheng, 1977), P. 

liratum (Zhao et Zheng, 1977), P. platyventrum 

(Zhao et Zheng, 1977), P. spirale 

(Zhao et Zheng, 1977), and Pericycloceras 

costatum (Zhao et Zheng, 

1977). 

2010010244 

克里米亚山脉早白垩世 Bochianitidae 

科菊石代表 = Representatives of the 

family Bochianitidae (Ammonoidea) 

from the Lower Cretaceous of the Crimean 

Mountains. ( 英文 ). Arkadiev V V. 


468-478 6 图版 . 

The heteromorph ammonites of the 

family Bochianitidae from the Lower 

Cretaceous of the Crimean Mountains 

are revised. The validity of the genus 

Janenschites, separated from the genus 

Bochianites is confirmed. The species 

Bochianites neocomiensis (d’Orbigny), 

B. goubechensis Mandov, B. levis sp. 

nov. and B. crymensis sp. nov. are described 

from the Berriasian and the species 

Janenschites oosteri (Sarasin et 

Schöndelmayer) and J. incisus sp. nov. 

are described from the Lower Barremian. 

The family Bochianitidae first appeared 

at the beginning of the Berriasian in the 

southern regions (Africa and the Crimea), 

and spread to the northern regions 

of western Europe in the Valanginian- 

Hauterivian. 

2010010245 

显生宙双壳类分类多样性动态变化 = 

Dynamics of taxonomic diversity of bivalves 

in the Phanerozoic. ( 英文 ). Nevesskaya 

L A. Paleontological Journal, 

2008, 42(4): 335-342 2 图版 . 

Changes in the taxonomic composition 

of bivalves during the Phanerozoic 

are considered. Each period is characterized 

by a special set of taxa, in particular, 

families. Changes in taxonomic diversity, 

the episodes of maximum and minimum 

diversity are established and compared 

with those of other invertebrate groups. 

In general, the taxonomic diversity of 

bivalves gradually increased, except for 

a sharp decrease in the Early Triassic. 

2010010246 

极北区东部二叠纪似迭瓦蛤双壳类分 

类系统的新思考 = New ideas on the 

system of the Permian Inoceramus -like 

bivalves of the eastern Boreal zone. ( 英 

文 ). Biakov A S. Paleontological Journal, 

2008, 42(3): 232-242 2 图版 . 

New concepts of systematics and phylogeny 

of the Permian Inoceramus-like 

bivalve mollusks of the eastern part of 

the Boreal zone are discussed based on 

analysis of the group’s historical development. 

All taxa studied are referred to 

the family Kolymiidae Kusnezov, which 

is divided into two subfamilies, Kolymiinae 

and Atomodesmatinae. In the subfamily 

Kolymiinae, two new genera are 

described: Praekolymia with the type 

species P. archboldi sp. nov. and P. urbajtisae 

sp. nov., and Taimyrokolymia 

with the type species T. ustritskyi sp. 

nov. In the subfamily Atomodesmatinae, 

two new genera, Costatoaphanaia and 

78

Okhotodesma, are described. The development 

of the group is shown to be generally 

autochthonous with some invasions 

(genus Atomodesma and, probably, 

Trabeculatia) from extraboreal regions. 

2010010247 

伊朗侏罗纪双壳类新发现 = New bivalves 

from the Jurassic of Iran. ( 英文 ). 

Repin Yu S. Paleontological Journal, 

2008, 42(3): 243-250 2 图版 . 

Three new subgenera, Gervillaria 

(Platygervillaria), Isognomon (Iranognomon), 

and Mytilaster (Persiaster), and 

seven new species, Gervillaria (Platygervillaria) 

alifera, Isognomon (Iranognomon) 

arkelli, Inoperna (Inoperna) 

striata, Mytilaster (Persiaster) ancestralis, 

Astarte persipulla, Orthotrigonia 

fazli, and Gissaromya abramovi, from 

the Jurassic of Iran are described. 

2010010248 

俄罗斯地台 Ryazanian 阶特提斯型菊 

石属 Riasanites Spath = Ammonites of 

Tethyan origin from the Ryazanian of 

the Russian platform: Genus Riasanites 

spath. ( 英文 ). Mitta V V. Paleontological 

Journal, 2008, 42(3): 251-259 3 图 

版 . 

The genus Riasanites, represented in 

Central Russia by two successive dimorphic 

species, is revised. R. swistowianus 

is found in the basal beds of the 

rjasanensis Zone. Its descendant R. 

rjasanensis is also found in this zone, 

but upwards in the section, including the 

beds with Surites spasskensis and Externiceras 

solowaticum. The representatives 

of Riasanites from the Crimea and 

Northern Caucasus are assigned to two 

species, R. crassicostatus and R. maikopensis, 

respectively. It is suggested that 

Riasanites evolved from Sub- 

Mediterranean Himalayatidae, which 

migrated from the Western Tethys via 

the Polish Passage into the Central Russian 

Basin, and from there to Mangyshlak, 

the Northern Caucasus, and the 

Crimea. 

2010010249 

俄罗斯地台中侏罗世巴通期 - 卡洛夫期 

菊石属 Kepplerites 

( Kosmoceratidae , 菊石亚纲 ) = 

The genus Kepplerites Neumary et Uhlig 

(Kosmoceratidae, Ammonoidea) in 

the Bathonian-Callovian beds (Middle 

Jurassic) of the Russian Platform. ( 英文 ). 

Mitta V V. Paleontological Journal, 

2008, 42(1): 5-14 5 图版 . 

The succession of early species of the 

genus Kepplerites is established in the 

Upper Bathonian-Lower Callovian beds 

of Central Russia and compared with the 

ammonoid succession of East Greenland 

and Western Europe. Late Bathonian 

members of the genus Kepplerites from 

the Middle Volga Region are generally 

similar, though not identical to those 

from Greenland, whereas the Early 

Callovian Kepplerites species and their 

immediate Bathonian ancestors are represented 

by species common to all three 

regions. The analysis of the ammonoid 

distribution suggests a connection between 

the East Greenland and Central 

Russian marine basins in the Early and 

Middle Bathonian and in the Early Callovian, 

and their short-term isolation in 

the Late Bathonian. A new species, 

Kepplerites (Kepplerites) aigii sp. nov., 

is described from the Upper Bathonian 

(keuppi Zone) of the Alatyr River basin 

(Middle Volga Region). 

2010010250 

瑞典中部上奥陶统 Boda 灰岩中披甲 

环节动物和软体动物 = Armoured annelids 

and molluscs from the Upper Ordovician 

Boda Limestone, central Sweden. 

( 英文 ). Hogstrom A E S; Ebbestad 

J O R; Suzuki Y. GFF, 2009, 131(3): 

245-252 

Sclerites of machaeridians (Annelida) 

and polyplacophorans (Mollusca) from 

the Upper Ordovician (Katian- 

79

Hirnantian) Boda Limestone of the Siljan 

district, central Sweden are described 

for the first time. Four taxa of 

machaeridians were found, but with one 

exception they are either known from a 

single isolated sclerite or only one type 

of sclerite. The largest taxon is represented 

by an inner modified sclerite of 

Plumulites sp. A from Osmundsberget 

Quarry. The complete scleritome is estimated 

to have reached a length of 12- 

15cm. A more diverse material allows 

the description of Plumulites eueides sp. 

nov. from Kallholn Quarry. Within 

smaller cavities in Solberga Quarry 

minute sclerites of two taxa were found; 

Lepidocoleus sp., and Turrilepas sp. The 

latter record represents the third known 

Ordovician occurrence and the youngest 

from that period. Association with minute 

blind trilobites and concentrations of 

tiny articulated ostracodes suggest that 

these small cavities represented cryptic 

habitats. Two polyplacophoran sclerites 

are also described: one intermediate 

sclerite of Chelodes sp. A from Jutjarn 

Quarry, with only the outer surface exposed, 

and one intermediate sclerite of 

Spicuchelodes? sp. from Kallholn 

Quarry, with only the inner surface exposed. 

These represent rare examples of 

Ordovician chitons recorded from outside 

Laurentian terranes. 

2010010251 

华南十万大山盆地中侏罗世珠蚌类 

( 非海相双壳纲 )—— 以 Cuneopsis 

Simpson 为重点 = Middle Jurassic unionids 

(non-marine Bivalvia) from the 

Shiwandashan Basin, southern China, 

with special emphasis on Cuneopsis 

Simpson. ( 英文 ). Pan Y H; Sha J G. 

GFF, 2009, 131(1-2): 183-194 10 图版 . 

Articulated non-marine unionid bivalves 

from red beds of the Middle Jurassic 

lower member of the Nadang 

Formation of Banyou, Shiwandashan 

Basin, Guangxi province, southern 

China, comprise five morphotypes of 

Cuneopsis johannisboehmi (Frech). 

They have been recognised on the basis 

of a population study by their: (1) transversely 

elliptical shape, with subparallel 

and substraight dorsal and ventral margins, 

(2) elongated cuneiform shape, 

with a shallow concavity near the posteroventral 

margin, (3) elongated cuneiform 

shape, with a sharp posterior end, 

but without a clear posteroventral concavity, 

(4) sub-triangular shape, with a 

sharply pointed posterior and a relatively 

rounded anterior margin and gently convex 

ventral margin and (5) suboval 

shape, with a convex ventral margin. 

The analysis demonstrates that these unionids 

are morphologically variable and 

leads to revision of at least 15 species of 

unionids, which are merged into Cuneopsis 

johannisboehmi. In the Shiwandashan 

Basin, the unionids are preserved 

in two types of shell assemblage (2D 

and 3D). Morphological features such as 

relatively thick shells, medium to large 

inflation, a large H/L ratio (more than 

0.5) and anteriorly placed umbones all 

indicate a habitat of large rivers for this 

unionid. 

2010010252 

西班牙东北部上侏罗统基末利阶下部 

Platynota 时间带地层的对比潜力 = 

Correlation potential of the Upper Jurassic 

(lower Kimmeridgian) Platynota 

Chronozone deposits in northeastern 

Spain. ( 英文 ). Moliner L; Oloriz F. 

GFF, 2009, 131(1-2): 205-213 5 图版 . 

Ammonite biostratigraphy and its correlation 

potential are evaluated for the 

lower Kimmeridgian, Platynota Chronozone, 

in the eastern Iberian Range, E-NE 

Spain. The presence of the Orthosphinctes, 

Ardescia desmoides and Schneidia 

guilherandense subzones has been confirmed. 

Four formal ammonite "intrasubzone 

biodivisions" (i.e. so-called horizons 

or biohorizons) are recognised, 

one of them defined for the first time - 

the Olorizia olorizi "intra-subzone biodivision". 

Based on the discovery of 

80

new ammonite assemblages, the biostratigraphic 

scheme proposed at the 

biozone level is considered to have 

strong correlation potential for successions 

deposited in Tethyan epicontinental 

and oceanic fringe environments. The 

potential for correlation at the intra-zone 

level is higher with respect to epicontinental 

than oceanic fringe deposits, but 

precise correlation at the subzone and 

"intra-subzone biodivision" levels between 

the eastern Iberian Range and SE 

France remains difficult. An updated 

subdivision of the Sutneria platynota 

Biozone is interpreted for oceanic fringe 

sections. Additionally, the ammonite 

genus Olorizia Moliner is erected and 

briefly discussed. 

2010010253 

Didacna 属 ( 双壳类 : 鸟蛤科 ) 的历 

史 = History of the genus Didacna (Bivalvia: 

Cardiidae). ( 英文 ). Nevesskaja L 

A. Paleontological Journal, 2007, 41(9): 

861-949 25 图版 . 

The history of the Quaternary genus 

Didacna, which is endemic to the Ponto- 

Caspian Sea, is discussed. Quaternary 

stratigraphy of this region and Didacna 

assemblages recorded in the Neopleistocene 

sequence are characterized. The 

development of this genus against the 

background of the Ponto-Caspian history 

is reconstructed; the replacement of 

species and associations of Didacna, the 

character of speciation, and examples of 

homeomorphism are discussed. Seventyseven 

species of this genus, which appeared 

over slightly more than 600 thousand 

years, are described; this indicates 

an extremely intense speciation in Pleistocene 

brackish-water basins, which 

were inhabited by only five bivalve genera 

belonging to two families. 

2010010254 

北高加索埃姆斯期菊石的发现 = Discovery 

of Emsian Ammonoids in the 

Northern Caucasus. ( 英文 ). Nikolaeva1 

S V. Paleontological Journal, 2007, 

41(5): 506-512 4 图版 . 

The Lower Devonian beds of the Bechasyn 

zone of the Northern Caucasus 

(Kabardino-Balkaria, middle reaches of 

the Malka River) contain an assemblage 

of the Early Emsian Ammonoids including 

the characteristic genera Erbenoceras, 

Mimosphinctes, Teicherticeras, 

Mimagoniatites, and Gyroceratites. The 

taxonomic composition of the assemblage 

is similar to that of synchronous 

assemblages of Turkey and Tian Shan, 

differing from the assemblage of Morocco 

by the presence of Teicherticeras. 

Different approaches to the taxonomy of 

the family Teicherticeratidae are discussed 

and it is concluded that it is in 

need of serious revision. A new species 

Teicherticeras lakhranense is described. 

2010010255 

上 Don 盆地更新世腹足类新种 = New 

gastropod species from the Pleistocene 

of the Don basin. ( 英文 ). Kondrashov P 

E. Paleontological Journal, 2007, 41(5): 

513-519 2 图版 . 

Two new species of fossil freshwater 

gastropods, Borysthenia intermedia sp. 

nov. and Tanousia krasnenkovi sp. nov., 

from the Tiraspol deposits of the Middle 

Pleistocene of the Oka-Don Plain are 

described. Parafossarulus priscillae (Girotti, 

1972), Viviparus diluvianus (Künth, 

1865), and Lithoglyphus jahni Urbasnski, 

1975 are reported from Russia for the 

first time. The status of some problematic 

species of freshwater gastropods 

from the Middle Pleistocene of the region 

studied is discussed. The chronological 

and environmental significance 

of all gastropods studied is given. 

2010010256 

乌克兰始新世晚期的 Triphorids( 腹 

足纲 : 三口螺科 ) = Triphorids (Gastropoda: 

Triphoridae) from the Upper 

Eocene of Ukraine. ( 英文 ). Amitrov O 

81

V; Zhegallo E A. Paleontological Journal, 

2007, 41(4): 370-381 2 图版 . 

The history of the study of triphorids 

and the principles of their systematics 

are discussed. The specific and generic 

identifications of five forms from the 

Mandrikovka beds of the Dnieper- 

Donets depression are considered. Subviriola 

vermiculoides gen. et sp. nov. is 

described. It seems plausible that “Triforis” 

vermicularis Koenen, 1891 from 

the Latdorfian of Germany also belongs 

to this new genus. 

2010010257 

Clathrobaculus Cossmann ( 腹足纲 , 

Mathildidae) 的系统分类和演化 = 

Systematics and evolution of the genus 

Clathrobaculus Cossmann, 1912 (Gastropoda, 

Mathildidae). ( 英文 ). Guzhov 


41(4): 382-394 5 图版 . 

The morphology and ontogeny of Jurassic 

gastropods those have been included 

in the genera Clathrobaculus 

Cossmann, 1912 and Gordenella 

Gründel, 1990 are discussed. Based on 

the ontogenetic research of their shells, 

several types of ontogeny are established 

in the species of these genera. The suggestion 

is made that the genus Gordenella 

should be considered as a junior 

synonym of Clathrobaculus within the 

family Mathildidae. The protoconchs of 

Clathrobaculus species are studied to 

reveal their morphological variability 

and a number of distinguishing characters 

in which they differ from the protoconchs 

of other mathildid genera. Four 

species of Clathrobaculus, of which two 

are new (C. medidilatatus and C. inconstantiplicatus), 

are described from the 

Jurassic deposits of the European part of 

Russia. The composition of C. 

fahrenkohli (Rouillier, 1846) and C. 

krantzi (Rouillier, 1849) is emended, 

and the protoconchs of these species and 

of the species C. inconstantiplicatus are 

described for the first time. 

2010010258 

寒武纪腹足类壳体手征和 Aldanella 

属的左旋成员 = Shell chirality in Cambrian 

gastropods and sinistral members 

of the genus Aldanella Vostokova, 1962. 

( 英文 ). Parkhaev P Yu. Paleontological 

Journal, 2007, 41(3): 233-240 3 图版 . 

Shell chirality among Cambrian gastropods 

is discussed. It is demonstrated 

that the earliest members of the class 

include chiral aberrations with abnormal 

opposite coiling of the shell. It is assumed 

that, in Cambrian gastropods, 

speciation could have occurred by mutation 

in the locus determining the chirality, 

as is proposed for extant gastropods. 

In contrast to modern gastropods, the 

existence of chiral morphs within single 

species has not been recorded in Cambrian 

mollusks, whereas the presence of 

chiral twin species is possible. The systematic 

position of sinistral representatives 

of the genus Aldanella Vostokova, 

1962 is considered. Aldanella golubevi 

sp. nov. with sinistral shell is described 

from the base of the Tommotian Stage 

of the Anabar Region. Aberrant sinistral 

specimens of the normally dextral species 

Aldanella utchurica Missarzhevsky 

in Rozanov et al., 1969 and Pelagiella 

adunca Missarzhevsky in Rozanov et al., 

1969 are figured. 

2010010259 

西伯利亚北部卡洛夫期晚期 — 牛津期 

早期 cardioceratids 类菊石一新属 = A 

new genus of cardioceratids (Ammonoidea) 

from the Upper Callovian-Lower 

Oxfordian of northern Siberia. ( 英文 ). 

Stolyarova L R. Paleontological Journal, 

2007, 41(3): 241-247 6 图版 . 

A new genus, Anabariceras, and two 

new species, A. meledinae and A. aspectabile, 

are described from the Upper 

Callovian-Lower Oxfordian boundary 

beds from the Anabar River basin. 

Based on analysis of the ontogenetic development 

of major characters (suture, 

82

shell shape, and ornamentation), the affinity 

of this genus to the subfamily 

Quenstedtoceratinae is substantiated. 

2010010260 

华南湖南二叠纪菊石 Guiyangoceras 

的异常大型标本 = Unusually large 

specimens of the Permian ammonoid 

Guiyangoceras from Hunan, South 

China. ( 英文 ). Zhou Zuren. Paleontological 

Journal, 2007, 41(2): 123- 

127 5 图版 . 

Exceptionally large specimens of the 

Permian genus Guiyangoceras are discovered 

from the Permian (Roadian) of 

south Hunan, South China. The giant 

size, mature stage of the sutural elements, 

and shape variation in respect to 

ontogenetic development extend the 

definition of this endemic genus. 

2010010261 

西伯利亚中部和北部贝利阿斯阶 

kochi 带菊石属 Boreophylloceras 

Alekseev et Repin 的一新种 = A new 

species of the genus Boreophylloceras 

Alekseev et Repin, 1998 (Ammonitida) 

from the Berriasian kochi zone of northcentral 

Siberia. ( 英文 ). Igolnikov A E. 


128-131 3 图版 . 

Study of the shells of phylloceratids 

from the kochi Zone (Berriasian) of 

north-central Siberia (Boyarka River, 

basin of the Kheta River) allowed their 

assignment to the genus Boreophylloceras 

Alekseev et Repin, 1998. A new 

species B. densicostatum is described. 

2010010262 

泛里海地区古近纪腹足类 Scalaspira 

= Scalaspira (Gastropoda) from the Paleogene 

of the Transcaspian Region. ( 英 

文 ). Amitrov O V; Zhegallo E A. Paleontological 

Journal, 2007, 41(1): 15- 

27 2 图版 . 

The composition and distribution of 

the species of the genus Scalaspira Conrad, 

1862 in the Eocene-Oligocene of 

western Kazakhstan are revised. Following 

Tembrock we assign this genus to 

Buccinidae and synonymize Aquilofusus 

Kautsky, 1925 with it. The stratigraphic 

interval studied contains at least eight 

species. Three species are new: S. 

alexeevi (Middle? and Upper Eocene, 

Chegan Formation), S. korobkovi, and S. 

kumsuatensis (Upper Oligocene, Karatomak 

Beds). 

2010010263 

二叠纪 Spirolegoceratidae 科 ( 棱角 

菊石目 , 菊石亚纲 ) 的演化 = Evolution 

of the Permian family Spirolegoceratidae 

(Goniatitida, Ammonoidea). 

( 英文 ). Leonova T B; Shilovsky O P. 


28-38 4 图版 . 

The evolution of the Permian ammonoid 

family Spirolegoceratidae is 

discussed and a new phylogenetic reconstruction 

is proposed based on new data. 

Two subfamilies are recognized within 

the family Spirolegoceratidae: Spirolegoceratinae 

Nassichuk and Sverdrupitinae 

subfam. nov. A new genus, 

Archboldiceras, is proposed to accommodate 

the Australian species Uraloceras 

lobulatum and U. whitehousei. 

Species of the genus Sverdrupites Nassichuk, 

1970 are described based on new 

material from the Volga-Urals Region. 

The new species S. bogoslovskayae from 

the Gerkinskaya Formation of Novaya 

Zemlya previously identified by M.F. 

Bogoslovskaya as S. amundseni is described. 

2010010264 

泥盆纪 Palliocerida 新发现 ( 头足 

纲 ,Astrovioidea) = New Devonian 

Palliocerida (Cephalopoda, Astrovioidea). 

( 英文 ). Zhuravleva F A. Paleontological 

Journal, 2006, 40(6): 617- 

625 4 图版 . 

Eight new species of Ostreioceratidae 

are described from the Lower and Upper 

83

Devonian of Novaya Zemlya, Lower 

Devonian of the Pechora River basin, 

North Ural Mountains, and the Zeravshan 

Range: Ostreioceras admotum, 

O. simile, O. abruptum, O. sobolevi, 

Plagiostomoceras kuzmini, P. adumbratum, 

P.? acerbum, and P. vinogradovi. 

A new family Bogoslovskyidae is established 

in the order Palliocerida. 

2010010265 

俄罗斯欧洲部分中部早、中卡洛夫期 

腹足类组合 = Lower and Middle Callovian 

gastropod assemblages from central 

European Russia. ( 英文 ). Guzhov A 


500-506 4 图版 . 

Two gastropod assemblages from the 

Lower Callovian of the Kostroma Region 

and the Middle Callovian of the 

Yaroslavl’ Region are studied and compared 

with synchronous assemblages of 

the Kostroma, Moscow, Bryansk, and 

Kursk regions. It is suggested that gastropods 

from the Yaroslavl’ and Kostroma 

regions inhabited colder water basins 

than gastropods from more southern 

regions. A new genus and species Znamenkiella 

ovalis gen. et sp. nov. (family 

Pseudomelaniidae) are described from 

the Lower Callovian of the Kostroma 

Region. 

2010010266 

双壳类软体动物行为 - 营养群及其在显 

生宙的分布 = Ethological-trophic 

groups of bivalve mollusks and their distribution 

in the Phanerozoic. ( 英文 ). 

Nevesskaja L A. Paleontological Journal, 

2006, 40(4): 375-390 3 图版 . 

Based on their adaptations to substrates, 

degree of mobility, and feeding 

modes, bivalve mollusks are subdivided 

into 30 ethological-trophic groups. This 

paper presents an account of their morphological 

characteristics, distribution in 

the Phanerozoic, and taxonomic changes 

through time. 

2010010267 

莫斯科台坳北部 Kulogory 组二叠纪 

腹足类 = Permian gastropods from the 

Kulogory Formation of the northern 

Moscow Syneclise. ( 英文 ). Mazaev A V. 


391-403 4 图版 . 

Permian gastropods from the Kulogory 

Formation (Sakmarian) were studied 

based on the author’s material and 

the collection of Yakowlew (Central Research 

Geological Prospecting Museum 

(TsNIGR Museum), St. Petersburg). 

Lectotypes for Arribazona tschernyschewi 

(Yakowlew, 1899) and Microdoma 

kulogorae (Yakowlew, 1899) 

were designated. Six species are described; 

four of them are new and two 

are assigned to the new genera (Biarmeaspira 

verideclinata gen. et sp. nov., 

Globodoma yakowlewi gen. et sp. nov., 

Glabrocingulum (Glabrocingulum) 

stankovskyi sp. nov., and Euconospira? 

pinegensis sp. nov.). The high degree of 

polymorphism in the dominant species 

of uniform assemblages is probably the 

result of their development in “undersaturated” 

paleocommunities of closed 

lagoons with gradually increasing concentration 

of sulfate ions. 

2010010268 

副特提斯东部内陆盆地鸥螺科形态发 

生学 = Morphogenesis of Rissoidae in 

the inland basins of the Eastern 

Paratethys. ( 英文 ). Iljina L B. Paleontological 

Journal, 2006, 40(4): 404- 

414 3 图版 . 

Miocene rissoids from the heterochronous 

low-salinity seas of the Eastern 

Paratethys (Early Chokrakian, Karaganian, 

Late Konkian, Early Sarmatian, 

and Early Maeotian) were revised. The 

polyphyletic genus Mohrensternia is 

subdivided into several generic and subgeneric 

taxa. The new genus Zhgentia 

and the new subgenera Rissoa (Turboellina), 

R. (Pseudoturboellina), and R. 

(Maeotia) are established. 

84

2010010269 

奥地利 Calcareous Alps 北部欧洲最 

老的侏罗纪菊石及其全球意义 = On 

the oldest Jurassic ammonites of Europe 

(Northern Calcareous Alps, Austria) and 

their global significance. ( 英文 ). Hillebrandt 

A V; Krystyn L. Neues Jahrbuch 

fur Geologie u. Palaontologie / Abhandlungen, 

2009, 253(2-3): 163-195 

The earliest ammonite species of Jurassic 

type, Psiloceras spelae, was unknown 

till 1998. This species bridges the 

long gap between the latest Triassic and 

the earliest Jurassic ammonoids. It was 

discovered in North America, then in 

South America and finally in Europe. 

The species is proposed as boundary 

marker for the base of the Jurassic system. 

It is known in two forms which are 

regarded as subspecies. 

2010010270 

腹足类 Aldanella 属 (Archaeobranchia, 

Pelagielliformes) 形态新资料 = New 

data on the morphology of ancient gastropods 

of the genus Aldanella 

Vostokova, 1962 (Archaeobranchia, 

Pelagielliformes). ( 英文 ). Parkhaev P 

Yu. Paleontological Journal, 2006, 

40(3): 244-252 5 图版 . 

The position of attachment of the 

shell muscle is discovered in the columellar 

area of the shell of the Early 

Cambrian univalved genus Aldanella 

(family Aldanellidae, order Pelagielliformes, 

subclass Archaeobranchia), the 

structure of its protoconch is described, 

and the presence of series of septa in the 

embryonic part of their shell is confirmed. 

These new features confidently 

support the position of the family 

Aldanellidae within the gastropod class 

and allow them to be considered ancestral 

to younger gastropod lineages with a 

turbospiral shell. 

2010010271 

显生宙正常海相双壳类软体动物的分 

类多样化 = Taxonomic diversification 

of normal-marine bivalve mollusks in 

the Phanerozoic. ( 英文 ). Dmitriev V Yu; 

Nevesskaja L A. Paleontological Journal, 

2006, 40(3): 253-260 6 图版 . 

The dynamics of the taxonomic diversification 

of normal-marine bivalve mollusks 

and that of the entire fossil marine 

skeletal fauna are compared. A major 

Early Permian turnover has been revealed. 

The changes in the proportions 

of the bivalve mollusks to the entire marine 

fauna during the Phanerozoic are 

studied. 

2010010272 

亚洲东北部卡尼阶 Apartidae 科菊石 

的首次发现 = The first discovery of 

Apartidae (Ammonoidea) in the Carnian 

of northeastern Asia. ( 英文 ). Konstantinov 

A G. Paleontological Journal, 2006, 

40(3): 261-265 4 图版 . 

A new genus Siberioklipsteinia (with 

the type species S. dagysi sp. nov.) and a 

new species Arctoarpadites nelgesensis 

are described from the Carnian of the 

Kharaulakh Range and Yana Upland 

(eastern Yakutia). The new data allow 

refinement of the taxonomy of Carnian 

ammonoids of northeastern Asia and 

emendation of some details of their geographical 

differentiation. The new ammonoid 

taxa belong to the family Arpaditidae, 

which was not previously recorded 

from the eastern Boreal Realm. 

2010010273 

伏尔加河地区 Ulyanovsk 一带欧特里 

夫期腹足类软体动物 :2. Khetella 属 

和 Cretadmete 新属 = Gastropod mollusks 

from the Hauterivian of Ulyanovsk 

(Volga Region): 2. Genera Khetella 

Beisel, 1977 and Cretadmete gen. nov.. 

( 英文 ). Blagovetshenskiy I V; Shumilkin 

I A. Paleontological Journal, 

2006, 40(2): 143-149 2 图版 . 

85

The diagnosis of the genus Khetella 

Beisel, 1977 is emended, and a new genus, 

Cretadmete, is described. Two new 

species belonging to these genera, K. 

trautscholdi and C. neglecta, are established 

from the Upper Hauterivian of 

Ulyanovsk (Volga Region). 

2010010274 

头足类宏系统 : 历史回顾、研究现状 

和未解决的问题 :3. 杆石亚纲和菊石 

亚纲的分类 = The cephalopod macrosystem: 

A historical review, the present 

state of knowledge, and unsolved problems: 

3. Classification of Bactritoidea 

and Ammonoidea. ( 英文 ). Shevyrev A 

A. Paleontological Journal, 2006, 40(2): 

150-161 

A new classification is proposed in 

which Bactritoidea and Ammonoidea 

are considered as subclasses. The subclass 

Bactritoidea includes a single order, 

Bactritida. The subclass Ammonoidea 

includes ten orders: Anarcestida (suborders 

Agoniatitina, Auguritina, Anarcestina, 

Gephurocerina, Timanocerina, and 

Prolecanitina), Tornocerida, Goniatitida 

(with suborders Goniatitina and 

Cyclolobina), Praeglyphiocerida, Clymeniida 

(with suborders Gonioclymeniina 

and Clymeniina), Medlicottiida, 

Ceratitida (with suborders Paraceltitina, 

Otocerina, Meekocerina, Sagecerina, 

Ptychitina, Ceratitina, Pinacocerina, 

Megaphyllitina, Arcestina, and Lobitina), 

Phyllocerida, Lytocerida (with suborders 

Lytocerina and Turrilitina), and Ammonitida 

(with suborders Psilocerina, 

Haplocerina, Stephanocerina, Cardiocerina, 

and Ancylocerina). 

2010010275 

Auricullina 属以及寒武纪 

helcionelloid 类软体动物的壳孔 = On 

the genus Auricullina Vassiljeva, 1998 

and shell pores of the Cambrian helcionelloid 

mollusks. ( 英文 ). Parkhaev P 

Yu. Paleontological Journal, 2006, 

40(1): 20-33 9 图版 . 

The genus Auricullina Vassiljeva, 

1998 and its type species A. papulosa 

Vassiljeva, 1998 are redescribed based 

on new well-preserved material, which 

allows me to revise the generic diagnosis 

and greatly add to the morphological 

characterization of the type species. A 

new species, A. granulosa sp. nov., is 

described from the Botomian of Australia. 

The synonymy of the taxa is improved. 

The morphology and function of 

shell pores in Cambrian univalved mollusks 

are discussed. 

2010010276 

伏尔加河地区 Ulyanovsk 一带欧特里 

夫期腹足类软体动物 :1. Aporrhaidae 

科 = Gastropod mollusks from the 

Hauterivian of Ulyanovsk (Volga Region): 

1. Family Aporrhaidae. ( 英文 ). 

Blagovetshenskiy I V; Shumilkin I A. 


34-45 6 图版 . 

Data on the detailed stratigraphic 

range of eight species of gastropod mollusks 

from the Upper Hauterivian of 

Ulyanovsk (Volga Region) are presented. 

A new genus, Trilemma, is established 

within the family Aporrhaidae. Two new 

species of this genus, T. russiense sp. 

nov. and T. striatocarinatum (Sinzow, 

1880), are described. 

2010010277 

头足类宏系统 : 历史回顾、研究现状 

和未解决的问题 :2. 鹦鹉螺类的分类 

= The cephalopod macrosystem: A historical 

review, the present state of 

knowledge, and unsolved problems: 2. 

Classification of nautiloid cephalopods. 

( 英文 ). Shevyrev A A. Paleontological 

Journal, 2006, 40(1): 46-54 

Major classifications of nautiloid 

cephalopods are critically reviewed. It is 

suggested that this cephalopod group is 

subdivided into 5 subclasses and 17 orders: 

Ellesmeroceratoidea (including the 

orders Plectronocerida, Protactinocerida, 

Yanhecerida, and Ellesmerocerida), En- 

86

doceratoidea (including the orders Endocerida 

and Intejocerida), Actinoceratoidea 

(including the order Actinocerida), 

Nautiloidea (with the orders Basslerocerida, 

Tarphycerida, Lituitida, Discosorida, 

Oncocerida, and Nautilida), 

and Orthoceratoidea (including the orders 

Orthocerida, Ascocerida, Dissidocerida, 

and Bajkalocerida). The above 

orders are briefly described. 

节肢动物 

2010010278 

中国二叠纪的一种吮食 

Noeggerathialean 花粉的昆虫新属种 

Circulipuncturites discinisporis Labandeira, 

Wang, Zhang, Bek et Pfefferkorn 

( 曾归入中华盘穗孢 ) = 

Permian Circulipuncturites discinisporis 

Labandeira, Wang, Zhang, Bek et Pfefferkorn 

gen. et spec. nov. (formerly 

Discinispora) from China, an ichnotaxon 

of a punch-and-sucking insect on Noeggerathialean 

spores. ( 英文 ). Wang J; 

Labandeira C C; Zhang G F; Bek J; 

Pfefferkorn H W. Review of Palaeobotany 


156(3-4): 277-282 2 图版 . 

The generic name Discinispora Wang, 

Zhang, Bek et Pfefferkorn was originally 

created for spores with an operculum-like 

structure that were found in a 

permineralized Noeggerathialean cone. 

Subsequently it was observed that up to 

three round and smooth openings can 

occur in different positions on the surface 

of a single spore. In light of the new 

observations, the previous interpretation 

as an operculum cannot be sustained. An 

interpretation implicating insect punchand-sucking 

activity was suggested for 

these round structures. This new interpretation 

makes it necessary to withdraw 

the original diagnosis and the taxon. The 

insect-inflicted damage now is assigned 

to the ichnotaxon Circulipuncturites 

discinisporis Labandeira, Wang, Zhang, 

Bek et Pfefferkorn under the rules of the 

ICZN, rather than those of the ICBN 

that typified the insect-damaged hostplant 

spore. 

2010010279 

埃及东西奈 Gabal Arif El-Naga 背斜 

森诺曼阶 - 麦斯里希特阶的介形类 = 

Cenomanian - Maastrichtian ostracods 

from Gabal Arif El-Naga anticline, 

Eastern Sinai, Egypt. ( 英文 ). El-Nady H; 

Abu-Zied R; Ayyad S. Revue de Paleobiologie, 

2008, 27(2): 533-573 

135 surface samples are collected from the 

Cenomanian-Maastrichtian succession of Gebel 

Arif El-Naga anticline, eastern Sinai 

(Egypt) and examined for their ostracodal 

content. 76 ostracod species and subspecies 

were recognized and discussed. The lithological 

characteristics of this succession were also 

subdivided into five formations, from base to 

top as follow : Halal Formation (Cenomanian), 

Abu Qada, Wata Formations (Turonian), 

Themed Formation (Coniacian-Santonian) and 

Sudr Formation (Campanian-Maastrichtian). 

Most of the recorded species in these rock 

units were correlated with their counterparts in 

the Levant, Middle East and North Africa and 

some with West Africa, Europe and South 

America suggesting biogeographic relationships 

between these regions across the Cretaceous 

Trans-Saharan Seaway. The stratigraphic 

range of these ostracods pointed out to 

the occurrence of 10 local ostracod assemblage 

zones in the present study. These zones 

were correlated with the planktonic foraminiferal 

zones of the same area and ranges from 

base to top as follow : Metacytheropteron- 

Cytherella-Neocythere Assemblage zone 

(early Cenomanian), Dolocytheridea atlasica– 

Neocyprides vandenboldi Assemblage zone 

(late Cenomanian), Xestoleberis derorimensis- 

Oertliella dextrospinata Assemblage zone 

(early Turonian), Cythereis-Asciocythere- 

Ovocytheridea Assemblage zone (late Turonian), 

Cythereis oertlii-Phyrocythere lata 

Assemblage zone (Coniacian), Cythereis cretaria 

cretaria-Limburgina miarensis Assemblage 

zone (Santonian), Leguminocythereis 

dorsocostatus-Protobuntonia campania Assemblage 

zone (early Campanian), Brachycythere 

beershevaensis-Spinoleberis megiddoensis 

Assemblage zone (late Campanian), 

Rushdisaidina supracretacea Zone Assemblage 

zone (early Maastrichtian) and Cristaeleberis 

fornicata Assemblage zone (late Maastrichtian). 

A correlation between the recorded 

87

assemblages and their regional and worldwide 

equivalents has been achieved. 

2010010280 

埃及东沙漠西北部 Qattamiya 地区中 

始新世的介形类 : 系统学、生物地层 

学及古生物地理学研究 = Middle Eocene 

ostracodes of the Qattamiya area, 

northwest Eastern Desert, Egypt: Systematics, 

biostratigraphy and paleobiogeography. 

( 英文 ). Shahin A; El Halaby 

O; El Baz S. Revue de Paleobiologie, 

2008, 27(1): 123-157 

The Middle Eocene Observatory and 

Qurn Formations that are exposed in the 

Qattamiya area, northwestern part of the 

Eastern Desert are carefully studied for 

their ostracod content. The detailed investigation 

of the ostracod content has 

led to the recognition of 51 species and 

subspecies belonging to 31 genera and 

12 families. Their vertical distribution in 

the three studied sections enables the 

detection of three local assemblage 

zones. The paleoecology of each assemblage 

zone is also discussed. Both the 

Observatory and Qurn Formations were 

deposited in shallow reefal carbonate 

platform of less than 100 m depth. Some 

intervals were deposited in lagoonal 

tropical and hypersaline conditions with 

occasionally relatively deeper oscillation 

within the back reef area. The paleobiogeographic 

distribution of the recorded 

ostracodes reveals that there was a direct 

connection between the Southern 

Tethyan Real and the Western Europe 

Tethyan Real through which the migration 

of the ostracodes had occurred. 

2010010281 

埃及西奈中西部麦斯里希特期 - 早始新 

世的介形类 : 分类学、生物地层学、 

古生态学及古生物地理学研究 = 

Maastrichtian-Early Eocene ostracodes 

from west-central Sinai, Egypt - taxonomy, 

biostratigraphy, paleoecology and 

paleobiogeography. ( 英文 ). Morsi A-M; 

Faris M; Zalat A-E; Salem R. Revue de 

Paleobiologie, 2008, 27(1): 159-189 

Detailed study of ostracodes from the 

Maastrichtian-Early Eocene sections at Gebel 

Nukhul and Wadi Feiran in west-central Sinai 

yielded 38 ostracode species and subspecies 

belonging to 26 genera. Biostratigraphically, 

they are divisible into five kinds : taxa restricted 

to the Maastrichtian, taxa crossing the 

K/P boundary, taxa restricted to the Paleocene, 

taxa crossing the P/E boundary, and taxa only 

found in the Early Eocene. The recorded faunas 

have a wide geographic distribution 

throughout North Africa and the Middle East. 

They are generally assigned to outer shelf - 

upper bathyal settings of normal marine environments 

and belong to the type of species 

termed as the “South Tethyan Type” that 

wandered along southern shores of the Tethys 

during this time. The presence of taxa which 

are also found in West Africa emphasizes faunal 

exchange between the Southern Tethys 

and the West African basins during the Maastrichtian 

- Early Eocene. 

2010010282 

大洋洲新生代甲壳动物介形类 

Alataleberis 属的评述和新属 

Alatapacifica 的描述 = Review of Alataleberis 

McKenzie and Warne, 1986 

and description of Alatapacifica gen. 

nov. (Ostracoda, Crustacea) from the 

Cenozoic of Australasia. ( 英文 ). Warne 

M T. Alcheringa, 2010, 34(1): 37 - 60 

Species originally assigned to the 

pterygocytherine genus Alataleberis by 

McKenzie & Warne, 1986 are placed 

here in two genera—Alataleberis sensu 

stricto and Alatapacifica gen. nov. Alataleberis 

species possess poorly defined 

dorsal ridges marked by a few spines in 

adult specimens and lack a subcentral 

tubercle. Alatapacifica species possess 

well-developed and buttressed dorsal 

ridges and a well-developed subcentral 

tubercle. Pterygocytherine genera/species 

groups recognized here from 

the southwest Pacific region are Alataleberis, 

Alatapacifica (septarca and robusta 

species groups), Alatahermanites 

Whatley & Titterton, 1981 and the 

88

velivola species group of Pterygocythereis 

Blake, 1933. 

2010010283 

美国西部大盆地下奥陶统双股尾虫型 

三叶虫一新属 Heckethornia, = Heckethornia, 

a new genus of dimeropygid trilobites 

from the Lower Ordovician 

(Ibexian; Tulean and Blackhillsian) of 

the Great Basin, western USA. ( 英文 ). 

McAdams N E B; Adrain J M. Canadian 

Journal of Earth Sciences, 2009, 

46(12): 875-914 

Heckethornian. gen. is a morphologically 

striking clade of dimeropygid trilobites 

known from the Pogonip Group 

(Ordovician; Ibexian Series, Tulean and 

Blackhillsian stages) of western Utah 

and eastern Nevada. It includes seven 

species based on silicified material. All 

occur in the Fillmore Formation of 

western Utah, and four are also known 

from the Yellow Hill Limestone of eastern 

Nevada. Diagnostic features of 

Heckethornia include a highly vaulted 

exoskeleton with a tall pygidial “wall” 

made of fused outer pleurae, three pairs 

of large glabellar spines, two to three 

pairs of prominent pygidial spines, a 

single (or paired) large occipital spine(s), 

and an arc of tubercles on the librigenal 

field. Cladistic parsimony analysis suggests 

that the genus comprises two subclades, 

one including species with a single 

median occipital spine, and species 

with paired occipital spines or tubercles 

in the other. New species are H. smithi, 

H. hyndeae, H. numani, H. bowiei, H. 

morrisseyi, and H. ballionae. 

2010010284 

阿根廷东科迪耶拉 Pascha-Incamayo 

地区新的笔石、胞石和疑源类 = New 

graptolite, chitinozoan and acritarch records 

from the Pascha-Incamayo area, 

Cordillera Oriental, Argentina. ( 英文 ). 

Toro B A; Susana de la Puente G; 

Rubinstein C V. Comptes Rendus 

Palevol, 2010, 9(1-2): 23-30 

A new fossil assemblage bearing 

graptolites, chitinozoans and acritarchs 

is analyzed based on material collected 

in the Pascha-Incamayo area, Salta 

Province, NW Argentina. The occurrence 

of Hunnegraptus copiosus (Lindholm, 

1991), associated with specimens 

of the genus Tetragraptus (Salter, 1863), 

is highly relevant to improve the age assignment 

and correlate the fossil-bearing 

levels previously assigned to the Devendeus 

Formation. Different stages in 

the development of the index species of 

the Upper Tremadocian H. copiosus 

Biozone are described and illustrated. 

The precise stratigraphic ranges of the 

associated chitinozoans and acritarchs 

are discussed, according to the biostratigraphic 

analysis, and the stratigraphic 

relationships for the studied section are 

considered 

2010010285 

欧洲 , 亚洲和南非的三叠纪及侏罗纪 

Geinitziidae 科 ( 昆虫纲 : 

Grylloblattida ) 鲜为人知的新发现 

grylloblattids = New and little-known 

grylloblattids of the family Geinitziidae 

(Insecta: Grylloblattida) from the Triassic 

and Jurassic of Europe, Asia, and 

South Africa. ( 英文 ). Aristov D S; 

Wappler T; Rasnitsyn A P. Paleontological 

Journal, 2009, 43(4): 418- 

424 2 图版 . 

The fossil history of the family Geinitziidae 

is reviewed. New taxa are described 

in the family: Shurabia hissarica, 

sp. nov. (Lower Jurassic of Tajikistan), 

Sh. shartegica, sp. nov. (Upper Jurassic 

of Mongolia), Sh. serrata, sp. nov. and 

Ginitzia sagulensis, sp. nov. (both 

Lower Jurassic of Kyrgyzstan). The subfamily 

Stegopterinae Sharov, 1961 is 

synonymized under Geinitziinae Handlirsch, 

1906. The genera Minesedes Fujiyama, 

1973 and Ominea Fujiyama, 

1973 (Upper Triassic of Japan) are synonymized 

under Shurabia Martynov, 

1937 and Geinitzia Handlirsch, 1906, 

89

espectively. Geinitzia varia Bode, 1953 

(Lower Jurassic of Germany) and 

Fletchizia picturata Riek, 1976 (Upper 

Triassic of South Africa) are redescribed 

from their holotypes. F. kapokraalensis 

Wappler, 2001 and F. aleda Wappler, 

2001 (both Upper Triassic of South Africa) 

are transferred to the genus Shurabia. 

2010010286 

俄罗斯外贝加尔地区白垩纪 

Glaresidae 科类金龟子甲虫类新种 

( 鞘翅目 : 金龟总科 ) = New species 

of scarabaeoid beetles from the family 

Glaresidae (Coleoptera: Scarabaeoidea) 

from the Cretaceous of Transbaikalia. 

( 英文 ). Nikolajev G V. Paleontological 

Journal, 2009, 43(4): 425-427 1 图版 . 

A new species from the family Glaresidae, 

Cretoglaresis ovalis, sp. nov., is 

described from the Lower Cretaceous 

site Baisa in Transbaikalia. Improved 

diagnosis of the genus Cretoglaresis Nikolajev, 

2007 is given. 

2010010287 

外贝加尔早白垩世纹蓟马科和蓟马科 

( 昆虫纲 : 缨翅目 ) 中的最老成员 = 

The oldest members of the families Aeolothripidae 

and Thripidae (Insecta: Thysanoptera) 

from the Lower Cretaceous 

of Transbaikalia. ( 英文 ). Shmakov A S. 


428-432 2 图版 . 

Fusithrips crassipes Shmakov, gen. et sp. 

nov. (Aeolothripidae) and Convexithrips 

robustus Shmakov, gen. sp. nov. (Thripidae), 

the oldest members of these families, are 

described from the Lower Cretaceous of the 

Baissa locality. This allowed the improvement 

of the time of emergence of the Recent 

Thysanoptera assemblage, which includes 

phloeothripids along with aeolothripids and 

thripids. 

2010010288 

西伯利亚二叠纪末 limnadiidae, falsiscidae 

和 glyptoasmussiidae 科 ( 节 

肢动物门介甲目 ) 和分布和微细结构 

= Distribution and microsculpture of 

limnadiidae, falsiscidae, and glyptoasmussiidae 

(Conchostraca) of the terminal 

Permian of Siberia. ( 英文 ). Orlova E 

F; Sadovnikov G N. Paleontological 

Journal, 2009, 43(6): 631-639 3 图版 . 

New data on the distribution of conchostracans 

in volcanogenic deposits of 

the terminal Permian of the Tunguska 

Syneclise (Vyatkian and Taimyrian 

stages of the Tatarian Series) are presented. 

Based on the SEM study of these 

conchostracans their minute ornamentation 

patterns are described: microsculpture 

of Eulimnadia consisting of pits and 

cells with rounded cells separated by 

flattened interspaces, cellular microsculpture 

of Limnadia with rounded 

cells separated by convex interspaces 

(family Limnadiidae), honeycomblike 

cellular microsculpture of Falsisca (new 

family Falsiscidae), and microsculpture 

of Loxomicroglypta (?) consisting of 

small uniform rounded cells separated 

by narrow convex or angular interspaces 

(family Glyptoasmussiidae). The diagnoses 

of the genera and species are 

emended. 

2010010289 

Palaeonothrus Krivolutskii et Sidorchuk 

2003( 昆虫纲 : 膜翅目 : 姬蜂总 

科 , 非真螨目 , 甲螨目 ) 的分类学位 

置 = On the taxonomic position of Palaeonothrus 

Krivolutskii et Sidorchuk 

2003 (Insecta: Hymenoptera: Ichneumonoidea, 

non Acariformes, Oribatida). 

( 英文 ). Sidorchuk E A; Rasnitsyn A P. 


640-642 2 图版 . 

The taxonomic position of the genus 

Palaeonothrus Krivolutskii et Sidorchuk, 

2003 described from the Holocene of 

Arkhangelsk oblast is reconsidered. The 

fossils, which were originally attributed 

to moss mites (Acariformes: Oribatida), 

turned out to be isolated mesonota of 

some Ichneumonidae or Braconidae 

90

wasps, which were impossible to identify 

more precisely. Consequently, it is 

proposed to treat the genus Palaeonotrus 

as Ichneumonoidea incertae sedis until 

the source insects are identified. 

2010010290 

二叠纪 grylloblattida( 昆虫纲 ) 的地 

层分布综述及新分类单位的描述 = 

Review of the stratigraphic distribution 

of Permian grylloblattida (Insecta), with 

descriptions of New Taxa. ( 英文 ). Aristov 

D S. Paleontological Journal, 2009, 

43(6): 643-651 3 图版 . 

New taxa of grylloblattid insects 

(Grylloblattida) are described: Tshekardomina 

mongolica, sp. nov. (Tshekardominidae) 

from Bor-Tologoi locality 

(Severodvinian Stage of Mongolia), 

Permoshurabia mesenensis, gen. et sp. 

nov. (Geinitziidae) from Soyana fossil 

site (Kazanian Stage of Arkhangelsk 

oblast), Khosaridelia vyatica, sp. nov. 

(Permotermopsidae) from Karaungir II 

locality (Vyatkian Stage of Kazakhstan), 

Euremisca kazanica, sp. nov. (Euremiscidae) 

from Soyana fossil site (Kazanian 

Stage of Arkhangelsk oblast), Megakhosarina 

vyaznikensis, sp. nov. (Megakhosaridae) 

from Balymotikha locality 

(Vyatkian Stage of Vladimir oblast), and 

Parascalicia prokopensis, gen. et sp. 

nov. (Skaliciidae) from Prokop’evsk 

fossil site (Kazanian Stage of Kemerovo 

oblast). The genera Lodevopterum 

Béthoux, Nel, Lapeyrie et Gand, 2005 

(Lodève fossil site, France), Elmopterum 

Béthoux et Beckemeyer, 2007, and Sigmophlebia 

Béthoux et Beckemeyer, 

2007 (Elmo and Midco fossil sites, 

United States) are transferred from Grylloblattida 

incertae sedis to families 

Euremiscidae, Aliculidae, and Tshekardominidae, 

respectively. The stratigraphic 

distribution of Permian grylloblattid 

families is reviewed. 

2010010291 

中国中侏罗世的新 coptoclavid 幼虫 

( 鞘翅目 : 肉食亚目 :Dytiscoidea 总 

科 ) 以及它的系统发育学含义 = A 

new coptoclavid larva (Coleoptera: 

Adephaga: Dytiscoidea) from the Middle 

Jurassic of China, and its phylogenetic 

implication. ( 英文 ). Wang B; Ponomarenko 

A G; Zhang H Ch. Paleontological 

Journal, 2009, 43(6): 652- 

659 6 图版 . 

Daohugounectes primitivus, a new 

genus and species of coptoclavid beetles, 

is described from 67 fossil larvae from 

the Jurassic locality of Daohugou, 

northeastern China. It differs from other 

coptoclavids in the combination of the 

following characters: lateral lobes of nasale 

present; legs relatively short, with 

tarsi flat and slightly dilated; abdominal 

tergite VIII almost circular; derivative of 

abdominal segment IX present; urogomphi 

short; and helical thickening of tracheae 

weak. Most of these features are 

plesiomorphic for the family Coptoclavidae 

and the superfamily Dytiscoidea. 

Among dytiscoids, a derivative 

of abdominal segment IX is present only 

in the larvae of the recently discovered 

relic family Aspidytidae. 

2010010292 

蒙古中生代的新水生食腐动物甲壳虫 

( 鞘翅目 : 水龟甲 ) = New water 

scavenger beetles (Coleoptera: Hydrophilidae) 

from the mesozoic of Mongolia. 

( 英文 ). Prokin A A. Paleontological 

Journal, 2009, 43(6): 660-663 3 图版 . 

A new genus and two new species of 

water scavenger beetles, Hydrophilopsia 

bontsaganica, sp. nov. and Prospercheus 

cristatus, gen. et sp. nov., are 

described from the Upper Jurassic and 

Lower Cretaceous of Mongolia. The 

systematic position of the new genus is 

discussed. 

91

2010010293 

乌克兰罗夫诺始新世琥珀中的石蝇 

( 昆虫纲 : 襀翅目 ) 新发现 = New 

stoneflies (Insecta: Perlida = Plecoptera) 

from Eocene Rovno amber, Ukraine. ( 英 

文 ). Sinitshenkova N D. Paleontological 

Journal, 2009, 43(6): 664-668 4 图版 . 

A new genus, Rovnocapnia gen. nov., 

with new species R. atra sp. nov. and R. 

ambita sp. nov., from the family Capniidae, 

and a new genus and species Palaeoleuctra 

acuta gen. sp. nov., from the 

family Leuctridae, of the suborder Nemourina 

(Euholognatha), are described 

from Late Eocene Rovno amber. Familial 

assignment of one additional specimen 

(suborder Perlina, infraorder Perlomorpha 

(Systelognatha)), represented 

by a nymphal skin, is obscure due to its 

incomplete preservation. 

2010010294 

乌克兰罗夫诺始新世琥珀中的牧草虫 

( 缨翅目 , 昆虫纲 ) = Thrips (Thysanoptera, 

Insecta) from the Rovno amber, 

Eocene of Ukraine. ( 英文 ). Shmakov 

A S; Perkovsky E E. Paleontological 

Journal, 2009, 43(6): 669-674 1 图 

版 . 

Seventy-six thrips were discovered in 

Rovno amber. Among these, 67 were 

identified to suborder, 52, to family, 45, 

to genus, and 41, to species level. In total, 

five species, six genera, five families, 

and two suborders are recorded. No undescribed 

taxa have been found so far. 

All the identified thrips, except those of 

the genus Phloeothrips, belong to fossil 

taxa, previously known only from the 

Baltic and Bitterfeld ambers. However, 

the composition of species in the Rovno 

amber is highly unusual due to domination 

of Praedendrothrips avus Priesner, 

1924. This species, rare in the Baltic 

amber, constitutes 49% of all the Rovno 

records. Thus, the Rovno amber, in contrast 

to the Baltic and Bitterfeld ambers, 

is characterized by poor taxonomic diversity 

of thrips and presence of a 

clearly dominant species. 

2010010295 

北欧亚大陆晚新生代的昆虫 = Late 

Cenozoic insects of northern Eurasia. 

( 英文 ). Kiselev S V; Nazarov V I. Paleontological 

Journal, 2009, 43(7): 723- 

850 5 图版 . 

Quaternary and Late Tertiary fossil 

insects from different regions of Eurasia 

are studied. The main areas are northeastern 

Eurasia (Part 1) and Belarus and 

adjacent regions (Part 2). Paleoenvironmental 

and climatic reconstructions for 

these regions are provided and compared 

with other parts of Europe, Asia, and 

North America. Hundreds of fossil insect 

localities are described; thousands 

of insect sclerites are recognized. 

2010010296 

节肢动物在大陆生物群发展中所起的 

作用 = The role of arthropods in the development 

of continental biota. ( 英文 ). 

Ponomarenko A G. Paleontological 

Journal, 2009, 43(8): 852-857 

Arthropods appeared in the Early 

Cambrian and by the end of this period 

had begun colonizing dry land and continental 

waters. Remains and supposed 

tracks of euthycarcinoids are already 

known by the end of the Cambrian. Ordovician 

deposits contain burrows of 

wormlike animals, which assimilated 

organic material from algal-bacterial 

mats and began creating hydromorphic 

protosoils by mixing this material with 

products of erosion. By the end of the 

Silurian, a coadapted complex of soil 

organisms, no less complex than the recent 

one, had already formed. Its principal 

components were arthropods. Then 

the algal-bacterial mats began being replaced 

by vascular plants. Slowly decaying 

lignin and cellulose significantly 

stabilized the soil ecosystems. The most 

important role in the formation of continental 

ecosystems was played by cheli- 

92

cerates and myriapodlike creatures, 

which were particularly characteristic of 

the Late Paleozoic. By the end of the 

Paleozoic, insects began to play an important 

role. 

2010010297 

当代和一些树脂化石中的节肢动物 = 

Arthropods in contemporary and some 

fossil resins. ( 英文 ). Zherikhin V V; Sukacheva 

I D; Rasnitsyn A P. Paleontological 

Journal, 2009, 43(9): 987- 

1005 

More than 4800 arthropod inclusions 

were isolated and identified from resin 

of various contemporary conifer trees in 

various parts of northern Eurasia. Their 

composition is compared with that in 

representative collections of Baltic and 

Rovno ambers (Upper Eocene) and with 

that in Dominican amber (Lower Miocene). 

The original composition of inclusions 

of Dominican amber is reconstructed 

for the first time using a procedure 

intended to reduce the effect of 

human bias. Taphonomical characteristics 

of resins and their effects on the 

composition of inclusions are studied. 

The actuapaleontological approach reveals 

a trend towards a decrease in the 

relative abundance of arboreal springtails 

and nematoceran dipterans and an 

increase in that of the true bugs, beetles, 

lepidopterans, and hymenopterans (especially 

ants) between the Eocene and 

the present. Relative abundances of spiders 

and mites show no clear trend. The 

available data on other arthropods are 

still insufficient for elucidating evolutionary 

trends. Surprisingly, a small contemporary 

sample from Taimyr (N. Siberia) 

was inexplicably more similar to 

the Eocene amber than to other contemporary 

resins. No other significant differences 

in composition of inclusions, 

compared across different conifer genera 

or geographic areas, have been revealed. 

A more detailed comparison between 

contemporary and fossil hymenopteran 

and beetle inclusions reveals correlations 

with both age (= evolutionary 

change) and geography. The absolute 

dominance of ants, particularly Formicinae 

and Myrmicinae, and, among solitary 

hymenopterans, Ichneumonidae, 

Braconidae, and Pteromalidae, and a 

corresponding decline in the abundance 

of Scelionidae and Dolichoderinae in 

contemporary resins compared to amber 

reflect evolutionary changes. In contrast, 

the overwhelming abundance of Formicinae 

and consistent occurrence of 

sawflies in contemporary resins of 

northern Eurasia appear to be explained 

by geography. The Eocene assemblages 

of beetle inclusions are characterized by 

a wider and more variable set of dominant 

families, in sharp contrast to contemporary 

resins, which are uniformly 

dominated by Curculionidae, Chrysomelidae, 

and Staphylinidae. Additional 

analyses are needed to explain this 

difference. 

2010010298 

萨克森阶琥珀中发现与蚂蚁 

Monomorium mayrianum ( 同翅目 , 蚁 

科 ) 同包含的单爪蚜虫 Germaraphis 

ungulata( 同翅目 , 蚜虫类 ) = On 

finding a single-clawed aphid, Germaraphis 

ungulata (Homoptera, Aphidinea), 

in a syninclusion with the ant 

Monomorium mayrianum (Hymenoptera, 

Formicidae) in the Saxonian amber. ( 英 

文 ). Perkovsky E E. Paleontological 

Journal, 2009, 43(9): 1006-1007 

The first syninclusion of the myrmicine 

Monomorium mayrianum 

Wheeler (two workers) and the aphid 

Germaraphis ungulata Heie (one nymph) 

is described from the Bitterfeld amber. 

Additionally, G. ungulata is recorded in 

a syninclusion with Ctenobethylus 

goepperti (Mayr) in the Rovno amber 

for the first time. 

2010010299 

波罗的海琥珀中的 Achilini 族 ( 同翅 

目 , 蜡蝉总科 ,Achilidae 科 ) 中的蜡 

93

蝉新发现 = New planthoppers of the 

tribe Achilini (Homoptera, Fulgoroidea, 

Achilidae) from Baltic amber. ( 英文 ). 

Emeljanov A F; Shcherbakov D E. Paleontological 

Journal, 2009, 43(9): 

1008-1018 5 图版 . 

New taxa of Achilini (Achilidae) are 

described from Baltic amber: Paratesum 

rasnitsyni gen. et sp. nov., Protomenocria 

notata gen. et sp. nov., Psycheona 

variegata gen. et sp. nov., P. 

striata sp. nov. Protepiptera kaweckii 

Usinger, 1939 (= Cixidia christinae Lefebvre, 

Bourgoin et Nel, 2007, syn. nov.) 

is redescribed with designation of a neotype. 

“Cixius” testudinarius Germar et 

Berendt, 1856, “C.” longirostris Germar 

et Berendt, 1856 and “Oliarus” oligocenus 

Cockerell, 1910 are transferred to 

Achilini. A key to the genera of Achilidae 

known from Baltic amber is provided. 

2010010300 

罗夫诺琥珀中的一种泥蜂新属 

Rovnoecus( 膜翅目 , 方头泥蜂科方 

头泥蜂科 , 短柄泥蜂亚科 ) = Rovnoecus, 

a new genus of digger wasps 

(Hymenoptera, Crabronidae, Pemphredoninae) 

from the Rovno amber. ( 英文 ). 

Antropov A V; Perkovsky E E. Paleontological 

Journal, 2009, 43(9): 1019- 

1023 1 图版 . 

A new fossil digger wasp Rovnoecus 

klesovicus gen. et sp. nov. (Hymenoptera, 

Crabronidae, Pemphredoninae, 

Pemphredonini) is described from the 

Upper Eocene Rovno amber. The genus 

Rovnoecus gen. nov. is characterized by 

an incomplete occipital carina, partly 

reduced second discoidal cell, and the 

presence of spines on all tibiae. Rovnoecus 

gen. nov. is most similar to the 

fossil genus Eoxyloecus Budrys, 1993 

from the Baltic amber. The two genera 

form a monophyletic group that is a sister 

group to the group formed by the 

genera Passaloecus Shuckard, 1837 and 

Eopinoecus Budrys, 1993. This indirectly 

corroborates the hypothesis of the 

geographically different origin of the 

Rovno and Baltic ambers. 

2010010301 

中欧和东欧晚始新世琥珀中的蚂蚁 

( 昆虫纲 : 胡蜂科 : 蚁科 ) 胡蜂科胡 

蜂科 = Ants (Insecta: Vespida: Formicidae) 

in the upper Eocene amber of central 

and Eastern Europe. ( 英文 ). Dlussky 

G M; Rasnitsyn A P. Paleontological 

Journal, 2009, 43(9): 1024-1042 7 图版 . 

A total of 5754 ant inclusions from 13 

European collections of Baltic, Bitterfeld, 

Rovno, and Scandinavian ambers 

are studied and identified as belonging 

to 147 species, 57 genera, and 9 subfamilies. 

The taxonomic composition 

and relative species abundances of species 

in representative collections are 

analyzed and considerable differences 

between the above four types of amber 

are shown. These differences appear to 

reflect differences in ecological conditions 

rather than in age. The Baltic and 

Bitterfeld ant assemblages are shown to 

be most similar, the Scandinavian assemblage 

turns out to be most dissimilar 

to these, and the Rovno assemblage is 

shown to be intermediate. 

2010010302 

欧洲晚始新世琥珀中的蚂蚁亚科 

Ponerinae, Cerapachyinae 和 Pseudomyrmecinae( 

膜翅目 , 蚁科 ) = 

The ant subfamilies Ponerinae, Cerapachyinae, 

and Pseudomyrmecinae 

(Hymenoptera, Formicidae) in the Late 

Eocene ambers of Europe. ( 英文 ). 

Dlussky G M. Paleontological Journal, 

2009, 43(9): 1043-1086 13 图版 . 

The ant subfamilies Ponerinae, Cerapachyinae 

and Pseudomyrmecinae are 

revised in the Baltic, Bitterfeld, Rovno, 

and Scandinavian ambers of the Late 

Eocene age. Thirteen new species are 

described: Amblyopone groehni sp. n., A. 

electrina sp. n., Pachycondyla conservata 

sp. n., P. tristis sp. n., Ponera lobu- 

94

lifera sp. n., P. mayri sp. n., P. wheeleri 

sp. n., Gnamptogenys rohdendorfi sp. n., 

Bradoponera similis sp. n., Proceratium 

eocenicum sp. n. (Ponerinae), Procerapachys 

sulcatus sp. n. (Cerapachyinae), 

Tetraponera europaea sp. n., and T. 

groehni sp. n. (Pseudomyrmecinae). 

Tetraponera angustata (Mayr) is synonymized 

with T. simplex (Mayr). Keys 

to species are provided. 

2010010303 

罗夫诺琥珀中的蚂蚁 ( 膜翅目 , 蚁 

科 ) 按重量分配的种类组成差异 = 

Differences in ant (Hymenoptera, Formicidae) 

species composition between 

weight fractions of Rovno amber. ( 英文 ). 

Perkovsky E E. Paleontological Journal, 

2009, 43(9): 1087-1091 

Arboreal specialists (including Ctenobethylus 

goepperti) comprise 54% of all 

ant inclusions in Rovno amber pieces 

weighing up to 1.5 g and 43% of those 

in larger pieces. In the small-size amber 

fraction, syninclusions containing more 

than a single worker ant are represented 

exclusively by the arboreal Dolichoderus 

spp. and C. goepperti, while syninclusions 

in larger amber pieces often 

contain workers of Lasius spp., which 

are not associated with trees. Species of 

Lasius comprise 15% of ants in the 

smaller and 28% in the larger amber 

pieces. It seems that the smaller pieces 

of amber have formed on the thinner 

branches of the amberproducing trees 

and, consequently, contain a larger proportion 

of arboreal ant species. Comparison 

of composition of inclusions between 

different weight fractions of amber 

is a promising tool to study fossil 

faunas and environments. 

2010010304 

波罗的海和罗夫诺琥珀 ( 晚始新世东 

欧 ) 中拟花蚤科甲虫属 Anaspis 新种 

( 昆虫纲 : 鞘翅目 : 拟花蚤科 ) = A 

new species of the scraptiid beetle genus 

Anaspis (Insecta: Coleoptera: Scraptiidae) 

from the Baltic and Rovno ambers 

(Upper Eocene of Eastern Europe). ( 英 

文 ). Perkovsky E E; Odnosum V K. Paleontological 

Journal, 2009, 43(9): 

1092-1094 1 图版 . 

A new fossil species, Anaspis 

(Spanisa) horaki sp. nov., is described 

from the Baltic and Rovno ambers. It 

differs from the recent species in the 

shapes of its last maxillary palpus segment 

and its antennal club. 

2010010305 

罗夫诺琥珀中 tumbling flower 甲虫属 

新种 Glipostena( 昆虫纲 : 鞘翅目 : 

花蚤科 ) = New species of the tumbling 

flower beetle genus Glipostena 

(Insecta: Coleoptera: Mordellidae) from 

Rovno amber. ( 英文 ). Odnosum V K; 


2009, 43(9): 1095-1096 1 图版 . 

A new fossil species of the tumbling 

flower beetle genus Glipostena is described 

from Rovno amber. It differs 

from its recent and fossil congeners in 

the shapes and proportions of the antennomeres, 

and the number and position of 

lateral ridges on the hind tibia. 

2010010306 

罗夫诺琥珀中象鼻虫 Dryophthoridae 

科 ( 鞘翅目 ,Dryophthoridae: Stromboscerinae) 

的一新属和一新种 = A 

new genus and species of dryophthorid 

weevils (Coleoptera, Dryophthoridae: 

Stromboscerinae) from the Rovno amber. 

( 英文 ). Nazarenko V Yu; Perkovsky E E. 


1097-1100 2 图版 . 

Stenommatomorphus hexarthrus gen. 

et sp. nov. (Dryophthoridae: Stromboscerinae) 

is described from the Late Eocene 

Rovno amber. This is the first fossil 

representative of the subfamily. The 

new genus is most close to Synommatus 

Pascoe, from which it differs in the 

pronotum and elytra less coarsely sculp- 

95

tured, the intervals not carinate, and the 

scutellum present. 

2010010307 

晚始新世琥珀中 Leptosynini 族五倍 

子蝇新种 ( 双翅目 , 瘿蚊科 ) 以及 

Heteropezidi 亚族的分类 = New gall 

midges of the tribe Leptosynini (Diptera, 

Cecidomyiidae) from the Late Eocene 

ambers and the classification of the supertribe 

Heteropezidi. ( 英文 ). Fedotova 

Z A; Perkovsky E E. Paleontological 

Journal, 2009, 43(9): 1101-1147 29 图 

版 . 

Three new genera and 27 new species 

of gall midges are described from the 

Late Eocene ambers: Henria baltica sp. 

nov., Frirenia manca sp. nov., F. musicata 

sp. nov., Leptosyna samlandica sp. 

nov., L. fastosa sp. nov. from Baltic amber 

and H. xystica sp. nov., H. liquida sp. 

nov., Stellasegna vlaskini gen. et sp. 

nov., S. vaporea sp. nov., S. nexa sp. 

nov., Rasnitsia verticosa gen. et sp. nov., 

F. rohdendorfi sp. nov., F. schevchenkoi 

sp. nov., F. melica sp. nov., F. lukashevichae 

sp. nov., F. leporidis sp. nov., F. 

marmarygma sp. nov., F. vesana sp. 

nov., Vincinescia alisae gen. et sp. nov., 

L. margarita sp. nov., L. munifera sp. 

nov., L. sukachevae sp. nov., L. assa sp. 

nov., L. larga sp. nov., L. vegeta sp. 

nov., L. vaticina sp. nov., and L. shcherbakovi 

sp. nov. from Rovno amber. 

Strobliella capitata Fedotova is redescribed 

as Henria capitata (Fedotova, 

2004) (comb. nov.). Diagnoses of Henria 

(= Electroxylomyia Nel et Prokop, 

syn. nov.), Frirenia, and Leptosyna are 

revised. As a result, Henria comprises 3 

extant and 5 extinct (Late Eocene) species, 

including H. eocenica (Nel et Prokop), 

comb. nov. (= Electroxylomyia 

eocenica), Frirenia comprises 1 extant 

and 10 Late Eocene species, and Leptosyna 

comprises 3 extant and 11 Late Eocene 

species. The tribe Heteropezini is 

elevated to the supertribal rank (Heteropezidi) 

and included in the subfamily 

Lasiopterinae. Leptosynini is treated as a 

separate tribe, and Lasiopterinae is considered 

as part of Cecidomyiidae s. str. 

(i.e., excluding Lestremiidae). Keys to 

the tribes and genera of Heteropezidi 

and to species of Henria, Stellasegna, 

Frirenia, and Leptosyna are provided. 

The gall midge faunas of the Rovno and 

Baltic ambers are compared. Phylogenetic 

relationships within the supertribe 

are hypothesized. 

2010010308 

哈萨克斯坦特马豆克阶燧石中的介形 

类 = Find of Tremadocian ostracodes in 

cherts of Kazakhstan. ( 英文 ). Melnikova 

L M; Tolmacheva T Yu; Ushatinskaya 

G T. Paleontological Journal, 2010, 

44(1): 36-40 4 图版 . 

First late Tremadocian (Early Ordovician) 

ostracodes were found in cherts of 

the Burubaital Formation near the “Burultas” 

deposit in southern Kazakhstan. 

The preservation of carbonate ostracode 

shellshells in siliceous environment is 

discussed. The monotypic ostracode assemblage 

includes the newly described 

form, Burultalina nikitinae gen. et sp. 

nov. 

2010010309 

北极第四纪介形类及在古环境重建中 

的使用 = Arctic quaternary ostracods 

and their use in paleoreconstructions. 

( 英文 ). Stepanova A Yu; TaldenkovaH 

E E; Bauch A. Paleontological Journal, 

2010, 44(1): 41-48 1 图版 . 

The paper deals with original and 

published data on fossil ostracodal assemblages 

from the Eurasian Arctic 

Kara, Laptev and Chuckchi seas. As a 

whole, six ecologically different assemblages 

were distinguished (freshwater, 

brackish water, marine of the inner, 

middle and outer shelves and upper continental 

slope), they replace each other 

upcore reflecting a gradual increase in 

water depth and distance from the coast. 

These assemblages are stable in the en- 

96

tire Arctic region and can be used for 

interpretation of environments in different 

Arctic areas. 

2010010310 

Isady 地点二叠纪 Palaeonemouridae 

科石蝇 ( 昆虫纲 : 襀翅目 ) 新属种 = 

New Permian stoneflies of the family 

Palaeonemouridae (Insecta: Perlida = 

Plecoptera) from the Isady locality. ( 英 

文 ). Sinitshenkova N D; Aristov D S. 


49-52 1 图版 . 

New stonefly species of the family 

Palaeonemouridae, Palaeonemoura issadensis, 

sp. nov., Palaeotaeniopteryx 

laeta, sp. nov., and P. triternata, sp. nov., 

are described from the Tatarian (Upper 

Permian) locality of Isady (Severodvinian 

Stage of the Vologda Region). 

2010010311 

波罗的海和比特费尔德琥珀中的树汁 

甲虫 ( 鞘翅目 : 露尾甲科 : 

Nitidulini) 新种 = New species of sap 

beetles (Coleoptera: Nitidulidae: 

Nitidulini) from the Baltic and Bitterfeld 

ambers. ( 英文 ). Kirejtshuk A G; Kurochkin 

A S. Paleontological Journal, 

2010, 44(1): 53-67 7 图版 . 

A new genus, Microsoronia, gen. nov., 

and new species of this genus, M. hoffeinsorum, 

sp. nov. from the Bitterfeld 

amber and M. kerneggeri sp. nov., M. 

nigerrima sp. nov., and M. interfax, sp. 

nov. from the Baltic amber, are described. 

The earliest known member of 

the genus Phenolia, P. (Lasiodites) angustitibialis, 

sp. nov., is described from 

the Baltic amber. The systematic position 

of these two genera, their possible 

evolution, as well as the possible ecology 

and bionomics of their members are 

discussed. It is shown that “Phenolia” 

incapax Scudder, 1890 should be included 

in the family Peltidae, rather than 

Nitidulidae. 

2010010312 

瓢甲科 ( 鞘翅目 : 瓢甲科 ) 物种的同 

异名 :3 = Species names homonymy in 

ladybirds (Coleoptera: Coccinellidae): 3. 

( 英文 ). Ukrainsky A S. Paleontological 

Journal, 2010, 44(1): 104 

2010010313 

萨拉托夫地区晚桑托阶和早麦斯里希 

特阶介形虫类新资料 = New data on 

late Santonian and early Maastrichtian 

ostracodes of the Saratov Region. ( 英文 ). 

Tesakova E M. Paleontological Journal, 

2010, 44(2): 168-179 3 图版 . 

The article presents a paleoenvironmental 

analysis of ostracode assemblages 

from Mezino-Lapshinovka (Upper 

Santonian) and Lokh (Lower Maastrichtian) 

Formations of the Vishnevoe 

section (Saratov Region). Two new species 

Cytherelloidea vishneviensis sp. nov. 

and Mauritsina mandelstami sp. nov. are 

described. 

2010010314 

外贝加尔和蒙古早白垩世亚科 

Tanychorinae 的 Ichneumonids( 昆 

虫纲 : 膜翅目 : 姬蜂科 ) = Ichneumonids 

of the subfamily Tanychorinae 

(Insecta: Hymenoptera: Ichneumonidae) 

from the Lower Cretaceous of Transbaikalia 

and Mongolia. ( 英文 ). Kopylov D 

S. Paleontological Journal, 2010, 44(2): 

180-187 5 图版 . 

A new species, Tanychora loki, sp. 

nov., and a new genus and species, 

Megachora sibirica gen. et sp. nov., are 

described from the Lower Cretaceous of 

Transbaikalia and Mongolia. The genus 

Tanychora Townes, 1973 is divided into 

two genera: Tanychora s. str., composed 

of T. petiolata Townes, 1973 (type species), 

T. sinensis Zhang, 1991, and T. 

loki sp. nov., and Amplicella, gen. nov., 

composed of A. sessilis (Townes, 1973) 

(type species), A. exquisite (Zhang et 

Rasnitsyn, 2003), A. beipiaoensis 

(Zhang et Rasnitsyn, 2003), and A. spinata 

(Zhang et Rasnitsyn, 2003). The 

97

frequency of occurrence of ichneumonids 

in the principal Cretaceous localities 

of central and northern Asia is 

calculated. 

2010010315 

蒙古晚侏罗世草蜻蛉 ( 昆虫纲 : 脉翅 

目 :Grammolingiidae) 一新种 = A 

new lacewing (Insecta: Neuroptera: 

Grammolingiidae) from the Upper Jurassic 

of Mongolia. ( 英文 ). Khramov A 


188-191 2 图版 . 

A new lacewing species, Leptolingia 

shartegica sp. nov., (Grammolingiidae), 

from the Upper Jurassic of the Mongolian 

Shar-Teg locality is described. 

2010010316 

外贝加尔中生代 Anaidinae 亚科一新 

属 ( 鞘翅目 , 金龟总科 , 驼金龟科 ) 

= A new genus of the subfamily Anaidinae 

(Coleoptera, Scarabaeoidea, Hybosoridae) 

from the Mesozoic of Transbaikalia. 

( 英文 ). Nikolajev G V. Paleontological 

Journal, 2010, 44(2): 192- 

194 1 图版 . 

A new genus and species, Protanaides 

sibiricus gen et sp. nov., of the 

subfamily Anaidinae (family Hybosoridae) 

from the Lower Cretaceous Baisa 

locality in Transbaikalia is described. 

This find adds considerably to knowledge 

of the diversity of this subfamily in 

the Mesozoic of Asia and gives evidence 

of the relict status of the Recent Anaidinae. 

2010010317 

库尔斯克区晚卡洛期介形虫新发现 = 

New lower Callovian ostracodes from 

the Kursk Region. ( 英文 ). Tesakova E 

M; Strezh A S; Gulyaev D B. Paleontological 

Journal, 2009, 43(3): 258- 

271 4 图版 . 

Lower Callovian deposits (subpatruus 

and koenigi ammonite zones) in 

the Mikhailovskii Mine section (Central 

Russia, Kursk Region) yielded 13 ostracode 

species (two of them are new) belonging 

to ten genera. This ostracode 

assemblage corresponds to ostracode 

beds with Praeschuleridea wartae- 

Pleurocythere kurskensis. The stratigraphic 

range of these beds corresponds 

to three ammonite biohorizons: 

Chamoussetia crobyloides, Kepplerites 

gowerianus gowerianus, and K. indigestus. 

Three distinct ostracode assemblages 

have been defined in the section 

based on their taxonomy and occurrence 

pattern. Two new species, Pleurocythere 

kurskensis sp. nov. and Pseudohutsonia 

wienholzae sp. nov., are described. 

2010010318 

俄罗斯二叠纪 Lemmatophoridae 科 

新种 ( 昆虫纲 ,Grylloblattida ) = 

New grylloblattids of the family Lemmatophoridae 

(Insecta: Grylloblattida) 

from the Permian of Russia. ( 英文 ). 

Aristov D S. Paleontological Journal, 

2009, 43(3): 272-276 2 图版 . 

New grylloblattids of the family 

Lemmatophoridae (Insecta: Grylloblattida), 

Artinska sojanensis sp. nov., Sylvaprisca 

colorata sp. nov., and Uraloprisca 

lisca gen. et sp. nov., from the 

Soyana locality (Lower Kazanian, Arkhangelsk 

Region) and Paraprisca 

solikamskensis sp. nov. from the 

Tyul’kino locality (Ufimian, Perm Region) 

are described. Two species are 

transferred from the genus Paraprisca to 

Uraloprisca gen. nov.: Uraloprisca 

uralica (G. Zalessky, 1952), comb. nov. 

and Uraloprisca causaria (Novokshonov, 

2000), comb. nov. (both from 

the Kungurian of the Perm Region). The 

evolution of the family is discussed. 

2010010319 

俄罗斯 , 哈萨克斯坦以及蒙古白垩纪 

宝石甲虫新发现 ( 鞘翅目 : 吉丁虫 

科 ) = New jewel beetles (Coleoptera: 

Buprestidae) from the Cretaceous of 

Russia, Kazakhstan, and Mongolia. ( 英 

98

文 ). Alexeev A V. Paleontological 

Journal, 2009, 43(3): 277-281 2 图版 . 

A new jewel beetle genus, with one 

species (Cretofrontolina kzyldzharica 

gen. et sp. nov.) from the Upper Cretaceous 

of Kazakhstan is described based 

on a body; and three new species of the 

formal genus Metabuprestium are described 

based on isolated elytra: Metabuprestium 

sibiricum sp. nov. and M. 

arkagalense sp. nov. come from the 

Arkagala locality (Upper Cretaceous of 

Russia) and M. ichbogdense sp. nov. is 

from the Shar Tologoi locality (Lower 

Cretaceous of Mongolia). 

2010010320 

欧亚大陆中生代毛翅目 ( 昆虫纲 : 毛 

翅目 ) 的一些分布特征 = Some characteristics 

of the trichoptera distribution 

in the Mesozoic of Eurasia (Insecta: 

Trichoptera). ( 英文 ). Ponomarenko A G; 

Sukatsheva I D; Vasilenko D V. Paleontological 

Journal, 2009, 43(3): 282- 

295 2 图版 . 

The stratigraphic distribution and peculiarities 

of burial of caddis cases from 

293 Mesozoic localities in Eurasia are 

analyzed. An attempt is made to analyze 

and interpret the co-occurrence of 

trichopteran cases and adults in the major 

localities. The main stages in the 

evolution of the building behavior of 

trichopteran larvae in the Mesozoic have 

been elucidated. 

2010010321 

波罗的海琥珀中化石属 

Archaeotinodes 石蛾新发现 ( 昆虫 

纲 : 毛翅目 : 长须石蛾科 ) = A new 

caddisfly of the fossil genus Archaeotinodes 

(Insecta: Trichoptera: Ecnomidae) 

from the Baltic amber. ( 英文 ). Melnitsky 

S I. Paleontological Journal, 2009, 

43(3): 296-299 2 图版 . 

A new caddisfly species of the fossil 

genus Archaeotinodes, A. igneusaper sp. 

nov., is described from the Upper Eocene 

Baltic amber. The new species is 

close to A. pauper Ulmer, 1912 and A. 

lanceolata Ulmer, 1912 from the Baltic 

amber, differing from these in the structure 

of the male genitalia. 

2010010322 

介形类的形态学及其环境、功能和分 

类学意义 = Morphology of ostracods 

and its significance of environment,function 

and taxonomy. ( 中文 ). 王 

亚琼 ; 沙金庚 . 微体古生物学报 , 2009, 

26(3): 283-290 

化石介形类分类依据 ——— 壳体形 

态 , 包括壳体的大小、形状、装饰和诸 

如毛孔、叠覆、似犁状构造、喙、铰 

合构造等构造特征都与介形类的栖息 

环境 , 包括地理、气候 ( 季节、纬度 

等 ) 、水体的深度、化学性质和稳定 

程度 , 食物的富集程度和群落的组成及 

个体数量以及性别息息相关。因此 , 正 

确理解介形类的形态学特征及其功能 

学 , 不仅能揭示介形类的生活习性 , 推 

测化石介形类的生活环境 , 从而为古环 

境和古群落生态重建提供依据 , 而且可 

以提高化石介形类个体发育、系统分 

类和演化研究结果的可靠性。 

2010010323 

Enikal 海峡 ( 副特提斯东部 ) 晚中新 

世介形类 ( 甲壳纲 ) 可作为盐度改变的 

指示剂 = Late miocene ostracodes (Ostracoda, 

Crustacea) from the Enikal 

Strait (Eastern Paratethys) as indicators 

of salinity changes. ( 英文 ). Rostovtseva 

Yu V; Tesakova E M. Paleontological 

Journal, 2009, 43(2): 170-177 3 图版 . 

The species composition of ostracodes 

from the upper Maeotian and 

lower Pontian deposits of the Kerch- 

Taman Depression (Enikal Strait, Eastern 

Paratethys) is reported. The sedimentological 

and paleoenvironmental 

study shows that mass ostracode occurrences 

were controlled by hydrological 

changes in the Late Miocene brackishwater 

basins under consideration. 

99

2010010324 

俄罗斯中二叠世 Grylloblattida 目 

( 昆虫纲 ) 的一新科 = A new family 

of the order Grylloblattida (Insecta) 

from the Middle Permian of Russia. ( 英 

文 ). Aristov D S. Paleontological Journal, 

2009, 43(2): 178-182 2 图版 . 

A new family, Ivapteridae fam. nov. 

(Insecta; Grylloblattida), is described 

from the Middle Permian locality of 

Soyana (Arkhangelsk Region; Kazanian 

Stage). It is most similar to Sojanoraphidiidae 

O. Martynova, 1952, differing 

from it in the subcostal field being traversed 

in the basal half of the wing by 

long, curved, and strongly oblique 

crossveins that form a double row of 

cells, the base of CuA being free, and 

CuA 1 thin compared to CuA 2 . The new 

family is represented by a single species, 

Ivaptera sharovi, gen. et sp. nov. An 

overview of the modern system of the 

order Grylloblattida is included. 

2010010325 

对侏罗纪石蝇属 Dobbertiniopteryx 

Ansorge 和 Karanemoura Sinitshenkova 

修正 ( 昆虫纲 : 襀翅目 ¬) 以及中 

国道虎沟村新种描述 = A revision of 

the Jurassic Stonefly Genera Dobbertiniopteryx 

Ansorge and Karanemoura 

Sinitshenkova (Insecta: Plecoptera), 

with the description of new species from 

the Daohugou locality, China. ( 英文 ). 

Liu Y S; Sinitshenkova N D; Ren D. Paleontological 

Journal, 2009, 43(2): 183- 

190 6 图版 . 

The stonefly genera Dobbertiniopteryx 

Ansorge and Karanemoura Sinitshenkova 

are revised. Based on new material 

from the Middle Jurassic of Daohugou, 

China, two new species, D. juracapnia 

sp. nov. and K. manca sp. nov., 

are described and Karanemoura abrupta 

Sinitshenkova, 1987 is redescribed. K. 

desiliens Sinitshenkova, 1987 is excluded 

from Karanemoura; its position 

within the family Perlariopseidae remains 

uncertain. The placement of Dobbertiniopteryx 

in the modern family 

Capniidae is confirmed. The perfect 

state of preservation of the nearly complete 

adult stonefly remains from China 

made it possible to improve and extend 

the diagnoses of the Perlariopseidae and 

Dobbertiniopteryx. The geological 

background of the Daohugou deposits is 

briefly discussed. 

2010010326 

对美国弗洛里森特一些寄生蜂 ( 膜翅 

目 : 细蜂总科广义的 ) 的修正 = Revision 

of some parasitic wasps (Hymenoptera: 

Proctotrupoidea sensu lato) from 

the Florissant locality, United States. ( 英 

文 ). Kolyada V A. Paleontological 

Journal, 2009, 43(2): 191-196 4 图版 . 

The types of the parasitic wasps described 

in the families Proctotrupidae, 

Diapriidae, and Scelionidae (Hymenoptera) 

from the Upper Eocene Florissant 

locality (Colorado, United States) are 

revised. All the specimens are shown to 

belong to the family Proctotrupidae, representing 

the genera Oxyserphus, 

Mischoserphus, Nothoserphus, and Palaeoteleia. 

The known species are redescribed 

and two new species, 

Mischoserphus bruesi sp. nov. and Nothoserphus 

rasnitsyni sp. nov., are described. 

A new combination, Oxyserphus 

exhumatus (Brues, 1910), comb. 

nov., and a new synonymy, Paramesius 

defectus Brues, 1910, syn. nov. = Oxyserphus 

exhumatus (Brues, 1910), are 

established. 

2010010327 

Karatau 中 - 晚侏罗世叩头虫蚴型甲虫 

一新属 ( 鞘翅目 , 多食目 ) = A new 

genus of Elateriform beetles (Coleoptera, 

Polyphaga) from the Middle-Late Jurassic 

of Karatau. ( 英文 ). Yan E V. Paleontological 

Journal, 2009, 43(1): 78- 

82 3 图版 . 

A new coleopteran genus, Anacapitis 

gen. nov., comprising A. karataviensis 

sp. nov., A. incertus sp. nov., and A. ob- 

100

longus sp. nov., is described from the 

Karabastau Formation of the Karatau 

locality (southern Kazakhstan, Middle- 

Late Jurassic) in the infraorder Elateriformia. 

The systematic position of the 

new genus within the suborder Polyphaga 

is discussed. 

2010010328 

外贝加尔和蒙古 ( 昆虫纲 : 膜翅目 : 

姬蜂科 ) 早白垩世 ichneumonid 一新 

亚科 = A new subfamily of ichneumonids 

from the Lower Cretaceous of 

Transbaikalia and Mongolia (Insecta: 

Hymenoptera: Ichneumonidae). ( 英文 ). 

Kopylov D S. Paleontological Journal, 

2009, 43(1): 83-93 16 图版 . 

A new subfamily of ichneumonids, 

Palaeoichneumoninae, is described from 

the Lower Cretaceous of Transbaikalia 

(Baisa locality) and Mongolia (Bon Tsagan 

and Kholbotu Gol localities). The 

new subfamily is intermediate between 

the archaic subfamily Tanychorinae and 

the Recent Ichneumonidae. It includes 

12 new species, described in three new 

genera: Palaeoichneumon freja gen. et 

sp. nov., P. ornatus sp. nov., P. danu sp. 

nov., P. micron sp. nov., P. mirabilis sp. 

nov., P. tenebrosus sp. nov., P. townesi 

sp. nov., Rudimentifera mora gen. et sp. 

nov., R. suspecta sp. nov., Dischysma 

maculata gen. et sp. nov., D. similis sp. 

nov., and D. ramulata sp. nov. 

2010010329 

以蓝细菌为食的昆虫 = On insect feeding 

on cyanobacteria. ( 英文 ). 

Krivosheina M G. Paleontological 

Journal, 2008, 42(6): 596-599 

A review of 19 dipteran species of the 

families Chironomidae, Ceratopogonidae, 

and Ephydridae, feeding on cyanobacteria, 

which are toxic to the majority 

of other animals, is given. Certain aspects 

of biology and evolution of the 

family Ephydridae, allowing them to 

utilize this food source, are discussed. 

2010010330 

俄罗斯欧洲部分北部三叠纪甲虫新发 

现 ( 鞘翅目 ) = New Triassic beetles 

(Coleoptera) from northern European 

Russia. ( 英文 ). Ponomarenko A G. Paleontological 

Journal, 2008, 42(6): 600- 

606 2 图版 . 

Beetle remains from the Triassic 

Khey-Yaga locality, Nenets National 

District, Korotaikha Basin, Nyadeita 

Formation, Olenekian-Anisian are described. 

Only isolated elytra have been 

found. Tetracoleus tshalyshevi gen. et sp. 

nov. and T. minimus sp. nov. are described 

and assigned to Tricoleidae, and 

six new species are described in formal 

taxa. Tetracoleus is close to Permian tricoleids 

just found in the Newcastle 

Group of Australia and the Vyatkian 

Aristovo locality of northern European 

Russia. The composition of elytra in the 

locality is closer to that of Lower Triassic 

localities than other Middle Triassic 

localities and characterizes the beginning 

of a recovery after the Permian- 

Triassic ecological crisis. Longxianocupes 

Hong in Liu, Liu et Hong, 1985 is 

shown to be a junior synonym of Sogdelytron 

Ponomarenko, 1969. The species 

Palademosyne ovum Ponomarenko, 

2004, P. elongatum Ponomarenko, 2004, 

and P. latum Ponomarenko, 2004 are 

transferred to the genus Pseudochrysomelites 

Handlirsch, 1906. 

2010010331 

鄂西志留纪早期三叶虫 Latiproetus 

Lu,1962 的新材料 = New Material Of 

The Proetid Trilobite Latiproetus 

Lu,1962 From Aeronian (Llandovery,Silurian) 

Of Western Hubei,China. 

( 中文 ). 袁文伟 ; 周志强 ; 周志毅 . 古生物 

学报 , 2009, 48(4): 628-636 

本文描述湖北宜昌、兴山志留纪兰 

多维列世艾隆期蚜头虫类三叶虫 

Latiproetus latili mbatus(Grabau,1925) 

和 Latiproetus 

tenuisChang,1974 的新材料。 

101

Latiproetus Lu,1962 的有效性长期 

多有争论 , 通过新材料研究确认 , 该属 

和 Prantlia Pribyl,1946 的区别在于其 

较短的鞍前区 , 向前收缩较少的头鞍 , 

较微弱的尾肋沟和间肋沟 , 并不具鞍前 

区横脊。该属和 Astroproetus 

Begg,1939 的区别在于其较深的 S1, 清 

晰的 S2, 较小的活动颊刺 , 及宽而清晰 

的尾边缘。因此 , 笔者认为 

Latiproetus 应为有效属。 

2010010332 

中国石蚕巢化石 ( 昆虫纲 , 毛翅目 ) 的发 

现与初步研究 = The Discovery And 

Priliminary Syudy Of Fossil Caddis 

Case In China. ( 中文 ). 黄迪颖 ; 吴灏 ; 董 

发兵 . 古生物学报 , 2009, 48(4): 646- 

653 

毛翅目昆虫幼虫俗称石蚕 , 大部分石 

蚕就地取材 , 构筑不同形状 , 不同质地 

的巢 , 多数为管状。石蚕巢化石是一类 

较重要的遗迹化石 , 在国外中、新生代 

报道较多 , 但在我国未见发表。本文根 

据作者十多年来在华北及东北地区的 

大量野外工作 , 报道了石蚕巢化石在我 

国的发现。介绍了石蚕巢在中侏罗世 

道虎沟动物群 , 早白垩世热河动物群及 

卢尚坟昆虫群中的类型与特征。石蚕 

巢是我国遗迹化石研究中的薄弱环节 , 

实际上它们在中生代中期以后的陆相 

地层分布很广。由于这类昆虫对水质 

变化的敏感性和适应的相对狭隘性 , 可 

用于恢复古环境。一些特殊类型的出 

现 , 对地层对比也将起到作用。 

2010010333 

伊朗厄尔布尔士中部晚白垩世一龙虾 

新种 Paraclytia valashtensis = A new 

lobster Paraclytia valashtensis (Crustacea, 

Decapoda, Nephrobidae) from the 

Late Cretaceous of the crntral Alborz 

Range, Iran. ( 英文 ). McCobb L M E; 

Hairapetian V. Palaeontologische 

Zeitschrift, 2009, 83(2): 419-430 

A new species, Paraclytia valashtensis 

is described. The discovery is a notable 

addition to the sparse decapod fossil record 

of Iran, and this is the first record 

of the genus outside crntral Europe. The 

four previously known species of Paraclytia 

are from Germany and the Czech 

Republic, so this discovery represents a 

significant expansion of the palaeogeographic 

range of the genus. 

2010010334 

希腊克里特地区上中新统 Polyrhachis 

的首例化石记录 = The first fossil record 

of Polyrhachis (Hymenoptera; 

Formicidae: Formicinae) from the Upper 

Miocene of Crete (Greece). ( 英文 ). 

Wappler T; Dlussky G M; Reuter M. 

Palaeontologische Zeitschrift, 2009, 

83(2): 431-438 

Polyrhachis annosus n. sp., based on 

part and counterpart of a unique ant 

worker specimen from Late Miocene 

deposits of the island of Crete (Greece), 

is figured and described here. Features 

of P. annosus unique for the large recent 

genus Polyrhachis include a large first 

gastral segment, a scapus attached at 

some distance from the clypeus, and an 

alitrunk (mesosoma) and petiole each 

with a pair of teeth or spines. The new 

taxon represents the first occurrence of 

the genus in the fossil record. The origin 

and rise of one of the world's largest and 

most distinct ant genera are still a puzzle, 

and closely related genera are quite diverse 

in Tertiary amber deosits. Interestingly, 

the abundance of Polyrhachis in 

Indonesian copal confirms the statement 

that their absence in Baltic amber is not 

casual. 

2010010335 

乌克兰始新世罗夫诺琥珀中牧草虫 

( 缨翅目 , 昆虫纲 ) = Thrips (Thysanoptera, 

Insecta) from the Rovno amber, 

Eocene of Ukraine. ( 英文 ). Shmakov 

A S; Perkovsky E E. Paleontologi- 

102

cal Journal, 2008, 42(6): 669-674 1 图 

版 . 

Seventy-six thrips were discovered in 

Rovno amber. Among these, 67 were 

identified to suborder, 52, to family, 45, 

to genus, and 41, to species level. In total, 

five species, six genera, five families, 

and two suborders are recorded. No undescribed 

taxa have been found so far. 

All the identified thrips, except those of 

the genus Phloeothrips, belong to fossil 

taxa, previously known only from the 

Baltic and Bitterfeld ambers. However, 

the composition of species in the Rovno 

amber is highly unusual due to domination 

of Praedendrothrips avus Priesner, 

1924. This species, rare in the Baltic 

amber, constitutes 49% of all the Rovno 

records. Thus, the Rovno amber, in contrast 

to the Baltic and Bitterfeld ambers, 

is characterized by poor taxonomic diversity 

of thrips and presence of a 

clearly dominant species. 

2010010336 

欧洲晚始新世琥珀中 Formicini 群落 

蚂蚁 ( 膜翅目 , 蚁科 ) = Ants of the tribe 

Formicini (Hymenoptera, Formicidae) 

from Late Eocene amber of Europe. ( 英 

文 ). Dlussky G M. Paleontological 

Journal, 2008, 42(5): 500-513 4 图版 . 

The tribe Formicini (Formicinae) 

from the Late Eocene Baltic, Bitterfeld, 

Rovno, and Scandinavian ambers is revised. 

Ants are recorded for the first 

time from the Bitterfeld and Scandinavian 

ambers. Two new genera (Cataglyphoides 

gen. nov. and Conoformica gen. 

nov.) and six new species (Cataglyphoides 

intermedius sp. nov., Conoformica 

bitterfeldiana sp. nov., Formica 

kutscheri sp. nov., F. palaeopolonica sp. 

nov., F. radchenkoi sp. nov., F. 

zherikhini sp. nov.) are described. A new 

combination, Cataglyphoides constrictus 

(Mayr, 1868), comb. nov., is established. 

A lectotype of Camponotus constrictus 

Mayr, 1868 and a neotype of Formica 

phaethusa Wheeler, 1915 are designated. 

Formica clymene Wheeler, 1915 is recognized 

as a new synonym of F. 

phaethusa Wheeler, 1915. An identification 

key for workers of Formicini species 

from Late Eocene European ambers 

is provided. 

2010010337 

阿穆尔地区上白垩统水生植物 

Quereuxia 叶子上的昆虫卵 = Insect 

ovipositions on aquatic plant leaves 

Quereuxia from the Upper Cretaceous of 

the Amur region. ( 英文 ). Vasilenko D V. 


514-521 4 图版 . 

New form taxa of insect ovipositions 

on aquatic plant leaves Quereuxia from 

the Campanian locality of Udurchukan 

(Amur Region) are described. Endophytic 

ovipositions Paleoovoidus flabellatus 

sp. nov. and P. arcuatus sp. nov. 

do not differ in shape from ovipositions 

of recent damselflies. Exophytic ovipositions 

Palaexovoidus ovoideus gen. 

et sp. nov., P. catenulatus sp. nov., P. 

multus sp. nov., and P. amplus sp. nov. 

belong to insects that develop in the water, 

probably dragonflies of the suborder 

Anisoptera. A new family Palaexovoididae 

fam. nov. is erected. 

2010010338 

Peronopsis Hawle 和 Corda 属 ( 球接 

子目亚目 Agnostina) 的形态发生学 

= Morphogenesis in the genus Peronopsis 

Hawle et Corda (Agnostina). ( 英文 ). 

Naimark E B. Paleontological Journal, 

2008, 42(4): 389-400 4 图版 . 

The morphogenesis of the early 

members of the genus Peronopsis (Trilobita, 

Agnostina) is studied. The pygidium 

of Agnostina exhibits growthrelated 

changes more clearly than the 

cephalon. In Peronopsis inarmata Hutchinson, 

1962 and P. brighamensis 

Resser, 1938 the axial furrow develops 

around the anteroglabella in meraspid 

degree 0. The most significant changes 

occur in the shape of the pygidium axis 

103

and the postaxial field; posterolateral 

spines do not change throughout growth. 

Specific characters continue to develop 

until the advanced holaspid stage. 

Within the genus Peronopsis, three distinct 

growth patterns of the pygidium are 

recognized. Different relative growth 

rates of different parts of the pygidium 

were responsible for the evolutionary 

transitions between the growth patterns. 

The growth pattern when the pygidium 

lacks a postaxial furrow was the most 

primitive and gave rise to a number of 

species with a long axis reaching the 

border, a growth pattern that in turn 

gave rise to the species with the 

postaxial furrow (a character typical of 

Agnostina). The evolution of these 

growth patterns is inferred from ontogenetic 

observations and is supported by 

the stratigraphic succession of Peronopsis 

and their immediate descendants in 

different regional faunas. 

2010010339 

俄罗斯欧洲部分二叠纪 Kaltanidae 

( 昆虫纲 : 长翅目 :Kaltanidae) = 

The first record of Kaltanidae (Insecta: 

Mecoptera: Kaltanidae) from the Permian 

of European Russia. ( 英文 ). Bashkuev 

A S. Paleontological Journal, 

2008, 42(4): 401-405 3 图版 . 

Two new species and a new genus of 

scorpionflies of the family Kaltanidae, 

Pseudochorista occidentalis sp. nov. and 

Kamochorista novokshonovi gen. et sp. 

nov. (Mecoptera: Kaltanidae), are described 

from the Urzhumian of Udmurtia 

(Chepanikha locality). This is the 

first record of kaltanids on the Russian 

Platform. 

2010010340 

罗夫诺琥珀 ( 昆虫纲 : 鞘翅目 : 小蠹 

科 ) 的小蠹虫新种 = New species of 

bark beetles from the Rovno amber (Insecta: 

Coleoptera: Scolytidae). ( 英文 ). 

Petrov A V; Perkovsky E E. Paleontological 

Journal, 2008, 42(4): 406- 

408 4 图版 . 

Two new species of bark beetles are 

described from the Late Eocene Rovno 

amber. Xylechinus mozolevskae sp. nov. 

(Hylesininae: Tomicini) is the first fossil 

representative of this genus, differing 

from recent species in having large triangular 

scales along the suture. 

Taphramites rovnoensis sp. nov. (Scolytinae: 

Dryocoetini) differs from the 

closest species, T. gnathotrichus from 

Baltic amber, in the presence of short 

thin hairs on the elytra. 

2010010341 

俄罗斯二叠纪 Megakhosaridae 科 

( 昆虫纲 ,Grylloblattida) 新发现 = 

New Grylloblattids of the family 

Megakhosaridae (Insecta: Grylloblattida) 

from the Permian of Russia. ( 英文 ). 

Aristov D S. Paleontological Journal, 

2008, 42(3): 269-272 3 图版 . 

New Megakhosaridae (Insecta: Grylloblattida) 

are described from the Permian 

of Russia: Ivakhosara pectinimedia 

gen. et sp. nov., Megakhosarina intricata 

sp. nov. and M. minuscula sp. 

nov. from the Lower Kazanian of Soyana 

(Arkhangelsk Region), M. magna sp. 

nov. from the Urzhumian of Chepanikha 

(Udmurtia), Kargalokhosara terraefossa 

gen. et sp. nov. from the Urzhumian of 

Kargala (Orenburg Region), and Alekhosara 

reticulata gen. et sp. nov. from 

the Severodvinian of Novo- 

Aleksandrovka (Orenburg Region). 

2010010342 

俄罗斯 Udmurtia 地区 Chepanikha 中 

二叠世昆虫新发现 ( 昆虫纲 : 长翅 

目 ,Grylloblattida ) = New insects 

(Insecta: Mecoptera, Grylloblattida) 

from the Middle Permian Chepanikha 

locality, Udmurtia. ( 英文 ). Aristov D S; 

Bashkuev A S. Paleontological Journal, 

2008, 42(2): 159-165 3 图版 . 

New scorpionflies, Asiachorista europaea 

sp. nov. and Petromantis udmur- 

104

tica sp. nov. (Mecoptera: Permochoristidae), 

and new grylloblattids, 

Tshepanichoptera lacera gen. et sp. nov. 

(Grylloblattida: Aliculidae) and Miralioma 

urzhumica sp. nov. (Liomopteridae), 

are described from the Urzhumian 

of Udmurtia (Chepanikha locality). 

Liomopterites novissimus Aristov, 2004 

(Liomopteridae) is redescribed. 

2010010343 

罗夫诺琥珀中 porricondylinae 和 

lasiopterinae 亚科 ( 双翅目 , 瘿蚊 

科 ) 瘿蚊新分类单位 = New gall 

midge taxa of the subfamilies porricondylinae 

and lasiopterinae (Diptera, 

Cecidomyiidae) from the Rovno amber. 

( 英文 ). Perkovsky E E; Fedotova Z A. 


166-175 5 图版 . 

Five new gall midge taxa of the subfamilies 

Porricondylinae and Lasiopterinae 

are described from the Late Eocene 

Rovno amber: Adsumyia integra gen. et 

sp. nov. (Dicerurini), Gratomyia inexigentis 

gen. et sp. nov. (Holoneurini), 

Winnertzia recusata sp. nov. (Winnertziini), 

Kovaleviola injusta gen. et sp. nov., 

and Spungisiola insuperabilis gen. et sp. 

nov. (Brachineurini). 

2010010344 

二叠 - 三叠纪昆虫动物群及其生物地 

理学和二叠 - 三叠纪大灭绝 = On Permian 

and Triassic insect faunas in relation 

to biogeography and the Permian- 

Triassic crisis. ( 英文 ). Shcherbakov D E. 


15-31 8 图版 . 

The taxonomic diversity dynamics of 

pterygote insects in the Permian and 

Triassic at the family/age level are considered. 

Different metrics of taxonomic 

diversity are compared. Biogeographic 

and taphonomic aspects of changes in 

the composition of insect faunas in the 

Permian and about the P-T transition are 

discussed. Some changes in the Permian 

insect faunas are of a biogeographic nature 

and do not indicate global changes 

in diversity. Insects with aquatic immatures 

were rather common in the Permian 

and Early Triassic, but these immatures 

are well represented in only few 

localities. 

2010010345 

European Russia Tatarian 地区 

Chaulioditinae 亚科 ( 昆虫纲 : 

Grylloblattida: Chaulioditidae) 的新 

代表 = New Tatarian representatives of 

the subfamily Chaulioditinae (Insecta: 

Grylloblattida: Chaulioditidae) from 

European Russia. ( 英文 ). Aristov D S. 


32-35 2 图版 . 

New Late Permian grylloblattids of 

the subfamily Chaulioditinae (Chaulioditidae) 

are described: Chauliodites afonini 

sp. nov. (Sokovka locality, Vladimir 

Region; Vyatkian Stage), Ch. gomankovi 

sp. nov. (Novo-Aleksandrovka locality, 

Orenburg Region; Severodvinian 

Stage), and Ch. ponomarenkoi sp. nov. 

(Isady locality, Vologda Region, upper 

Severodvinian Stage). Stratigraphic distribution 

of the subfamily is discussed. 

2010010346 

蒙古 Houtiyn-Hotgor 地区晚侏罗世蟑 

螂 ( 昆虫纲 , 蜚蠊目 ) = Late Jurassic 

cockroaches (Insecta, Blattaria) from the 

Houtiyn-Hotgor locality in Mongolia. 

( 英文 ). Vršanský Peter. Paleontological 

Journal, 2008, 42(1): 36-42 2 图版 . 

A low-diversity cockroach assemblage 

from the Upper Jurassic of the 

Houtiyn-Hotgor locality in Mongolia is 

described, comprising Solemnia alexandri 

gen. et sp. nov. (Caloblattinidae), 

Blattula choutinensis sp. nov. (Blattulidae) 

and a presumed Triassic relict Irreblatta 

relicta gen. et sp. nov. (incertae 

familiae). The carnivorous Raphidiomimidae 

supposedly originated directly 

from the Caloblattinidae. 

105

2010010347 

黎巴嫩琥珀 ( 蜚蠊目 ,Blattina) 中 

的 Blattulidae 科蟑螂一新属和新种 = 

A new genus and species of the cockroach 

family Blattulidae from Lebanese 

amber (Dictyoptera, Blattina). ( 英文 ). 

Anisyutkin L N; Gorochov A V. Paleontological 

Journal, 2008, 42(1): 43-46 2 

图版 . 

A new genus and species of the cockroach 

family Blattulidae, Ocelloblattula 

ponomarenkoi gen. et sp. nov., are described 

from the Early Cretaceous Lebanese 

amber. In the wing venation, the 

new genus is extremely similar to the 

Jurassic genus Blattula Handlirsch, differing 

from the latter in a number of 

characters in its body structure. This find 

reveals much about the body structure of 

the extinct family Blattulidae, which is 

related to ancestors of the suborders 

Mantina and Blattina. 

2010010348 

侏罗纪牧草虫 Liassothrips crassipes 

(Martynov, 1927) 以及它在缨翅目中 

的分类学位置 = The Jurassic thrips Liassothrips 

crassipes (Martynov, 1927) 

and its taxonomic position in the order 

Thysanoptera (Insecta). ( 英文 ). Shmakov 

A S. Paleontological Journal, 2008, 

42(1): 47-52 2 图版 . 

The Late Jurassic thrips Liassothrips 

crassipes (Martynov) is redescribed, and 

its taxonomic position discussed. It is 

shown that the male genitalia of Liassothrips 

are similar to the terebrantian 

type, while the female genitalia resemble 

the tubuliferan type. Therefore, the 

Liassothripidae shows the possible evolutionary 

pathway of tubuliferan thrips. 

Liassothrips is treated as the oldest 

known member of the suborder Tubulifera 

(previously known beginning from 

the Eocene), the ancestors of which belonged 

to the family Aeolothripidae 

(Terebrantia) rather than Thripidae. 

2010010349 

亚洲白垩纪和古近纪早期宝石甲虫 

( 鞘翅目 : 吉丁甲科 ) 新发现以及相 

似甲虫 = New jewel beetles (Coleoptera: 

Buprestidae) and similar beetles from 

the Cretaceous and Early Paleogene of 

Asia. ( 英文 ). Alexeev A V. Paleontological 

Journal, 2008, 42(1): 53-59 2 

图版 . 

A new genus and two new species of 

jewel beetles are described, Andakhudukia 

ponomarenkoi gen. et sp. nov. 

from the Lower Cretaceous of Mongolia 

and Metabuprestium ustkivdense sp. nov. 

from the lowermost Paleogene of the 

Amur Region. In addition, four new 

monotypic genera that share some features 

with jewel beetles are described: 

Cretoelaterium kazanovense gen. et sp. 

nov. from the Lower Cretaceous of 

Eastern Transbaikalia and Cretopoena 

gratshevi gen. et sp. nov. from the 

Lower Cretaceous of Mongolia have 

been referred to the families Elateridae 

and Eucnemidae; Cretofalselaterium 

baiankhongoricum gen. et sp. nov. from 

the Lower Cretaceous of Mongolia and 

Cretogermen turonicum gen. et sp. nov. 

from the Upper Cretaceous of Kazakhstan 

have been erected for isolated elytra 

and placed in Coleoptera incertae sedis. 

2010010350 

罗夫诺琥珀中 Glaesotropis 属新种 

( 昆虫纲 : 鞘翅目 : 长角象虫科 ) = 

New species of the genus Glaesotropis 

(Insecta: Coleoptera: Anthribidae) from 

Rovno amber. ( 英文 ). Gratshev V G; 


2008, 42(1): 60-62 1 图版 . 

A new species of the fungus weevil 

genus Glaesotropis is described from the 

Late Eocene Rovno amber. G. diadiasashai 

sp. nov. differs from G. weitschati 

and G. minor described from Baltic amber 

in having a longer rostrum and in the 

structure of its antennae, with the third 

and fourth antennomeres being longer 

than the first and second ones. Addition- 

106

ally, the new species differs from G. 

weitschati in being smaller, in having 

unswollen frons, and weakly and 

smoothly concave elytral margin near 

hind coxae. The new species also differs 

from G. minor in having an uninterrupted 

posterior transverse carina on the 

pronotum, elytra less convex longitudinally, 

and a slightly broadened rostrum 

at the attachment of antennae. 

2010010351 

波罗的海琥珀中木材甲虫一新属和新 

种 ( 鞘翅目 :Lymexylidae) = A new 

genus and species of timber beetle (Coleoptera: 

Lymexylidae) from the Baltic 

amber. ( 英文 ). Kirejtshuk A G. Paleontological 

Journal, 2008, 42(1): 63-65 1 

图版 . 

Ponomarenkylon alexandri gen. et sp. 

nov. (Melittommatinae) from the Late 

Eocene Baltic amber is described. The 

long filiform antennae and the apparent 

absence of sensillary organs, which are 

frequently present on modified maxillary 

palps in other lymexylids, are evidence 

of the primitive state of the new 

genus. 

2010010352 

褶蚊科 ( 昆虫纲 : 双翅目 ): 研究历史 

和科的限定 = Ptychopteridae (Insecta: 

Diptera): History of its study and limits 

of the family. ( 英文 ). Lukashevich E D. 


66-74 2 图版 . 

The history of the study of extant and 

extinct ptychopterids is reviewed. The 

morphology of the ptychopterid imago 

and preimaginal stages is discussed. 

Synonymy of Eoptychopteridae under 

Ptychopteridae is demonstrated. A new 

system of the family Ptychopteridae is 

proposed; it comprises the subfamilies 

Proptychopterininae (genus Proptychopterina), 

Eoptychopterinae (genera Eoptychoptera, 

Architendipes, Crenoptychoptera, 

Doptychoptera, Nedoptychoptera, 

Leptychoptera), Eoptychopterininae 

(genera Eoptychopterina, 

?Bolboia), Ptychopterinae (genera 

Ptychoptera, Brodilka), and Bittacomorphinae 

(genera Bittacomorpha, 

Bittacomorphella, Probittacomorpha, 

Zhiganka). Ptychopterids appear to 

originate in the Early Jurassic. 

2010010353 

化石鹬虻 ( 双翅目 : 鹬虻科 ) 新属 : 

Protorhagio = Contributions to the 

study of fossil snipe flies (Diptera: 

Rhagionidae): The genus Protorhagio. 

( 英文 ). Mostovski M B. Paleontological 

Journal, 2008, 42(1): 75-80 4 图版 . 

Three new species of the snipe fly genus 

Protorhagio, viz. P. karataviensis sp. 

nov., P. ponomarenkoi sp. nov., and P. 

ruptus sp. nov., are described from the 

Middle-Upper Jurassic Karabastau Formation 

in Kazakhstan. The type species 

of the genus, P. capitatus, is redescribed. 

A key is provided to all known species 

of Protorhagio. 

2010010354 

印度早或中侏罗世膜翅目昆虫 ( 昆虫 

纲 : 胡蜂科 ) 新发现 = New hymenopteran 

insects (Insecta: Vespida) from the 

lower or middle Jurassic of India. ( 英文 ). 

Rasnitsyn A P. Paleontological Journal, 

2008, 42(1): 81-85 3 图版 . 

Hymenopterans Xyelula alexandri 

Rasnitsyn, sp. nov. (Sepulcidae) and Kotaphialtites 

frankmortoni Rasnitsyn, gen. 

et sp. nov. (Ephialtitidae) are described 

from the Lower or Middle Jurassic Kota 

Formation, Andhra Pradesh, India. 

These finds prove a considerable similarity 

between the Gondwanan and 

Laurasian hymenopteran faunas during 

the Jurassic, as well as during the Triassic 

and Cretaceous. 

2010010355 

外贝加尔早白垩世网蝽科 ( 昆虫纲 : 

半翅目 : 异翅亚目 ) 一新种 = A new 

species of Tingidae (Insecta: Hemiptera: 

Heteroptera) from the Lower Cretaceous 

107

of Transbaikalia. ( 英文 ). Golub V B; 

Popov Yu A. Paleontological Journal, 

2008, 42(1): 86-89 3 图版 . 

A new species of lace-bug Sinaldocader 

ponomarenkoi sp. nov. (Tingidae: 

Phatnomatini) is described from the 

Lower Cretaceous Transbaikalian locality 

Baissa. The new species differs from 

the type species S. drakei Popov, 1989 

from the Lower Cretaceous of Mongolia 

in the well-developed lateral carinae of 

pronotal disc and in the details of hemelytral 

venation. 

2010010356 

以色列 Negve 的白垩系化石煤层组合 

中发现的短暂成煤证据 = Evidence of 

temporary mining in the Cretaceous fossil 

mine assemblage of Negev, Israel. 

( 英文 ). Krassilov; Valentin A.. Insect 

Science, 2008, 15(3): 285-290 

Temporary mining is a peculiar behavioral 

trait in leaf parasites requiring 

adaptations of consecutive larval stages 

to the endophytic and ectophytic life. 

The first fossil evidence for the origin of 

the trait comes from the Cretaceous (Turonian) 

plant-insect locality of the 

Negev Desert containing rich trace assemblages 

of leaf parasites, including 

blotch mines with leaf pieces cut out for 

case construction, as well as attached 

larval cases. The host plants are deciduous 

broadleafs or aquatic angiosperms 

with emergent leaves, suggesting that 

initial acquisition of the habit might 

have been related to leaf abscission and 

the risk for the larva being chocked in 

the mine during floods. Unlike tracks of 

permanent miners, temporary mines 

never co-occur on leaves with other type 

mines, which attests to their effect of 

enhancing plant resistance. Mine predation 

appears to have been widespread in 

the Cretaceous biotic community, suggesting 

a possibility of top-down regulation 

of mining habits at this early stage 

of their evolutionary development. 

2010010357 

中国内蒙古中侏罗统道虎沟组发现的 

新的蜉蝣化石 ( 昆虫纲 : 蜉蝣目 ) = 

New fossil mayflies (Insecta : Ephemeroptera) 

from the Middle Jurassic of 

Daohugou, Inner Mongolia, China. ( 英 

文 ). Huang Jian-Dong; Ren Dong; Sinitshenkova 

Nina D; Shih Chung-Kun. Insect 

Science, 2008, 15(2): 193-198 

Jurassonurus amoenus, a new genus 

and species of Siphlonuridae s. l. is described 

from the Middle Jurassic Jiulongshan 

Formation of the Daohugou 

Village, Shantou Township, Ningcheng 

County, Inner Mongolia, China. The 

new species is established by more than 

20 imago and subimago specimens in 

relatively good condition. Detailed description 

and illustration of the specimens 

along with a review of fossil Siphlonuridae 

s. l. are given. Comparing 

with two known dominant nymph species 

Fuyous gregarious Zhang and Kluge, 

2007 and Shantous lacustri Zhang and 

Kluge, 2007 from the same locality, we 

could not find any relationship among 

them. The new species is another dominant 

species in Daohugou beds. 

2010010358 

瑞典 Oland 中寒武世奇异虫属 

paradoxissimu 超带 = The Middle 

Cambrian Paradoxides paradoxissimus 

Superzone on Oland, Sweden. ( 英文 ). 

Weidner T; Nielsen AT. GFF, 2009, 

131(3): 253-268 

Trilobites from the Middle Cambrian 

Paradoxides paradoxissimus Superzone 

on Oland are reviewed, including species 

found in glacial erratic boulders in 

Germany and Denmark. The fauna recorded 

contains 20 species including 10 

agnostids. The succession, up to 70m 

thick, comprises the Aleklinta Member 

of the Borgholm Formation (previously 

known as the Paradoxissimus sandstone 

or siltstone) and a thin overlying conglomerate, 

here informally referred to as 

the Morbylilla conglomerate, forming 

108

the base of the Alum Shale Formation. 

The thin Granulata Conglomerate, including 

a limestone layer previously correlated 

with the Exsulans Limestone, 

forms the base of the Aleklinta Member. 

It has yielded several species characteristic 

of the Triplagnostus gibbus Zone, 

e.g. Ctenocephalus exsulans, Bailiella 

tenuicincta, Solenopleura parva, Parasolenopleura 

aculeata and T. gibbus. The 

Aleklinta Member contains T. gibbus, 

Ellipsocephalus lejostracus and P. aculeata, 

all indicative of the T. gibbus 

Zone. The overlying Morbylilla conglomerate 

contains reworked (?) specimens 

of E. lejostracus and T. gibbus associated 

with Acidusus atavus, Tomagnostus 

fissus, Ptychagnostus affinis, 

Onymagnostus hybridus, Tomagnostella 

cf. truncata, Hypagnostus parvifrons and 

H. mammillatus. Most of these agnostids 

are found in small stinkstone pockets 

within the conglomerate. Tomagnostus 

bothrus? is recorded in Scandinavia for 

the first time. The fauna shows that the 

conglomerate represents the A. atavus 

Zone. The stinkstone pockets indicate 

that the conglomerate was deposited under 

dysoxic oAlum Shaleo conditions. In 

the beach section at Morbylilla, the 

0.16m thick Morbylilla conglomerate is 

overlain by an anthraconite bed, up to 

0.6m thick, representing the Exporrecta 

Conglomerate Bed. 

2010010359 

陆地草食的起源 : 节肢动物对植物组 

织消费的初步模式 = The origin of herbivory 

on land: Initial patterns of plant 

tissue consumption by arthropods. ( 英 

文 ). Labandeira Conrad. Insect Science, 

2008, 14(4): 259-275 

The early fossil record of terrestrial 

arthropod herbivory consists of two 

pulses. The first pulse was concentrated 

during the latest Silurian to Early Devonian 

(417 to 403 Ma), and consists of the 

earliest evidence for consumption of 

sporangia and stems (and limited 

fungivore borings). Herbivorization of 

most of these tissues was rapid, representing 

0 to 20 million-year (m.y.) lags 

from the earliest occurrences of these 

organs in the fossil record to their initial 

consumption (Phase 1). For approximately 

the next 75 m.y., there was a 

second, more histologically varied origination 

and expansion of roots, leaves, 

wood and seeds, whose earliest evidence 

for herbivorization occurred from the 

Middle-Late Mississippian boundary to 

the Middle Pennsylvanian (327 to 309 

Ma). The appearance of this second herbivory 

pulse during the later Paleozoic 

(Phase 2) is accompanied by major lags 

of 98 to 54 m.y. between times of appearance 

of each of the four organ and 

tissue types and their subsequent herbivory. 

Both pulses provide a context for 

three emerging questions. First is an explanation 

for the contrast between the 

near instantaneous consumption of plant 

tissues during Phase 1, versus the exceptionally 

long lags between the earliest 

occurrences of plant tissues and their 

subsequent herbivorization during Phase 

2. Second is the identity of arthropod 

herbivores for both phases. Third is the 

cause behind the overwhelming targeting 

of seed-fern plant hosts during Phase 

2. Regardless of the answers to these 

questions, the trace fossil record of 

plant-arthropod associations provides 

primary ecological data that remain unaddressed 

by the body-fossil record 

alone. 

2010010360 

寒武纪节肢动物抚仙湖虫新议 = A 

new view of the Cambrian arthropod 

Fuxianhuia. ( 英文 ). Bergstrom J; Hou X 

G; Zhang X G; Clausen S. GFF, 2008, 

130(4): 189-201 

Fuxianhuia from the Chengjiang 

fauna is one of the least derived Cambrian 

arthropods. A supposed pair of 

hook-shaped post-antennal appendages 

(Chen et al. 1995) was later reinterpreted 

as a pair of gut diverticula situated in a 

carapace fold (Waloszek et al. 2005). 

109

The latter interpretation of the diverticular 

nature of this structure is verified, but 

we show that the diverticula are situated 

inside a head capsule. This capsule carries 

a pair of antennae. It is shown that 

the head has also a pair of ordinary locomotory 

limbs. It is also demonstrated 

that a number of body segments have 

more than one pair of leas. There is indication 

of a possible pair of small eyes in 

addition to the large pair. The gut may 

include sediment from the substrate, 

which indicates that sediment was ingested. 

Fuxianhuiids share with many 

lobopodians characters such as a lack of 

specialisation between and within the 

ventral appendages. The exopod rises as 

a lateral fold on a straight limb axis, indicating 

an origin as a secondary addition 

to a uniramous limb. The terms Arthropoda 

s.l. (or pan-Arthropoda) and 

Arthropoda s.s. are replaced by Aiolopoda 

Hou & Bergstrom, 2006, and Arthropoda 

(in the original sense). The 

origination of the arthropods is discussed. 

2010010361 

三叶虫呼吸作用的重新评估 = Respiration 

in trilobites: a reevaluation. ( 英 

文 ). Suzuki Y; Bergstrom J. GFF, 2008, 

130(4): 211 - 229 

It has often been taken for granted 

that the outer branch of trilobite limbs 

had a gill function. Since there are no 

thorough analyses of the case, we decided 

to make an attempt. Morphological 

characteristics of arthropod gills are 

defined. There is it need for a large 

area/volume ratio with a cuticle thin 

enough to perform gaseous exchange 

and an anastomosing hemocoel for 

blood circulation. Protection and stability 

are often provided in carapace folds, 

where the upper/dorsal sheet is sclerotized 

and the lower one houses the gill 

area. Where the bivalved ostracode 

carapace is not attached to the body, it is 

such a fold. More often segmental folds 

are in the shape of lateral tergopleurae 

without ventral gill areas. Vascular 

channels and pillars connecting the sclerotized 

and non-sclerotized cuticle of the 

two sides are typical features, and are 

traced in trilobites. The trace is seen 

only as a pattern in the pleural exoskeleton 

between the axis and the doublure, 

exactly the area where there was no ventral 

exoskeleton. This therefore seems to 

be the place for the gills. The gill lamellae 

in limulids are folds from the basal 

part of the appendage, whereas the 

lameLae in trilobites are setae on a distal 

limb branch, the exopod; the two types 

of lamellar structures thus are not homologous. 

It was concluded in it previous 

study Of Ours that the exopod setae 

of trilobites had mechanical rather than 

respiratory functions. The conservation 

of the trilobite type of exopod throughout 

the lamellipedians indicates a fundamental 

role as ventilator of the gills. 

2010010362 

瑞典 Oland 南部特马豆克阶 Djupvik 

和 Kopingsklint 组的三叶虫生物和生 

态地层学 (A. serratus 三叶虫带 ) = 

Trilobite bio- and ecostratigraphy of the 

Tremadocian Djupvik and Kopingsklint 

formations (A. serratus trilobite Zone) 

on southern Oland, Sweden. ( 英文 ). 

Frisk A M; Ebbestad J O R. GFF, 2008, 

130(3): 153-160 

Trilobites of the late Tremadocian 

Apatokephalus serratus trilobite Zone, 

the Ceratopyge fauna, are abundant and 

widely distributed across Baltoscandia. 

During the Tremadocian they occur in 

the initial stable carbonate deposits on 

the platform (the Bjorkasholmen Formation 

in the west; Djupvik and Kopingsklint 

formations in the east). Two 

sections at Ottenby and Degerhamn, 

southern Oland, Sweden, were investigated 

for trilobite abundance distribution. 

At Degerhamn and Ottenby the fauna is 

restricted to 70 and 78 cm respectively. 

In the Degerhamn quarry the fauna appears 

in the Djupvik Formation. At both 

localities the abundance distributions are 

110

similar, with an initial dominance of 

Ceratopyge acicularis and Shumardia 

pusilla, followed by a marked shift to a 

dominance of nileid species (Symphysurus 

angustatus, Varvia longicauda, 

Niteus limbatus). Comparisons with the 

Oslo Region showed a remarkably similar 

distribution pattern, and three biofacies 

are recognized. In the Oslo Region 

the Ceratopyge-Shumardia biofacies, the 

Bienvillia biofacies, and the nileid biofacies 

are developed. Only two of these 

are present on Oland, where the short 

lived drowning represented by the Bienvillia 

biofacies in the Oslo Region is not 

recorded. Within the nileid biofacies, 

Nileus and Varvia are more frequent on 

Oland than in the Oslo Region. The 

three biofacies may be applied to other 

areas of the Baltoscandian platform 

where this facies is present and potentially 

be used to discriminate depth gradients. 

2010010363 

北美和格陵兰下寒武统 ( 第二统第四 

阶 ) 的 Perissopyge( 三叶虫 ) = Perissopyge 

(Trilobita) from the lower 

Cambrian (Series 2, Stage 4) of North 

America and Greenland. ( 英文 ). Stein M; 

Peel J S. GFF, 2008, 130(2): 71-78 

The distinctive trilobite Perissopyge 

phenax was originally described from 

the Henson Gletscher Formation (Cambrian 

Series 2, Stage 4) of central North 

Greenland and reported from the Sekwi 

Formation of Yukon Territory, Canada. 

This latter material is illustrated herein 

for the first time. Perissopyge phenax is 

also currently described from the Paralleldal 

Formation of Peary Land, North 

Greenland, some 100 km east of the type 

locality, where overlying strata correlate 

with the middle-upper Toyonian Stage 

of Siberia (Cambrian Stage 4). Perissopyge 

triangulata, from the Harkless 

Formation (Cambrian Stage 4) of Nevada, 

is also discussed and tectonic deformation 

of the type suite is recognized. 

An indeterminate species of Perissopyge 

is identified in the Ella Island Formation 

of North-East Greenland. The Ella Island 

Formation yields Olenellus hanseni, 

which is possibly synonymous with O. 

cf. truemani from the Henson Gletscher 

Formation. Together, these occurrences 

enhance stratigraphical correlation between 

central North Greenland and 

North-East Greenland and suggest some 

utility for Perissopyge in correlation of 

the lower half of the Laurentian Cambrian. 

2010010364 

瑞典早寒武世似 Walcottella 的金臂 

虫 = A Walcottella-like bradoriid (Arthropoda) 

from the lower Cambrian of 

Sweden. ( 英文 ). Streng M; Ebbestad J O 

R; Moczydlowska M. GFF, 2008, 

130(1): 11-19 

A probable new bradoriid genus and 

species, represented by a single specimen, 

is described tentatively as Walcottella? 

aff. apicalis Ulrich & Bassler from 

lower Cambrian strata of Sweden. The 

specimen comes from the Bergmyrhobben 

section west of Storuman in Vasterbotten 

County, northern Sweden. It was 

found in mudstone in the lower part of 

the Grammajukku Formation, cooccurring 

with a rich acritarch assemblage 

of the Skiagia ornata- 

Fimbriaglomerella membranacea acritarch 

Zone that corresponds to the 

Schmidtiellus trilobite Zone. The specimen 

represents one of the oldest bradoriids 

known from the paleocontinent 

Baltica. Characteristics of the specimen 

are a dorsomedian to mid-dorsal acuminate 

nod and a flattened shell border 

along the free margin, the latter feature 

unknown from other bradoriid taxa. The 

specimen occurs at the same level where 

the first trilobites were found in the investigated 

section. The biogeographic 

affinities of the Baltic bradoriid genera 

to the bradoriid fauna of Avalonia, western 

Gondwana and Laurentia are reviewed 

and discussed. 

111

2010010365 

在塔斯马尼亚的单食性生态系统与古 

老被子植物进化 = Ecological monophagy 

in Tasmanian Graphium macleayanum 

moggana with evolutionary 

reflections of ancient angiosperm hosts. 

( 英文 ). Scriber J Mark; Allen Geoff R; 

Walker Paul W. Insect Science, 2008, 

13(6): 451-460 

Local host plant specialization in an 

insect herbivore may be caused by numerous 

factors, including host-specific 

natural enemy pressures or a local lack 

of suitable host-plant choices that are 

available elsewhere in its range. Such 

local specialization or "ecological monophagy", 

for whatever reason, may reflect 

reduced ability to behaviourally 

accept or physiologically utilize other 

allopatric hosts that are naturally used 

elsewhere by the species. We tested this 

feeding specialization hypothesis using 

the Tasmanian subspecies of Macleay's 

swallowtail butterfly, Graphium macleayanum 

moggana (Papilionidae), 

which uses only a single host-plant species, 

Antherosperma moschatum (southern 

sassafras, of the Monimiaceae). Further 

north, this same butterfly species (G. 

m. macleayanum) uses at least 13 hostplant 

species from seven genera and four 

families (Lauraceae, Rutaceae, Winteraceae, 

and Monimiaceae). Our larval 

feeding assays with G. m. moggana 

from Tasmania showed that certain 

Magnoliaceae and Lauraceae could support 

some larval growth to pupation. 

However, such growth was slower and 

survival was lower than observed on 

their normal southern sassafras host 

(Monimiaceae). We also found that toxicity 

of particular plant species varied 

tremendously within plant families (for 

both the Magnoliceae and the 

Monimiaceae). 

2010010366 

蜻蜓的化石卵 : 回顾和阐释 = Fossil 

ovipositions of dragonflies: Review and 

interpretation. ( 英文 ). Vasilenko D V; 

Rasnitsyn A P. Paleontological Journal, 

2007, 41(11): 1156-1161 2 图版 . 

The paper deals with the stratigraphic 

range and morphology of fossil formations 

on plants interpreted as insect ovipositions. 

Our analysis of the insect fossil 

record has shown that the endophytic 

ovipositions probably belong to the 

Kennedyina and Triadophlebiina (in the 

Paleozoic and Lower Mesozoic) and to 

the Calopterygina (in the Upper Mesozoic 

and Cenozoic). 

2010010367 

西伯利亚地台 (Khorbosuonka 河剖 

面 ) 东北部早寒武世三叶虫 

Eodiscina 亚目 = Trilobites of the suborder 

Eodiscina from the Lower Cambrian 

of the northeastern Siberian platform 

(Khorbosuonka River section). ( 英 

文 ). Korovnikov I V. Paleontological 

Journal, 2007, 41(6): 614-620 3 图版 . 

Trilobites of the suborder Eodiscina 

from the Lower Cambrian section of the 

Khorbosuonka River (Siberian Platform, 

Olenek Uplift) are studied. The stratigraphic 

distribution of these forms in the 

section is shown Two new species, Hebediscus 

sublongus sp. nov. and 

Korobovia khorbosuonica sp. nov., are 

described. This is the first occurrence of 

the genus Korobovia on the Siberian 

Platform. The new record provides additional 

data on morphology and expands 

the paleogeographic range of the genera 

represented by the newly described species. 

2010010368 

古生代 Mesotitanina 亚目的最早代表 

及对巨翅目 ( 昆虫纲 : 多新翅部 ) 系 

统和演化的注释 = The first representative 

of the suborder Mesotitanina from 

the Paleozoic and notes on the system 

and evolution of the order Titanoptera 

(Insecta: Polyneoptera). ( 英文 ). Goro- 

112

chov A V. Paleontological Journal, 

2007, 41(6): 621-625 2 图版 . 

A new subfamily, genus, and species 

(Deinotitaninae subfam. nov., Deinotitan 

orenburgensis gen. et sp. nov.) of 

the family Mesotitanidae (Titanoptera) 

are described from the Severodvinian 

(Upper Permian) of the Orenburg Region. 

This family belongs to the suborder 

Mesotitanina; both are recorded in 

the Paleozoic for the first time. The present 

finding and unpublished data suggest 

that the Mesozoic stage of the evolution 

of the superorder Orthopteroidea 

might start in the Late Permian. Taxonomy 

and early evolution of the order Titanoptera 

are discussed. Minititan nom. 

nov. is proposed for Microtitan Gorochov, 

2003 (nec Microtitan Granger et 

Gregory, 1943). 

2010010369 

多明尼加琥珀中 Micromalthus 成虫 

( 鞘翅目 , 复变甲科 ) 的发现 = On 

the find of adult Micromalthus (Coleoptera, 

Micromalthidae) in Dominican amber. 

( 英文 ). Perkovsky E E. Paleontological 

Journal, 2007, 41(6): 626- 

628 1 图版 . 

An adult of Micromalthus is discovered 

in amber for the first time. The species, 

from the Miocene Dominican amber, 

is described as M. anansi sp. nov., 

and is generally similar to Recent M. 

debilis, but differs in the longer legs and 

antennae. The Miocene species appears 

to be less fetalized than its modern counterpart. 

2010010370 

波罗的海和多明尼加琥珀 Nitidulini 

古土著类群 ( 露尾甲科 : 鞘翅目 ) 中 

古特有树汁甲虫两属新种 = Species of 

two paleoendemic sap beetle genera of 

the Tribe Nitidulini (Nitidulidae: Coleoptera) 

from the Baltic and Dominican 

amber. ( 英文 ). Kirejtshuk A G; Jr. G 

Poinar. Paleontological Journal, 2007, 

41(6): 629-641 7 图版 . 

Omositoidea gigantea Schaufuss, 

1892 is redescribed; O. pubescens sp. 

nov. from the Baltic amber, Palaeometopia 

dominicana gen. et sp. nov. 

and P. colorata gen. et sp. nov. from the 

Dominican amber are described. The 

taxonomic position of the two genera 

and their probable bionomy are discussed. 

2010010371 

瘿蚊化石研究的问题和前景 . 对 M. 

Jaschhof 评论的回复 = Problems and 

prospects in the study of fossil gall 

midges. Reply to the criticism of M. 

Jaschhof. ( 英文 ). Fedotova Z A; 


2007, 41(6): 696-702 

2010010372 

西伯利亚上石炭统蟑螂新发现 ( 昆虫 

纲 : 网翅目 ,Mylacridina) = New 

cockroaches from the Upper Carboniferous 

of Siberia (Insecta: Dictyoptera, 

Mylacridina). ( 英文 ). Anisyutkin L N. 


542-548 3 图版 . 

Cockroaches (Dictyoptera, Mylacridina) 

from the Chunya locality (Upper 

Carboniferous of the Central Siberian 

Plateau) are considered. New representatives 

of the family Phyloblattidae 

Schneider, 1983 (Phyloblatta majuscula 

sp. nov., P. chunyensis sp. nov., Hesperoblatta 

vishniakovae sp. nov., and H. 

secunda sp. nov.) are described. 

2010010373 

罗夫诺琥珀中 Lestremiinae 亚科 ( 双 

翅目 , 瘿蚊科 ) 瘿蚊新发现 = New 

gall midges of the subfamily Lestremiinae 

(Diptera, Cecidomyiidae) from the 

Rovno amber. ( 英文 ). Fedotova Z A; 


2007, 41(4): 437-450 8 图版 . 

Two new genera and eight new species 

of the gall midges subfamily 

Lestremiinae, viz. Berestella insuperabilis 

gen. et sp. nov., Monardia impellu- 

113

cida sp. nov., Xylopriona aristata sp. 

nov. (Micromyini), Aprionus improvisus 

sp. nov., A.? vlaskini sp. nov. (Aprionini), 

Vicemyia immediata gen. et sp. 

nov. (Peromyiini), Cordylomyia cauta 

sp. nov. (Campylomyzini) and Bryomyia 

necessaria sp. nov. (Bryomyiini) from 

the Late Eocene Rovno amber are described. 

New combinations, i.e., Cordylomyia 

declinata (Fedotova, 2004), 

comb. nov. and Cordylomyia magnifica 

(Nel et Prokop, 2006), comb. nov. (both 

are transferred from Neurolyga) are proposed. 

No species in common with the 

fauna from the Baltic amber are recorded. 

2010010374 

直翅目 ( 昆虫纲 ) 翅脉讨论 = On the discussion 

of the wing venation of (Archae)Orthoptera 

(Insecta). ( 英文 ). Rasnitsyn 

A P. Paleontological Journal, 

2007, 41(3): 341-344 

Alternative current approaches to homology 

and nomenclature of the insect 

wing venation are discussed. The differences 

between the opposing viewpoints 

are found to be not as deep as they have 

sometimes been supposed to be, and 

more so, there are some observations 

that could help to smooth current contradictions. 

However, this requires an 

understanding of the evidence presented 

by the disputants and, particularly, an 

understanding of their terminology. 

2010010375 

树脂化石中鲜为人知的直翅类昆虫 

( 多新翅部 ) 新发现 : 第二次交流 = 

New and little known orthopteroid insects 

(polyneoptera) from fossil resins: 

Communication 2. ( 英文 ). Gorokhov A 


156-166 6 图版 . 

New taxa of the suborder Blattina 

(order Dictyoptera), possibly belonging 

to the family Corydiidae (Erucoblatta 

semicaeca gen. et sp. nov., Miocene; 

Proholocompsa gen. nov., Eocene; and 

Holocompsa nigra sp. nov. and H. abbreviata 

sp. nov., Miocene) and belonging 

to the family Ectobiidae (Plectoptera 

electrina sp. nov., Miocene; Agrabtoblatta 

symmetrica gen. et sp. nov. 

and ?Symploce rete sp. nov., Pleistocene) 

are described. The taxonomic position of 

the enigmatic genus Raphidiomimula 

Grimaldi et Ross from the Upper Cretaceous 

is discussed. 

2010010376 

agnostina 不同种间个体发育比较 = 

Comparative ontogeny of different species 

of agnostina. ( 英文 ). Naimark E B. 


69-78 2 图版 . 

This study is focused on the growth 

pattern of agnostids, a group of organisms 

that were very abundant in the 

Cambrian. The developmental patterns 

of six agnostid species are compared. It 

is shown that, like other trilobites, agnostids 

have two developmental stages, 

i.e., meraspid degrees 0 and 1 and the 

holaspid stage. Meraspid degrees are 

named according to the number of released 

thoracic segments. Several molts 

took place during every meraspid stage 

resulting in successive instars with a 

unique set of features. Meraspid degree 

0 includes two or three instars, the first 

and last of which have a distinctive 

morphology and have been encountered 

in most of the species studied. During 

meraspid degree 1, the animal molted 

from two to four times. The number of 

molt stages appears to be speciesspecific. 

The first and last instars are 

easily distinguished from other developmental 

forms. Early holaspids of the 

majority of agnostid species studied also 

have certain features in common. 

2010010377 

评两篇最近发表的关于罗夫诺琥珀中 

含 Lestremiinae( 双翅目 : 瘿蚊科 ) 

包裹体的文章 = A Neontologist’s review 

of two recently published articles 

114

on inclusions of Lestremiinae (Diptera: 

Cecidomyiidae) in Rovno amber. ( 英文 ). 

Jaschhof M. Paleontological Journal, 

2007, 41(1): 103-106 

Two articles on fossil Lestremiinae 

(Diptera: Cecidomyiidae) in Rovno amber 

(Perkovsky and Fedotova, 2004; Fedotova 

and Perkovsky, 2004) are reviewed 

and discussed. As a result, the 

following gall midges species are considered 

Lestremiinae incertae sedis: + 

Aprionus admirandus Fed., + Conarete 

laesus Fed., + Heterogenella sparsa 

Fed., + Micromyia convoluta Fed., + 

Peromyia autonoma Fed., + Peromyia 

miranda Fed., + Peromyia sukachevae 

Fed., + Peromyia zherikhini Fed. (all in 

Perkovsky and Fedotova, 2004), + 

Campylomyza falciformis Fed., + Campylomyza 

superposita Fed., + Neurolyga 

declinata Fed., + Strobliella appropinquata 

Fed., and + Strobliella capitata 

Fed. (all in Fedotova and Perkovsky, 

2004). 

2010010378 

外贝加尔东部中生代晚期 Isophlebiid 

蜻蜓 ( 蜻蜓目 :Isophlebiidae ) = 

Isophlebiid dragonflies from the Late 

Mesozoic of eastern Transbaikalia 

(Odonata: Isophlebiidae). ( 英文 ). Pritykina 

L N. Paleontological Journal, 

2006, 40(6): 636-645 5 图版 . 

Based on the study of more than 300 

isophlebiid specimens from several Late 

Mesozoic sites in eastern Transbaikalia 

(Ukurei, Tergen’, Glushkovo, and Byankino 

formations), new genera and 

species are described: Xeta olovica, Dahurium 

draco, and Sinitsia sophiae. The 

insect-bearing deposits are dated Late 

Jurassic according to analysis of their 

odonatofauna. 

2010010379 

树脂化石中鲜为人知的直翅类昆虫 

( 多新翅部 ) 新发现 : 第一次交流 = 

New and little known orthopteroid insects 

(Polyneoptera) from fossil resins: 

Communication 1. ( 英文 ). Gorokhov A 


646-654 3 图版 . 

New taxa of uncertain position within 

the infraclass Polyneoptera (Gryllomantidae 

fam. nov.: Gryllomantis gen. nov., 

Lower Cretaceous; Mantoblattidae fam. 

nov.: Mantoblatta mira gen. et sp. nov., 

Upper Cretaceous) and within the order 

Dictyoptera (Pseudojantaropterix gen. 

nov., Lower Cretaceous) are described. 

The superfamily Umenocoleoidea of uncertain 

position within the latter order is 

discussed on the basis of new information 

on Jantarimantidae and some other 

Cretaceous Dictyoptera. 

2010010380 

球接子类 Pentagnostus proanabarensis 

Fedoseev, 1999 的生长阶段 = 

Growth and development of agnostids 

Pentagnostus proanabarensis Fedoseev, 

1999. ( 英文 ). Naimark E B. Paleontological 

Journal, 2006, 40(5): 541- 

552 7 图版 . 

Juvenile development of the Middle 

Cambrian agnostid trilobite Pentagnostus 

proanabarensis Fedoseev, 1999 is 

studied. A sequence of eight juvenile 

stages is defined based on changes in 

morphology and measurements. Three 

of them belong to meraspid degree 0, 

another three refer to meraspid degree 1, 

and two represent early holaspid stages. 

Neither the frequency distribution of the 

length of cephalons and pygidia nor the 

length-width scatter diagrams give clear 

clusters of molts; the number of juvenile 

molts can be estimated through the 

analysis of the posteroaxis length distribution. 

Thus, the measurements and 

morphology of some juvenile pygidia 

with vestiges of the pleural and postaxial 

furrows allow reconstruction of the 

number of segments during individual 

growth. At the initial stage of development, 

the pygidial axis of P. proanabarensis 

probably had four segments, 

115

the pygidial axis increased up to no less 

than six segments in adults. 

2010010381 

中国东北和北方侏罗纪蜉蝣 ( 昆虫纲 : 

蜉蝣目 ) 新发现 = New mayfly nymphs 

from the Jurassic of Northern and 

Northeastern China (Insecta: Ephemeroptera). 

( 英文 ). Zhang Junfeng. Paleontological 

Journal, 2006, 40(5): 553- 

559 2 图版 . 

Four new species of mayfly nymphs, 

Furvoneta relicta sp. nov., Clavineta 

eximia sp. nov. (originally Mesoneta antiqua), 

Mesobaetis latifilamentacea sp. 

nov., and Stackelbergisca cylindrata sp. 

nov. are described from the Jurassic of 

China. All these species may have inhabited 

lakes rather than flowing water. 

The geological age and stratigraphical 

correlation of the nymph-bearing strata 

are briefly reviewed. 

2010010382 

罗夫诺和波罗的海琥珀中始新世晚期 

皮蠹新种 ( 鞘翅目 , 皮蠹科 ) = New 

species of Late Eocene dermestid beetles 

(Coleoptera, Dermestidae) from the 

Rovno and Baltic ambers. ( 英文 ). Zhantiev 

R D. Paleontological Journal, 2006, 

40(5): 560-563 3 图版 . 

Fossil beetles of the family Dermestidae 

are reviewed. Three new species are 

described: Dermestes progenitor and 

Megatoma electra from the Baltic amber 

and Dermestes vetustus from the Rovno 

amber (Late Eocene). 

2010010383 

论寒武纪三叶虫定远虫与双岛虫 = On 

The Cambrian Trilobites Tingyuania 

And Dinesus. ( 中文 ). 朱学剑 ; 袁金良 ; 边 

荣春 ; 胡有山 ; 杜圣贤 . 古生物学 

报 , 2009, 48(4): 681-687 

材料表明定远虫 (Tingyuania) 和双岛 

虫 (Dinesus) 这两个三叶虫属是有效的 , 

前者并不是后者的晚出异名。双岛虫 

类的地质延限被下延至传统早寒武世 

晚期的清虚洞组。补充描述首次发现 

的定远虫的尾部 , 并描述双岛虫的一新 

种。 

2010010384 

再论三叶虫 Megapalaeolenus 

Chang,1966 属的无效地位 = Further 

Discussion On The InvaLlidity Of 

Megapalaeolenus Chang,1966. ( 中文 ). 

林天瑞 ; 彭善池 . 古生物学报 , 2009, 

48(4): 695-700 

作者 2004 年根据保存于法国的模 

式标本和产自我国三峡地区的新材料 

以及对以往所发现的化石材料的研究 , 

认为 Megapalaeolenus Chang,1966 一 

属不能成立 , 是 Palaeolenus Mansuy,1912 

的晚出异名 ; 其模式种 

Palaeolenus deprati Mansuy,1912 

也是 Palaeolenus 的模式种 

Palaeolenus douvillei,Mansuy,1912 

的晚出异名。提出属名 

Megapalaeolenus Chang 和种名 

Palaeolenus deprati Mansuy 均应废 

弃的结论。最近 , 罗惠麟等发表了一系 

列采自模式标本产地附近的标本 , 为笔 

者的上述结论提供了更有力的证据。 

根据这些新材料 , 笔者不同意罗惠麟等 

认为 Megapalaeolenus 继续有效、 

Palaeolenus deprati 能够成立的观 

点。 

2010010385 

Krasnoyarsk 地区早石炭世 

Adelophthalmus( 板足鲎亚纲 ) 一新 

种 = A new species of Adelophthalmus 

(Eurypterida) from the lower Carboniferous 

of the Krasnoyarsk Region. ( 英文 ). 

Shpinev E S. Paleontological Journal, 

2006, 40(4): 431-433 2 图版 . 

A new species of Adelophthalmus, a 

genus recorded infrequently in the former 

Soviet Union, is described from the 

Tournaisian of the Krasnoyarsk Region. 

116

2010010386 

西伯利亚二叠纪末期 Lioestheria, 

Mimoleaia 和 Echinolimnadia( 介甲 

目 ) 的微观纹饰 = Microornamentation 

of Lioestheria, Mimoleaia, and Echinolimnadia 

(conchostraca) from the terminal 

Permian of Siberia. ( 英文 ). Orlova E 

F; Sadovnikov G N. Paleontological 

Journal, 2006, 40(3): 276-285 3 图版 . 

Previously unknown minute ornamentation 

patterns of conchostracans are described 

based on SEM investigation of 

several collections from the terminal 

Permian volcanic deposits of the Tunguska 

Syneclise. Lioestheria (Lioestheriidae) 

shows ovally elongated cells 

arranged in rows along the growth bands, 

Mimoleaia (Leaiidae) has large polygonal 

cells with double walls, and Echinolimnaia 

(Echinolimnadiidae fam. nov.) 

displays a pattern with small polygonal 

cells bearing small spines along their 

walls. Diagnoses of genera and species 

are refined. New data about their distribution 

are presented. 

2010010387 

中国东北侏罗纪 Proptychopterina 

( 双翅目 :Eoptychopteridae ) = 

Proptychopterina (Diptera: Eoptychopteridae) 

from the Jurassic of Northeastern 

China. ( 英文 ). Lin Q B; Lukashevich 

E D. Paleontological Journal, 2006, 

40(3): 290-294 2 图版 . 

A complete well-preserved male fly 

from the Jurassic of Daohugou locality 

(Northeastern China) is described as 

Proptychopterina opinata sp. nov. The 

distribution of Proptychopterina is discussed, 

this genus is re-diagnosed, and a 

key to species is provided based on the 

wings. 

2010010388 

通古斯河盆地二叠纪 Taldycupes 属 

(Taldycupedidae, 鞘翅目 ) 一新甲虫种 

= A new bettle species of the genus 

Taldycupes (Taldycupedidae, Coleoptera) 

from the Permian of the Tunguska 

River basin. ( 英文 ). Ponomarenko A G. 


295-296 1 图版 . 

Taldycupes rosanovi sp. nov. is described 

from an isolated elytron from the 

locality of Ilimpeya, Krasnoyarsk Krai, 

Tunguska River basin, Limptekon Formation. 

2010010389 

西伯利亚中生代 ( 昆虫纲 : 毛翅目 ) 

石蛾幼体 = Larvae of caddisflies (Insecta: 

Trichoptera) from the Mesozoic of 

Siberia. ( 英文 ). Ivanov V D. Paleontological 

Journal, 2006, 40(2): 178- 

189 6 图版 . 

Body fossils of caddisfly larvae are 

described for the first time based on material 

from the Lower Cretaceous of Siberia 

(Baissa locality, Neocomian). The 

material includes a fully grown larva of 

Baissoplectrum separatum gen. et sp. 

nov. (Brachycentridae), Creterotesis 

coprolithica gen. et sp. nov. (Leptoceridae), 

and Cretolype minuta gen. et sp. 

nov., a tiny larva probably belonging to 

an uncertain family of the suborder Annulipalpia 

(Hydropsychina). C. coprolithica 

built unusually soft larval cases 

of pellets; these cases are described as a 

separate new indusigenus and indusispecies 

Coprindusia pallida gen. et sp. nov. 

Bionomics, taxonomy, and evolution of 

the Mesozoic larvae of Trichoptera are 

discussed. 

2010010390 

萨克森阶和罗夫诺琥珀中蚂蚁 ( 膜翅 

目 , 蚁科 ) 和蚜虫 ( 同翅目 , 

aphidinea) 的共生现象 = Occurrence 

of ant (hymenoptera, formicidae) and 

aphid (homoptera, aphidinea) syninclusions 

in Saxonian and Rovno ambers. 

( 英文 ). Perkovsky E E. Paleontological 

Journal, 2006, 40(2): 190-192 

Ant species found as syninclusions 

with aphids in Rovno and Saxonian ambers 

are listed for the first time. In a collection 

of 143 pieces of Rovno amber 

117

with worker ants, aphids were found in 

only one syninclusion with Ctenobethylus 

goepperti (Mayr). In a collection of 

Saxonian amber, 53 aphids of the genus 

Germaraphis were found in 152 amber 

pieces with ant workers; five syninclusions 

with aphids contained 19 specimens 

of C. goepperti; two syninclusions 

contained ten specimens of Lasius 

schiefferdeckeri Mayr; and three syninclusions 

contained one specimen each: 

one Camponotus mengei Mayr, one 

Anonichomyrma constricta (Mayr), and 

one Formica flori Mayr. Considering 

that the Rovno and Saxonian collections 

are nearly equal in the number of amber 

pieces, the fundamental difference in the 

number of syninclusions is striking. The 

number of C. goepperti in syninclusions 

is disproportionately high; the proportion 

of syninclusions with aphids and C. 

goepperti is 1.6 times that of all inclusions 

of workers of this species. They 

are found in 31% of examined inclusions 

of workers in the collection of the 

Saxonian amber, but in 50% of syninclusions 

of the entire collection. This 

strongly suggests that C. goepperti and 

Germaraphis formed an association during 

their lifetime. 

2010010391 

化石 grylloblattid nymphs( 昆虫纲 : 

Grylloblattida) 分类学 = Taxonomy 

of the fossil grylloblattid nymphs (Insecta: 

Grylloblattida). ( 英文 ). Aristov D 

S; Novokshonov V G; Pan’kov N N. Paleontological 

Journal, 2006, 40(1): 79- 

89 3 图版 . 

Nymphs of fossil grylloblattid insects 

are revised. Newly described taxa are 

Lemmatonympha gracilissima gen. et sp. 

nov. and Kaltanympha vorcutensis sp. 

nov. from the Verkhne-Syr’yaginsk locality 

(Ufimian, Lek-Vorkuta Formation 

in the Vorkuta Coal Basin), genera Sylvalitoralis 

gen. nov. and Tshebardanympha 

gen. nov. from the Tshekarda 

locality (Kungurian, Koshelevka Formation, 

Middle Urals), Tataronymphakamensis 

gen. et sp. nov. from the 

Tikhie Gory locality (Lower Kazanian, 

linguloid beds of the Baitugan Formation, 

Tatarstan), and Kaltanympha ornata 

sp. nov. from the Kerbo locality 

(Upper Tatarian, lower part of the Degali 

Formation, Evenki Autonomous 

Region). Liomopterites (?) gracilis 

Sharov, 1961 from Lower Kazanian deposits 

of the Kuznetsk Formation in the 

Kuznetsk Basin is transferred to the genus 

Kaltanympha Sharov, 1961; Permonympha 

arcuata Sharov, 1957 from 

the same locality is synonymized under 

Permonympha gracile Sharov, 1957; the 

nymph described from the Karatau locality 

(Upper Jurassic, Karabastau Formation 

in southern Kazakhstan) as Blattogryllus 

karatavicus Rasnitsyn, 1976 is 

excluded from grylloblattids. Keys to 

extinct grylloblattid nymphs are provided. 

2010010392 

伦敦自然历史博物馆中生代 

archostematan 甲虫 ( 昆虫纲 , 鞘翅 

目 , 原鞘亚目 ) 类型 = On the types of 

mesozoic archostematan beetles (Insecta, 

Coleoptera, Archostemata) in the Natural 

History Museum, London. ( 英文 ). 

Ponomarenko A G. Paleontological 

Journal, 2006, 40(1): 90-99 7 图版 . 

About 40 type specimens of archostematan 

beetles from the Jurassic, 

Lower Cretaceous, and Paleogene of 

England, named by P. Brodie, J.O. 

Westwood, C. Giebel, A. Handlirsch, F. 

Zeuner, P. Whalley, and R. Crowson 

and stored in the Paleontological Department 

of the Natural History Museum 

(London) are redescribed. Nine genera 

and 11 species are recognized, three 

genera are assigned to Archostemata for 

the first time. One new species, Tersus 

crowsoni (Schizophoridae), is described. 

2010010393 

拉普捷夫海更新世晚期 - 全新世及近代 

介形类及其对古环境重建的重要性 = 

118

Late Pleistocene-Holocene and Recent 

Ostracoda of the Laptev Sea and their 

importance for paleoenvironmental reconstructions. 

( 英文 ). Stepanova A Yu. 

Paleontological Journal, 2006, 

40(Supplement 2): S91-S204 25 图版 . 

This work is the first detailed description 

of the Late Pleistocene-Holocene 

and Recent Ostracoda of the Laptev Sea. 

A total of 45 species in 22 genera and 13 

families have been identified. All these 

species are described monographically. 

Three different ecological assemblages 

of ostracodes corresponding to different 

combinations of environmental parameters 

have been established; they are restricted 

to three regions of the sea: western-central, 

eastern, and southern. The 

recent ostracode assemblages of the 

Laptev Sea have been compared with 

those from other Arctic areas and are 

most similar to those of the Beaufort and 

Kara seas. Data on recent Ostracoda are 

used for paleoenvironmental reconstructions 

on the eastern shelf and western 

continental slope of the Laptev Sea. For 

this purpose, ostracodes from five sections 

obtained from these parts of the sea 

have been examined. The oldest sediments, 

which are of Late Pleistocene age 

(15.8 cal. ka BP), have been recovered 

in a core from the western continental 

slope. These yielded five ostracode assemblages, 

which correspond to different 

paleoenvironments and replaced 

each other in the course of the rapid 

postglacial sea-level rise, thus showing 

variations in the Atlantic water inflow 

from the west and freshwater discharge 

from the subaerially exposed shelf. On 

the outer shelf of the eastern part of the 

sea, the rapid sea-level rise in the Early 

Holocene (lowermost dating 11.3 cal. ka 

BP) led to a rapid transition from assemblages 

of brackish-water near-shore 

environments to those of modernlike 

normal marine environments; modern 

environments were established about 8.2 

cal. ka ago. Since the core sections from 

the inner shelf correspond to the time 

when the level of the sea had already 

reached its modern values, the changes 

in the taxonomic composition of ostracode 

assemblages primarily mirror 

variations in river runoff. 

棘皮动物 

2010010394 

爪哇中中新世棘皮动物头帕海胆类 

Goniocidaris 属的一个新种 = A new 

species of Goniocidaris Desor (Echinoidea, 

Cidaroida) from the middle Miocene 

of Java. ( 英文 ). Donovan S 

K;Renema W; Lewis D N. Alcheringa, 

2010, 34(1): 87 - 95 

A distinctive suite of cidaroid echinoid 

spines from the middle Miocene 

Bulu Formation of Java is described as 

Goniocidaris paraplu sp. nov. The apical 

primary spines of this species are of 

no more than moderate length, with a 

thorny shaft bearing linear tuberculations; 

the tip is flared and umbrella-like, 

with radial, unbranched thorns. The secondary 

spines are more elongate and 

have incomplete basal discs. No subgeneric 

assignment is attempted, which 

will require more complete material. 

Other Miocene Goniocidaris, mainly 

from Australia, but also Qatar, show no 

close similarities with the Javan species. 

2010010395 

中国贵州省早、中寒武世 Gogiids 

( 始海百合纲 , 棘皮动物门 ) 的形 

态、个体发育和异时发生 = Morphology, 

ontogeny, and heterochrony in 

lower and middle Cambrian Gogiids 

(Eocrinoidea, Echinodermata) from 

Guizhou Province, China. ( 英文 ). Parsley 

Ronald. Paleontological Journal, 

2009, 43(11): 1406-1414 5 图版 . 

Gogiid eocrinoids from the Lower 

Cambrian (Balang Formation — 

Guizhoueocrinus) and basal Middle 

Cambrian (Kaili Formation — Sinoeocrinus, 

Globoeocrinus) in Guizhou 

Province, China are found in great numbers 

and are extremely well preserved as 

119

high fidelity molds in shale/mud sized 

siliciclastics. Because of their numbers, 

complete ontogenetic growth sequences 

have been observed. Significant differences 

in growth patterns (heterochrony) 

are present between Lower and Middle 

Cambrian genera: thecal plates tend to 

be paedomorphic in development, while 

the sutural pores developed between 

them are peramorphic in their development. 

Because of the large surface area 

of theca and brachioles relative to the 

size of the attachment area, considerable 

drag in ambient currents would necessitate 

a strong attachment medium. Anchoring 

by “biogluing”, possibly by collagen, 

directly to the substrate or to biodetritus 

is proposed as the method of attachment. 

2010010396 

沟头帕海胆类的形态学、系统分类位 

置和分布 = Morphology, systematic 

position, and distribution of Bothriocidaroid 

echinoids. ( 英文 ). Solovjev A N. 


1415-1424 14 图版 . 

This is a brief review of conceptions 

of morphology, distribution and systematic 

position of the most ancient echinoid 

group—order Bothriocidaroida. It 

comprises 3 genera: Bothriocidaris, 

Neobothriocidaris, and Unibothriocidaris. 

More than 20 species of these genera 

are distributed from Upper Ordovician 

(Caradocian) to Lower Silurian (Llandoveri) 

in North Western Europe and 

North America. The question of whether 

this group belongs to the class Echinoidea 

or not has been the subject to discussions 

several times, particularly 

based on cladistic methodology. In my 

opinion the peculiarities of bothriocidaroids 

are quite typical of archetype definition 

of this class, however, so-called 

unique modalities of its merons are actually 

prone to variation both inside the 

group and among other echinoid groups. 

For example, Bothriocidaris maquoketensis 

has a structure transitional from 

uniserial to biserial interambulacra, 

however uniserial interambulacra are 

found in Paleozoic family Cravenechinidae 

and in some Cretaceous holasteroids 

and Cenozoic clypeasteroids. 

Unfortunately, such an important feature 

as the apical system is found only in one 

genus Bothriocidaris. 

2010010397 

蒙古奥陶纪瓶形海林檎目棘皮动物的 

发现 = Discovery of Rhombifera (Echinoderms) 

in the Ordovician of Mongolia. 

( 英文 ). Rozhnov S V; Minjin Ch; 

Kushlina V B. Paleontological Journal, 

2009, 43(11): 1425-1431 4 图版 . 

Two new rhombiferan species Echinosphaerites 

mongolicus sp. nov. and 

Stichocystis altaicus sp. nov., described 

from a recently discovered Upper Ordovician 

locality in the Mongolian Altai, 

on the Chegertei River, suggest possible 

biogeographic links between this region 

and Gondwana and Baltica in the Ordovician. 

In the Upper Ordovician beds in 

the East Gobi Depression near Saishand 

Well, we identified the crinoid Ristnacrinus, 

previously recorded from the 

Ordovician of Estonia and Central Asia. 

2010010398 

德国 Eifel 山和波兰 Holy Cross 山 

中、晚泥盆世 Parahexacrinidae 科海 

百合萼杯的首次发现 = First report of 

aboral cups of the crinoid family Parahexacrinidae 

from the Middle and Upper 

Devonian of the Eifel (Germany) and 

the Holy Cross Mountains (Poland). ( 英 

文 ). Bohatý Jan. Paleontological Journal, 

2009, 43(12): 1569-1577 5 图版 . 

The rare Palaeozoic crinoid family 

Parahexacrinidae is reported here for the 

first time from the Lower Givetian of the 

Eifel Synclines (Rhenish Massif), expanding 

the geographic range to Germany. 

Shevchenkocrinus looghiensis 

gen. et sp. nov. is described based on 

isolated ossicles and two aboral cups 

from the Gerolstein and Hillesheim Eifel 

120

synclines and assigned to the family 

Parahexacrinidae. Furthermore, “Hexacrinites 

sp.” sensu Głuchowski (1993), 

from the Upper Frasnian of the Holy 

Cross Mountains (Poland), is transferred 

to the family Parahexacrinidae and classified 

as Parahexacrinitidae sp. I. comb. 

nov. Numerous parahexacrinitid species 

were erected based on the description of 

isolated columnals. New material from 

the Eifel proved that several of these 

species are not distinguishable from 

other crinoid groups, which is demonstrated 

for “Parahexacrinus ellipticus” 

and Melocrinites pyramidalis. 

2010010399 

泥盆纪 Helianthasteridae 科 ( 海星纲 : 

棘皮动物门 ) 的重新评价 = Reevaluation 

of the Devonian family Helianthasteridae 

Gregory, 1899 (Asteroidea: 

Echinodermata). ( 英文 ). Blake D B. Palaeontologische 

Zeitschrift, 2009, 83(2): 

293-308 

Because of their taxonomic and morphologic 

diversity, the asteroids of the 

Lower Devonian Hunsruck Slate of 

Germany are important to both an understanding 

of the history of the class 

Asteroidea and to the interpretation of 

community evolution during the Paleozoic. 

The Helianthasteridae Gregory is 

restricted to Helianthaster and Arkonaster 

Kesling, 1982 (Middle Devonian, 

Canada); Lepidsterella Schuchert is 

similar to other two genera but known 

specimens are of poor quality and as resut 

the status of the genus is uncertain. 

Neither Helianthaster nor other Hunsruck 

asteroids appear closely linked to 

the crown group; instead, functional patterns 

apparently re-emerged through 

time, although identification of specific 

behavior of ancient asteroids is difficult 

to impossible. 

2010010400 

前乌拉尔早二叠世 Catillocrinidae 科 

的多臂海百合新发现 = New multiarmed 

crinoids of the family Catillocrinidae 

from the Lower Permian of 

the Fore-Urals. ( 英文 ). Arendt Yu A. 


61-68 2 图版 . 

New Catillocrinidae Allocatillocrinus 

rarus sp. nov., with a previously unknown 

tegmenal structure, Paracatillocrinus 

shamovi sp. nov., and P. shakhtauensis 

sp. nov., with an unusual relative 

position of the crown and stem are 

described from the Artinskian Stage 

(Lower Permian) of the western slope of 

the Middle and Southern Ural Mountains 

(Boets, Krasnoufimsk, and Shakh- 

Tau localities). The genus Allocatillocrinus 

has not previously been recorded 

from the Permian, while Paracatillocrinus 

has only previously been reported 

from the Upper Permian of Timor 

Island. 

2010010401 

西伯利亚 Lena 河下游中寒武统 

Mayaktakh 组的 Carpozoan 类棘皮动 

物 = Carpozoan echinoderms from the 

Middle Cambrian (Mayaktakh Formation) 

of Siberia (lower reaches of the 

Lena River). ( 英文 ). Rozhnov S V. Paleontological 

Journal, 2006, 40(3): 266- 

275 7 图版 . 

Two new monotypic genera and a 

new monotypic family Rozanovicystidae 

of the class Cincta are described from 

the Middle Cambrian (Mayaktakh Formation) 

of the northeastern part of the 

Siberian Platform. Based on data obtained 

by morphofunctional analysis, 

there is a possibility that these animals 

could move by jet propulsion by ejecting 

water from the opercular aperture. Probable 

homologies of the main skeletal 

parts are discussed. 

分类位置不明 

2010010402 

巴西北部亚马孙盆地 Trombetas 群几 

丁虫 = The Trombetas Group chitinozoans 

of the Amazon Basin, Northern Bra- 

121

zil. ( 英文 ). Azevedo-soares H L C. 

Neues Jahrbuch fur Geologie u. Palaontologie 

/ Abhandlungen, 2009, 253(1): 

133-143 

Using palynological and biostratigraphical 

methods an attempt was made 

to elate the age of the Nhamunda, Pitinga 

and Manacapuru Formations of the 

Trombetas Group by studying chitinozoans 

from fifteen boreholes and thirteen 

outcrops. Up to ninety-one different 

species were found in the outcrops comprising 

for example Margachitina margaritana, 

Sphaerochitina densibaculata 

and Pogonochitina djalmai. The boreholes 

yielded assemblages of twentyfive 

species. 

2010010403 

湖北宜昌陈家河下奥陶统分乡组和红 

花园组的几丁虫序列 = Early Ordovician 

chitinozoans from the Fenghsiang 

and Hunghuayuan Formations in Chenjiahe 

of Yichang, Hubei. ( 中文 ). 张淼 ; 

陈孝红 . 地层学杂志 , 2009, 33(4): 425- 

431 2 图版 . 

系统介绍湖北宜昌陈家河剖面下奥 

陶统分乡组和红花园组的几丁虫分布 

发育特征 , 将分乡组和红花园组的几丁 

虫自下而上划分为 Lagenochitina 

destombesi 带和 Euconochitina symmetrica 

带 , 阐述了几丁虫组合特征 , 并 

与国外同期几丁虫生物带进行了对 

比。 

2010010404 

瑞典中寒武世和晚奥陶世 “ 地中海省 ” 

软舌螺化石 = Mediterranean Province' 

hyoliths from the middle Cambrian and 

Upper Ordovician of Sweden. ( 英文 ). 

Malinky J M; Eriksson M E; Ahlberg P. 

GFF, 2009, 131(4): 281-291 

Nine species of hyoliths are described 

based on material collected in Skane, 

southern Sweden, during the first half of 

the last century. The material derives 

from the middle Cambrian (Cambrian 

provisional Series 3) Exsulans Limestone 

Bed at Almbacken east of Lund 

and the Upper Ordovician (Katian- 

Hirnantian) Lindegard Formation at 

Tommarp west of Simrishamn. The 

Almbacken assemblage consists of three 

taxa; Nephrotheca ruderalis Marek, 

1989?, Buchavilites sp., and Orthothecid 

sp. 3. The Tommarp assemblage comprises 

Bactrotheca deleta Novak, 1891, 

Circotheca sp., Sololites sp., Orthothecid 

sp. 1 and 2, and one species of Quadrotheca 

Sysoev, 1958. Albeit small, the 

collections, altogether comprising some 

twenty specimens, have important paleobiogeographic 

implications for these 

metazoans. All hyoliths documented 

herein were formerly regarded as occurring 

solely in the 'Mediterranean' paleobiogeographic 

province, encompassing 

central and southwestern Europe, and 

North Africa. The material at hand reveals 

that the distribution of Buchavilites 

Marek, 1975, Circotheca 

Sysoev, 1958, Nephrotheca Marek, 1967, 

Quadrotheca, and Sololites Marek, 1967 

is now extended to Baltica, further eroding 

the assumed strongly provincial nature 

of these organisms. 

2010010405 

白海地区东南部文德期底栖的两侧对 

称生物 Palaeophragmodictya spinosa 

( 新种 ) = Palaeophragmodictya 

spinosa sp. nov., a bilateral benthic organism 

from the Vendian of the Southeastern 

White Sea Region. ( 英文 ). 

Serezhnikova E A. Paleontological 

Journal, 2007, 41(4): 360-369 7 图版 . 

A fossil organism, Palaeophragmodictya 

Gehling et Rigby, 1996, previously 

classified within sponges, is found 

for the first time in the Vendian of the 

Arkhangelsk Region. Based on the new 

finds, Palaeophragmodictya is interpreted 

as an attachment disc of a problematic 

animal with combined coelenterate 

and sponge morphology. Typical 

and unique preservational forms from 

the same bedding plane are described. 

122

Three-dimensional fossils are preserved 

as flat impressions at random horizontal 

levels. Bilateral symmetry discovered in 

the ontogeny of Palaeophragmodictya 

spinosa sp. nov. supports the hypothesis 

of initial bilaterality of Cnidaria. 

2010010406 

俄罗斯中部卡洛期晚期一些龙介虫 

( 环节动物门 , 多毛纲 ) 修订 : 第二 

部分 = Contribution to the revision of 

some late Callovian serpulids (Annelida, 

Polychaeta) of Central Russia: Part 2. 

( 英文 ). Ippolitov A P. Paleontological 

Journal, 2007, 41(4): 429-436 1 图版 . 

This paper deals with the revision of 

the species of the genera Mucroserpula, 

Propomatoceros, and Spiraserpula 

(family Serpulidae) from the Upper 

Callovian of the locality Peski (Moscow 

Region). All taxa are described in accordance 

with the current classification of 

fossil serpulid tubes. Two new species 

are described: Propomatoceros barskovi 

sp. nov. and Spiraserpula oligospiralis 

sp. nov. 

2010010407 

俄罗斯中部卡洛期晚期一些龙介虫 

( 环节动物门 , 多毛纲 ) 修订 : 第一 

部分 = Contribution to the revision of 

some late Callovian serpulids (Annelida, 

Polychaeta) of central Russia: Part 1. ( 英 

文 ). Ippolitov A P. Paleontological 

Journal, 2007, 41(3): 260-267 1 图版 . 

Representatives of the families Serpulidae 

and Sabellidae from the Upper 

Callovian of the locality Peski (Moscow 

Region) are described in accordance 

with the current state of supraspecific 

systematics. Species of the genera Cycloserpula, 

Filogranula, Tetraserpula, 

and Metavermilia are revised. One of the 

genera, Cycloserpula, which was previously 

assigned to the family Serpulidae, 

is transferred to the family Sabellidae. A 

new replacement name, Metavermilia 

goldfussi nom. nov., is proposed for the 

species that was previously described as 

Serpula tricarinata Goldfuss, 1831. 

2010010408 

西伯利亚地台寒武纪叶状假足动物和 

毛颚类动物新材料 = New Cambrian 

lobopods and chaetognaths of the Siberian 

Platform. ( 英文 ). Demidenko Yu E. 


234-243 5 图版 . 

The association of isolated remains of 

lobopods with a netlike structure, including 

plates of Microdictyon rozanovi 

sp. nov. and sclerites with spinelike 

process of Onychomicrodictyon 

spiniferum gen. et sp. nov., as well as 

saberlike sclerites of Protohertzina yudomica 

sp. nov. interpreted as grasping 

spines of chaetognaths, is described 

from the middle part of the Inikan Formation 

of the Toyonian Stage of the 

Lower Cambrian (Lermontovia 

dzevanovskii Zone). The diagnoses and 

species composition of the genera Microdictyon 

and Protohertzina are refined. 

古脊椎动物学 

综论 

2010010409 

脊椎动物古生物学中的神经生物学方 

法 = Neurobiological approaches in vertebrate 

paleontology. ( 英文 ). Saveliev S 


573-580 

The study of the central nervous system 

in extinct vertebrates is discussed. 

Historical development of the nervous 

system is restricted to a few morphological 

patterns. The foundation of structural 

conservatism of the nervous system 

is provided by the multifunctional character 

of any adaptive changes in the 

brain of vertebrates. The functional 

structural features allow the use of the 

nervous system for the resolution of 

some difficult questions of vertebrate 

evolution. 

123

2010010410 

波兰中泥盆世早期四足动物的足迹 = 

Tetrapod trackways from the early Middle 

Devonian period of Poland. ( 英文 ). 

Niedźwiedzki G; Szrek P; Narkiewicz K; 

Narkiewicz M; Ahlberg P E. Nature, 

2009, 463(7277): 43-48 

The fossil record of the earliest 

tetrapods (vertebrates with limbs rather 

than paired fins) consists of body fossils 

and trackways. The earliest body fossils 

of tetrapods date to the Late Devonian 

period (late Frasnian stage) and are preceded 

by transitional elpistostegids such 

as Panderichthys and Tiktaalik that still 

have paired fins. Claims of tetrapod 

trackways predating these body fossils 

have remained controversial with regard 

to both age and the identity of the track 

makers. Here we present well-preserved 

and securely dated tetrapod tracks from 

Polish marine tidal flat sediments of 

early Middle Devonian (Eifelian stage) 

age that are approximately 18 million 

years older than the earliest tetrapod 

body fossils and 10 million years earlier 

than the oldest elpistostegids. They force 

a radical reassessment of the timing, 

ecology and environmental setting of the 

fish–tetrapod transition, as well as the 

completeness of the body fossil record. 

鱼类 

2010010411 

来自图瓦晚泥盆世沟鳞鱼的新资料 = 

New data on late Devonian bothriolepidid 

Placoderms (Pisces, Antiarchi) 

from Tuva. ( 英文 ). Moloshnikov S V. 


558-568 6 图版 . 

Bothriolepis sibirica Obruchev and B. 

dorakarasugensis sp. nov. (Pisces, Antiarchi) 

from the Frasnian beds (Upper 

Devonian) of central Tuva are described. 

These species differ from the majority of 

congeners in the pattern of contact between 

the anterior mediodorsal and anterior 

dorsolateral, i.e., in the anterior part 

of contact, the anterior medio-dorsal 

overlies the anterior dorsolateral, while, 

in the posterior part, they change places. 

New data supplement the description of 

B. sibirica Obr. and show certain age 

changes in trunk shield bones of this 

species. 

2010010412 

来自副特提斯东部地区的早 

Sarmatian 期鱼 = On early Sarmatian 

fishes from the Eastern Paratethys. ( 英 

文 ). Bannikov A F. Paleontological 

Journal, 2009, 43(5): 569-573 2 图版 . 

Early Sarmatian bony fish assemblages 

from the Pshekha River (northern 

Caucasus) and the village of Naslavcea 

(northern Moldova) are compared. It is 

proposed that, in the Early Sarmatian, 

connection between the North Caucasian 

and Moldavian basins was hampered 

and the two fish localities were formed 

under different conditions. The impoverished 

taxonomic composition of Sarmatian 

fishes from the Eastern Paratethys is 

attributable to unfavorable chemical 

composition (increased alkalinity) rather 

than to low salinity. 

2010010413 

俄罗斯欧洲部分南部地区泥盆纪胴甲 

鱼 = Devonian antiarchs (Pisces, Antiarchi) 

from central and Southern European 

Russia. ( 英文 ). Moloshnikov S V. Paleontological 

Journal, 2008, 42(7): 691- 

773 53 图版 . 

Antiarchi (Pisces, Placodermi) from 

the Devonian of central and southern 

European Russia (Central Devonian 

Field) are studied. Antiarchs belong to 

three families, the Asterolepididae, Remigolepididae 

(suborder Asterolepidoidei), 

and Bothriolepididae (suborder 

Bothriolepidoidei). The diagnoses of the 

order, two suborders, three families, and 

five genera (two of which are new) are 

given. Sixteen species, including one 

new, are described; ten taxa are determined 

in open nomenclature. Morphological 

structures of representatives of 

124

these families are considered in detail. 

Classifications of antiarchs and their position 

in the system of the lower vertebrates 

are discussed. Devonian vertebrate 

localities of central and southern 

European Russia that have yielded antiarchs 

are listed. Each locality is characterized 

by its ichthyoassemblage. 

2010010414 

俄罗斯下弗拉斯阶 Plourdosteus 

livonicus 及 Mikhailovskii 鱼群的营养 

结构 = The placoderm Plourdosteus 

livonicus (Eastman) in the early Frasnian 

of the Central Devonian Field and 

the trophic structure of the Mikhailovskii 

Fish Assemblage. ( 英文 ). 

Moloshnikov S V. Paleontological 

Journal, 2008, 42(6): 607-614 5 图版 . 

The placoderm Plourdosteus livonicus 

(Eastman) (Euarthrodira, Coccosteina) 

from the Upper Timanian Mikhailovskii 

Fish Assemblage of the Central Devonian 

Field is described. The composition 

and structure of the assemblage are discussed 

and compared with later Frasnian 

fish assemblages of the Central Devonian 

Field. 

2010010415 

北高加索始新世中期鳞鲀科一新属新 

种 : 鳞鲀科的最早成员 = A new genus 

and species of triggerfish from the Middle 

Eocene of the Northern Caucasus, 

the earliest member of the Balistidae 

(Tetraodontiformes). ( 英文 ). Bannikov 

A F; Tyler J C. Paleontological Journal, 

2008, 42(6): 615-620 2 图版 . 

Until now, the earliest known members 

of the triggerfish family Balistidae 

have been two genera from the Oligocene. 

Herein is described the new balistid 

Gornylistes prodigiosus gen. et sp. 

nov. from the uppermost Middle Eocene 

(Kuma Horizon) of the Northern Caucasus 

(Gorny Luch locality); it is as thoroughly 

modern in its bauplan as the taxa 

of balistids from the Oligocene and 

more recent periods, and far more advanced 

morphologically than the several 

stem taxa of the balistoid + ostracioid 

clade known from earlier in the Middle 

and Lower Eocene and from the Upper 

Paleocene. 

2010010416 

俄罗斯中部 Evlanovo 盆地盾皮鱼捕 

食的可能证据 = Possible evidence of 

predation in placoderms (Pisces) of the 

Evlanovo basin of central Russia. ( 英文 ). 

Zakharenko G V. Paleontological Journal, 

2008, 42(5): 522-525 3 图版 . 

Two placoderms of different orders 

from a concretion of the Zyabrevo locality 

(Evlanovo Regional Stage, Frasnian) 

in central Russia are described. Five 

plates of the ventral and lateral sides of 

the trunk armor are assigned to a plourdosteid 

arthrodire. Three bones located 

in the region of its stomach are determined 

as a juvenile ptyctodontid, Ctenurella 

sp. Records providing actual evidence 

of predation in Devonian vertebrates 

are extremely scarce. Finds of this 

kind are listed for the first time. 

2010010417 

高加索北部始新世河豚 Eotetraodon 

属一新种 = A new species of the 

pufferfish Eotetraodon (Tetraodontiformes, 

Tetraodontidae) from the Eocene 

of the Northern Caucasus. ( 英文 ). Bannikov 

A F; Tyler J C. Paleontological 

Journal, 2008, 42(5): 526-530 2 图版 . 

The Eocene pufferfish genus Eotetraodon 

(Tetraodontidae) has previously 

been known only on the basis of E. 

pygmaeus (Zigno, 1887) from the lowermost 

Middle Eocene of Monte Bolca, 

Italy. To Eotetraodon we now add E. 

gornylutshensis sp. nov. from the uppermost 

Middle Eocene of the Kuma 

Horizon of the northern Caucasus 

(Gorny Luch locality). E. gornylutshensis 

sp. nov. differs from E. pygmaeus by 

having much longer ribs and one less 

vertebra in the caudal peduncle. 

125

2010010418 

amphiaspids 分类多样性的演化以及 

在有利生态条件下灭绝的原因 = Evolution 

of taxonomic diversity in amphiaspids 

(Agnatha, Heterostraci: Amphiaspidiformes) 

and the causes of extinction 

in ecologically favorable conditions. 

( 英文 ). Novitskaya L I. Paleontological 

Journal, 2008, 42(2): 181-191 3 图版 . 

Changes in the taxonomic composition 

of Early Devonian amphiaspids represented 

in Siberia by two assemblages 

(from the northwestern Siberian Platform 

and Taimyr) are analyzed. The 

study is performed at the generic level 

and represented by diagrams. Changes 

in the amphiaspid composition are compared 

with changes in the development 

of the Taimyr and platform paleobasins. 

It is shown that shifts in ecological conditions 

at the stages of extinction of amphiaspids 

occurred within the limits of 

changes of abiotic factors (depth, salinity, 

etc.) that are usual for heterostracans. 

The disappearance (extinction) of amphiaspids 

is attributable to the level of 

their morphological organization, which 

caused inefficient adaptations to the developing 

paleoecosystems. The disappearance 

(extinction) of groups resulting 

from inadequate vital adaptations to the 

changing structure of paleoecosystems is 

considered to be a general law of evolution. 

2010010419 

俄罗斯地台中心区域上弗拉斯阶厚甲 

鱼一新种 = A new pachyosteomorph 

arthrodire (Pisces: Placodermi) from the 

Upper Frasnian of the Central Devonian 

Field, Russia. ( 英文 ). Zakharenko G V. 


642-655 7 图版 . 

A new genus and species of pachyosteomorph 

arthrodire, Omalosteus 

krutoensis gen. et sp. nov. from shallowwater 

marine deposits of the Evlanovo 

Regional Stage (Upper Frasnian, Upper 

Devonian) of the Central Devonian Field 

is described. It is tentatively referred to 

the family Trematosteidae Gross, 1932, 

which was earlier believed to be endemic 

to central Europe. The new genus 

is characterized by a rounded, dorsoventrally 

compressed cross section of the 

pectoral region and smooth head shield 

and postcranial membrane bones. The 

centrale is elongated, forming a narrow 

lateral lobe. The praeorbitale, postorbitale, 

and centrale come in contact in the 

center of the orbital region. The mediodorsale 

is wide, its carinal process projects 

considerably posteriorly. The anterior 

margin of the anterior ventrolaterale 

lacks articular facets for the interlaterale. 

2010010420 

俄罗斯库尔斯克市地区 Mikhailovskii 

矿弗拉斯阶下部的 Psammosteiforms 

= Psammosteiforms (Agnatha, Heterostraci) 

from the Lower Frasnian of the 

Mikhailovskii Mine, Kursk Region, 

Russia. ( 英文 ). Moloshnikov S V. Paleontological 

Journal, 2007, 41(5): 558- 

563 4 图版 . 

Psammosteiforms, including Tartuosteus 

(?) zheleznogorskensis, sp. nov. 

and Psammosteus cf. P. praecursor 

Obruchev, from the Lower Frasnian 

(Upper Devonian) of the Mikhailovskii 

Mine (Kursk Region) are described. Agnathans, 

placoderms, crossopterygians, 

and acanthodians from this locality are 

determined. The similarity of the Mikhailovskii 

Fish Assemblage to the assemblage 

of southern Timan suggests it 

be assigned to the Upper Timan Regional 

Stage. 

2010010421 

无颌类属种多样性的演化 = Evolution 

of generic and species diversity in agnathans 

(Heterostraci: Orders Cyathaspidiformes, 

Pteraspidiformes). ( 英文 ). Novitskaya 

L I. Paleontological Journal, 

2007, 41(3): 268-280 4 图版 . 

The evolution of generic and species 

diversity in agnathans (orders Cyathas- 

126

pidiformes and Pteraspidiformes) is analyzed. 

Cyathaspids appeared in the Silurian 

and achieved the peak of diversity 

in the first half of the Early Devonian 

(Lochkovian Stage and its analogues), as 

did pteraspids. Cyathaspids are absent 

from later beds. Pteraspids persisted to 

the end of the Early Devonian, although 

they sharply decreased in number in the 

second half of the Early Devonian 

(Pragian Stage and its analogues in 

Europe and America). Adaptive features 

of cyathaspids and pteraspids are considered. 

Some data on accompanying 

groups are discussed. It is proposed that 

these heterostracan orders became extinct 

mostly because of archaic locomotor 

adaptations and insufficient protection 

from predators. The insufficient 

protection primarily concerns juvenile 

cyathaspids. Cyathaspid and pteraspid 

genera included in the diagrams of 

changes in taxonomic diversity are listed. 

2010010422 

俄罗斯欧洲部分晚二叠世 

Discordichthyiformes = Late Permian 

Discordichthyiformes (Osteichthyes) 

from European Russia. ( 英文 ). Minikh 


40(5): 564-571 3 图版 . 

New Late Permian fishes combining 

features characteristic of several classes 

are analyzed and redescribed. They were 

assigned to the family Discordichthyidae 

of the order Discordichthyiformes comprising 

three genera and four species: 

Mutovinia stella Minich, Geryonichthys 

longus A. Minich, G. burchardi A. 

Minich, and Discordichthys spinifer A. 

Minich (Minikh, 1998). A new species, 

Mutovinia sennikovi sp. nov., is described. 

Due to rapid evolutionary replacement, 

discordichthyids are rather 

useful stratigraphically. The photographs 

of the skeleton and membrane 

bones of these fishes are published for 

the first time. 

2010010423 

“ 泥泞 ” 中的四足动物起源 = Muddy 

tetrapod origins. ( 英文 ). Janvier P; Clément 

G. Nature, 2009, 463(7277): 40-41 

The tracks left by organisms are 

among the most difficult of fossils to 

interpret. But just such evidence puts 

debate about the origins of four-limbed 

vertebrates (which include ourselves) on 

a changed footing 

2010010424 

Rhipidistians 的舌鳃骨骨骼和下鳃肌 

= Hyobranchial skeleton and hypobranchial 

muscles of rhipidistians. ( 英文 ). 

Kanyukin A A. Paleontological Journal, 

2006, 40(3): 297-311 9 图版 . 

The hyobranchial skeleton of the 

porolepiform rhipidistian Laccognathus 

panderi Gross is described. The double 

composition of the ceratohyal in crossopterygians 

is proposed. The urohyal of 

porolepiforms, like that of Latimeria, 

consists of cartilaginous axial and membranous 

peripheral portions. The differences 

between porolepiforms and osteolepiforms 

in the structure of the hyobranchial 

skeleton, particularly, in the 

shape of the urohyal are attributable to 

different arrangements of the hypobranchial 

muscles. Porolepiforms and coelacanths 

have retained the coracomandibularis 

muscle inherited from early gnathostomes, 

whereas the same muscle of 

osteolepiforms was transformed into the 

geniohyoideus muscle. This transformation 

is accounted for by functional 

changes in the hyobranchial apparatus. 

2010010425 

拉脱维亚泥盆纪 Laccognathus 一新 

种 = A new species of Laccognathus 

(Porolepiform Crossopterygii) from the 

Devonian of Latvia. ( 英文 ). Vorobyeva 

E I. Paleontological Journal, 2006, 

40(3): 312-322 8 图版 . 

A new species of the genus Laccognathus, 

L. grossi sp. nov., from the upper 

strata of the Gauja Formation of the 

127

Main Devonian Field (Lode locality, 

Latvia) is established. Morphological 

similarity and differences of the new 

species from the previously described L. 

panderi Gross from the lower strata of 

the Gauja and the Amata Formation of 

Latvia are discussed. 

2010010426 

Iyalepis:Angarichthys 的新替名 = 

Iyalepis nom. nov., a new replacement 

name for Angarichthys Sytchevskaya et 

Yakovlev, 1985 (Pisces, Palaeonisciformes, 

Coccolepididae). ( 英文 ). 

Sytchevskaya E K. Paleontological 

Journal, 2006, 40(3): 339 

2010010427 

Bassanichthys , 始新世鱼 Bassania 

Bannikov, 2004 的新替通用名 ( 真骨 

鱼目 , 鲈形目 ) = Bassanichthys, a 

new replacement generic name for the 

Eocene fish Bassania Bannikov, 2004 

(Teleostei, Perciformes). ( 英文 ). Bannikov 

A F. Paleontological Journal, 

2006, 40(3): 340 

2010010428 

副特提斯东部中新世 centracanthidae 

= On the miocene centracanthidae 

(Teleostei, Perciformes) from the eastern 

Paratethys. ( 英文 ). Bannikov A F. Paleontological 

Journal, 2006, 40(1): 100- 

102 2 图版 . 

A new genus, Naslavcea, is erected 

for the Middle Miocene species Spicara 

fundata Bannikov, 1990 (Centracanthidae) 

from the Lower Sarmatian of 

northern Moldova. This genus is characterized 

by the relatively small number of 

rays in the dorsal and anal fins. At the 

same time, Pelates islamdagicus Prokofiev, 

2001 from the Lower Miocene of 

the Apsheron Peninsula (Azerbaijan) is 

transferred from the family Terapontidae 

to Centracanthidae and referred to the 

genus Spicara. 

2010010429 

亚洲中部和西伯利亚南部早志留世 

thelodonts 的古生物地理学意义 = Palaeobiogeographical 

significance of 

Early Silurian thelodonts from central 

Asia and southern Siberia. ( 英文 ). Zigaite 

Z; Blieck A. GFF, 2006, 128(2): 

203-206 

Early Silurian vertebrates, especially 

agnathans, from central Asia (Tuva and 

northwestern Mongolia) and southern 

Siberia are abundant and diverse. The 

numerous microremains indicate that the 

strata of this region were deposited in 

warm, productive, shallow marine basins. 

The thelodont microremains concerned 

with in this paper are assigned to 

three genera, viz., Loganellia Turner, 

1991, Angaralepis Karatajte-Talimaa, 

1997, and Talimaalepis Zigaite, 2004, of 

which the latter two are endemic to the 

region. In central Tuva, L. tuvaensis 

Karatajte-Talimaa, 1978 is restricted to 

the Lower Silurian. This species is, 

however, considered to occur also in the 

Upper Silurian-Lower Devonian of 

north Greenland. Taking into account 

the taxonomic record of early thelodonts, 

central Asia and southern Siberia may 

be considered as a centre of origin and 

radiation of Silurian thelodonts. It may 

have corresponded to a palaeobiogeographical 

province. 

两栖类 

2010010430 

摩尔多瓦首次发现中新世锄足蟾 = 

The first find of a spadefoot toad (Anura, 

Pelobatidae) in the Miocene of Moldova. 

( 英文 ). P P Skutschas; A F Bannikov. 


433-437 3 图版 . 

A skeleton fragment of a spadefoot 

toad (family Pelobatidae Bonaparte, 

1850) from the Middle Miocene (Early 

Sarmatian) of the Karpov Yar locality 

(northern Moldova) is described. Since 

the material is incomplete, it is only determined 

as Pelobatidae gen. indet. This 

128

is the first spadefoot toad from the Miocene 

of Moldova. 

2010010431 

东欧 Trematosauroid 新发现 : 

1.Inflectosaurus = New data on Trematosauroid 

labyrinthodonts of Eastern 

Europe: 1. Genus Inflectosaurus Shishkin, 

1960. ( 英文 ). Novikov I V. Paleontological 

Journal, 2007, 41(2): 167- 

174 1 图版 . 

New materials and previously unpublished 

data on trematosaurid labyrinthodonts 

from the Early Triassic Bolshoe 

Bogdo locality (Astrakhan Region) are 

described. All cranial trematosaurid 

specimens from this locality are assigned 

to the monotypic genus Inflectosaurus 

based on the postorbital length of 

the skull roof. The diagnosis of the genus 

is amended. The intermediate position 

of Inflectosaurus between Angusaurus 

and Trematosaurus is marked. 

爬行类 

2010010432 

法国晚白垩世土仑期一新的水生 

pythonomorph = A new aquatic pythonomorph 

(Reptilia, Squamata) from 

the Turonian (Late Cretaceous) of 

France. ( 英文 ). Houssaye A. Comptes 

Rendus Palevol, 2010, 9(1-2): 39-45 

Disarticulated vertebrae from the Turonian 

of France display a distinctive 

suite of characters and probably represent 

a new pythonomorph. This taxon 

displays some degree of vertebral 

pachyostosis s.s., often observed in varanoid 

squamates from the Cenomanian- 

Turonian interval of the ‘Mediterranean’ 

portion of the Tethys. The discovery of 

this new material highlights the importance 

of also describing possibly new 

taxa based on isolated remains. 

2010010433 

德国 Sandelzhausen 和 Rothenstein 

13 两产地早 / 中中新世的蛇类动物群 = 

Snake fauna (Reptilia: Serpentes) from 

the Early/Middle Miocene of Sandelzhausen 

and Rothenstein 13 (Germany). 

( 英文 ). Szyndlar Z. Palaeontologische 

Zeitschrift, 2009, 83(1): 55-66 

The Early/Middle Miocene localities 

of Sandelzhausen and Rothenstein 13 in 

southern Germany have yielded remains 

of about 13 ophidian taxa. Both faunas 

document a transitional phase from 

those reported from several late Early 

and Middle Miocene sites of Central and 

Western Europe. The climates of Sandelzhausen 

and Rothenstein 13, as indicated 

by ophidian fossils, were warm, 

although not tropical or subtropical. 

2010010434 

俄罗斯雅库特 Teete 地区中生代晚期 

四足类埋藏学 = Taphonomy of the 

Upper Mesozoic tetrapod Teete locality 

(Yakutia). ( 英文 ). Kolosov P N; vensen 

G V; Mikhailova T E; Kurzanov S M; 

Efimov M B; Gubin Yu M. Paleontological 

Journal, 2009, 43(2): 201- 

207 7 图版 . 

The fauna of the Teete locality (Neocomian, 

Yakutia) includes bivalve and 

gastropod mollusks, palaeoniscid and 

chondrostean fishes, caudate and anuran 

amphibians, choristoderes, lizards, phytophagous 

and predatory dinosaurs, and 

theromorphs (cynodonts). The flora includes 

mosses, horsetails, lycopods, 

ferns, and conifers. The petrographic 

study showed the prevalence in the section 

of volcano-sedimentary rocks. The 

Teete paleobiota dwelled on the alluviallacustrine 

plain in conditions of warm 

humid climate influenced by intense 

volcanic activity. 

2010010435 

蒙古晚白垩世恐龙一新属新种 : 

Ceratonykus oculatus = Ceratonykus 

oculatus gen. et sp. nov., a new dinosaur 

(?Theropoda, Alvarezsauria) from the 

Late Cretaceous of Mongolia. ( 英文 ). 

Alifanov V R; Barsbold R. Paleon- 

129

tological Journal, 2009, 43(1): 94-106 3 

图版 . 

A new dinosaur, Ceratonykus oculatus 

gen. et sp. nov. (Parvicursoridae, Alvarezsauria), 

from the Upper Cretaceous 

(Baruungoyot Formation) of Mongolia 

is described based on a fragmentary 

skeleton. It differs from other alvarezsaurians 

in many characters, including 

the short femora, long tarsometatarsals, 

and considerably reduced third 

metatarsals. The carpometacarpals contain 

spikelike bones. The natural endocast 

of the new taxon shows large acoustic 

tubercles, the ventral position of the 

optic lobes in the midbrain, and the absence 

of a vertical flexure at the brain 

floor. The data obtained cast doubt on 

the taxonomic position of alvarezsaurians 

in the Theropoda. 

2010010436 

巴西东北部阿拉里皮纳盆地一新鳄鱼 

标本 = A new crodogylomorph specimen 

from the Araripe Basin (Crato 

Member, Santana Formation), northeastern 

Brazil. ( 英文 ). Figueiredo R G; 

Kellmer A W A. Palaeontologische 

Zeitschrift, 2009, 83(2): 323-331 

The fossil fauna of the Santana Formation 

comprises many distinct taxa, 

but crocodylomorphs are poorly understood. 

Here we describe a new specimen 

that consists of a complete hind limb 

found in the Crato Member, the basal 

section of the Santana Formation. On the 

basis of a comparative anatomical study 

of the hind limb, whih shows no similarities 

between MPSC-R1137 and other 

crocodylomorphs from the Araripe Basin, 

we tentatively classify this new 

specimen as cf. Susisuchus sp., and provide 

new anatomical information for this 

rather derived crocodylomorph. 

2010010437 

Nedoceratops 和 Diceratus 属同义名 

= Synonymy of the genera Nedoceratops 

Ukrainsky, 2007 and Diceratus Mateus, 

2008 (Reptilia: Ornithischia: Ceratopidae). 

( 英文 ). Ukrainsky A S. Paleontological 

Journal, 2009, 43(1): 116 

2010010438 

东欧二叠纪 Dinomorpha 颅骨形态学 

和演化 = Cranial morphology and evolution 

of Permian Dinomorpha (Eotherapsida) 

of eastern Europe. ( 英文 ). 

Ivakhnenko M F. Paleontological Journal, 

2008, 42(9): 859-995 69 图版 . 

A Revision of the cranial morphology 

of Middle and Late Permian East European 

Dinomorpha (Theromorpha, Eotherapsida) 

resulted in a clarification of 

the taxonomic relationships within this 

group. As the system was constructed, 

four parameters, i.e., morphological, 

biomorph, and geographical and stratigraphic 

ranges, were taken into account 

in each subordinate taxon. The taxon 

Theromorpha is ranked as class, since it 

was primarily formed as a pilidosic 

group (covered with hair), in contrast to 

the class Reptilia, a pholidosic group 

(covered with scales). 

2010010439 

蒙古晚白垩世罕见新角龙一新属和新 

种 :Gobiceratops minutus = The tiny 

horned dinosaur Gobiceratops minutus 

gen. et sp. nov. (Bagaceratopidae, Neoceratopsia) 

from the Upper Cretaceous 

of Mongolia. ( 英文 ). Alifanov V R. Paleontological 

Journal, 2008, 42(6): 621- 

633 3 图版 . 

A new horned dinosaur, Gobiceratops 

minutus gen. et sp. nov. (Bagaceratopidae, 

Neoceratopsia), from the Upper 

Cretaceous Baruungoyot Formation of 

the Khermin Tsav locality (southern 

Mongolia) is described based on a 3.5- 

cm-long skull. The nasal included in the 

orbital border suggests relationship between 

the new taxon and Bagaceratops 

rozdestvenskyi. It is proposed that, 

unlike other neoceratopsian families, the 

130

family Bagaceratopidae is of Paleoasiatic 

origin. 

2010010440 

伏尔加河流域晚白垩世 azhdarchid 一 

新属新种 = A new late Cretaceous 

azhdarchid (Pterosauria, Azhdarchidae) 

from the Volga Region. ( 英文 ). Averianov 

A O; Arkhangelsky M S; Pervushov 

E M. Paleontological Journal, 

2008, 42(6): 634-642 4 图版 . 

A new azhdarchid genus and species, 

Volgadraco bogolubovi gen. et sp. nov., 

is described based on an anterior fragment 

of the mandibular symphysis 

(mandibular beak) and some postcranial 

elements from the Rybushka Formation 

(Upper Cretaceous, Lower Campanian) 

of the Shirokii Karamysh 2 locality, 

Saratov Region. The new taxon is intermediate 

in size and vascularization of 

the mandibular beak between mediumsized 

Turonian-Santonian azhdarchids 

(Azhdarcho, Bakonydraco) and the giant 

Maastrichtian azhdarchid Quetzalcoatlus. 

2010010441 

河北侏罗 - 白垩纪界线最古老的恐爪龙 

类足迹 = The Earliest Known Deinonychosaur 

Tracks From The Jurassic- 

Cretaceous Boundary IN Hebei Province,China. 

( 英文 ). 邢立达 ; 杰瑞德 D 

哈里斯 ; 孙登海 ; 赵慧强 . 古生物学 

报 , 2009, 48(4): 662-671 

记述中国河北省赤城县倪家沟化石 

点一组恐龙行迹 , 并命名一新属新种 --- 

中国猛龙足迹 (Menglongipus sinensis 

ichnogen.et ichnosp.nov.)。足迹来自土 

城子组 , 位于侏罗 - 白垩纪界线。相邻 

的义县组曾发现最古老的恐爪龙类骨 

骼化石 , 而中国猛龙足迹的发现表明恐 

爪龙类早在义县组之前便出现在该地 

区。中国猛龙足迹的造迹者体长约 

65cm, 非常接近于基干的近鸟类。此 

外 , 为四川伶盗龙足迹 

(Velociraptorichnus sichuanensis) 的模 

式标本提供更多细节 , 并讨论驰龙类足 

迹型与其他兽脚类足迹之间的联系。 

2010010442 

蒙古南部始新世中期边齿蜥蜴 ( 蜥蜴 

目 ) 新发现 = New acrodont lizards 

(Lacertilia) from the Middle Eocene of 

southern Mongolia. ( 英文 ). Alifanov V 

R. Paleontological Journal, 2008, 42(6): 

675-685 2 图版 . 

The problematic lizard family Changjiangosauridae, 

representatives of which 

inhabited Asia in the Early Paleogene, is 

discussed. Six new species of this group, 

including Acrodontopsis robustus gen. et 

sp. nov., Agamimus gracilis gen. et sp. 

nov., Graminisaurus interruptus gen. et 

sp. nov., Khaichinsaurus reshetovi gen. 

et sp. nov., Lavatisaurus elegans gen. et 

sp. nov., and Lentisaurus giganteus gen. 

et sp. nov., from the Middle Eocene of 

the Khaichin Uul 2 locality (southern 

Gobi, Mongolia) are described. It is 

shown that Changjiangosauridae are 

probably related to the Late Cretaceous 

Isodontosauridae and recent Uromastycidae; 

independent development of a 

number of dental features in different 

lineages of Acrodonta (Iguania) is corroborated. 

2010010443 

原角龙 ( 鸟臀目 : 新角龙类 ) 的适应 

性特征 = Adaptive features of protoceratopoids 

(Ornithischia: Neoceratopsia). 

( 英文 ). Tereschenko V S. Paleontological 

Journal, 2008, 42(3): 273- 

286 5 图版 . 

The analysis of some morphological 

characteristics of protoceratopoid skeletons, 

the extent of mobility of the vertebral 

column, and the probable adaptive 

significance of these features suggest 

that Bagaceratops had a mostly aquatic 

mode of life, Protoceratops was 

semiaquatic, Udanoceratops was facultatively 

aquatic, and Leptoceratops was 

predominantly terrestrial. Protoceratopoids 

were quadrupeds, with the preva- 

131

lence of hind limbs, probably using slow 

or rapid trotlike gait. An asymmetrical 

locomotion was most likely impossible. 

On dry land, Bagaceratops and Protoceratops 

moved slowly. Udanoceratops 

and Leptoceratops approximately 

equally used rapid and slow locomotor 

modes, although the second could run 

for a longer time than the first. 

2010010444 

沃罗涅什地区白垩纪鱼龙遗迹 = On 

ichthyosaur remains from the Cretaceous 

of the Voronezh Region. ( 英文 ). 

Arkhangelsky M S; Averianov A O; 

Pervushov E M; Ratnikov V Yu; 

Zozyrev N Yu. Paleontological Journal, 

2008, 42(3): 287-291 2 图版 . 

A new ichthyosaur, Platypterygius 

ochevi sp. nov., from the Albian- 

Cenomanian of the Voronezh Region is 

described based on a partial forefin. It 

differs from congeners in the very large 

facet for the lageniformis on the humerus. 

2010010445 

萨拉托夫地区坎帕阶 Polycotylidae 中 

的短颈蛇颈龙 = Short-necked plesiosaurs 

of the family Polycotylidae from 

the Campanian of the Saratov Region. 

( 英文 ). Arkhangelsky M S; Averianov 

A O; Pervushov E M. Paleontological 

Journal, 2007, 41(6): 656-660 2 图版 . 

Fragments of the anterior part of a 

mandibular rostrum and a maxillary 

bone of the plesiosaur Polycotylidae indet. 

from the Karyakino and Beloe Ozero 

localities of the Saratov Region 

(Upper Cretaceous, Campanian) are described. 

The specimens belong to a relatively 

long-snouted polycotylid with a 

mandibular symphysis incorporating 13 

pairs of teeth. A unique feature of this 

plesiosaur is the fact that, in the symphysis, 

the splenial extends to the very 

anterior end of the rostrum. The polycotylid 

from the Campanian of the Saratov 

Region is probably closely related or 

identical to Georgiasaurus from the 

Santonian of the Penza Region, in which 

structural details of the mandibular symphysis 

remain uncertain. 

2010010446 

肉食性恐龙 Tarbosaurus bataar 脑部 

新研究 = A new study of the brain of 

the predatory dinosaur Tarbosaurus 

bataar (Theropoda, Tyrannosauridae). 

( 英文 ). Saveliev S V; Alifanov V R. Paleontological 

Journal, 2007, 41(3): 281- 

289 2 图版 . 

The brain morphology and the topography 

of the cranial nerves on an endocranial 

mold of the theropod dinosaur 

Tarbosaurus bataar (Tyrannosauridae) 

are examined. The brain of this dinosaur 

was constructed based on the reptile archetype, 

with a well-developed specialized 

olfactory analyzer. In terms of development, 

the visual centers were superseded 

not only by the olfactory centers, 

but also by the auditory centers. 

Comparative analysis of the brain structure 

of Tarbosaurus and Tyrannosaurus 

shows clear distinctions in the topography 

of roots of the accessory and 

trigeminal nerves. 

2010010447 

论蒙古 Protoceratopoid 的椎骨 = Key 

to Protoceratopoid vertebrae (Ceratopsia, 

Dinosauria) from Mongolia. ( 英文 ). 

Tereschenko V S. Paleontological Journal, 

2007, 41(2): 175-188 4 图版 . 

A detailed nomenclature and a measurement 

system for vertebrae of Mongolian 

Protoceratopoidea are proposed. A 

key to vertebrae that allow the determination 

of the region of the vertebral column 

and the serial number of each vertebra 

within each region is developed. 

Distinctions in vertebral column between 

two protoceratopoid families 

(Protoceratopidae and Bagaceratopidae) 

are summarized. 

132

2010010448 

俄罗斯 , 哈萨克斯坦和中亚晚白垩世 

Azhdarchids 的新记录 = New records 

of Azhdarchids (Pterosauria, Azhdarchidae) 

from the late Cretaceous of Russia, 

Kazakhstan, and Central Asia. ( 英文 ). 

Averianov A O. Paleontological Journal, 

2007, 41(2): 189-197 3 图版 . 

A review of 12 azhdarchid localities 

in Russia, Kazakhstan, Uzbekistan, and 

Tajikistan is given. New records of unidentifiable 

azhdarchids from the Khodzhakul 

(Cenomanian), Tyul’keli (Turonian-Coniacian), 

Kansai (Santonian), 

Malaya Serdoba, and Beloe Ozero 

(Campanian) localities and a new taxon, 

Aralazhdarcho bostobensis gen. et sp. 

nov. (Shakh-Shakh, Santonian- 

Campanian), are described. 

2010010449 

俄罗斯和乌兹别克斯坦中白垩世 

Ornithocheirids = Mid-cretaceous Ornithocheirids 

(Pterosauria, Ornithocheiridae) 

from Russia and Uzbekistan. 

( 英文 ). Averianov A O. Paleontological 

Journal, 2007, 41(1): 79-86 2 图版 . 

Ornithocheirid remains from 16 localities 

of Russia and Uzbekistan are reviewed. 

New material of ornithocheirids 

from the localities of Mogoito (Barremian-Aptian), 

Stoilo quarry (Albian- 

Cenomanian), and Khodzhakul (Cenomanian) 

is described. The Khodzhakul 

locality has yielded Ornithocheirus (the 

first record of this genus in Asia). 

2010010450 

Tatarstan 地区晚二叠世二齿兽一新 

种 = A new dicynodont (Anomodontia, 

Eotherapsida) from the Upper Permian 

of Tatarstan. ( 英文 ). Kurkin A A. Paleontological 

Journal, 2006, 40(4): 434- 

437 2 图版 . 

A new dicynodont genus and species, 

Idelesaurus tataricus sp. nov. (Cryptodontidae), 

from the Semin Ovrag locality 

(Tatarstan, Tetyushinskii District; 

Upper Permian, Upper Tatarian Substage, 

Severodvinian Horizon) is described. 

The skull patterns of the East 

European and South African Cryptodontidae 

and Aulocephalodontidae are compared 

from the morphofunctional point 

of view. 

2010010451 

困惑中的带羽毛的恐龙 = Feathered 

dinosaurs in a tangle. ( 英文 ). Witmer L 

M. Nature, 2009, 461(7264): 601-602 

dramatic feathered dinosaur fossil 

from the Jurassic of China resolves a 

'temporal paradox'. But it adds intriguing 

complications to the debates on the evolution 

of feathers and flight in birds. 

2010010452 

Fergana 地区森诺曼阶一只似鸟龙 

( 蜥臀目 , 似鸟龙类 ) = On an Ornithomimid 

dinosaur (Saurischia, Ornithomimosauria) 

from the Cenomanian of 

Fergana. ( 英文 ). Averianov A O. Paleontological 

Journal, 2006, 40(3): 323- 

327 2 图版 . 

A fragmentary coracoid of Ornithomimidae 

indet. from the Lower 

Cenomanian of the Abshir River (Kyrgyzstan) 

is described. This is the first 

record of this group in a Cenomanian 

locality of Fergana. The coracoid from 

the Abshir locality is similar in the lateral 

deflection of the glenoid to an endemic 

group of Asiatic Ornithomimidae 

that includes Anserimimus, Gallimimus, 

and taxa from the Cenomanian and Turonian 

of western Uzbekistan. It is most 

similar to the unnamed ornithomimid 

from the Cenomanian of Karakalpakia in 

having a distinct vertical crest that borders 

anteriorly a depression for the coracobrachialis 

brevis muscle. Dinosaurs 

recorded in the Cenomanian of Fergana 

are reviewed. 

2010010453 

生态上不同的恐龙姐妹群显示 

Ornithodira 早期多样性 = Ecologically 

distinct dinosaurian sister group 

133

shows early diversification of Ornithodira. 

( 英文 ). Nesbitt S J; Sidor C A; 

Irmis R B; Angielczyk K D; Smith R M 

H; Tsuji L A. Nature, 2010, 464(7285): 

95-98 

The early evolutionary history of Ornithodira 

(avian-line archosaurs) has 

hitherto been documented by incomplete 

(Lagerpeton) or unusually specialized 

forms (pterosaurs and Silesaurus). Recently, 

a variety of Silesaurus-like taxa 

have been reported from the Triassic period 

of both Gondwana and Laurasia, 

but their relationships to each other and 

to dinosaurs remain a subject of debate. 

Here we report on a new avian-line archosaur 

from the early Middle Triassic 

(Anisian) of Tanzania. Phylogenetic 

analysis places Asilisaurus kongwe gen. 

et sp. nov. as an avian-line archosaur 

and a member of the Silesauridae, which 

is here considered the sister taxon to Dinosauria. 

Silesaurids were diverse and 

had a wide distribution by the Late Triassic, 

with a novel ornithodiran bauplan 

including leaf-shaped teeth, a beak-like 

lower jaw, long, gracile limbs, and a 

quadrupedal stance. Our analysis suggests 

that the dentition and diet of silesaurids, 

ornithischians and sauropodomorphs 

evolved independently from a 

plesiomorphic carnivorous form. As the 

oldest avian-line archosaur, Asilisaurus 

demonstrates the antiquity of both Ornithodira 

and the dinosaurian lineage. The 

initial diversification of Archosauria, 

previously documented by crocodilianline 

archosaurs in the Anisian, can now 

be shown to include a contemporaneous 

avian-line radiation. The unparalleled 

taxonomic diversity of the Manda archosaur 

assemblage indicates that archosaur 

diversification was well underway 

by the Middle Triassic or earlier. 

2010010454 

塔吉克斯坦晚白垩世沉积中似鸟龙 

(Saurischia, 似鸟龙下目 ) 发现 = 

On the finding of ornithomimid dinosaurs 

(Saurischia, Ornithomimosauria) 

in the Upper Cretaceous beds of Tajikistan. 

( 英文 ). Alifanov V R; Averianov 

A O. Paleontological Journal, 2006, 

40(1): 103-108 2 图版 . 

Fragmentary remains of ornithomimids 

(Ornithomimidae indet.) 

from the Lower Santonian (Upper Cretaceous) 

Kansai locality in northwestern 

Fergana (Tajikistan) are described, and 

the composition of its dinosaurian assemblage 

is updated. 

2010010455 

俄罗斯晚二叠世最早的滑行爬行动物 

= The first gliding reptiles from the upper 

Permian of Russia. ( 英文 ). Bulanov 

V V; Sennikov A G. Paleontological 

Journal, 2006, 40(Supplement 5): S567- 

S570 2 图版 . 

Two new gliding reptiles from the 

Late Permian Kul’chumovo-A locality 

(Orenburg Region), Rautiania alexandri 

gen. et sp. nov. and R. minichi sp. nov., 

are described and assigned to the family 

Weigeltisauridae. These finds substantially 

expand the knowledge of the morphology 

of this group and suggest the 

climax state of terrestrial tetrapod communities 

of eastern Europe in the pre- 

Triassic Time, which resulted in the development 

of ecological niches not typical 

of earlier terrestrial vertebrate faunas. 

2010010456 

丹麦博恩霍尔姆岛 Berriasian Rabekke 

组中两栖类和小型爬行类 = 

Amphibians and small reptiles from the 

Berriasian Rabekke formation on Bornholm, 

Denmark. ( 英文 ). Rees J; 

Lindgren J; Evans S E. GFF, 2005, 

127(4): 233-238 

A diverse microvertebrate assemblage 

has been extracted from a limnic lowermost 

Cretaceous (Berriasian) stratum on 

the island of Bornholm, Denmark. The 

assemblage includes numerous remains 

of a wide variety of vertebrate groups 

including fishes, amphibians, reptiles 

and mammals. Herein, we describe the 

134

amphibian and reptilian (excluding Archosauria 

and Chelonia) part of the assemblage 

including indeterminate salamanders, 

frogs and lizards. The former 

findings are of particular interest as they 

represent the first occurrence of Mesozoic 

amphibians in Denmark. 

鸟类 

2010010457 

新第三纪 phasianid 属 ( 鸟纲 : 雉 

科 ) 的系统发生学分析 = Phylogenetic 

analysis of some Neogene phasianid 

genera (Aves: Phasianidae). ( 英文 ). Zelenkov 

N V. Paleontological Journal, 

2009, 43(4): 438-443 1 图版 . 

Phylogenetic analysis based on osteological 

characters of some Neogene 

and Recent phasianids is performed. 

Phylogenetic tree shows close relationships 

of Plioperdix with Ammoperdix 

and Tologuica with Excalfactoria. 

Chauvireria is at the base of the clade 

(Alectoris + (Coturnix + (Excalfactoria 

+ Tologuica))). Palaeoperdix is relatively 

close to the lineage of large 

pheasants. 

2010010458 

恢复孔子鸟 ( 鸟纲 : 孔子鸟目 ) 生活 

方式初探 = An attempt to reconstruct 

the lifestyle of confuciusornithids (Aves, 

Confuciusornithiformes). ( 英文 ). Zinoviev 


43(4): 444-452 3 图版 . 

The lifestyle of some representatives 

of the family Confuciusornithidae is reconstructed 

based on the analysis of osteological 

data, horn structures, and taphonomy. 

Confuciusornithids, which 

resemble extant Phaethon in general appearance, 

fed on fish, catching them 

from the surface layer of freshwater 

lakes. They rested and probably nested 

in trees growing near the basin. When 

moving in the tree canopy, they used the 

second digit of the wing, free from an 

alula and equipped with a welldeveloped 

claw. Unable to take off from 

the ground, they used the fourth digit of 

the forearm, which was free from feathers, 

for climbing tree trunks. A pair of 

elongated caudal feathers (rectrices) 

were probably used to attract mates. 

2010010459 

中亚新近纪 phasianid : 1. 新属 

Tologuica = Neogene phasianids (Aves: 

Phasianidae) of Central Asia: 1. Genus 

Tologuica gen. nov.. ( 英文 ). Zelenkov N 

V; Kurochkin E N. Paleontological 

Journal, 2009, 43(2): 208-215 3 图版 . 

A new genus, Tologuica, with two 

species (T. aurorae sp. nov. and T. karhui 

sp. nov.), from the Middle Miocene 

of the Sharga locality (western Mongolia) 

is described. The new genus shares some 

characters with the extinct genera Palaeocryptonyx, 

Palaeortyx, and Plioperdix 

and with extant Coturnix. The foot 

structure suggests that Tologuica resembled 

in ecology the European genus Palaeortyx 

and was probably adapted to an 

arboreal mode of life, in contrast to the 

terrestrial Coturnix and Plioperdix. 

2010010460 

鴷形类鸟足的构造和可能的演化成因 

机制 ( 鸟纲 : 鴷形目 ) = The structure 

and probable mechanism of evolutionary 

formation of the foot in piciform birds 

(Aves: Piciformes). ( 英文 ). Zelenkov N 


290-297 4 图版 . 

The foot structure of piciform and 

coraciiform birds is examined in detail. 

Certain similarity in foot structure between 

woodpeckers and woodhoopoes is 

shown and provides the basis for the 

model of the evolutionary formation of 

the zygodactyl foot. It is shown that African 

mousebirds and the Madagascan 

Leptosomus discolor are probably the 

closest relatives of piciforms. A brief 

review of fossil groups presumably belonging 

to the piciform stem is provided. 

135

2010010461 

俄罗斯欧洲部分晚白垩世原始鸟的大 

脑 = On the brain of a primitive bird 

from the upper Cretaceous of European 

Russia. ( 英文 ). Kurochkin E N; Saveliev 

S V; Postnov A A; Pervushov E M; 

Popov E V. Paleontological Journal, 

2006, 40(6): 655-667 6 图版 . 

Cerebavis cenomanica gen. et sp. nov. 

from the Middle Cenomanian of the 

Volgograd Region (Russia) is described 

based on a brain mold. The brain of 

Cerebavis is characterized by a mosaic 

combination of primitive and advanced 

features. The brain weight is estimated 

as approximately 1 g. The cerebrum is 

relatively very large, but lacks sulci. The 

brain mold has long olfactory lobes with 

large olfactory bulbs, a well-developed 

epiphysis, and a parietal organ. The 

auditory tubercles on the dorsal surface 

of the midbrain are well developed. The 

optical lobes are located under the auditory 

lobes, caudoventral to the cerebral 

hemispheres. The cerebellum is not preserved, 

but its imprints just behind the 

midbrain suggest that it was probably 

relatively small and extended dorsoventrally. 

The brain of Cerebavis is similar 

in some features to that of Archaeopteryx, 

but is substantially more advanced 

and more specialized. Cerebavis is similar 

to living ornithurine birds in the large 

cerebral hemispheres, but differs in the 

absence of a well-developed neostriatum, 

the presence of excessively developed 

olfactory lobes, and in the pattern of the 

midbrain. Thus, senses of smell, eyesight, 

and hearing were well developed 

in Cerebavis. It could have been equally 

active in the afternoon and at night. The 

unique brain design demonstrated by 

Cerebavis has not been repeated in subsequent 

evolution. It provides evidence 

for a wide diversity of feathered creatures 

in the past. Cerebavis probably belongs 

to the Enantiornithes. 

哺乳类 

2010010462 

欧洲绝灭的更新世洞穴熊 Ursus spelaeus 

的咬合力 = Bite force of the extinct 

Pleistocene Cave bear Ursus spelaeus 

Rosenmüller from Europe. ( 英文 ). 

Grandal-d’Anglade A. Comptes Rendus 

Palevol, 2010, 9(1-2): 31-37 

In this paper, I have made a theoretical 

calculation of the Cave bear's bite 

force (BF) following the “dry skull 

method” and I present for the first time 

BF data that can be of interest to elucidate 

the mechanisms underlying the dietary 

choice of the Cave bears. In the 

skulls studied, males show higher BF 

than females in absolute terms, but more 

similar with regard to their body mass, 

which partly compensates for the 

smaller size of the females. The whole 

sample studied shows lower BF in the 

upper carnassial than those of large cats, 

similar to the one calculated for the Giant 

panda and higher than that of Polar 

bear. 

2010010463 

匈牙利外多瑙河南部晚第四纪毛状猛 

犸化石 = Late Quaternary woolly 

mammoth (Mammuthus primigenius 

Blum) remains from southern Transdanubia, 

Hungary. ( 英文 ). Konrád G; 

Kovács J; Halász A; Sebe K; Pálffy H. 

Comptes Rendus Palevol, 2010, 9(1-2): 

47-54 

Six samples of subfossil tusk, bone 

and tooth remains from the woolly 

mammoth (Mammuthus primigenius 

Blum) were discovered in south-western 

Hungary. The remains are relatively 

well preserved in a Late Pleistocene 

loess deposit. The samples have been 

radiocarbon dated (AMS) and are of 

Late Weichselian (MIS 2) age (21.8– 

24.1 ka cal BP). The skull fragments, the 

tusks and maxillary teeth are in close 

proximity to associated postcranial remains, 

indicating that the mammoth died 

where it was found. The size and characteristics 

of skeletal elements have al- 

136

lowed us to determine that this was a 

mature male of about 38 years of age. 

2010010464 

西西伯利亚早白垩纪哺乳动物 :2. 

Tegotheriidae = Early Cretaceous 

mammals of Western Siberia: 2. Tegotheriidae. 

( 英文 ). Lopatin A V; Averianov 

A O; Maschenko E N; Leshchinskiy 

S V. Paleontological Journal, 2009, 

43(4): 453-462 7 图版 . 

New specimens of the tegotheriid 

docodont Sibirotherium rossicum 

Maschenko et al., 2003, including a 

maxillary fragment with two posterior 

teeth, an isolated upper molar, and mandibular 

fragments with teeth from the 

Early Cretaceous Shestakovo locality 

are described. The dental formula of Sibirotherium 

is I 1 + ? C1P 6 M 6? . The upper 

molars of Sibirotherium, with two main 

labial and three lingual cusps, are convergently 

similar to the molars of tribosphenic 

mammals. In the dentary, the 

symphysis is short and Meckel’s groove 

is reduced. Sibirotherium is similar in 

the structure of lower teeth to Tegotherium 

from the Upper Jurassic of Mongolia; 

it is the latest known representative 

of Docodonta. 

2010010465 

俄罗斯 Chleuastochoerus 的首次发现 

= The first record of Chleuastochoerus 

(Suidae, Artiodactyla) in Russia. ( 英文 ). 

Vislobokova I A. Paleontological Journal, 

2009, 43(6): 686-698 7 图版 . 

A new species, Chleuastochoerus tuvensis, 

from the Late Miocene Taralyk- 

Cher locality in Tuva is described. Phylogenetic 

relationships and lifestyle of 

Chleuastochoerus, a unique member of 

the family Suidae, are discussed. 

2010010466 

哺乳类动物中耳可能的二源成因 : 单 

孔目兽亚纲 = Probable diphyletic formation 

of the mammalian middle ear: 

Monotremata and Theria. ( 英文 ). 

Tatarinov L P. Paleontological Journal, 

2009, 43(12): 1578-1599 29 图版 . 

The first steps in the formation of the 

middle ear of the mammalian type, with 

the tympanum and three auditory ossicles, 

have only been passed by higher 

cynodonts. They have an incipient 

malleus, which developed from the anterior 

process of the articulare rather than 

the retroarticular process, which is rudimentary 

in cynodonts. The tympanic 

bone is formed of the anterior projections 

of the angulare. In some gorgonopians, 

the retroarticular process is elongated 

and curved anteriorly, resembling 

the malleus of mammals; however, this 

is only convergent similarity. 

2010010467 

哺乳纲中耳鼓膜的起源 = On the origin 

of the tympanic membrane the middle 

ear of mammals. ( 英文 ). Tatarinov L 

P. Paleontological Journal, 2010, 44(1): 

92-94 0 图版 . 

The tympanic membrane appeared in 

the evolution of archaic mammals, when 

the articulare had already lost its function 

in the jaw articulation. Even earlier 

the quadrate and, then, the articular bone 

had acquired the role of additional auditory 

ossicles. 

2010010468 

单孔目起源于 Eotherapsid 的假说 = 

Eotherapsid hypothesis for the origin of 

Monotremata. ( 英文 ). Ivakhnenko M F. 


237-250 9 图版 . 

Comparative study of the cranial 

structures (lateral wall of the braincase, 

temporal and tympanic regions) of 

mammals and theromorphs shows that 

Monotremata evolved from the eotherapsid 

stem of theromorphs, while 

therian mammals are descendants of 

eutherapsids. 

137

2010010469 

德国南部 Sandelzhausen 中新世兔形 

类 = Lagomorphs from the Miocene of 

Sandelzhausen (southern Germany). ( 英 

文 ). Angelone C. Palaeontologische 

Zeitschrift, 2009, 83(1): 67-75 

Three gnera of lagomorphs, Prolagus, 

Lagopsis, and "Amphilagus," were identified 

during a revision of the lagomorph 

material from Sandelzhausen. Evidence 

of two morphological and dimensional 

classes were observed at some tooth positions 

in Prolagus (some p3 show an 

unmistakable P. oeningensis morphology, 

others closely resemble P. crusafonti), 

but not at other tooth positions 

(e.g., M1-2). Insufficient data from Sandelzhausen 

precludes identification of 

two different species of Prolagus from 

this locality, and to define the characteristics 

2010010470 

Anthitherium aurelianense: 德国中新 

世 Sandelzhausen 地区食草大哺乳动 

物群落中一杂食的食草动物 = Anchitherium 

aurelianense (Equidae, 

Mammalia): a brachydont "dirty 

browser" in the community of herbivorous 

large mammals from sandelzhausen 

(Miocene, Germany). ( 英文 ). Kaiser T 

M. Palaeontologische Zeitschrift, 2009, 

83(1): 131-140 

The mesowear method was applied to 

reconstruct the dietary regime of A. aurlianense 

from Sandelzhausen. Hierarchical 

cluster statistics and principal 

component analysis was performed on 

mesowear variables. Thirty-five upper 

cheek teeth of A. aurelianense were analysed, 

and mesowear signatures compared 

with those of five ruminant species 

from Sandelzshausen. The extant 

analogue species indicate that A. 

aurelianense at Sandelzhausen had a dietsimilar 

in abrasiveness to that of extant 

mixed feeders and that the Sandelzhausen 

ruminants all occupied a browsing 

niche with little or no abrasives in 

their diet. 

2010010471 

德国 Sandelzhausen 地点中新世 

Keramidomys = The Miocene Keramidomys 

( Rodentia, Eomyidae) from the 

Sandelzhausen locality (Germany). ( 英 

文 ). Mein P. Palaeontologische 

Zeitschrift, 2009, 83(1): 141-150 

In this note the taxonomic position of 

the tiny eomyid genus Keramidomys 

from the Early-Middle Miocene boundary 

locality of Sandelzhausen in the Bavarian 

Upper Freshwater Molasse is reexamined. 

It is shown that the Sandelzhausen 

eomyid must be called K. thaleri 

Hugueney & Mein, 1968 on the basis of 

several morphological dental differences 

from K. carpathicus Schaub & Zapfe, 

1953. This rodent seems to be an immigrant 

from East Asia into Europe. Even 

if K. thaleri is known in many european 

localities, all correlated to MN5, it is always 

a rare element of European rodent 

faunas. Differentiation from K. carpathicus 

is not easy and requires a sufficiently 

large sample. 

2010010472 

德国 Sandelzhausen 产地中新世食肉 

动物群落 = The carnivoran community 

from the Miocene of Sandelzhausen 

(Germany). ( 英文 ). Nagel D; Stefen C; 

Morlo M. Palaeontologische 

Zeitschrift, 2009, 83(1): 151-174 

From the Bavarian Early/Middle 

Miocene site Sandelzhausen, nine species 

of carnivoran mammals are identified 

including the hemicyonine ursid- 

Hemicyon stehlini, the amphicyonids 

Amphicyon cf. major and Pseudarctos 

bavaricus, the mustelids Ischyrictis zibethoides 

and Martes cf. munki, the mephitid 

Proputorius pusillus, viverrid 

Leptoplesictis cf. aurelianensis, the felid 

Pseudaelurus romieviensis, and finally 

the recrntly described barbourofelid 

Prosansanosmilus eggeri. With these 

138

taxa present, Sandelzhausen shows a 

carnivoran community typical, though 

deprived, for lthe Lower to Middle Miocene 

of Europe, but different from 

roughly contemporary Mediterranean 

faunas such as those from Candir or 

Pasalar in Turkey. 

2010010473 

德国南部 Sandelzhausen 产地中新世 

海狸 = The beaver (Mammalia, Castoridae) 

from the Miocene of Sandelzhausen 

(southern Germany). ( 英文 ). Stefen C. 


83(1): 183-186 

The Early-Middle Miocene boundary 

locality Sandelzhausen yielded three 

beaver teeth: one lower incisor fragment 

and two strongly worn upper premolars, 

a right and a left one. The latter are so 

similar in wear, height, size, and enamel 

pattern that they probably represent one 

individual. Although the teeth have been 

referred to Chalicomys jaegeri Kaup, 

1832, it seems more likely that they belong 

to Steneofiber depereti Mayet, 

1908. However, the assignment of the 

present material to either one of these 

species is difficult, besause in the advanced 

wear stage some diagnostic 

characteristics cannot be assessed. 

2010010474 

德国南部 Sandelzhausen 产地中新世 

Democricetodon 和 Megacricetodon = 

Democricetodon and Megacricetodon 

(Mammalia, Cricetidae) fom the Miocene 

of sandelzhausen, southern Germany. 

( 英文 ). Wessels W; Reumer B M. 


83(1): 187-205 

The cricetid species Memocricetodon 

gracilis, Democricetodon mutilus, 

Megacricetodon bavaricus, and 

Megacricetodon minor from Sandelzhausen 

are represented by more than 

2,000 molars providing substantial data 

on the variability in sizes and on variation 

in morphologies. Temporal and spatial 

distributions of these species indicate 

that they are probablyimmigrants in 

SE Germany, originating from southeastern 

or more southern areas. Except 

for M. minor, whose origin is not clear 

and could be regarded as an immigrant 

frommore eastern areas. Using the 

length of the mesoloph in the second 

upper molars as an indicator of habitat, 

D. gracilis and M. minor had a preference 

for a humid habitat, D. mutilus and 

M. bavaricus a preference for drier habitats. 

2010010475 

德国南部 Sandelzhause 产地中新世大 

哺乳动物的稳定同位素生态学 = Stable 

isotope ecology of Miocene large 

mammals from Sandelzhausen, southern 

Germany. ( 英文 ). Tutken T; Vennemann 

T. Palaeontologische 

Zeitschrift, 2009, 83(1): 207-226 

The carbon, oxygen, and strontium 

isotope composition of enamel from 

teeth of larg Miocene herbivorous 

mammals from sandelzhausen in the 

North Alpine foreland basin, were analyzed 

to infer diet and habitat. Most taxa 

were C3 browsers in a forested and humid 

floodplain environment in the Molasse 

Basin, which experienced a warmtemperate 

to subtropical climate and 

possibly low seasonality. 

2010010476 

德国 Dorn-Durkheim 1 产地的牛科 = 

The Bovidae of Dorn-Durkheim 1, 

Germany (Turolian age). ( 英文 ). Gentry 

A W; Kaiser T M. Palaeontologische 

Zeitschrift, 2009, 83(2): 373-392 

Tree bovid species are present at 

Dorn-Durkheim 1. The overwhelmingly 

abundant species is a boselaphine, Miotragocerus 

sp., with smaller and less advanced 

teeth than Tragoportax amalthea 

from Pikermi, Greece. Miotragocerus 

was present in the latest middle Miocene 

and Vallesian of western and central 

Europe and survived into the Turolian. 

139

The other two bovid species remain enigmatic 

and of uncertain tribal affiliation. 

Each is represented by very few teeth, 

none of them associated. One species is 

larger and the other smaller than the Miotragocerus 

sp. 

2010010477 

蒙古始新世中期 aichin Ula II 动物群 

巨猪超科 ( 偶蹄目 , 猪形亚目 ) 最古 

老代表以及此超科演化特征 = The 

oldest representative of Entelodontoidea 

(Artiodactyla, Suiformes) from the Middle 

Eocene of Khaichin Ula II, Mongolia, 

and some evolutionary features of this 

superfamily. ( 英文 ). Vislobokova I A. 


643-654 3 图版 . 

The oldest representative of the family 

Entelodontidae (suborder Suiformes), 

Proentelodon minutus gen. et sp. nov, is 

described from the Middle Eocene Khaichin 

Ula II Fauna in Mongolia. In addition 

to the genus Proentelodon, the new 

subfamily Proentelodontinae includes 

the genus Eoentelodon from the Middle- 

Upper Eocene of China, Mongolia, and 

Kazakhstan. The new data bring clues to 

the origin and systematic position of Entelodontidae, 

features of their evolution, 

dispersal, and changes in taxonomic diversity. 

They also elucidate the early 

evolutionary stages of Suiformes. 

2010010478 

俄罗斯 Chleuastochoerus( 猪科 , 偶 

蹄目 ) 首次发现 = The first record of 

Chleuastochoerus (Suidae, Artiodactyla) 

in Russia. ( 英文 ). Vislobokova I A. Paleontological 

Journal, 2008, 42(6): 686- 

698 7 图版 . 

A new species, Chleuastochoerus tuvensis, 

from the Late Miocene Taralyk- 

Cher locality in Tuva is described. Phylogenetic 

relationships and lifestyle of 

Chleuastochoerus, a unique member of 

the family Suidae, are discussed. 

2010010479 

Včeláre 2( 斯洛伐克东南部 ) 上新世 

晚期食肉动物 = Late Pliocene carnivores 

from Včeláre 2 (Southeastern Slovakia). 

( 英文 ). Sabol M; Holec P; Wagner 

J. Paleontological Journal, 2008, 

42(5): 531-543 5 图版 . 

Carnivores from the Late Pliocene site 

of Včeláre 2 are described and their taxonomy 

is discussed. The carnivore assemblage 

includes nine specimens of the 

families Felidae (Homotherium crenatidens), 

Ursidae (Ursus minimus), and 

Ailuridae (Parailurus sp.). The scimitartoothed 

cat and ursid are common representatives 

of the Pliocene European 

fauna, whereas the lesser panda is 

probably a new species of Parailurus, 

which differs from both Pliocene species, 

P. anglicus and P. hungaricus. As a part 

of a more or less uniform Pliocene carnivore 

fauna of the Northern Hemisphere, 

the Včeláre 2 assemblage represents 

a forest and (or) open grassland 

environment. 

2010010480 

东欧二叠纪末期最早的 Whaitsiid 类 

= The first Whaitsiid (Therocephalia, 

Theromorpha) from the terminal Permian 

of eastern Europe. ( 英文 ). 

Ivakhnenko M F. Paleontological Journal, 

2008, 42(4): 409-413 1 图版 . 

The first representative of the family 

Whaitsiidae, Megawhaitsia patrichae 

gen. et sp. nov., from the terminal Permian 

of eastern Europe is described. 

This is a very large predator that appeared 

in the Vyazniki Tetrapod Assemblage 

in conditions of large predatory 

biomorph deficiency. 

2010010481 

欧亚大陆北部上新世 - 更新世早中期偶 

蹄目群落演化的主要阶段 : 第二部分 

= Main stages in evolution of Artiodactyla 

communities from the Pliocene- 

Early Middle Pleistocene of northern 

Eurasia: Part 2. ( 英文 ). Vislobokova I A. 

140


414-424 5 图版 . 

Changes in diversity of Artiodactyla 

from the Pliocene to Middle Pleistocene 

of northern Eurasia are considered. The 

major turnovers of artiodactyl communities 

correlate with the major global cooling 

events at the boundaries of epochs 

and ages and were accompanied by migrations. 

A correlation of the main biotic 

events in northern Eurasia and adjacent 

areas is presented. Zoogeographical features 

of Artiodactyla evolution in northern 

Eurasia and the role of Artiodactyla 

in the establishment of different bioms 

are addressed. 

2010010482 

西伯利亚东部更新世晚期的窄头野鼠 

( 啮齿目 , 田鼠亚科 ) 是北美移民 = 

Egorov’s narrow-skulled vole (Rodentia, 

Arvicolinae) from the Late Pleistocene 

of Eastern Siberia, a North American 

immigrant. ( 英文 ). Golenishchev F N. 


292-296 5 图版 . 

A comparative study of the Late 

Pleistocene Egorov’s narrow-skulled 

vole from the Indigirka River basin is 

performed. The taxon was previously 

regarded as a subspecies of Microtus 

(Stenocranius) gregalis (Pallas, 1779). 

Based on a number of morphological 

characters, it is shown that this vole is 

closer to the American species Mynomes 

(Vocalomys) miurus (Osgood, 1901). It 

is proposed that Mynomes (V.) miurus 

egorovi (Fejgin in Baranova et Fejgin, 

1980) penetrated into northeastern Siberia 

during the Zyryanian glacial. 

2010010483 

欧亚大陆北部上新世 - 更新世早中期偶 

蹄目群落演化的主要阶段 : 第一部分 

= The major stages in the evolution of 

artiodactyl communities from the Pliocene-early 

Middle Pleistocene of northern 

Eurasia: Part 1. ( 英文 ). Vislobokova 

I A. Paleontological Journal, 2008, 

42(3): 297-312 2 图版 . 

Seven main stages in the evolution of 

Pliocene-Pleistocene artiodactyl communities 

from Russia, Ukraine, Moldova, 

Georgia, Kazakhstan, and Tajikistan 

within the interval from 5.3 through 0.4 

Ma are characterized. The dominant 

groups are briefly revised. The major 

biotic events and the development of the 

main phyletic lineages are discussed. 

2010010484 

外贝加尔 ( 俄罗斯 ) 上新世 

Parailurus 一新种 = A new species of 

lesser panda Parailurus (Mammalia, 

Carnivora) from the Pliocene of Transbaikalia 

(Russia) and some aspects of 

ailurine phylogeny. ( 英文 ). Sotnikova M 


90-99 5 图版 . 

A new species of the lesser panda, 

Parailurus baikalicus sp. nov., from the 

Pliocene of Transbaikalia is described. 

In contrast to the European taxa P. anglicus 

and P. hungaricus, it retains a 

primitive occlusal pattern of M 1 -M 2 , 

with a concave buccal outline, small 

mesostyle on M 1 , and undeveloped 

styles on M 2 . At the same time, the 

Transbaikalian panda is more advanced 

than other representatives of Parailurus 

in the upper molars with a reduced lingual 

cingulum and an enlarged paraconule, 

which is partially (M 1 ) or completely 

(M 2 ) separated from the protocone. 

This combination of primitive and 

advanced characters points to the separation 

of the Asian branch at the earliest 

stages of the genus development. The 

Transbaikalian lesser panda may represent 

a terminal form of this phylogenetic 

lineage. 

2010010485 

根据一颅腔模型重建 Paroxyaena 

pavlovi 大脑的形态功能 = Morphofunctional 

reconstruction of the brain of 

Paroxyaena pavlovi (Hyaenodontidae, 

141

Creodonta) based on a natural endocranial 

cast. ( 英文 ). Saveliev S V; Lavrov 


41(6): 661-670 4 图版 . 

The study of a natural endocranial 

cast of Paroxyaena has shown that its 

vision was an important system of afferentation, 

but did not prevail over others, 

unlike that of Neohyaenodon. The olfaction 

was much better developed than in 

Neohyaenodon. The large gyrus prorealis 

suggests the presence of a long mobile 

nose. The well-developed sensomotoric 

cortex is evidence that the forepaw 

of Paroxyaena showed a high mobility. 

2010010486 

蒙古新近纪羊亚科 ( 牛科 , 偶蹄目 , 

哺乳纲 ) = Caprinae (Bovidae, Artiodactyla, 

Mammalia) from the Neogene 

of Mongolia. ( 英文 ). Dmitrieva E L. Paleontological 

Journal, 2007, 41(6): 671- 

682 2 图版 . 

Gobiocerus mongolicus Sokolov, 

1952, Turcocerus kekemaidengensis Ye 

Jie et al., 1999; and Hypsodontus sp. 

were recorded in Miocene deposits of 

the Valley of Lakes (MN4-MN8) and 

Oioceros atropatenes (Rodler et 

Weithofer, 1890) occurred in the Mio- 

Pliocene (MN11-MN20) of northwestern 

Mongolia. Gobiocerus, Turcocerus, 

and Hypsodontus represent the same 

evolutionary lineage. Thus, Caprinae 

existed in Central Asia in the Early Miocene. 

They diverged from the Bovidae at 

the Oligocene-Miocene boundary. The 

presence of early bovids in this region 

suggests that this group could have appeared 

in Central Asia. 

2010010487 

Oka-Don 平原 Kuznetsovka 地区更新 

世的软体动物和小型哺乳动物 = Mollusks 

and small mammals from the 

Kuznetsovka locality, Pleistocene of the 

Oka-Don Plain. ( 英文 ). Agadjanian A K; 

Kondrashov P E. Paleontological Journal, 

2007, 41(4): 395-406 4 图版 . 

Kuznetsovka, a very rich locality of 

Interglacial mollusks and small mammals 

overlies the Donian Glacial strata 

of the Oka-Don Plain. Mollusks and 

small mammal from this locality are described 

in detail. The crucial stage in the 

development of Middle Pleistocene mollusk 

and mammal faunas is investigated. 

The data obtained allow the dating of 

fossiliferous deposits and reconstruction 

of sedimentation and environmental 

conditions of the fauna. The comparison 

of the Kuznetsovka Fauna with materials 

from central and western Europe permits 

its direct correlation with the fauna of 

the Cromerian stratotype in West Runton 

(Norfolk, England). Thus, the deposits 

of the Kuznetsovka section were 

formed during the second half of the 

early Middle Pleistocene. 

2010010488 

奥地利 Kohfidisch 地区中新世晚期哺 

乳动物新发现 = New data on late Miocene 

mammals of Kohfidisch, Austria. 

( 英文 ). Vislobokova I A. Paleontological 

Journal, 2007, 41(4): Cervidae ; 

Bovidae; Turolian; Late Miocene; 

Austria 3 图版 . 

Cervids and bovids of the Early Turolian 

mammalian fauna of Kohfidisch 

(Austria) are reviewed. A new species, 

Micromeryx mirus sp. nov. (Moschidae) 

is described. 

2010010489 

法国凯尔西地区始新世晚期磷灰岩中 

Paroxyaena 一新种 = A new species of 

Paroxyaena (Hyaenodontidae, Creodonta) 

from phosphorites of Quercy, 

Late Eocene, France. ( 英文 ). Lavrov A 


298-311 5 图版 . 

An almost complete skull without a 

lower jaw of Paroxyaena pavlovi sp. 

nov. (Pterodontinae) is described. A new 

tribe, Paroxyaenini tribe nov., is established. 

The round foramen and orbital 

fissure of Paroxyaenini are completely 

142

fused, whereas those of Pterodontini are 

separate. The deciduous teeth of Paroxyaena 

are described for the first time. 

2010010490 

西伯利亚西部中侏罗世的 Itatodon 

tatarinovi 以及柱齿兽目的系统发育 

学分析 = Itatodon tatarinovi (Tegotheriidae, 

Mammalia), a docodont from 

the Middle Jurassic of Western Siberia 

and phylogenetic analysis of Docodonta. 

( 英文 ). Averianov A O; Lopatin A V. 


668-677 3 图版 . 

Itatodon tatarinovi Lopatin et Averianov, 

2005 is represented by two lower 

molars and a lower molar fragment from 

the upper part of the Itat Formation (Bathonian 

Stage) of the Berezovskii quarry 

(southern Krasnoyarsk Region). Based 

on the presence of a pseudotalonid, bordered 

by the crests a-b, b-e, e-g, and a-g, 

Itatodon is assigned to the endemic 

Asian family Tegotheriidae. In this genus, 

the crest a-b is reduced and the 

thick lingual cingulid is better developed 

than that of other docodonts. Phylogenetic 

analysis of Docodonta shows paraphyly 

of Morganucodonta relative to 

docodonts and independent development 

of the pseudotalonid in the Tegotheriidae 

and the clade comprising Krusatodon, 

Castorocauda, Cyrtlatherium, and 

Dsungarodon. 

2010010491 

甘肃东乡首次发现熊亚科化石 —— 龙 

担哺乳动物群补充报道之二 = First 

Ursine Bear Material From Dongxiang, 

Gansu——Addition to the Longdan 

Mammalian Fauna. ( 英文 ). 邱占祥 ; 邓 

涛 ; 王伴月 . 古脊椎动物学报 , 2009, 

47(4): 245-264 

2006 年作者在和政县发现了两件产 

自东乡龙担动物群的熊类化石 : 一完整 

下颌 (HMV1422) 和一个咬合在一起的 

头骨及下颌 (HMV 1454)。熊类系龙担 

哺乳动物群中未曾描述过的新成员。 

这两件标本虽然有少许不同 , 但都和李 

亦征 (1993) 所记述的沂南熊 

Ursus(Protarctos)yinanensis 十分接近 , 

而被归入该种。该种修订后的鉴别特 

征是 : 头骨长头型 , 头长接近中等大小 

的现生黑熊 , 头骨最大宽约为最大长的 

一半 ; 矢状嵴长 , 约为顶长的 1/3; 眶下孔 

与眼眶前缘相距近 , 两者均在 M1 上方 ; 

颧骨前端仅组成眼眶下缘 , 其后端止于 

关节窝前缘水平 ; 硬腭短 , 齿列之后的 

腭长小于 P4 长的 1.5 倍或 M2 长的 

3/4。前臼齿数目全 ;P4 原尖小 , 位于裂 

凹正内方 ;M1 短长方形 , 宽 / 长 ~ 

80%;M2 跟座中长 ,M2 宽 / 长 56%~ 

58%;M2 长 /M1 长 133%~153%。m1 

无前下后尖及前下内尖 , 分隔下三角座 

和跟座的横沟窄 ( 前后 ), 横沟中没有明 

显的嵴和沟 ;m2 短于 m1, 其前、后接近 

等宽。与 U.boeckhi 相比 ,P4 相对更小 ; 

臼齿相对更窄长 ;M1 不呈五边形 ;M2 

跟座更大 ;m1 横沟短 ,V 形。 

2010010492 

中国新近纪牛科分类及演化规律 = 

Taxonomy And Evolutionary Process Of 

Neogene Bovidae From China. ( 中文 ). 

陈冠芳 ; 张兆群 . 古脊椎动物学报 , 2009, 

47(4): 265-281 

我国新近纪的牛科相当繁盛。至今 

已记录了 30 属 , 归入 5 个亚科 

(Hypsodontinae, Urmiatheriinae, Caprinae, 

Antilopinae 和 Bovinae)。化石主要 

出现在我国北方且大部分为土著类型 , 

以颊齿中等高冠至高冠、前臼齿列 

短、头骨粗壮、弯曲和角心特化为特 

征。在整个新近纪时期 , 牛科经历了 5 

个发展阶段和 4 次大的更替。与同时 

代欧亚大陆其他地区的牛科类群相比 , 

中国牛科化石出现的时间早 , 且基本组 

成不同。在中新世 , 我国的牛科主要由 

Hypsodontinae,Urmiatheriinae,Caprinae 

的早期特化类型和 Gazella 组 

成 ,Boselaphini 稀少并缺乏转角羚羊 

(Antilopinae); 在上新世 , 除 Gazella 外 , 

143

我国北方仍生活着 Caprinae 的一组土 

著类型。 

2010010493 

哺乳动物化石群落线指示的甘肃临夏 

盆地晚新生代环境演变 = Late Cenozoic 

Environmental Changes In The 

Linxia Basin(Gansu,China) As Indicated 

By Cenograms Of Fossil Mammals. ( 英 

文 ). 邓涛 . 古脊椎动物学报 , 2009, 

47(4): 282-298 

哺乳动物群的演替过程在重建古环 

境和古气候中具有重要的作用。群落 

线 (cenogram) 是将陆生哺乳动物群中 

非肉食性种类按体重分布顺序排列的 

一种曲线 , 并可在图中将肉食性种类单 

独排序 , 以便显示动物群的整体组成。 

通过与现生哺乳动物群的比较 , 化石动 

物群的群落线已经被用来推断古环境 

及其在地质历史时期的变化。基于甘 

肃临夏盆地晚新生代哺乳动物群的群 

落线进行古环境重建 , 时代从晚渐新世 

直到早更新世。大多数化石种类的体 

重通过下第一臼齿面积与体重的回归 

公式来估计 , 少数种类用其他牙齿或肢 

骨来估计。大多数体重估计的测量数 

据来自临夏盆地的化石 , 少数取自文 

献。对 7 个化石动物群分别计算群落 

线的统计结果 , 在此基础上进行古环境 

解释。这些分析揭示了临夏盆地在晚 

中新世、早上新世和早更新世具有开 

阔的环境 , 晚渐新世是半开阔的林地 , 

而中中新世为比较紧密的森林 ; 在晚渐 

新世和晚中新世早期气候干燥 , 晚中新 

世的其他时段以及早上新世和早更新 

世为半干旱环境 , 而中中新世时期相当 

湿润。 

2010010494 

阿尔卑斯地区东部中新世生态系统反 

刍动物关系 = Associations of ruminants 

in Miocene ecosystems of Eastern 

Alpine Region. ( 英文 ). Vislobokova I A. 


438-447 2 图版 . 

The dynamics of biodiversity of ruminants 

and changes in their adaptations 

in the Late Miocene of Austria are analyzed 

in connection with changes in environment 

and climate. At the end of the 

Middle Miocene through the beginning 

of the Late Miocene, the major reorganization 

of ruminant associations was recorded 

at the Vallesian-Turolian transition 

(about 8.7 Ma). 

2010010495 

亚洲始新世兔形目 ( 哺乳纲 ):2. 

Strenulagus 和 Gobiolagus (Strenulagidae) 

= Eocene Lagomorpha (Mammalia) 

of Asia: 2. Strenulagus and Gobiolagus 

(Strenulagidae). ( 英文 ). Lopatin 

A V; Averianov A O. Paleontological 

Journal, 2006, 40(2): 198- 

206 5 图版 . 

Two species of early lagomorph, 

Strenulagus solaris sp. nov. (Monogolia, 

Khaychin-Ula 2 and 3 localities, Middle 

Eocene) and Gobiolagus hekkeri (Kyrgyzstan, 

Andarak 2 locality, terminal 

Lower Eocene), are described. A revision 

of Romanolagus hekkeri Shevyreva 

from the Andarak 2 locality has shown 

that it belongs to the genus Gobiolagus; 

consequently, the monotypic genus Romanolagus 

Shevyreva, 1995 is a junior 

synonym of Gobiolagus Burke, 1941. 

The diagnoses and species compositions 

of the genera Strenulagus and Gobiolagus 

are revised. Zaissanolagus 

gromovi Erbajeva from the Lower Oligocene 

of eastern Kazakhstan is shown 

to be the latest representative of the genus 

Gobiolagus and the family Strenulagidae. 

2010010496 

亚洲早古近纪食虫类哺乳动物和食虫 

类主干群的建立 = Early Paleogene insectivore 

mammals of Asia and establishment 

of the major groups of Insectivora. 

( 英文 ). Lopatin A V. Paleontological 

Journal, 2006, 40(Supplement 

3): S205-S405 74 图版 . 

144

Early Paleogene insectivore mammal 

associations of Asia include true insectivores 

(superorder Insectivora: order Lipotyphla: 

suborders Erinaceomorpha 

and Soricomorpha; orders Didymoconida 

and Leptictida) and insectivore-like 

placentals (superorder Ferae: order Cimolesta: 

suborders Didelphodonta, Palaeoryctida, 

and Pantolesta). The associations 

from Mongolia are the most 

taxonomically diverse. 

2010010497 

西伯利亚晚中新世最古老的巨鹿及其 

该群演化的意义 = The most ancient 

megacerine deer from the Late Miocene 

of Siberia and its implications to the 

evolution of the group. ( 英文 ). Vislobokova 

I A. Palaeoworld, 2009, 18(4): 

278-281 

The oldest representative of giant deer 

(tribe Megacerini, family Cervidae) is 

found in the Late Miocene of the Taralyk-Cher 

locality in Tuva (Russia). The 

new findings enrich the history of the 

group and demonstrate the Central Asian 

origin of its Asiatic lineage Praesinomegaceros–Sinomegaceros 

2010010498 

斯堪迪纳维亚半岛首次发现中生代哺 

乳动物 = The first Mesozoic mammal 

from Scandinavia. ( 英文 ). Lindgren J; 

Rees J; Siverson M; Cuny G. GFF, 2004, 

126(4): 325-330 

Lowermost Cretaceous (Berriasian) 

strata of the Skyttegard Member (Rabekke 

Formation, Nyker Group) on the 

island of Bornholm, Denmark, have 

yielded a diverse terrestrial microvertebrate 

fauna. The assemblage is 

unique in several aspects, including e.g. 

the first Mesozoic mammal from Scandinavia. 

Here. we describe the mammal 

fossil, identified as a multituberculate 

upper premolar. The tooth is tentatively 

assigned to the monospecific genus 

Sunnyodon, as it shares the largest number 

of diagnostic dental features with the 

approximately coeval S. notleyi from the 

Purbeck Limestone Formation in southernmost 

England. 

古人类学 

古人类学 

2010010499 

北亚早期人类文化的发展 = Development 

of early human culture in northern 

Asia. ( 英文 ). Derevianko A P; Shunkov 

M V. Paleontological Journal, 2009, 

43(8): 881-889 2 图版 . 

An archeological complex in the 

Pleistocene deposits of the Altai Mountains 

currently provides the most complete 

information about early human occupation 

in northern and Central Asia. It 

is best represented in studies of multilayered 

Paleolithic sites in the Anui 

River valley in the northwestern part of 

the Altai Mountains. The general stratigraphic 

profile, which includes Middle 

and Upper Pleistocene deposits, has 

been defined based on the data obtained 

from a number of sites in this region. 

Available information reflects the development 

of early human culture and 

environmental fluctuations from the 

early to the late stages of the Paleolithic. 

2010010500 

旧石器时代人活动和生物资源变迁机 

制 , 以阿尔泰山脉西北部为例 = The 

dynamics of bioresources and activity of 

the paleolithic man, using the example 

of northwestern Altai Mountains. ( 英文 ). 

Agadjanian A K. Paleontological Journal, 

2006, 40(4): S482-S493 3 图版 . 

Long-term studies of living and fossil 

mammals of the Altai Mountains (= 

Gornyi Altai) revealed the pattern of the 

dynamics of small mammal communities 

in this region in the second half of 

the Pleistocene, in the Holocene, and the 

present time. The fossil fauna of the 

Anui River valley differs significantly 

from the modern one. The Pleistocene 

fauna of Paleolithic sites reflects a considerably 

more diverse biotopic situation 

145

and high landscape diversity compared 

with the present time. This diversity depended 

on a stronger role in the communities 

of steppe and highland elements. 

The influence of Paleolithic man on Late 

Pleistocene populations of ungulates and 

large predators is detected. 

2010010501 

以阿尔泰西北部 denisova 洞穴为例 , 

说明蝙蝠可指示旧石器时代人类活动 

= Bats as an indicator of human activity 

in the paleolithic, using the example of 

denisova cave, northwestern Altai. ( 英 

文 ). Rossina V V. Paleontological Journal, 

2006, 40(4): S494-S500 7 图版 . 

Landscape and climatic changes in 

northwestern Altai at the end of the 

Middle Pleistocene were accompanied 

by a transformation in the taxonomic 

composition of the bat community and 

abundance of some species. The dynamics 

of the bat community is very important 

for the study of the activity of Paleolithic 

man. The high sensitivity of 

bats to human disturbance allowed the 

time of colonization and nature of usage 

of Denisova cave by humans to be recognized. 

In this respect, bats are a very 

important indicator of events in the surrounding 

ecosystem. 

2010010502 

俄罗斯阿尔泰中部 Charyshskii Naves 

洞穴附近更新世晚期和全新世人类栖 

息地环境重建 = Paleoreconstruction of 

Pleistocene environments of human 

habitats in the Late Pleistocene and 

Holocene near the Charyshskii Naves 

cave, Central Altai, Russia. ( 英文 ). 

Serdyuk N V. Paleontological Journal, 

2006, 40(4): S501-S507 5 图版 . 

The results of the study of the small 

mammal fauna from the Charyshskii 

Naves cave (Central Altai, Russia) in the 

2003 field season are provided. The dynamics 

of fossil small mammals was 

studied and the natural habitats of the 

ancient man were reconstructed on this 

basis. Two stages of sedimentation, corresponding 

to the domination of different 

biotopes, were recognized. 

历史地质学、地层学 

综论 

2010010503 

朝鲜半岛早太古代到中侏罗世的演化 

及和中国克拉通的对比 : 来自 

SHRIMP U-Pb 锆石年龄的约束 = 

Early Archean to middle Jurassic evolution 

of the Korean Peninsula and its correlation 

with Chinese cratons: SHRIMP 

U-Pb zircon age constraints. ( 英文 ). 

Jeon H;Cho M;Kim H;Horie K;Hidaka 

H. Journal of Geology, 2007, 115(5): 

525-539 

U- Pb zircon ages of tuffs and sandstones 

of the Daedong Supergroup (Bansong 

and Nampo groups) in the Korean 

Peninsula were determined using a sensitive 

high- resolution ion microprobe 

(SHRIMP) in order to constrain their 

age of sedimentation and to unravel discrete 

geologic events as recorded in detrital 

zircons. The ages of four tuffaceous 

samples from the Bansong 

Group imply that the Daedong Supergroup 

formed at ca. 187 - 172 Ma in association 

with the Early- Middle Jurassic 

orogeny. These data are in marked contrast 

with paleomagnetic arguments suggesting 

that the Bansong and Nampo 

groups are precollisional Early- Middle 

Triassic deposits that are correlative 

with the North and South China blocks, 

respectively. Detrital zircons of the 

Daedong Supergroup define seven age 

components: (1) Early- Middle Archean 

(3.64 - 2.97 Ga), (2) Late Archean - 

middle Early Proterozoic (2.63 - 2.33 

Ga), ( 3) late Early Proterozoic (1.98 - 

1.75 Ga), (4) Middle- Late Proterozoic 

(1.2 - 0.6 Ga), ( 5) Devonian (400 - 355 

Ma), (6) Early Permian (280 255 Ma), 

and (7) Middle Triassic - Early Jurassic 

(240 - 180 Ma). These age distributions, 

together with available geochronological 

data, suggest that crustal growth of the 

146

Korean Peninsula has continued since ca. 

3.6 Ga and culminated at ca. 2.5 and 1.9 

- 1.8 Ga. Major age populations of detrital 

zircons of the Bansong and Nampo 

groups are similar, except for the presence 

of Middle-Late Proterozoic ages in 

the latter. Inasmuch as these ages are 

characteristic for the South China Block, 

the Gyeonggi massif, or at least the local 

source of the Nampo Group, is most 

likely a correlative of the South China 

Block. 

2010010504 

藏南康雄地区中喜马拉雅地块层序构 

造演化的地质年代学和岩石学研究 = 

Geochronological and petrological constraints 

for tectonic evolution of the central 

Greater Himalayan Sequence in the 

Kharta area, southern Tibet. ( 英文 ). Liu 

Y; Siebel W; Massonne H J; Xiao X C. 

Journal of Geology, 2007, 115(2): 215- 

230 

Within the Kharta area, east of Mount 

Qomolangma ( Everest), garnet sillimanite 

gneisses and granites including 

mafic lenses that form the Greater Himalayan 

Sequence (GHS) were displaced 

beneath the North Col Formation 

by the lower South Tibetan Fault (LSTF) 

and above the Lesser Himalayan Sequence 

by the Main Central Thrust 

(MCT). Zircons from mafic lenses, 

probably former dikes, were dated by 

thermal ionization mass spectrometry to 

yield discordant U-Pb results. One sample 

gave a discordia line with an upper 

intercept age of 971 Ma, suggesting a 

late Proterozoic age for emplacement of 

the dike. Zircon SHRIMP analyses show 

that the garnet sillimanite gneisses and 

granites were derived mainly from early 

Paleozoic rocks produced by hightemperature 

metamorphism and/or partial 

melting of Neoproterozoic ( meta) 

sedimentary rocks. These crystalline 

rocks were buried beneath southern Tibet 

and experienced metamorphic conditions 

of 750 degrees - 800 degrees C and 

14 kbar at Ma. After exhumation they 

were trans- 33 +/- 2 formed to lowpressure 

rocks at 23 +/- 2 Ma. Structural 

analyses have revealed that further exhumation 

of the GHS is attributed to the 

LSTF and MCT faults beginning at 12 - 

13 Ma, according to monazite U-Th-Pb 

dating. Finally, these rocks underwent 

north-south-trending folding at shallow 

depths after 12 Ma. 

2010010505 

西班牙中部地壳下部麻粒岩捕掳体锆 

石的 U-Pb 研究 : 伊利比亚新元古代 

到三叠纪岩石圈演化的记录 = A U-Pb 

study of zircons from a lower crustal 

granulite xenolith of the Spanish central 

system: A record of Iberian lithospheric 

evolution from the Neoproterozoic to the 

Triassic. ( 英文 ). Fernandez-Suarez J; 

Arenas R; Jeffries T E; Whitehouse M J; 

Villaseca C. Journal of Geology, 2006, 

114(4): 471-483 

A U-Pb laser ablation inductively 

coupled plasma mass spectrometry and 

secondary ion mass spectrometry geochronological 

study has been performed 

on zircons from a felsic granulite xenolith 

from the lower crust under the 

Variscan belt of Iberia. The ages obtained 

reveal zircon-forming events that 

span from the late Neoproterozoic 

(Cadomian-Avalonian orogeny) to the 

early stages of the opening of the Atlantic 

Ocean in the Mesozoic, through 

Cambro-Ordovician rifting, Devono- 

Carboniferous Variscan-Alleghenian 

collision, and Permian-Triassic extension 

and uplift. The U-Pb age groups 

found in zircons from this single lower 

crustal xenolith ( ca. 220, 250, 280-310, 

460-490, 525, and 550-590 Ma) record 

at least one complete cycle of closing 

and opening of oceanic basins and collision 

of continental masses. Zircons from 

the felsic granulite xenolith contain a 

synthesis of the geochronological information 

found on the surface geology and 

record most but not all major lithospheric 

events in the region in a ca. 400- 

m. yr. period. 

147

2010010506 

北美宏观地层学 = Macrostratigraphy 

of North America. ( 英文 ). Peters S E. 


412 

The geological record is a threedimensional 

mosaic of gap-bound rock 

bodies that, at any given scale of temporal 

resolution, were emplaced more or 

less continuously. At any geographic 

location, the irregular alternation of 

processes responsible for the formation 

and destruction of rock bodies results in 

the preservation of hiatus-bound rock 

packages that have a distinct time of first 

occurrence (base, or oldest portion), a 

time of last occurrence (top, or youngest 

portion), and a suite of defining characters 

(e. g., lithologies, thickness, fossils, 

etc.). Many important aspects of the 

geologic record can be quantified by 

compiling the stratigraphic ranges of 

such gap-bound rock packages. These 

include the quantity and spatial and 

temporal distribution of preserved rock, 

rates of rock formation, sequence stratigraphic 

architecture, and area-weighted 

rates of expansion and contraction/erosional 

truncation of rock emplacement 

settings. This approach to 

characterizing the rock record is scalable, 

permitting application to records encompassing 

entire continents and hundreds 

of millions of years as well as individual 

basins and geologically short 

time intervals. To illustrate the utility of 

this approach and to provide a new highresolution 

analysis of the temporal structure 

of the geologic record, gap-bound 

rock packages in the continental United 

States and southern Alaska were compiled 

directly from the American Association 

of Petroleum Geologists Correlation 

of Stratigraphic Units of North 

America (COSUNA) charts. The 

COSUNA charts were assembled at a 

temporal resolution of approximately 1- 

3 million years (m. yr.) in the Phanerozoic 

and contain 4173 gap-bound rock 

packages. Many important aspects of the 

North American geologic record are revealed 

by the temporal distribution of 

gap-bound rock packages, including 

rock quantity, long-term rates of sediment 

accumulation, and basin turnover. 

The durations of gap-bound sedimentary 

successions are approximately exponentially 

distributed, with a mean duration 

of 25.2 m. yr. and a median duration of 

16.9 m. yr. The probability of initiation 

and truncation among sedimentary 

packages does not increase or decrease 

substantially during the Phanerozoic, but 

these parameters do vary on shorter 

timescales in response to tectonically 

and glacioeustatically driven changes in 

sea level. The largest increase in the rate 

of sediment truncation occurs at the end- 

Permian, which marks a clear and fundamental 

temporal discontinuity in the 

sedimentary record of North America. 

Smaller discontinuities occur at the end- 

Ordovician, the end-Triassic, and the 

end-Cretaceous. Lithologically, Cambrian-Mississippian 

sedimentary successions 

are dominated by carbonates, and 

post-Paleozoic successions are dominated 

by terrigenous clastics. The quantity 

of preserved rock, the carbonate/siliciclastic 

ratio, and the dominant 

lithology comprising terrigenous clastics 

all vary substantially from interval to 

interval during the Phanerozoic, indicating 

that processes governing the formation 

and destruction of sedimentary 

rocks vary on timescales of ! 5 m. yr. 

2010010507 

由硬体部分输入率的增加和沉积速率 

的增加之间的正向反馈导致的原生贝 

壳层的保存 = Preservation of autochthonous 

shell beds by positive feedback 

between increased hardpart-input rates 

and increased sedimentation rates. ( 英 

文 ). Tomasovych A; Fursich F T; Wilmsen 

M. Journal of Geology, 2006, 114(3): 

287-312 

148

The preservation of nonrapidly buried 

autochthonous shell concentrations with 

noncementing epifaunal animals in life 

position presents a taphonomic dilemma 

if in fact an increase in shelliness is 

driven by a decrease in sedimentation 

rate. A 150-cm-thick, densely packed 

shell bed with brachiopods from the 

Lower Jurassic of Morocco shows lower 

levels of postmortem alteration than 

shell-poor beds, indicating that its formation 

is primarily governed by variations 

in hardpart-input rates. Varying 

dominance and size structure of the 

main shell producer, brachiopod Zeilleria 

rehmanni, indicate that its increased 

population density was the main trigger 

in the shell bed formation. Thinner and 

less common microbial crusts in the 

shell bed than in shell-poor beds indicate 

that higher shelliness is not due to lack 

of sediment. On the basis of actualistic 

data from modern mussel and oyster 

shell beds, the suspension feeding of a 

high-density population leads to high 

biodeposition rates through production 

of feces and pseudofeces, which substantially 

exceed natural sedimentation 

rates. In addition, shell-rich areas preferentially 

trap more suspended sediment 

than shell-poor areas. Therefore, an increase 

in population density of shelly 

biodeposit producers should lead to 

higher biodeposition rates. This assumption 

is supported by a positive correlation 

between brachiopod shelliness and 

pellet abundance. Both active biodeposition 

and passive trapping of sediment 

would have increased sedimentation rate, 

thus leading to a decreased rate of shell 

destruction through suppression of 

predators or borers as well as stabilization 

and protection of the shell concentration. 

Under optimum ecologic conditions, 

these processes result in a positive 

feedback between an increased hardpartinput 

rate and increased biogenic sedimentation 

rate. This scenario thus provides 

one alternative pathway for formation 

of well-preserved shell concentrations 

formed by epifaunal suspension 

feeders. Identifying the importance of 

biodeposition is of environmental significance 

because it implies that carbonate 

sediment was produced largely in 

situ and was directly or indirectly related 

to the activity of shell producers. Recognizing 

the role of varying hardpartinput 

rates in shell concentration genesis 

is of ecologic significance because shelliness 

can directly reflect abundance 

fluctuations of shell producers. 

2010010508 

南美南部的能量危机 : 煤田的意义 = 

The energy crisis in southern South 

America: the importance of coal deposits. 

( 英文 ). Alfaro Hanne G. Neues 

Jahrbuch fur Geologie u. Palaontologie 

/ Abhandlungen, 2009, 253(1): 3-14 

The recent energy crisis in Chile and 

Argentina was effected by growing 

economy and the relatively little natural 

gas and liquid hydrocarbons production, 

reflected by diminishing reserve / consumption 

relation. Coal is an alternative 

energy source. In the present study, the 

main chatacteristics of the coal basins of 

both countries are presented. Coal blend 

combustion, coal gasification and methane 

from Coal recovery are proposed as 

part of the solution to the energy crisis. 

2010010509 

测井信息用于层序地层单元划分及对 

比研究综述 = Advances in the study of 

sequence stratigraphic division and correlation 

usingwell log information. ( 中 

文 ). 闫建平 ; 蔡进功 ; 赵铭海 ; 郑德顺 . 地 

层学杂志 , 2009, 33(4): 441-450 

测井曲线是载有地层沉积旋回信息 

的信号 , 运用测井信息划分层序地层单 

元及地层对比研究自开始以来已取得 

了长足进步 , 从定性的分析、识别发展 

到现在可半定量、定量提取不同级别 

的沉积单元界面及进行层序地层对比 , 

更进一步克服了地质学家手工划分层 

序中人为因素的影响 , 进而也推进了层 

149

序地层学研究的定量化发展。岩性突 

变、沉积韵律是影响其测井响应及曲 

线形态的两个重要因素 , 测井响应对沉 

积单元界面上下岩性的类型及粒度的 

不同而产生的声、放、电性质的变化 , 

是利用测井信息划分沉积单元界面的 

基础。随着层序地层学研究的深入 , 沉 

积单元界面识别及层序地层对比的测 

井研究将向更深层次、更定量化的方 

向发展 , 短周期及超短周期沉积旋回的 

测井曲线形态内部特征提取及划分、 

层序地层智能动态匹配对比的方法研 

究将是今后开展研究的新方向。关键 

词 : 层序地层 , 沉积单元 , 地层对比 , 测井 , 

旋回 , 频谱属性分析 

2010010510 

印度 Deccan 火山省西部 Sangamner 

镁铁质岩墙群地质和地球化学 : 对区 

域地层的启示 = Geology and geochemistry 

of the Sangamner mafic dike 

swarm, western Deccan Volcanic Province, 

India: Implications for regional 

stratigraphy. ( 英文 ). Bondre N R; Hart 

W K; Sheth H C. Journal of Geology, 

2006, 114(2): 155-170 

Numerous large, NE-SW- to E-Wtrending 

mafic dikes outcrop around 

Sangamner in the western Deccan Volcanic 

Province. This area is part of a 

broader region postulated to be a shieldlike 

feature and a major eruption center. 

A combination of field, geochemical, 

and isotopic (Sr and Nd) characteristics 

is used here to understand the relationship 

of this dike swarm with the associated 

lava flows and their position in the 

established Deccan stratigraphy. Many 

dikes are compositionally similar to the 

Khandala and Poladpur formations belonging 

to the Lonavala and Wai subgroups, 

respectively, while one dike is 

similar to the Ambenali Formation. One 

dike has a composition distinct from all 

other dikes in this area as well as from 

most stratigraphic units, although there 

are many similarities in composition 

with the Bushe Formation as well as the 

Boyhare Member of the Khandala Formation. 

While several dikes are geochemically 

similar to specific 

flows/members within certain formations, 

their isotopic composition is often 

different, sometimes significantly so. 

This implies either that there is a greater 

range in isotopic composition for those 

members than previously realized or that 

magmas with different isotopic compositions 

underwent broadly similar petrogenetic 

evolution leading to similarities 

in elemental composition. NE-SWtrending 

Poladpur- and/or Khandala-like 

dikes are concentrated in the central part 

of the area; these dikes appear to represent 

a vent system that could have fed 

southern, western, or eastern exposures 

of these younger formations. It is also 

possible, however, that some or many of 

the dikes along this system were simply 

late-stage intrusions of magmas representing 

the younger formations. 

古地理学、古气候学 

2010010511 

3.2 Ma BP 以来河北黄骅地区孢粉地 

层学与古气候变迁 = Palynology stratigraphy 

and palaeoclimate evolution in 

Huanghua district of Hebei province 

since 3.2 ma BP. ( 中文 ). 范淑贤 ; 刘海 

坤 ; 赵华 ; 吉云平 ; 毛洪亮 . 微体古生物学 

报 , 2009, 26(2): 173-180 

依据河北省黄骅市八里庄村 HB1 孔 

孢粉、古地磁和光释光等资料 , 发现第 

四纪以来渤海西岸的古植被演变受气 

候变化的影响 , 也受沉积环境的制约。 

1. 6 —3. 2 Ma BP 期间河流发育时期 

孢粉不丰富 ; 孢粉富集带多出现在湖相 

地层 , 而且持续时间短 , 孢粉贫乏带多 

出现在河流相沉积地层 , 持续时间较 

长 ;0. 8 —1. 6 Ma BP 期间植被以疏林 

草原为主 , 局部草原存在 , 古气候温和 

偏干。0. 13 Ma BP 以来 , 随着明显的 

古季风变化 , 孢粉丰富 , 气候序列分辨 

率高 , 可与海洋氧同位素分期对比 ;11 

ka BP 以来气候变暖湿润 , 为针阔叶混 

150

交林草原或沼泽草甸植被 ,3 ka BP 之 

后为海退时期 , 气候变凉变干 , 植被由 

沼泽草甸演变为盐生草甸。尽管该孔 

是目前沿海平原深孔分析孢粉样品最 

密的钻孔 , 但是未能发现连续丰富的孢 

粉 , 可能与该孔位于相对较高部位 , 多 

与河流沉积环境有关 ; 故而 , 平原区内 

并非每一个钻孔皆足以反映整个第四 

纪孢粉地层学的全貌。 

2010010512 

阿拉斯加 Fisher 凝灰岩的喷发与沉 

积 : 火成碎屑流演化的证据 = Eruption 

and deposition of the Fisher Tuff 

(Alaska): Evidence for the evolution of 

pyroclastic flows. ( 英文 ). Gardner J E; 

Burgisser A; Stelling P. Journal of Geology, 

2007, 115(4): 417-435 

Recognition that the Fisher Tuff 

(Unimak Island, Alaska) was deposited 

on the leeside of an similar to 500-700- 

m-high mountain range (Tugamak 

Range) more than 10 km away from its 

source played a major role in defining 

pyroclastic flows as momentum-driven 

currents. We reexamined the Fisher Tuff 

to evaluate whether deposition from expanded 

turbulent clouds can better explain 

its depositional features. We studied 

the tuff at 89 sites and sieved bulk 

samples from 27 of those sites. We find 

that the tuff consists of a complex sequence 

of deposits that record the evolution 

of the eruption from a buoyant 

plume (22 km) that deposited similar to 

0.2 km(3) of dacite magma as a pyroclastic 

fall layer to erupting similar to 

10-100 km(3) of andesitic magma as 

Scoria-rich pyroclastic falls and flows 

that were mainly deposited to the north 

and northwest of the caldera, including 

those in valleys within the Tugamak 

Range. The distribution of the flow deposits 

and their welding, internal stratification, 

and the occurrence of lithic 

breccia all suggest that the pyroclastic 

flows were fed from a fountaining column 

that vented from an inclined conduit, 

the first time such a conduit has 

been recognized during a large-volume 

caldera eruption. Pyroclastic flow deposits 

before and after the mountain range 

and thin veneer deposits high in the 

range are best explained by a flow that 

was stratified into a dense undercurrent 

and an overriding dilute turbulent cloud, 

from which deposition before the range 

was mainly from the undercurrent. 

When the flow ran into the mountain 

range, however, the undercurrent was 

blocked, but the turbulent cloud continued 

on. As the flow continued north, it 

restratified, forming another undercurrent. 

The Fisher Tuff thus records the 

passing of a flow that was significantly 

higher (800-1100 m thick) than the 

mountain range and thus did not require 

excessive momentum. 

2010010513 

过去 300m.y. 的温室危机 = Greenhouse 

crises of the past 300 million 

years. ( 英文 ). Retallack G J. Geological 

Society of America Bulletin, 2009, 

121(9-10): 1441-1455 

Proxies of past CO 2 and climate over 

the past 300 m.y. now reveal multiple 

global climate change events in unprecedented 

detail. Evidence for past 

CO 2 spikes comes from expanded and 

refined stomatal index data of fossil 

Ginkgo and related leaves. New evidence 

for synchronous climatic change 

comes from paleosols in Montana, Utah, 

and neighboring states. Each CO 2 spike 

was coeval with unusually clayey, red, 

and decalcified paleosols that can be 

traced throughout the Colorado Plateau. 

Spikes in atmospheric CO 2 also were 

coeval with increases in paleosol alkali 

depletion as an indication of high temperature, 

and spikes in paleosol base depletion 

and depth to calcic horizons as 

indications of high precipitation. In the 

Colorado Plateau, times of warmer climate 

were also more humid, perhaps due 

to the greater moisture potential of 

warmer air. Seasonality of climate did 

not increase during warm-wet spikes. 

151

The Mesozoic greenhouse was not persistently 

hot with cool spells, but warm 

with hot flashes. These data furnish 

power laws predicting the sensitivity and 

magnitude of change in mean annual 

temperature (MAT) and mean annual 

precipitation (MAP) due to rising CO 2 in 

a mid-latitude, mid-continental region. 

The magnitude of the coming anthropogenic 

greenhouse pales in comparison 

with past greenhouse spikes at times of 

global mass extinctions. 

2010010514 

古生物地理学中的气候、气候生物地 

理和生物年代单位 = On the climatic, 

climatobiogeographic, and biochorologic 

units in paleobiogeography. 

( 英文 ). Yanin B T. Paleontological 

Journal, 2010, 44(1): 1-10 7 图版 . 

The use of terms in climatic, climatobiogeographic, 

and biochorologic studies 

are considered. The terms climatic 

zone, climatochore, biochore and their 

relationships are discussed, using an example 

of the Mesozoic sea areas. The 

historical development of the climatobiogeographic 

method of zonation is 

briefly described and examples of the 

establishment of climatic zonation and 

climatobiogeographic belts in some periods 

of the Phanerozoic are reported. 

2010010515 

化石和同位素数据指示东亚大陆边缘 

(Sikhote-Alin 地区 ) 二叠纪 — 白垩 

纪最早期气候波动 = Permian to earliest 

Cretaceous climatic oscillations in 

the eastern Asian continental margin 

(Sikhote-Alin area), as indicated by fossils 

and isotope data. ( 英文 ). Zakharov 

Y D; Sha J G; Popov A M; Safronov P P; 

Shorochova S A; Volynets E B; Biakov 

A S; Burago V I; Zimina V G; Konovalova 

I V. GFF, 2009, 131(1-2): 25- 

47 10 图版 . 

Palaeozoological, palaeobotanical and 

geochemical analyses of Lower Permian 

to the lowermost Cretaceous sediments 

exposed in the southern Russian Far 

East (Bureya-Jiamusi-Khanka superterrane 

and the Sergeevka terrane), and 

higher latitude areas (northern Russian 

Far East and Spitsbergen) suggest a direct 

relationship with global climatic 

events defined by the data from oxygenisotopic 

palaeotemperatures. Several 

positive carbon-isotopic anomalies discovered 

within the uppermost Cisuralian, 

Guadalupian, early Lopingian and 

Aalenian-Bajocian intervals are possibly 

connected to strong hydrological intermixing 

of oceanic waters under the influence 

of considerable thermal gradients. 

2010010516 

高分辨率泥炭沉积中发现的火山灰层 

及其对气候事件的指示意义 = Tephra 

discovered in high resolution peat sediment 

and its indication to climatic event. 

( 英文 ). Cheng S G;Mao X M;Wang F 

L;Hong Y T;Zhu Y Z;An Q. Journal of 

China university of geosciences, 2008, 

19(2): 174-183 

Floating tephra was deposited together 

with ice core, snow layer, abyssal 

sediment, lake sediments, and other geological 

records. It is of great significance 

to interpret the impact on the climate 

change of volcanic eruptions from these 

geological records. It is the first time 

that volcanic glass was discovered from 

the peat of Jinchuan Maar, Jilin Province, 

China. And it is in situ sediments from a 

near-source explosive eruption according 

to particle size analysis and identification 

results. The tephra were neither 

from Tianchi volcano eruptions, 

Changbai Mountain, nor from Jinlongdingzi 

volcano about 1600 aBP eruption, 

but maybe from an unknown eruption of 

Longgang volcano group according to 

their geochemistry and distribution. 

Geochemical characters of the tephra are 

similar to those of Jinglongdingzi, which 

are poor in silica, deficient in alkali, 

Na2O content is more than K2O content, 

and are similar to distribution patterns of 

152

REE and incompatible elements, which 

helps to speculate that they originated 

from the same mantle magma with rare 

condemnation, and from basaltic explosive 

eruption of Longgang volcano 

group. The tephra, from peat with age 

proved that the eruption possibly happened 

in 15 BC-26 AD, is one of Longgang 

volcano group eruption that was 

not recorded and is earlier than that of 

Jinglongdingzi about 1600 aBP eruption. 

And the sedimentary time of tephra is 

during the period of low temperature alteration, 

which may be the influence of 

eruption toward the local climate according 

to the correlativity of eruption to 

local temperature curve of peat cellulose 

oxygen isotope. 

2010010517 

基于湖泊沉积的西伯利亚东北部气候 

和植被重建 = A reconstruction of the 

climate and vegetation of northeastern 

Siberia based on lake sediments. ( 英文 ). 

Lozhkin A V; Anderson P A. Paleontological 

Journal, 2006, 40(Supplement 

5): S622-S628 3 图版 . 

Detailed palynological analysis of 

glacial, tectonic, and crater lakes of 

northeastern Siberia reveals continuous 

records of the changing vegetation during 

one or several climatic cycles of the 

Pleistocene and in the Holocene. The 

most continuous records in the mountain 

areas of the region are those of Lake 

Elikchan-4 (northern Okhotsk Sea Region). 

Pollen records of Lake 

El’gygytgyn, which was formed by the 

impact of a meteorite in the northern 

Chukchi Peninsula, reflect the response 

of land vegetation to the global climatic 

impact during the last 300 ka. 

前古生界 

2010010518 

印度中部 Chattisgarh 盆地最上部凝 

灰岩锆石的 SHRIMP 年龄指示印度 

元古代地层学 500Ma 的修正 = 

SHRIMP ages of zircon in the uppermost 

tuff in Chattisgarh Basin in central 

India require similar to 500-Ma adjustment 

in Indian Proterozoic stratigraphy. 

( 英文 ). Patranabis-Deb S; Bickford M E; 

Hill B; Chaudhuri A K; Basu A. Journal 

of Geology, 2007, 115(4): 407-415 

The Chattisgarh Basin of east central 

India and many unmetamorphosed Proterozoic 

sedimentary basins of Peninsular 

India have been considered mostly 

Neoproterozoic (1000-545 Ma) in age. 

A newly recognized succession of rhyolitic 

ignimbrite, ash beds, and volcaniclastic 

sandstones near the top of the 

similar to 2.2-km-thick sedimentary fill 

of the Chattisgarh Basin is a 

chronostratigraphic marker. Euhedral 

igneous zircons from these units give U- 

Pb SHRIMP ages of 990-1020 Ma, indicating 

that the basin fill beneath this 

marker horizon is pre-Neoproterozoic. 

On the basis of newly reported zircon 

ages of Ma from the basal part of the 

Vindhyan Basin and accepting the consensus 

that all 1631 +/- 5 virtually undeformed 

and unmetamorphosed cratoninterior 

Proterozoic sedimentary basins 

in peninsular India are approximately 

coeval, we conclude that these basins are 

approximately Mesoproterozoic (1600- 

1000 Ma) in age. The reassigned age for 

these rocks (1650 to 900 or possibly 

similar to 1000 Ma), up to 500 Ma in 

variance with the current notion (similar 

to 1100 to similar to 518 Ma; Naqvi 

2005), calls for a thorough rethinking of 

contemporary models concerning tectonics, 

sedimentation, and other geological 

activity that affected the Indian shield in 

the Proterozoic Era. 

2010010519 

赞比亚南部 Zambezi 外壳岩层序的地 

质年代学 : 沿刚果克拉通南缘新元古 

代离散过程的记录 = Geochronology of 

the Zambezi supracrustal sequence, 

southern Zambia: A record of Neoproterozoic 

divergent processes along the 

southern margin of the Congo Craton. 

153

( 英文 ). Johnson S P; De Waele B; Evans 

D; Banda W; Tembo F; Milton J A; 

Tani K. Journal of Geology, 2007, 

115(3): 355-374 

The Zambezi supracrustal sequence 

(ZSC) of southern Zambia comprises a 

metasedimentary package of clastics and 

carbonates, with a thick sequence of 

basal volcanics and lavas. The sequence 

has traditionally been interpreted as a 

Neoproterozoic continental rift succession, 

but the lack of reliable age constraints 

hinders any tectonic interpretation. 

In this article, we date magmatic 

and detrital zircons using the U-Pb 

SHRIMP method in order to better constrain 

the timing of rifting, volcanism, 

and basin deposition. The basal volcanoclastic 

Kafue Rhyolite and 

Nazingwe formations were erupted at ca. 

880 Ma, and the sequence was intruded 

by the Lusaka Granite at ca. 820 Ma, 

providing lower and upper limits on the 

age of sedimentation. Whole-rock Nd 

isotopic signatures of these volcanics 

indicate that they formed as a result of 

assimilation and recycling of basement 

gneisses, probably during crustal thinning 

and extension. We uphold the correlation 

between the ZSC and the Roan 

Group in the Zambian Copperbelt and 

suggest that both successions formed in 

discrete rift basins along the southern 

margin of the Congo-Tanzania- 

Bangweulu (CTB) Craton; however, extension 

at this time probably did not result 

in complete continental separation. 

If the CTB Craton were an integral part 

of Rodinia, then rifting at ca. 880 Ma 

would represent one of the first known 

records of attempted breakup of the supercontinent. 

2010010520 

Nzilo 群 (Kibaran 带 ) 碎屑锆石的 

U-Pb SHRIMP 定年 : 对非洲中部沉 

积物来源及中元古代演化的启示 = U- 

PbSHRIMP dating of detrital zircons 

from the Nzilo Group (Kibaran belt): 

Implications for the source of sediments 

and Mesoproterozoic evolution of central 

Africa. ( 英文 ). Kokonyangi J W; 

Kampunzu A B; Armstrong R; Arima M; 

Yoshida M; Okudaira T. Journal of Geology, 

2007, 115(1): 99-113 

The Kibaran Supergroup, a >= 13000- 

km-long belt of metasedimentary and 

igneous rocks in the southeastern Congo, 

is in a critical location between the 

Congo Craton (sensu stricto) and the 

Tanzania-Bangweulu Block. Understanding 

its tectonic evolution will shed 

much-needed light on the amalgamation 

history of sub-Saharan Africa. This 

study presents U-Pb SHRIMP age data 

for 150 detrital zircons from four metasedimentary 

formations of the Nzilo 

Group, the middle lithostratigraphic unit 

within the Kibaran Supergroup in Katanga 

Province. These samples yielded 

dates between 3214 +/- 7 and 1329 +/- 

32 Ma. Prismatic Mesoproterozoic detrital 

zircons (dated at 1499 +/- 49 to 1329 

+/- 32 Ma, with a peak at 1380 Ma) occur 

in all samples and are inferred to be 

derived from the Mitwaba orthogneisses, 

which intrude the Kiaora Group, the 

oldest lithostratigraphic unit of the Kibaran 

Supergroup. More than threequarters 

of the zircon population is 

composed of recycled grains, yielding 

dates between and Ma, with 2434 +/- 5 

1696 +/- 18 peaks at 2050 and 1850 Ma. 

These peaks overlap with the timing of 

geological events in the adjacent Paleoproterozoic 

Bangweulu Block, including 

the Ubendian-Usagaran belts. Archean 

zircons were not found in the oldest 

Nzilo units and are restricted to the 

youngest Nzilo rocks, where they form 

only a minor component (

geochronological data, coupled with the 

regional geology, indicate that a substantial 

portion of the Nzilo Group detritus 

came from interbasinal reworking of 

the underlying Kiaora Group and its associated 

1.38-Ga orthogneisses, with a 

significant contribution from the Tanzania-Bangweulu 

Block. The data support 

a previously proposed subductional 

model for the Kibaran belt and constrain 

the paleotectonic environment during 

the deposition of the Nzilo Group. 

2010010521 

Limpopo 复合体中心区域的地质历 

史 : 西 Alldays 地区 = Geologic history 

of the Central Zone of the Limpopo 

Complex: The West Alldays area. ( 英 

文 ). Boshoff R; Van Reenen D D; Smit 

C A; Perchuk L L; Kramers J D; Armstrong 

R. Journal of Geology, 2006, 

114(6): 699-716 

New field, structural, petrologic, and 

age data show that tectonic styles and 

metamorphic histories in the West Alldays 

area of the Central Zone of the 

Limpopo Complex, southern Africa, can 

be linked to neo-Archean and Paleoproterozoic 

high-grade ( granulite facies) 

tectonometamorphic events. The styles 

comprise ( 1) a regionally developed 

high-grade (S-2) gneissic fabric that 

evolved into a regional (D-2) system of 

sheath folds mapped as circular to ovalshaped 

structures with lineations plunging 

steeply to the WSW and ( 2) a system 

of mainly N-S-trending and northverging 

(D-3) shear zones characterized 

by high-grade tectonites ("straight 

gneisses") with well-developed (S-3) 

gneissic fabrics. In the West Alldays 

area, the superimposition of D-3 onto 

the regional D-2 fold pattern produced 

the kilometer-scale N-S-trending 

Baklykraal shear zone, which, before 

this study, was mapped as the Baklykraal 

fold and interpreted as part of the 

regional D-2 fold pattern in the Central 

Zone. The Paleoproterozoic hightemperature 

D-3 shear event is accurately 

constrained to 2023 +/- 11 Ma by 

a Pb/Pb stepwise leaching garnet date 

that reflects the syntectonic crystallization 

of a garnet-cordierite-sillimanitebiotite-quartz 

paragenesis formed during 

shearing. This tectonite records a retrograde 

pressure-temperature (PT) path 

from 780 degrees C at 5.7 kbar to 600 

degrees C at 3.3 kbar. The neo-Archean 

age of the M-2 granulite facies metamorphism, 

coeval with the tight D-2 

folding preserved within the Baklykraal 

shear zone, is evident from several garnet 

Pb/Pb stepwise leaching experiments 

that gave dates intermediate between 

2000 and 2600 Ma, with large scatter in 

the data arrays ( thus interpreted as 

mixed ages), and from zircon ages of 

protoliths of the syn-D-2 Singelele-type 

quartzofeldspathic gneisses. A polymetamorphic 

garnet – cordierite - 

orthopyroxene – biotite - quartz paragenesis 

from a D-2 outcrop within the 

Baklykraal shear zone records two PT 

paths: a decompression-cooling PT path 

from similar to 850 degrees C at similar 

to 8.5 kbar to similar to 675 degrees C at 

similar to 6 kbar at similar to 2600 Ma 

and an isobaric ( 6 kbar) heating event 

from similar to 675 degrees C to similar 

to 770 degrees C that was immediately 

followed by a decompression-cooling 

path that reflects the uplift of the highgrade 

rocks toward the Earth's surface 

( to the level of about 8 - 10 km). Polymetamorphic 

granulites that resulted 

from the isobaric heating event introduce 

new petrologic and geochronologic 

problems. On the basis of new data, we 

thus document previously unrecognized 

N-S-trending high-temperature shear 

zones and associated polymetamorphic 

granulites from the Central Zone of the 

Limpopo Complex. These shear zones 

developed in the Paleoproterozoic and 

were superimposed onto older ( neo- 

Archean) regional fold structures. The 

tectonic history of the Central Zone of 

the Limpopo Complex is therefore characterized 

by two high-grade tectono- 

155

metamorphic events separated by at least 

550 m. yr. These data require that existing 

models for crust formation in the 

Central Zone, including those that argue 

for a single granulite facies event linked 

to an orogeny at similar to 2000 Ma, be 

reconsidered. 

2010010522 

前寒武纪早期地球生物系统的演化 = 

The evolution of the early Precambrian 

geobiological systems. ( 英文 ). Rozanov 

A Yu; Astafieva M M. Paleontological 

Journal, 2009, 43(8): 911-927 7 图版 . 

Bacterial paleontology provides vast 

opportunities for the study of all types of 

sedimentary and volcanic-sedimentary 

rocks, at any stage of metamorphism and 

of any age. Bacteria are shown to play 

an important role in weathering, transfer, 

sedimentation, and diagenesis of the 

sediments and in the formation of many 

minerals that have previously been 

thought to be abiogenic. 

2010010523 

古元古代石化的油田 (Shunga 事 

件 ) = Palaeoproterozoic petrified oil 

field (Shunga Event). ( 英文 ). Medvedev 

P V; Melezhik V A; Filippov M M. Paleontological 

Journal, 2009, 43(8): 972- 

979 5 图版 . 

Significant accumulation of autochthonous 

organic matter preserved in Palaeoproterozoic 

rocks is rare. One of the 

largest and most remarkable occurrences 

is the deposit at Shunga, in Karelia, 

northwestern Russia. This enormous accumulation 

of C-rich rocks is part of the 

world-wide Shunga Event. The integrated 

data suggest that the OM was 

most likely derived from planktonic microorganisms. 

This remarkable accumulation 

of OM and inferred generation of 

giant volume of petroleum took place in 

the aftermath of the ca 2330–2060 Ma 

Lomagundi—Jatulian Event—the largest 

positive excursion of δ 13 C carb of 

sedimentary carbonate in the Earth’s history. 

The formation of shungite carbon 

and its diagenetic, catagenetic and 

metamorphic transformation are related 

to fundamental problems of biological 

evolution, global carbon cycle and the 

earliest oil generation. 

2010010524 

湖北宜昌茅坪泗溪剖面埃迪卡拉系岩 

石地层和碳同位素地层研究 = Lithoand 

carbon isotope stratigraphy of the 

Ediacaran system in the Sixi Section 

(Yangtze Gorges) , Yichang, Hubei. ( 中 

文 ). 吕苗 ; 朱茂炎 ; 赵美娟 . 地层学杂 

志 , 2009, 33(4): 359-372 

华南埃迪卡拉系陡山沱组上部的 

δ13C 巨大负异常事件 (DOUNCE) 是 

当前埃迪卡拉系研究最受关注的焦点 

之一。在对湖北宜昌茅坪泗溪剖面埃 

迪卡拉系开展高精度的岩石地层和碳 

氧同位素研究的基础上 , 通过与黄陵背 

斜周缘其他剖面的对比 , 表明峡区陡 

山沱晚期 DOUNCE 事件的 δ13C 值变 

化由下降 — 负漂移 — 短期正漂移 — 回 

升 4 个阶段构成 , 但 DOUNCE 事件在 

不同剖面上的表现存在明显差异。详 

细的沉积岩相分析和地层对比表明 , 各 

剖面 δ13C 演化差异是由岩相变化导 

致的岩石地层发育差异引起的。泗溪 

剖面 DOUNCE 事件主体部分缺失与 

该剖面位于台内盆地斜坡环境 , 发育多 

层滑塌构造造成的地层缺失有关。研 

究结果表明在缺乏生物地层控制的埃 

迪卡拉系 ,δ13C 同位素地层是揭示沉 

积相变化造成的岩石地层差异和地层 

对比的重要手段。 

2010010525 

SHRIMP 锆石 U–Pb 年龄对中国西北 

部库鲁克塔格地区新元古代冰碛岩的 

时代限制 = SHRIMP zircon U–Pb age 

constraints on Neoproterozoic Quruqtagh 

diamictites in NW China. ( 英文 ). 

Xu Bei; Xiao Shuhai; Zou Haibo; Chen 

Yan; Li Zhengxiang; Song Biao; Liu 

Dunyi; Zhou Chuanming; Yuan Xunlai. 

156

Precambrian Research, 2009, 168(3-4): 

247-258 

The Neoproterozoic Quruqtagh Group 

in the Tarim Block, NW China, contains 

multiple diamictites in the Bayisi, Altungol, 

Tereeken, and Hankalchough 

formations. These diamictites may represent 

three or possibly four discrete 

glaciations, although evidence for a glacial 

origin of the Bayisi and Altungol 

diamictite is ambiguous. To constrain 

their age and duration, we dated three 

volcanic beds (V1, V2, and V3) in the 

Quruqtagh Group using the SHRIMP 

(sensitive high-resolution ion microprobe) 

zircon U–Pb method. Volcanic 

bed V1 near the base of the Bayisi 

diamictite yields a 740 ± 7 Ma age, volcanic 

bed V2 near the top of the Bayisi 

Formation gives a 725 ± 10 Ma age, and 

volcanic bed V3 between the Tereeken 

and Hankalchough diamictites yields a 

615 ± 6 Ma age. V1 and V2 have overlapping 

ages, and together these dates 

suggest that the Bayisi diamictite was 

deposited at around 730 Ma. The 

Tereeken and Altungol diamictites were 

deposited between 725 ± 10 Ma and 

615 ± 6 Ma, and the Hankalchough 

diamictite between 615 ± 6 Ma and 

542 Ma (i.e., the Neoproterozoic– 

Cambrian transition). These dates and 

previously published chemostratigraphic 

data are consistent with (but doe not require) 

the correlation of the Tereeken 

and Hankalchough diamictites with the 

635 Ma Nantuo and 582 Ma Gaskiers 

glaciations, respectively. However, the 

new dates are inconsistent with a single 

and globally synchronous Sturtian glaciation 

that occurred in the pre-Nantuo 

Neoproterozoic Era. Instead, currently 

available data necessitate that either 

multiple glaciations occurred, or a globally 

diachronous glacial event developed 

during a protracted period between 

750 Ma and 650 Ma. 

2010010526 

巴西 São Francisco 盆地 Vazante 群 

上部碳酸盐岩记录的中元古代晚期海 

洋氧化还原条件 : 来自稳定同位素和 

稀土元素的证据 = Oceanic redox conditions 

in the Late Mesoproterozoic recorded 

in the upper Vazante Group carbonates 

of São Francisco Basin, Brazil: 

Evidence from stable isotopes and REEs. 

( 英文 ). Azmy Karem; Sylvester P; 

Oliveira T F. Precambrian Research, 

2009, 168(3-4): 259-270 

The Vazante Group consists of a late 

Mesoproterozoic (1.0–1.1 Ga) carbonate-dominated 

marine platform sequence 

in east-central Brazil. The upper part of 

the sequence consists of a glaciomarine 

diamictite unit overlain by a cap carbonate. 

The δ 13 C profile of the upper 

Vazante shows significant negative 

plunges, one preglacial (drop of 5.5‰ 

VPDB) and two postglacial (drops of 9 

and 5‰VPDB, respectively). The C- 

isotope plunge in the preglacial carbonates 

is correlated with low Th/U ratios 

(0.1–1.4) and a negative Ce/Ce* shift 

(0.4), suggesting deposition under relative 

reducing conditions. In contrast, the 

C-isotope plunges in the postglacial carbonates 

are associated with high Th/U 

ratios (>2) and positive Ce/Ce* shifts 

(up to 1.5), thus reflecting oxidizing 

conditions. Variations in the redox conditions 

of the late Mesoproterozoic 

ocean, reflected by changes in the Th/U 

and Ce/Ce* ratios, are likely attributable 

to a combination of both global and local 

climatic and oceanographic changes, 

similar to what has been inferred for the 

Neoproterozoic oceans. 

2010010527 

古元古代晚期裂陷盆地的 Ar-Ar 和 

U-Pb 地质年龄 : 对与加拿大 

Nunavut 地区 Churchill 省西部哈德 

森造山运动具有成因联系的支持 = 

Ar-Ar and U-Pb geochronology of a late 

Paleoproterozoic rift basin: Support for a 

genetic link with Hudsonian orogenesis, 

157

western Churchill Province, Nunavut, 

Canada. ( 英文 ). Rainbird R H; Davis W 

J; Stern R A; Peterson T D; Smith S R; 

Parrish R R; Hadlari T. Journal of Geology, 

2006, 114(1): 1-17 

The Baker Lake Group ( Baker Sequence) 

represents the record of the 

formative stage of Baker Lake Basin, a 

series of generally elongate, northeaststriking, 

half-graben, and fault-bounded 

troughs filled with continental redbeds 

and coeval voluminous ultrapotassic 

volcanic rocks. An estimate for the time 

of basin initiation is given by a U-Pb 

( zircon) age of 1833 +/- 3 Ma, obtained 

from a basal volcanic flow at the western 

end of the basin, which is in agreement 

with a less precise Ar-40/Ar-39 

(phlogopite) step-heating plateau age of 

1811 +/- 12 Ma from a flow located at a 

similar stratigraphic level in the eastern 

Baker Lake Basin. Ar-40/Ar-39 analysis 

of phlogopite phenocrysts in a syenite 

that intrudes the lower part of the Baker 

Sequence yielded a plateau age of 1811 

+/- 12 Ma. The syenite also intrudes 

sandstones containing detrital zircons 

with xenotime (YPO4) overgrowths, 

known to form during burial diagenesis. 

In situ U/Pb SHRIMP analysis of these 

overgrowths yields an upper intercept 

age of 1838 +/- 27 Ma, which is within 

analytical uncertainty of the ages obtained 

from the volcanic flows. Alluvial 

conglomerates near the top of the Baker 

Sequence contain discontinuous layers 

of laminar carbonate cements interpreted 

as geothermal travertine. Specific calcite 

layers within the travertine have very 

high U-238/Pb-204 values and yield a 

Pb-Pb isochron age of 1785 +/- 3 Ma, 

considered to represent a minimum age 

for deposition of the Baker Sequence. 

Our data suggest that the Baker Sequence 

was deposited over an interval of 

approximately 55 m. yr. (1840-1785 

Ma), within error of the predicted periodicity 

of a second-order sequence. This 

interval coincides with collisional and 

postcollisional deformation and magmatism 

in the Trans-Hudson orogen and 

thus supports interpretations that the 

Baker Lake Basin formed in response to 

related far-field extension. 

2010010528 

斑脱岩中锆石 SHRIMP 测年在前寒 

武纪地层中的应用 —— 前寒武纪年代 

地层学研究的新思路 = Zircon 

SHRIMP dating of the K-bentonite in 

the Precambrian strata. ( 中文 ). 王泽九 . 

地层学杂志 , 2010, 34(1): 57-59 

建立中国晚前寒武纪年代框架始终 

是地学界关注的基础地质问题 , 然而多 

年来关键层位仍缺乏高质量同位素年 

龄的约束 , 随着 SHRIMP 测年的引进 

和大量层凝灰岩或斑脱岩在前寒武纪 

地层中不断被识别 , 测年技术提高后 , 

可完成对斑脱岩中岩浆型微小锆石颗 

粒的测年要求 , 使中、新元古代地层年 

代学的研究获得极大的突破 , 改变了我 

国使用了近 80 年的传统中、新元古 

代地层对比的认识。随着同位素年代 

学资料不断地为中、新元古代地层柱 

中的定位增添新的数据资料 , 它不仅再 

次准确地确定了地层的形成时代 , 而且 

对整个地台中、新元古代地层的地质 

演化史的认识和生物演化在中元古代 

年代地层柱准确定位都有着重要的地 

质意义 

古生界 

2010010529 

西澳大利亚坎宁盆地 Mowanbini 群岛 

岩岸外侧泥盆系生物礁复合体 = Outer 

rocky shores of the Mowanbini Archipelago, 

Devonian reef complex, Canning 

Basin, western Australia. ( 英文 ). 

Johnson M E; Webb G E. Journal of 

Geology, 2007, 115(5): 583-600 

The Oscar Range in Western Australia's 

Canning Basin features inliers of 

folded Paleoproterozoic quartzite, 

quartzitic conglomerate, and phyllite 

that formed islands during the Late Devonian. 

Undisturbed strata of the Pillara 

Limestone ( Upper Devonian, Frasnian 

158

Stage) surround individual paleoislands 

that rise above the former seabed with a 

maximum topographic relief of 90 m. 

On average, the Mowanbini Archipelago 

( aboriginal name for the Oscar Range) 

lies 15 km off the granitic and metamorphic 

mainland represented by the Kimberley 

Block to the north. Devonian facies 

on outer rocky shores were studied 

at three localities near the southeast end 

of the Oscar Range. At the west end of 

the study area, a Devonian reef margin 

sits unconformably on Paleoproterozoic 

phyllite, but to the east, the reef is separated 

from rocky shores by a wide lagoon. 

Massive clast- supported conglomerate 

and sandstone beds interfinger 

with backreef carbonates where the 

reef is closest to land. Across the lagoon 

2.5 km eastward, differential erosion between 

steeply dipping quartzite layers 

interbedded with softer phyllite resulted 

in low sea stacks, or skerries. Tabular 

quartzite cobbles and quartz sand were 

shed by the skerries as a unidirectional 

apron of " breccia" under shoal water 

conditions. Nearby offshore stromatoporoid 

thickets reflect growth orientation 

aligned with paleocurrents 

compatible with the breccia apron. On a 

smaller island 2.5 km farther east, lateral 

transport of debris from a quartzite shore 

to a contiguous phyllite sector of the 

coast conforms to the same pattern of 

water circulation. Overall, the physical 

geography of outer rocky shores in relation 

to the lagoon and barrier reef suggests 

that waves crashed over the reef to 

energize a longshore current that moved 

west to east at one end of the Oscar 

Range. A rapid rise in sea level probably 

promoted the burial and preservation of 

the Mowanbini Archipelago, characteristics 

shared with other examples of 

quartzite paleoislands that date from 

Cambrian to Cretaceous times. 

2010010530 

Talladega 带变质历史及同位素年龄 

的约束 : 沿劳伦古陆南部边缘岛弧岩 

浆作用和地体侵位时间的新证据 = 

Isotopic age constraints and metamorphic 

history of the Talladega belt: New 

evidence for timing of arc magmatism 

and terrane emplacement along the 

southern Laurentian margin. ( 英文 ). 

McClellan E A; Steltenpohl M G; Thomas 

C;Miller C F. Journal of Geology, 

2007, 115(5): 541-561 

U- Pb and 40Ar/ 39Ar dates from the 

Talladega belt, southernmost Appalachians, 

provide insight into the timing and 

nature of pre- Alleghanian tectonism in 

this region. Low- grade metasedimentary 

rocks of the Talladega belt represent 

the outermost preserved portions of the 

southern Laurentian margin, thus recording 

the earliest orogenic events that 

affected the margin, in addition to later 

overprinting events. These rocks are 

structurally overlain by the Hillabee 

Greenstone metavolcanic sequence, 

from which metadacite yields an age of 

470 +/- 4 Ma (ion microprobe U- Pb zircon 

age). Hillabee geochemistry indicates 

formation in an arc or back-arc setting. 

We suggest correlation of the Hillabee 

Greenstone with 460 - 470- Ma 

arc-related rocks in the Dahlonega gold 

belt, which extends along strike with the 

Hillabee through Georgia and into North 

Carolina, and interpret the Hillabee as 

the southernmost volcanic expression of 

an Early-Middle Ordovician arc that 

formed outboard of Laurentia. Rocks of 

the Talladega belt, including the Hillabee, 

preserve a record of only one Paleozoic 

dynamothermal metamorphic 

event. 40Ar/ 39Ar dates are consistent 

with metamorphism following deposition 

of the youngest biostratigraphically 

dated unit, the Erin Slate, which contains 

early Mississippian Periastron 

plant fossils (360 - 350 Ma). Muscovite 

(closure temperature 350 degrees - 400 

degrees C) yields internally consistent 

ages between 334 and 320 Ma. Metamorphism 

of the Talladega belt, therefore, 

is constrained to the interval between 

360 and 320 Ma. The pre- to 

159

synmetamorphic thrust contact between 

the Hillabee Greenstone and Talladega 

belt metasedimentary rocks must have 

formed after deposition of the Erin Slate 

at 360 - 350 Ma but before metamorphism 

of the Talladega belt (no later 

than similar to 320 Ma). We propose 

that the Ordovician HillabeeDahlonega 

arc terrane first collided with the 

Laurentian continental margin between 

360 and 320 Ma, with variations in timing 

of deformation and metamorphic 

character along the collision zone. 

2010010531 

落基山脉发现晚古生代峡谷 = An exhumed 

late Paleozoic canyon in the 

Rocky Mountains. ( 英文 ). Soreghan G S; 

Sweet D E; Marra K R; Eble C F; 

Soreghan M J; Elmore R D; Kaplan S A; 

Blum M D. Journal of Geology, 2007, 

115(4): 473-481 

Landscapes are thought to be youthful, 

particularly those of active orogenic 

belts. Unaweep Canyon in the Colorado 

Rocky Mountains, a large gorge drained 

by two opposite-flowing creeks, is an 

exception. Its origin has long been enigmatic, 

but new data indicate that it is 

an exhumed late Paleozoic landform. Its 

survival within a region of profound late 

Paleozoic orogenesis demands a reassessment 

of tectonic models for the Ancestral 

Rocky Mountains, and its form 

and genesis have significant implications 

for understanding late Paleozoic 

equatorial climate. This discovery highlights 

the utility of paleogeomorphology 

as a tectonic and climatic indicator. 

2010010532 

新英格兰东南部阿瓦龙带的寒武纪 - 奥 

陶纪古地理 : 对冈瓦那解体的启示 = 

Cambro-Ordovician paleogeography of 

the Southeastern New England Avalon 

Zone: Implications for Gondwana 

breakup. ( 英文 ). Thompson M.D; 

Grunow A M Ramezani J. Geological 

Society of America Bulletin, 2010, 

122(1-2): 76-88 

Paleomagnetic measurements and U- 

Pb geochronology of alkalic igneous 

rocks intruding the Ediacaran Cambridge 

Argillite and the Lower Cambrian 

Weymouth Formation north of Boston at 

Nahant, Massachusetts yield a wellconstrained 

paleopole. The oldest intrusive 

phases are a syenodiorite sill and a 

granite dike with 206 Pb/ 238 U crystallization 

ages of 490.19 ± 0.90 Ma and 

489.03 ± 0.82 Ma, respectively. This sequence 

along with undated mafic sills 

penetrating both the argillite and Weymouth 

strata are cut by 488.53 ± 0.81 

Ma gabbro locally associated with 

488.48 ± 0.79 Ma syenite forming a 

steep-sided intrusive plug. Ten paleomagnetic 

sampling sites within the mafic 

sills and the gabbro contain a stable A 

magnetic component with a mean direction 

of D = 278.5°, I = -76.7° (A 95 = 3.9°, 

N = 10). This is considered to be the 

primary magnetization direction because 

it passes both fold and reversals tests. 

The corresponding paleopole at 320°E, 

34°N (A 95 = 7.2°, N = 10) places the 

Southeastern New England Avalon Zone 

at a southerly paleolatitude of 65° 

slightly removed from the African margin 

of Gondwana and suggests that bimodal 

Nahant magmatism is linked with 

latest Cambrian-Early Ordovician rifting 

of West Avalonia to form the Rheic 

Ocean. 

Stable B and C magnetic components 

in Nahant syenodiorite and syenite give 

rise to virtual geomagnetic poles that 

track Late Silurian through Carboniferous 

segments of the North American apparent 

polar wander path, indicating 

docking of West Avalonia by mid- 

Paleozoic time. 

2010010533 

美国东部中阿巴拉契亚盆地晚泥盆世 

冰川相和共生的相 = Late Devonian 

glacigenic and associated facies from the 

central Appalachian Basin, eastern 

160

United States. ( 英文 ). Brezinski D K; 

Cecil C B; Skema V W. Geological Society 

of America Bulletin, 2010, 122(1- 

2): 265-281 

Late Devonian strata in the eastern 

United States are generally considered as 

having been deposited under warm 

tropical conditions. However, a stratigraphically 

restricted Late Devonian 

succession of diamictite-mudstonesandstone 

within the Spechty Kopf and 

Rockwell Formations that extends for 

more than 400 km along depositional 

strike within the central Appalachian 

Basin may indicate otherwise. This 

lithologic association unconformably 

overlies the Catskill Formation, where a 

3- to 5-m-thick interval of deformed 

strata occurs immediately below the 

diamictite strata. The diamictite facies 

consists of several subfacies that are interpreted 

to be subglacial, englacial, supraglacial 

meltout, and resedimented deposits. 

The mudstone facies that overlies 

the diamictite consists of subfacies of 

chaotically bedded, clast-poor mudstone, 

and laminated mudstone subfacies that 

represent subaqueous proximal debris 

flows and distal glaciolacustrine rhythmites 

or varvites, respectively. The pebbly 

sandstone facies is interpreted as 

proglacial braided outwash deposits that 

both preceded glacial advance and followed 

glacial retreat. 

Both the tectonic and depositional 

frameworks suggest that the facies were 

deposited in a terrestrial setting within 

the Appalachian foreland basin during a 

single glacial advance and retreat. Regionally, 

areas that were not covered by 

ice were subject to increased rainfall as 

indicated by wet-climate paleosols. 

River systems eroded deeper channels in 

response to sea-level drop during glacial 

advance. Marine facies to the west contain 

iceborne dropstone boulders preserved 

within contemporaneous units of 

the Cleveland Shale Member of the 

Ohio Shale. 

The stratigraphic interval correlative 

with sea-level drop, climate change, and 

glacigenic succession represents one of 

the Appalachian Basin's most prolific 

oil- and gas-producing intervals and is 

contemporaneous with a global episode 

of sea-level drop responsible for the 

deposition of the Hangenberg 

Shale/Sandstone of Europe. This interval 

records the Hangenberg biotic crisis near 

the Devonian-Carboniferous boundary. 

2010010534 

西伯利亚地台和俄罗斯地台奥陶纪古 

盆地海平面升降与生物事件的关系 = 

Correlation of eustatic and biotic events 

in the Ordovician paleobasins of the Siberian 

and Russian platforms. ( 英文 ). 

Dronov A V; Kanygin A V; Timokhin A 

V; Tolmacheva T Yu; Gonta T V. Paleontological 

Journal, 2009, 43(11): 

1477-1497 9 图版 . 

Nine sedimentary sequences are recognized 

in the Ordovician of the Siberian 

Platform. These sequences correspond 

to sea level fluctuations of the 3rd 

order, from 1 to 6 My. Correlation with 

the sequences recognized in the Ordovician 

of the Russian Platform suggest 

their possible eustatic nature. Cold water 

nontropical carbonates are suggested in 

the Ordovician of the Tungus Syneclise, 

which may be explained by the upwelling 

of cold oceanic waters. The upwelling 

was caused by re-distribution of 

oceanic currents due to largescale tectonic 

events in the mid-Ordovician. The 

Ordovician evolution of the Siberian 

Platform was much more similar to that 

of the North American Platform than of 

the Russian Platform. 

2010010535 

华南印支运动的起始 : 海南岛二叠纪 

岩浆弧的证据 = Initiation of the Indosinian 

Orogeny in South China: Evidence 

for a Permian magmatic arc on Hainan 

Island. ( 英文 ). Li X H; Li Z X; Li W X; 

161

Wang Y J. Journal of Geology, 2006, 

114(3): 341-353 

It has been widely accepted that an 

active continental margin existed along 

the coast of Southeast China during the 

Mesozoic time that produced extensive 

magmatism in the region. However, 

there is little constraint as to when this 

active margin was first initiated. Here 

we present new SHRIMP U-Pb zircon 

ages and geochemical and Sr-Nd isotopic 

data for syntectonic granites on 

Hainan Island. Our data demonstrate 

that these rocks, dated at 267-262 Ma, 

are typical of calc-alkaline I-type granites 

formed in continental arc environments. 

The age of this magmatic arc coincides 

with a sudden change in sedimentary 

environments in South China 

during the Permian time, suggesting that 

the South China Indosinian Orogeny 

was likely contemporaneous with the 

onset of continental arc magmatism. 

2010010536 

云南大理洱海砂子箐组的时代及谢尔 

普霍夫阶地层的发现 = The age of the 

Shaziqing Formation and the discovery 

of the Serpukhovian strata at the east 

bank of the Erhai,Dali,Yunnan. ( 中文 ). 

王平 ; 肖荫文 ; 王成源 ; 杨光华 ; 谢伟 . 微 

体古生物学报 , 2009, 26(3): 225-233 2 

图版 . 

云南大理洱海之东的砂子箐组产有 

牙形刺 Scaliognathus anchoralis , 

Gnathodus typicus , Gnathodus cf . 

girtyi 等化石 , 清楚地表明砂子箐组的 

地质时代为杜内期。在双廊镇大建旁 

村环海公路边灰岩中发现牙形刺 

Lochriea ziegleri , Gnathodus cantabricus 

, Gnathodus bilineatus remus , 

Gnathodus bilineatus romulus , 充分证 

明海东地区谢尔普霍夫阶地层的存 

在。 

2010010537 

冈瓦纳西部边缘晚元古代至早寒武世 

的沉积和岩浆作用 : 阿根廷 Sierras 

Norte de Cordoba 地区的变质沉积岩 

= Late Proterozoic to Early Cambrian 

sedimentation and magmatism at the 

western Gondwana margin: metasedimentay 

rocks in the Sierras Norte de 

Cordoba (Argentina). ( 英文 ). von Gosen 

W; Prozzi C. Neues Jahrbuch fur Geologie 

u. Palaontologie / Abhandlungen, 

2009, 253(1): 79-101 

Studies of clastic metasedimentary 

rocks in the Sierras Norte de Cordoba 

indicate a two-stage history of sedimentation, 

magmatism and initial tectonics. 

The basal clastic pile of rocks is recorded 

by coarse conglomerate and 

sandstone which overlie, and partly alternate 

with, rhyolite to rhyodacite. The 

conglomerates contain pebbles and 

partly boulders of acid magmatic rocks 

and widely distributed sandstone and 

siltstone derived from the local succession 

and a sedimentary cover sequence. 

They can be interpreted as fluvial 

to alluvial fan sediments presumably 

deposited during active normanl 

fault tectonics accompanied by acid volcanism. 

2010010538 

湖北建始黄岩及邻区二叠系大隆组生 

态地层 = Ecostratigraphy of the Permian 

Dalong Formation in the huangyan 

and adjacent area, Jianshi,Hubei. ( 中文 ). 

陈立德 . 地层学杂志 , 2009, 33(4): 432- 

440 

湖北建始黄岩及邻区二叠系大隆相 

区产丰富的菊石、双壳类、鱼类以及 

少量的壳薄体轻的腕足类和遗迹化石 

等底栖生物。根据建始黄岩和巫山纸 

厂沟剖面上化石的埋葬特征 , 以化石的 

形态功能分析为基础 , 将建始黄岩、巫 

山纸厂沟二叠纪大隆组 — 大冶组底部 

的生物群分为 9 个群落 , 根据群落对沉 

积盆地中游离氧的示踪 , 将区内群落划 

分为浮游微生物群落、游泳漂浮群 

落、底栖表生群落和底栖内生群落四 

种类型。在群落生态分析及群落带划 

162

分的基础上 , 分析了建始黄岩及邻区群 

落的时空分布及古地理演变特点。 

2010010539 

米仓山宝塔期碳酸盐岩海底峡谷的发 

现及其意义 = The discovery of an Ordovician 

carbonate submarine canyon 

system in the Micangshan area and its 

implication. ( 中文 ). 王永和 ; 焦养泉 ; 周 

志强 ; 雷桂侠 ; 李建星 . 地层学杂 

志 , 2009, 33(4): 351-358 

在米仓山元坝子一带 , 野外调查和室 

内显微岩石学研究发现宝塔组下部存 

在一套与正常宝塔组多角形网纹状泥 

晶灰岩完全不同的紫红色生物碎屑灰 

岩。紫红色生物碎屑灰岩具有特征的 

外部形态和内部结构。横向上 , 它以透 

镜状形式与多角形网纹状泥晶灰岩呈 

明显的相变关系 , 宽为 2 —2. 5km , 厚 

29. 3m; 纵向上 , 暴露地表的部分长度达 

600m。该沉积体以发育多级别的、典 

型正粒序沉积韵律为特征 , 构成生物碎 

屑灰岩的主要为异地搬运来的生物碎 

屑 , 它们具有明显的重力流色彩 , 是一 

种浊积水道沉积 , 将其解释为碳酸盐岩 

海底峡谷。区域调查与沉积学、古生 

物学研究表明 , 研究区的海底峡谷发育 

晚奥陶世卡拉道克中期 , 实测古水流方 

向指向为北西向 , 这与研究区总体处于 

浅外陆棚向深边缘海盆地过渡的古地 

理背景相吻合。宝塔组碳酸盐岩海底 

峡谷的发现 , 不仅为扬子地台西北缘奥 

陶纪古环境恢复提供了沉积学依据 , 同 

时也可以预测在研究区向西北方向可 

能存在海底峡谷 — 浊积扇沉积体系。 

2010010540 

浙江常山黄泥塘水库剖面的生物地层 

学 = Biostratigraphy of the Huangnitang 

reservoir Section in Changshan, Zhejiang 

Province. ( 中文 ). 张元动 ; 许红根 ; 

郭维民 ; 贺振宇 ; 周清 ; 王旭东 . 地层学杂 

志 , 2009, 33(4): 337-350 4 图版 . 

为有效保护我国第一个 “ 金钉子 ”— 

—— 浙江常山黄泥塘剖面的同时 , 又能 

较好地满足一般性补充研究的需求和 

普通大众对 “ 金钉子 ” 剖面化石的兴趣 

爱好 , 剖面保护单位在 “ 金钉子 ” 剖面附 

近水库边开辟了一条新剖面。该 

剖面地层序列完整 , 出露新鲜 , 自下而 

上包括印渚埠组上部、宁国组和胡乐 

组下部。剖面化石丰富 , 保存精美 , 除 

丰富的笔石外 , 还含有一些腕足动物、 

三叶虫、叶虾类和粪化石 , 自下而上可 

识别出 Corymbograptus deflexus 

带、Azygograptus suecicus 带、 

Exigraptus clavus 带、 

Undulograptus austrodentatus 带和 

Acrograptus ellesae 带等笔石带。 

整个剖面的岩石和笔石序列与黄泥塘 

“ 金钉子 ” 剖面一致 , 能进行良好对比 , 可 

作为 “ 金钉子 ” 剖面的一般性替代剖面 , 

从而为进一步开展达瑞威尔阶的后层 

型研究提供了新的证据来源。 

2010010541 

Delamerian 造山运动的定时及持续时 

间 : 与 Ross 造山带的对比及对冈瓦 

纳汇聚的启示 = The timing and duration 

of the Delamerian orogeny: Correlation 

with the Ross Orogen and implications 

for Gondwana assembly. ( 英文 ). 

Foden J; Elburg M A; Dougherty-Page J; 

Burtt A. Journal of Geology, 2006, 

114(2): 189-210 

The Antarctic Ross and the Australian 

Delamerian orogenies are the consequence 

of stress transfer to the outboard 

trailing edge of the newly assembled 

Gondwana supercontinent. This tectonic 

reorganization occurred in the Early to 

Middle Cambrian on completion of Pan- 

African deformation and subduction 

along the sutures between eastern and 

western Gondwanan continental fragments. 

Before this, Neoproterozoic to 

Early Cambrian rocks in eastern Australia 

were formed in a passive margin and 

record dispersion of Rodinia with consequent 

opening of the proto-Pacific. 

Our new U-Pb and Rb-Sr geochronology 

shows that in the South Australian (Ade- 

163

laide Fold Belt) domain of the Delamerian 

Orogen, contractional orogenesis 

commenced at 514 +/- 3 Ma and persisted 

for similar to 24 m.yr. until 490 

+/- 3 Ma, terminated by rapid uplift, 

cooling, and extension in association 

with posttectonic magmatism. Integration 

of new and published U-Pb and Ar- 

40-Ar-39 geochronology from the entire 

Ross-Delamerian belt shows that although 

both the Delamerian and Ross 

have a synchronous late magmatic and 

terminal cooling history, the Ross commenced 

its convergent orogenic history 

at similar to 540 Ma. This was 25 m.yr. 

before Delamerian deformation began. 

During the Early Cambrian, eastern 

Australia was still in a state of extension 

(or transtension), with opening of the 

Kanmantoo Basin and associated anorogenic, 

largely mafic magmatism. This 

basin received sediment from the already 

exposed Ross Orogen to the south. 

The simultaneous first occurrence of 

strain fabrics and subduction-related 

magmatism (including boninite, granite, 

and andesite lavas) at similar to 514 Ma 

in New Zealand, Victoria, South Australia, 

New South Wales, and Tasmania 

implies that the Delamerian Orogeny 

was driven by ridge-push forces transmitted 

on the initiation of westwarddipping 

subduction. Subsequent eastward 

slab rollback at 490 Ma may have 

occurred when the new slab had reached 

the transition zone at 650-km depth, resulting 

in upper plate extension and anorogenic 

Basin and Range-style magmatism 

in South Australia and Tasmania 

(Mount Read belt). The delayed onset of 

subduction in the Australian sector of 

the margin implies that westward motion 

of the Australian portion of eastern 

Gondwana continued to be accommodated 

during the late Early Cambrian by 

subduction or deformation along either 

the Mozambique Suture or at the northern 

end of the South Prince Charles 

Mountains-Prydz Bay suture. 

2010010542 

Baltoscandia 和不列颠群岛下志留统 

( 兰多维列统 )Osmundsberg K- 斑脱 

岩 : 化学特征识别和区域对比 = The 

lower Silurian (Llandovery) Osmundsberg 

K-bentonite in Baltoscandia and the 

British Isles: Chemical fingerprinting 

and regional correlation. ( 英文 ). Inanli F 

O; Huff W D; Bergstrom S M. 

GFF, 2009, 131(4): 269-279 

The lower Silurian Osmundsberg K- 

bentonite is a widespread altered volcanic 

ash bed that occurs throughout 

Baltoscandia and other parts of northern 

Europe. K-bentonite samples from sections 

containing the Osmundsberg K- 

bentonite bed were investigated to determine 

whether the chemical composition 

of this bed is sufficiently unique and 

diagnostic that it can serve as a basis for 

high-resolution chemostratigraphic correlation 

on a regional scale. Eleven 

known and five suspected Osmundsberg 

K-bentonite samples along with 26 samples 

of accompanying ash beds from 13 

different localities were analyzed for 

major and trace elements. The data were 

statistically treated using discriminant 

function analysis to determine if the 

trace element data provide a unique 

chemical fingerprint for the Osmundsberg 

K-bentonite bed. Comparison with 

the correlation model of Bergstrom et al. 

[Bergstrom, S.M., Huff, W.D. Kolata, 

D.R., 1998b: The lower Silurian Osmundsberg 

K-bentonite. Part I: Stratigraphic 

position, distribution, and palaeogeographic 

significance. Geological 

Magazine 135, 1-13.] based on biostratigraphic 

evidence shows that results from 

two independent techniques are in general 

agreement with the exception of 

five samples whose presumed Osmundsberg 

affinity is rejected. The results 

demonstrate that the unique and 

identifiable chemical fingerprint of the 

Osmundsberg K-bentonite bed can provide 

an additional stratigraphic tool for 

local and regional correlation of these 

K-bentonites. 

164

2010010543 

瑞典 Boda 灰岩中赫南特阶地层、碳 

酸盐相和三叶虫生态组合 = Stratigraphy, 

carbonate facies and trilobite associations 

in the Hirnantian part of the 

Boda Limestone, Sweden. ( 英文 ). Suzuki 

Y; Shiino Y; Bergstrom J. 

GFF, 2009, 131(4): 299-310 

The Hirnantian (Upper Ordovician) 

sequence of the Boda Limestone is defined 

and described as a new formal Upper 

Boda Member. It has four petrologically 

distinct, bedded units containing 

three strikingly different trilobite faunas. 

These differences are thought to be 

caused by a sea-level lowering leading 

to the first Hirnantian sea-level lowstand 

and successive transgression as well as 

to shifts in sea-water chemistry. This is 

indicated by the occurrence of a level 

with botryoidal carbonate cement. On 

top follows the upper Hirnantian 

Glisstjarn Formation. 

2010010544 

立陶宛文洛克统斑脱岩及其与爱沙尼 

亚、瑞典和挪威剖面斑脱岩的对比 = 

Wenlock bentonites in Lithuania and 

correlation with bentonites from sections 

in Estonia, Sweden and Norway. ( 英文 ). 

Kiipli T; Radzevicius S; Kallaste T; Motuza 

V; Jeppsson L; Wickstrom L M. 

GFF, 2008, 130(4): 203-210 

Seven Wenlock bentonite beds from 

four drill cores in Lithuania with sufficient 

thickness for sampling were analysed 

by XRD and XRF. The sanidine 

composition of bentonites combined 

with graptolite biozonation of the host 

rock were used for correlations. Two of 

the studied bentonite samples at the antennularius/flexilis 

biozone boundary 

can be confidently correlated between 

two Lithuanian sections. Four of the 

studied bentonites can be correlated with 

lower or higher probability with earlier 

studied bentonites in Estonia and Sweden. 

Identification of the Grotlingbo 

Bentonite in the Vidukle-61 drill core, 

and descriptions of other east Baltic sections 

enables composition of it thickness 

map of the Grotlingbo Bentonite. The 

thickness pattern with two axes, and the 

layered composition of the Grotlingbo 

Bentonite, indicate a change of the wind 

direction during a long lasting eruption. 

Hypothetical location of the volcanic 

source in the Silurian was within the 

zone of the Baltica-Laurentia collision. 

2010010545 

瑞典哥特兰岛志留纪非典型性地台内 

环境和生物群 = An atypical intraplatform 

environment and biota from the 

Silurian of Gotland, Sweden. ( 英文 ). 

Calner M; Eriksson M E; Clarkson E N 

K; Jeppsson L. GFF, 2008, 130(2): 79- 

86 

A condensed shale from the middle 

Silurian of Gotland (Sweden) is herein 

described with regard to its biotic and 

environmental significance. The fauna is 

characterised by an overall low diversity 

and anomalous abundance patterns, notably 

a mass-occurrence of scolecodonts. 

Other elements include abundant 

chitinozoans, dendroid and graptoloid 

graptolites, conodonts, eurypterids, and 

the brachiopod Lingula. An unusually 

good collection of the rare, minute 

conodont Aldridgeodus minimus gen. et 

sp. nov., was recovered and is therefore 

formally described herein. The conspicuous 

faunal composition and palaeogeographical 

position of the shale in 

the interior area of a carbonate platform 

is unique for any stratum of Gotland and 

may represent a rarely preserved environment 

for the lower Palaeozoic. 

2010010546 

下文洛克统 Hangvar 组 —— 瑞典哥特 

兰岛志留系 Hogklint 层和 Slite 层位 

之间出露的一段序列 = The lower 

Wenlock Hangvar Formation - a sequence 

previously split between the 

Hogklint and Slite beds (Silurian, Got- 

165

land, Sweden). ( 英文 ). Jeppsson L. 

GFF, 2008, 130(1): 31-40 

Conodont faunas solve the longstanding 

problem regarding the relationships 

between the Hogklint, Tofta, and 

lower Slite. The name Hangvar Formation 

is here formally introduced for the 

strata identified between the Tofta Formation 

and the Slite Group. The Hangvar 

Fm. includes marls as far SW as near 

Paviken (previously Slite Marl), argillaceous 

limestones (seen only in the most 

distal areas accessible) followed by reefs 

and associated limestones SE and NE of 

Visby (previously Slite Beds, mostly 

units a and b) and northeastwards to 

eastern Faro (from the area around Kappelshamnsviken 

and NE-wards, previously 

Hogklint Beds). The formation is 

delimited below and above by prominent 

discontinuities i.e. sequence boundaries. 

These coincide with biostratigraphical 

boundaries, i.e. they probably represent 

relatively long time intervals. The 

Hangvar formation includes two subzones, 

hence lower and upper parts can 

be distinguished. The upper Hangvar 

reef generation is the third in the 

Wenlock of Gotland. 

2010010547 

中国西南地区峨眉山火山作用前后沉 

积与岩相古地理 : 地幔柱活动在地表 

表现的新见解 = Sedimentation and 

lithofacies paleogeography in southwestern 

China before and after the Emeishan 

flood volcanism: New insights into 

surface response to mantle plume activity. 

( 英文 ). He B; Xu Y G; Wang Y M; 

Luo Z Y. Journal of Geology, 2006, 

114(1): 117-132 

Investigations into Permian sedimentation 

and reconstruction of paleogeography 

in SW China are aimed at 

characterizing sedimentary responses to 

the Emeishan mantle plume. In addition 

to erosional features on the sediments 

underlying the uplifted Emeishan basalts, 

unusual depositions of Permian age are 

also present in the Emeishan large igneous 

province ( LIP). Specifically, carbonate 

gravity flows and submarine incised 

canyon fillings were developed in 

the western margin of the postulated uplifted 

area, and rifting trenches were developed 

along the eastern margin; alluvial 

fan deposits occur at the boundary 

between the inner and intermediate 

zones. These depositions all rest on the 

Maokou Formation and are in turn covered 

by the Emeishan basalts, implying 

synchronism between crustal uplift and 

depositional events. These deposits and 

the associated extension and normal 

faulting along the margin of and within 

the LIP represent sedimentary features 

resulting from dynamic behavior of 

mantle plume. Comparison of lithofacies 

paleogeography before and after the 

Emeishan flood volcanism highlights the 

determinant role of mantle plume activity 

in the geological evolution in SW 

China. The rapid, differential erosion of 

the Maokou Formation was likely related 

to plume-induced dynamic uplift. 

This uplift was apparently followed by 

subsidence, given deposition of the marine 

clastic rocks sandwiched between 

basalts and the Maokou Formation in the 

east and submarine basalts along the 

margins of the province. A second-phase 

uplift, attributed to underplating of 

plume-derived melts at the crust-mantle 

boundary, was characterized by prolonged 

(similar to 45 m.yr.), plateautype 

uplift and was responsible for the 

appearance of the "Chuandian old land. 

Integration of these erosional and depositional 

characteristics allows us to depict 

how the surface geology responds to 

mantle plume, which explains some 

complex sedimentological problems in 

SW China. 

2010010548 

阿曼山脉构造深部岩层的年龄及地层 

相互关系 : 晚石炭世新特提斯断裂 U- 

Pb SHRIMP 证据 = Age and stratigraphic 

relationships of structurally 

166

deepest level rocks, Oman mountains: 

U/Pb SHRIMP evidence for Late Carboniferous 

Neotethys rifting. ( 英文 ). 

Gray D R; Gregory R T; Armstrong R A; 

Richards I J; Miller J M. Journal of Geology, 

2005, 113(6): 611-626 

Igneous zircons in felsic schist, or 

metatuff, infolded with mafic schist, 

calcschist, and quartz mica schist of the 

As Sifah lower plate window, NE Oman, 

have yielded a U/Pb SHRIMP crystallization 

age of 298 +/- 3 Ma. The metatuff 

was previously considered to represent 

Permian bimodal volcanism, but these 

data indicate that the magmatism is 

older and suggest that Neotethys intracontinental 

rifting on the Oman part 

of the Gondwana northern margin was 

initiated in the Late Carboniferous. This, 

combined with delta(13)C values of 

calcschists indicating a predominantly 

pre-Late Permian age for the basal lower 

plate metacarbonates, suggests that passive 

margin carbonate ramp development 

occurred in the Late Carboniferous/Early 

Permian during Neotethys 

oceanic spreading and not just in the 

Late Permian, as previously thought. 

The restricted occurrence of the metatuff 

to the Saih Hatat lower plate, a unique 

lower plate stratigraphy, and the unique 

delta(13)C values of the calcschists all 

suggest that the lower plate was certainly 

distal, and possibly exotic, to the 

Arabian Peninsula. The felsic schist 

sample was entrained within an eclogite 

megaboudin at As Sifah. The age relationships 

therefore suggest that the high- 

P rocks that reached pressures of up to 

20 kbar and are now part of the lower 

plate of Gregory and coworkers were 

either part of a subducted Florida-style 

promontory as part of the attenuated 

leading edge of the Arabian platform or 

part of a subducted microplate that was 

originally caught in the developing 

southern Neotethys ocean some 1300 

km from the margin. 

2010010549 

美国东北部寒武纪 — 奥陶纪沉积岩的 

地球化学特征 : 康塔造山作用初始沉 

积物源的改变 = Geochemistry of 

Cambro-Ordovician sedimentary rocks 

of the Northeastern United States: 

Changes in sediment sources at the onset 

of Taconian orogenesis. ( 英文 ). 

Hurowitz J A; McLennan S M. Journal 

of Geology, 2005, 113(5): 571-587 

Trace element and Nd isotopic compositions 

of Late Cambrian to Middle 

Ordovician passive margin metasediments 

from the northernmost Taconic 

Allochthon of the northeast United 

States indicate a provenance consistent 

with a two-component mixture of an 

evolved Grenville source and a rift 

source generated during the Late Proterozoic 

opening of the Iapetus Ocean. 

Initial epsilon(Nd) values for these preorogenic 

deposits range from -11.3 to - 

14.6 (average=-13.0). Samples of overlying 

mid-Ordovician Taconian sediments 

exhibit initial epsilon(Nd) values 

between -6.1 and -9.8 (average=-8.5). 

The trace element and Nd isotopic compositions 

of these synorogenic samples 

are consistent with a mixture of a less 

evolved Grenville Province source and 

recycled preorogenic passive margin deposits. 

No mantle-derived (ophiolitic or 

andesitic) source is unambiguously recognized 

in the synorogenic samples, 

consistent with published geochemical 

studies of other Taconian foreland sequences 

from this region. Sedimentary 

rocks from the northern Appalachians 

record a clear change in provenance at 

ca. 458 Ma, coincident with the onset of 

Taconian orogenesis and similar to patterns 

observed in other sedimentary sequences 

throughout North America. 

2010010550 

海平面升降旋回地层中生物的改变 : 

莫斯科 Peski 采石场石炭系莫斯科阶 

Domodedovo 组 = Biotic changes in a 

eustatic cyclothem: Domodedovo For- 

167

mation (Moscovian, Carboniferous) of 

Peski quarries, Moscow Region. ( 英文 ). 

Kabanov P B; Alekseev A S; Baranova 

D V; Gorjunova R V; Lazarev S S; 

Malkov V G. Paleontological Journal, 

2006, 40(4): 351-368 12 图版 . 

Stacking lithofacies in the Domodedovo 

Formation of Peski quarries show 

prominent changes in paleodepth and 

depositional environment. Distribution 

in the section of fusulinoids, algae, 

conodonts, and macrofossils are revealed. 

Among the latter, brachiopods 

and bryozoans are discussed in most detail. 

2010010551 

早古生代海生底栖生物群落的出现和 

演化 = Appearance and evolution of 

marine benthic communities in the Early 

Palaeozoic. ( 英文 ). Rozhnov S V. Paleontological 

Journal, 2006, 40(4): S444- 

S452 3 图版 . 

The development of marine benthic 

communities in the Early Palaeozoic occurred 

mainly in the shallow water epicontinental 

seas. It included those stages 

of the Cambrian and Ordovician evolutionary 

radiations that were dominated 

by a high rate of morphogenesis, when 

new food and territory resources were 

not limited. This provided many opportunities 

for coadaptation of emerging 

organisms. At the time of the Cambrian 

radiation, the body plans of all animals 

were formed, while in the Ordovician, 

the maximum rank of emerging taxa did 

not exceed the level of class. The beginning 

of each radiation was explosive. 

Vendian benthic communities developed 

in cold seas and in the shallowest areas 

of warm seas, where organic matter 

from the surface layers was available at 

the bottom because of the absence of a 

thermocline. The Cambrian radiation 

began with the appearance of pelagic 

suspension feeders, because of which 

much of the primary production could 

penetrate the thermocline and settle at 

the bottom. This allowed the occupation 

of warmer seas and greater depths. At 

the same time, the productivity of the 

pelagic region sharply increased because 

of the emergence of positive feedback 

between the producers and consumers in 

the water, leading to increased water 

transparency and elongation of trophic 

chains. Arthropods, the first suspension 

feeders, were the launch group of the 

Cambrian radiation. Cambrian benthic 

suspension feeders could seize only the 

smallest particles, mostly bacteria, and 

dissolved organic matter. This food resource 

was contained in the thin bottom 

water layer. Therefore, the food grasping 

structures of all the Cambrian suspension 

feeders were near the bottom, without 

forming tiers. The Ordovician evolutionary 

radiation began with the launch 

of the Pelmatozoan echinoderms, which 

were the first benthic suspension feeders 

to begin feeding on plankton. The exploitation 

of this resource led to the 

creation of a 1-m tier above the bottom 

and an increase in their calcite productivity. 

Positive feedback emerged between 

the grounds and the community of 

its inhabitants and considerably changed 

the composition and diversity of grounds, 

which sharply increased the diversity of 

benthos. The appearance of positive 

feedback between different components 

of ecosystems resulted in explosive evolution 

in both the Cambrian and Ordovician. 

2010010552 

二叠 - 三叠纪生态危机之前的陆相生物 

群改变 = Changes in terrestrial biota 

before the Permian-Triassic ecological 

crisis. ( 英文 ). Ponomarenko A G. Paleontological 

Journal, 2006, 40(4): S468- 

S474 3 图版 . 

The period around the Permian- 

Triassic boundary was marked by one of 

the most important and interesting 

events in the evolution of life. The diversity 

of both marine and continental 

biotas decreased. The changes were 

168

global and led to the establishment of 

the new Mesozoic World. Transformations 

of the organic world constituted a 

single process with changes in the inorganic 

components of the biosphere. The 

preceding glacial period had ended and 

the “cool,” zonal, and markedly seasonal 

climate was replaced by a “warm,” “equable,” 

virtually non-seasonal and 

azonal climate. The new climatic organization 

remained on Earth for more 

than two hundred million years. The biotic 

crisis was global: it involved the sea, 

the land, and inland waters. The changes 

on land began earlier and more superficial. 

The principal events were in the 

Kazanian and Vyatkian, before the end 

of the Permian. The crisis was caused to 

a greater extent by biospheric processes 

than by momentary external influences, 

the latter at most triggering the crisis. 

2010010553 

二叠纪末期 Vyazniki 生物组合 = 

Vyazniki biotic assemblage of the terminal 

Permian. ( 英文 ). Sennikov A G; 

Golubev V K. Paleontological Journal, 

2006, 40(4): S475-S481 7 图版 . 

A new unique and diverse biotic assemblage 

of the terminal Permian has 

recently been discovered in the town of 

Vyazniki (Central Russia). The Vyazniki 

terrestrial community is transitional between 

Permian and Triassic ones and 

represents the last, so far unknown stage 

of the global ecological crisis of the continental 

biota at the Permian-Triassic 

boundary. The successive development 

of land biotic crisis in the Late Permian, 

which was followed by mass extinction 

at the Permian-Triassic boundary, and 

long, successive postcrisis development 

and specialization of new Triassic 

groups as well as rearrangement and diversification 

of the biotic assemblage 

composition and community structure 

suggest predominance of intrinsic, biotic 

causes of this crisis, realized in destabilization, 

alteration, and new stabilization 

of continental communities and ecosystems. 

2010010554 

鄂尔多斯盆地东北部山西组 — 上石盒 

子组三角洲沉积及演化 = Delta deposits 

in the Shanxi and Shangshihezi Formations 

in the northeastern Ordos basin. 

( 中文 ). 陈安清 ; 陈洪德 ; 向芳 ; 侯中健 ; 林 

良彪 ; 徐胜林 . 地层学杂志 , 2010, 34(1): 

97-105 1 图版 . 

鄂尔多斯盆地东北部二叠系山西组 

和石盒子组是重要的天然气产层。综 

合野外露头和钻井的岩石学、沉积构 

造、剖面结构特征 , 分析了鄂尔多斯晚 

古生代陆内坳陷盆地 3 个演化阶段沉 

积充填的差异性 , 认为盆地形成阶段以 

大型辫状河潮控三角洲向陆相曲流河 

三角洲转化为特征 ; 发展阶段以大型陆 

相辫状河三角洲向陆相曲流河三角洲 

转化为特征 ; 成熟阶段以发育陆相网结 

河三角洲为特征 , 建立了 3 种适合研究 

区储集砂体预测和评价的 “ 大平原 , 小 

前缘 ” 三角洲模式 , 提出辫状河三角洲 

或曲流河三角洲的分流河道、水下分 

流河道和河口坝形成了粒度较粗、规 

模较大、厚度较稳定的有利于天然气 

运移聚集的砂体 , 是储层发育和分布的 

最有利相带 , 网结河三角洲和浅湖沉积 

了大量泥岩可作为盖层 , 加上太原组和 

山西组的聚煤作用 , 共同形成了该地区 

的天然气藏的生储盖组合。 

中生界 

2010010555 

利用计算机模拟地层学区分米兰科维 

奇驱动过程中岩石记录的随机性 = 

Distinguishing Milankovitch-Driven 

Processes in the Rock Record from Stochasticity 

Using Computer-Simulated 

Stratigraphy. ( 英文 ). Dexter T A; 

Kowalewski M; Read J F. Journal of 

Geology, 2009, 117(4): 349-361 

Repetitive patterns of facies recurrence 

are frequently reported from the 

shallow-water sedimentary rock record 

169

and are postulated to have been driven 

by orbital forcing on eustatic sea level. 

Consequently, multiple statistical techniques 

have been developed to evaluate 

whether patterns of stratigraphic succession 

are more consistent with a periodic 

sea level signal or are stochastic. Previous 

studies focused on development 

and/or application of such methods to 

test empirical geological records. However, 

the character of such records cannot 

be known a priori, as deposition, 

erosion, and preservation influence the 

resultant composition, nor can those records 

be readily manipulated to explore 

the sensitivity, robustness, and overall 

validity of statistical methods. Here we 

simulate carbonate layers using computer-modeled 

successions generated by 

periodic sea level changes. The resulting 

stratigraphic records were then evaluated 

statistically. Thickness distributions 

of simulated lithofacies were compared 

to distributions predicted for Poisson 

processes, which by definition are not 

driven by cyclical sea level changes. Our 

results suggest that periodic processes 

produce stratigraphic thickness frequencies 

that are difficult to distinguish from 

random frequencies except under highmagnitude 

sea level fluctuations. Similarly, 

autocorrelation fails to correctly 

recognize cyclic patterns in such simulated 

records. Models with highmagnitude 

sea level fluctuations (icehouse 

conditions) had thickness frequencies 

that are suggestive of orbital 

forcing, whereas low-magnitude sea 

level fluctuations (greenhouse conditions) 

appeared independent even 

though they were modeled using Milankovitch 

orbital forcing. The increasing 

evidence based on spectral data from 

real rock successions suggests that Milankovitch 

drivers are common in both 

icehouse and greenhouse periods. Because 

statistical approaches are unsuccessful 

in recognizing the cyclic driver 

of these simulated records, we infer that 

it is difficult to disprove independence 

from real stratigraphy even when orbital 

forcing is controlling the rock composition. 

Even in the necessarily simplified 

world of computer simulations, the numerous 

factors involved in depositing 

stratigraphic successions work to complicate 

or mask any periodic signal, thus 

generating the appearance of stochasticity 

in some successions. 

2010010556 

埋藏学和风暴沉积形成的陆壳层 : 以 

白垩纪西部内陆盆地为实例 = Taphonomy 

and sedimentology of stormgenerated 

continental shell beds: A case 

example from the Cretaceous western 

interior basin. ( 英文 ). Roberts, E M; 

Tapanila, L; Mijal, B. Journal of Geology, 

2009, 116(5): 462-479 

An extraordinary continental shell bed 

is reported from the Upper Cretaceous 

Kaiparowits Formation in southern Utah. 

This shell bed, referred to as the Kaiparowits 

Blues Ceratopsian shell bed, is 

highly unusual among fluvial-estuarine 

shell beds for its great thickness, surface 

area and shell density and its geometry. 

It covers > 850 m(2), ranges from 85 to 

280 cm thick, and consists of a series of 

10-50-cm-thick low-angle, dipping beds. 

The shells are generally undamaged and 

articulated (> 75%), commonly with 

valves still closed, and strongly oriented 

normal to the dip orientation of the shell 

layers. The shell bed is interpreted as a 

lateral accretion bar set that developed 

in a point bar or midchannel bar setting. 

Nearly 45% of shells are encrusted by 

the brackish-water bryozoan Conopeum 

sp., indicating that deposition transpired 

within the upper-fluvial to mixedfluvial-marine 

part of an estuarine channel 

system. At least five unionoid (Unionoidea) 

shell morphotypes are present, 

representative of both parautochthonous 

(intrachannel) and allochthonous (adjacent 

quiet-water pond/marsh) taxa. Taphonomic 

and sedimentologic investigations 

suggest that rapid winnowing and 

amalgamation of live and recently dead 

170

shells from nearby high-density mussel 

shoals and a smaller population of 

calmer-water morphotypes from surrounding 

floodbasin environments occurred 

during the waning stages of an 

unusually high intensity storm event, 

possibly a tropical storm or hurricane. A 

combination of extreme hydrologic 

events, such as catastrophic flooding, 

cyclonic winds, and storm surge, may 

have contributed to the development of 

the shell bed. At least 1.4 million individual 

unionoids are preserved in this 

deposit, making it one of the most voluminous 

and highest density 

fresh/brackish-water shell beds reported 

in the fossil or historical records. 

2010010557 

中国天山托云盆地巨晶颗粒与寄主玄 

武岩之间的外缘火山碎屑的联系 = A 

noncognate relationship between 

megacrysts and host basalts from the 

Tuoyun basin, Chinese Tian Shan. ( 英 

文 ). Han B F; Liu J B; Zhang L. Journal 

of Geology, 2009, 116(5): 499-509 

Abundant kaersutite and alkali feldspar 

megacrysts occur together with 

mantle-derived and lower crustal xenoliths, 

including kaersutite hornblendite 

and syenite, in the Early Cretaceous alkaline 

basalts of the Tuoyun basin in the 

westernmost Chinese Tian Shan. Particularly, 

several kaersutite hornblendite 

cumulate xenoliths have the assemblage 

of kaersutite + alkali feldspar + titanian 

mica +/- titanomagnetite +/- clinopyroxene, 

in which kaersutite occurs as an 

early-stage cumulus phase crystallized 

from a parental magma and alkali feldspar 

occurs as a late-stage intercumulus 

phase from the evolved magma between 

accumulating kaersutite grains. The 

megacrystic and xenolithic kaersutite 

has much higher Mg# values (0.70-0.96) 

than the host basalt (0.47-0.60). The 

kaersutite and alkali feldspar megacrysts 

have similar initial Sr-87/Sr-86 ratios 

(0.7032-0.7033 and 0.7035-0.7038, respectively), 

significantly different from 

their host basalts (0.7047-0.7054). 

Xenolithic petrography and megacrystic 

Sr isotope geochemistry support a common 

origin for the kaersutite and alkali 

feldspar megacrysts and preclude the 

precipitation of the megacrysts from 

their host basalts. As the fragments of 

kaersutite hornblendite and syenite that 

may have crystallized from a trachytic 

parental magma and its evolved magma 

underplated earlier in the crust-mantle 

transition zone, these megacrysts, together 

with other xenoliths, were captured 

and brought to the surface by the 

Early Cretaceous basalts. 

2010010558 

约兹加特基岩的 Ar-39/Ar-40 年龄 : 

土耳其晚白垩纪中心安纳托利亚结晶 

复合体外延时间的初步数据 = Ar- 

39/Ar-40 ages from the Yozgat batholith: 

Preliminary data on the timing of Late 

Cretaceous extension in the central Anatolian 

crystalline complex, Turkey. ( 英 

文 ). Isik V; Lo C H; Goncuoglu C; 

Demirel S. Journal of Geology, 2009, 

116(5): 510-526 

Isotopic dating of sheared and unsheared 

rocks can be important in understanding 

deformational processes in 

orogenic belts. This study examines Ar- 

40/Ar-39 dating of granitoids and mylonitic 

rocks to constrain intrusive and 

deformational events within the northern 

part of the central Anatolian crystalline 

complex (CACC). The Kerkenez granitoid 

within this complex, comprising 

primarily quartz monzonite and hornblende 

granite, contains discrete ductile 

shear zones. These zones are characterized 

by protomylonite and mylonite 

formations with metamorphism conditions 

that reach lower amphibolite facies, 

mylonitic foliations and lineations, and 

asymmetric kinematic indicators (e.g., 

asymmetric porphyroclasts, composite 

shear bands) with top-to-the-northwest 

shear senses. Considering the high closure 

temperatures (similar to 500 de- 

171

grees C for hornblende and similar to 

350 degrees C for K-feldspar), both 

hornblende quartz monzonite and hornblende 

granite in the Kerkenez granitoid 

may have cooled rapidly, suggesting that 

hornblende quartz monzonite may have 

been emplaced at around 81.2 +/- 0.5 

Ma and that it is older than hornblende 

granite, which has a well-defined plateau 

age (72.6 +/- 0.2 Ma). On the basis 

of intrusive relations and our Ar-40/Ar- 

39 age data, we can constrain the upper 

age limit (similar to 81 Ma) on the regional 

metamorphism in the northern 

part of the CACC. The Ar-40/Ar-39 dating 

of hornblendes in two mylonite 

samples from a ductile shear zone yields 

plateau ages of 71.6 +/- 0.3 and 71.7 +/- 

0.2 Ma, respectively. K-feldspars in the 

same samples yield plateau ages of 71.6 

+/- 0.2 and 81.3 +/- 0.2 Ma. Therefore, 

we adopt 71.6 +/- 0.3 and 71.7 +/- 0.2 

Ma as the cooling ages of hornblende 

and K-feldspar, respectively, in the ductile 

shear zone. On the other hand, an 

age of 81.3 +/- 0.2 Ma for deformed K- 

feldspar appears to reflect not the age of 

ductile deformation but rather the age of 

undeformed hornblende quartz monzonite. 

These age data suggest that the 

shear zones formed soon after the emplacement 

and cooling of hornblende 

granite. The cooling event of the shear 

zones is interpreted to be associated with 

the beginning of extension in the region. 

Furthermore, these data imply that 

metamorphism, emplacement, and cooling 

of the intrusives and ductile shearing 

of the intrusions were coeval in the region 

and occurred in the Late Cretaceous. 

2010010559 

喜马拉雅拉达克 ( 印度西北部 ) 印度 - 

亚洲碰撞带年龄和白垩纪 - 第三纪碳酸 

盐台地的演变 = Cretaceous-tertiary 

carbonate platform evolution and the age 

of the India-Asia collision along the 

Ladakh Himalaya (northwest India). ( 英 

文 ). Green O R; Searle M P; Corfield R 

I; Corfield R M. Journal of Geology, 

2008, 116(4): 331-353 

The India-Asia collision resulted in 

the formation and uplift of the Himalaya 

and the enhanced uplift of the Tibetan 

plateau. The transition from marine to 

continental facies within the Indus- 

Yarlung Tsangpo suture zone and along 

the northern margin of the Indian plate 

provides the most accurate method of 

dating the closure of the Tethys Ocean 

separating the Indian and Asian plates. 

Other indirect methods of dating the collision, 

such as paleomagnetism, dating 

the UHP metamorphism along the north 

margin of India, dating the youngest 

subduction-related granites along the 

southern margin of Asia, and dating the 

postorogenic Indus Molasse Group deposits 

within the suture zone, cannot 

provide such a precise or reliable age of 

collision. Ophiolite obduction onto the 

Indian passive margin occurred during 

the latest Cretaceous and predated initial 

collision of the two continental plates. 

Unconformities occur beneath the Late 

Maastrichtian Marpo Formation and beneath 

the Danian Stumpata Formation 

on the shelf and beneath the Upper Paleocene 

Sumda Formation in the suture 

zone. Stratigraphic and structural data 

from the Indian plate continental margin 

in the Ladakh and Zanskar Himalaya, 

northwest India, suggest that the final 

marine sediments were shallow marine 

limestones deposited during planktonic 

zone P8, corresponding to the Cusian 

stage of the late Lower Eocene 

(Ypresian) at 50.5 Ma. A regional unconformity 

across shelf and suture zones 

above these rocks marks the beginning 

of continental red bed deposition (Chulung-la 

and Nurla formations). The age 

of the final marine sediments is similar 

in Waziristan ( northwest Pakistan) to 

the west and the South Tibet region to 

the east, suggesting that there was no 

significant diachroneity along the Indus- 

Yarlung Tsangpo suture zone. South of 

172

the Himalaya in the Hazara syntaxis, 

Pakistan, the youngest marine sediments 

correspond to nummulite-bearing limestones 

of the shallow benthic zone 

SBZ10 and planktonic foraminifera P7 

zone (52-51 Ma). The timing of closure 

of Neo-Tethys between India and Asia 

corresponds closely to the ending of 

subduction-related granodiorite-granite 

magmatism along the Ladakh-Gangdese 

batholith ( southern, Andean-type margin 

of the Asian plate) and precedes the 

drastic slowing of the northward drift of 

India. Continental fluvial-deltaic red 

beds unconformably overlie all marine 

sediments, both in the suture zone and 

along the north Indian plate margin. 

2010010560 

地中海中西部阿尔比斯地区中三叠统 - 

下侏罗统大陆红层沉积演化的组成和 

地球化学特征 = Compositional and 

geochemical signatures for the sedimentary 

evolution of the Middle Triassic- 

Lower Jurassic continental redbeds from 

western-central Mediterranean Alpine 

chains. ( 英文 ). Critelli S; Mongelli G; 

Perri F; Martin A A; Martin M M; Perrone 

V; Dominici R. Journal of Geology, 

2008, 116(4): 375-386 

Compositional and chemical analyses 

suggest that Middle Triassic-Lower Liassic 

continental redbeds ( in the internal 

domains of the Betic, Maghrebian, and 

Apenninic chains) can be considered a 

regional lithosome marking the Triassic- 

Jurassic rift-valley stage of Tethyan rifting, 

which led to the Pangaea breakup 

and subsequent development of a mosaic 

of plates and microplates. Sandstones 

are quartzose to quartzolithic and represent 

a provenance of continental block 

and recycled orogen, made up mainly of 

Paleozoic metasedimentary rocks similar 

to those underlying the redbeds. Mudrocks 

display K enrichments; intense 

paleoweathering under a hot, episodically 

humid climate with a prolonged 

dry season; and sediment recycling. 

Redbeds experienced temperatures in 

the range of 100 degrees-160 degrees C 

and lithostatic/tectonic loading of more 

than 4 km. These redbeds represent an 

important stratigraphic signature to reconstruct 

a continental block (Mesomediterranean 

Microplate) that separated 

different realms of the western 

Tethys from Middle-Late Jurassic to 

Miocene, when it was completely involved 

in Alpine orogenesis. 

2010010561 

西藏南部橄榄玄粗岩记录晚侏罗世古 

特提斯洋内岛弧裂解 = Shoshonites in 

southern Tibet record Late Jurassic rifting 

of a Tethyan intraoceanic island arc. 

( 英文 ). Aitchison J C; McDermid I R C; 

Ali J R; Davis A M; Zyabrev S V. Journal 

of Geology, 2007, 115(2): 197-213 

Detailed field mapping combined 

with a petrologic and geochemical investigation 

of the Zedong terrane within 

the Yarlung Tsangpo suture zone provides 

insights to the evolution of now 

mostly subducted portions of Tethys 

during the Late Jurassic. The terrane is 

dominated by volcanic rocks of shoshonitic 

affinity, which were erupted in 

a submarine oceanic island arc setting. 

The volcanic island arc was built on a 

basement of oceanic crust, and the shoshonites 

locally overlie a thin section of 

pillowed island arc tholeiites and red 

ribbon - bedded radiolarian cherts. Geochemistry 

of the shoshonites suggests 

that their development occurred in a setting 

analogous to that of Late Miocene 

to Early Pliocene Fiji and was associated 

with an arc rifting. We speculate that 

this event may have been a far-field response 

to developments associated with 

Gondwana breakup. 

2010010562 

德克萨斯州 Trans-Pecos 地区晚白垩 

世火山活动的证据 = Evidence for Late 

Cretaceous volcanism in Trans-Pecos 

Texas. ( 英文 ). Breyer J A; Busbey A B; 

Hanson R E; Befus K E; Griffin W R; 

173

Hargrove U S; Bergman S C. Journal of 

Geology, 2007, 115(2): 243-251 

Cretaceous basaltic pyroclastic strata 

have been discovered in a fault block on 

the southern edge of the Rosillos Mountains 

laccolith in the Big Bend area of 

Trans-Pecos Texas. The sequence comprises 

base-surge and pyroclastic-fall 

deposits inferred to have accumulated on 

the flanks of a small phreatomagmatic 

volcano. A diverse assemblage of 

freshwater turtles (including Aspideretes), 

crocodile teeth, and dinosaur 

bones have been recovered from the uppermost 

part of the sequence. The fauna 

indicate a Late Cretaceous, probably 

Campanian age. An outward-dipping 

normal fault bounding the pyroclastic 

strata on the southeast juxtaposes sediments 

of the Upper Cretaceous Javelina 

Formation in the hanging wall with pyroclastic 

rocks in the footwall, indicating 

the pyroclastic strata must be Maastrichtian 

or older. U-Pb SHRIMP-RG 

analyses of zircons separated from a basaltic 

block thrown out of the volcano 

yield an inferred igneous crystallization 

age of Ma, consistent with the biostratigraphic 

and struc- 72.6 +/- 1.5 tural evidence. 

The pyroclastic strata in the fault 

block provide the first evidence for Late 

Cretaceous volcanism in the Trans- 

Pecos region. Previously, the onset of 

igneous activity in the area was thought 

to be no older than 64 Ma. We speculate 

that the basaltic pyroclastic rocks represent 

an extension of the Upper Cretaceous 

Balcones magmatic province into 

Trans-Pecos Texas. 

2010010563 

希腊 Cycladic 蓝片岩带变质火成岩和 

变质凝灰岩原岩的年龄 : 对锆石 U- 

Pb 测定的研究结果 = Protolith ages of 

meta-igneous and metatuffaceous rocks 

from the Cycladic blueschist unit, 

Greece: Results of a reconnaissance U- 

Pb zircon study. ( 英文 ). Brocker M; 

Pidgeon R T. Journal of Geology, 2007, 

115(1): 83-98 

The Cycladic blueschist unit (CBU) in 

the central Aegean Sea comprises a pre- 

Alpidic crystalline basement that is 

overlain by thrust sheets of a metamorphosed 

volcanosedimentary sequence. 

Melanges are widespread and enclose a 

wide variety of meta-igneous rock fragments 

in a serpentinitic and/or metasedimentary 

matrix. Previous geochronology 

has documented the general temporal 

framework for the Alpidic metamorphic 

history but did not produce 

well-constrained protolith ages for the 

main volcanosedimentary succession 

and for melange blocks. This issue is 

addressed here in an ion probe U-Pb zircon 

study focusing on the islands of Andros, 

Sifnos, and Ios. The new results 

indicate a consistent regional pattern of 

Triassic ages (ca. 237-245 Ma) for the 

magmatic precursors of metatuffaceous 

and metavolcanic rocks, which occur as 

intercalations within metasediments. 

This narrow range of igneous crystallization 

ages records an important period 

of volcanic activity in the larger study 

area. On Andros, such ages were also 

determined for a disrupted tabular body 

of meta-acidic gneisses ( several hundred 

meters in length) that has been considered 

an olistolith within a metaolistostrome. 

Field observations are 

compatible with the interpretation that 

this fragment represents a layer of the 

main succession that has been disrupted 

by large-scale boudinage. A metagabbro 

and a meta-acidic gneiss from a highpressure 

melange on Andros yielded Jurassic 

Pb-206/U-238 ages of and 156.2 

+/- 2.3 160.0 +/- 2.0 Ma, respectively, 

that correspond very well to ages reported 

for ophiolites from mainland 

Greece, the Balkan region, and Crete. 

The new results and literature data 

document that remnants of both Jurassic 

and Cretaceous meta-ophiolites are included 

in the melanges of the CBU. It is 

currently not known whether both age 

groups occur within the same melange 

174

or at different lithostratigraphic and/or 

tectonic levels. 

2010010564 

大型脊椎动物在雨水浸湿的中侏罗世 

沙丘中挖出的洞穴 = Burrows dug by 

large vertebrates into rain-moistened 

Middle Jurassic sand dunes. ( 英文 ). 

Loope D B. Journal of Geology, 2006, 

114(6): 753-762 

In south-central Utah, eolian crossstrata 

of the Escalante Member of the 

Entrada Sandstone contain inclined, cylindrical 

burrows up to 63 cm in diameter 

and 305 cm long. Of the 14 large 

tunnels located during this study, 12 descend 

from second- and third-order 

bounding surfaces that formed on the lee 

slopes of large dune ridges, well above 

the water table. The tunnels are inclined 

15 degrees-22 degrees; one tunnel ends 

in an expanded chamber. Eolian crossstrata 

fill proximal portions of four of 

the tunnels and indicate that after abandonment, 

sand drifts migrated as much 

as a meter into the open shafts. Structureless 

sand and breccia blocks that 

were generated by roof collapse fill 

other tunnels. Animals dug the tunnels 

in rain-moistened, cohesive sand. The 

burrows may have served as temporary 

shelters from severe diurnal conditions 

in the shadeless, subtropical Entrada 

dune field. 

2010010565 

西澳大利亚近海卡那封盆地 Tusk-1 

和 Tusk-2 井中侏罗世巴柔期 Athol 组 

时代的新证据 = New evidence for the 

age of the Athol Formation (Middle Jurassic; 

Bajocian) in the Tusk-1 and 

Tusk-2 wells, offshore Carnarvon Basin, 

Western Australia. ( 英文 ). Riding J B; 

Westermann G E G; Darbyshire D P F. 

Alcheringa, 2010, 34(1): 21 - 35 

The co-occurrence of ammonites with 

palynomorphs in the Athol Formation of 

the Tusk-1 and Tusk-2 wells drilled in 

the offshore Carnarvon Basin, Western 

Australia confirms the Early Bajocian 

(Middle Jurassic) age of the Dissiliodinium 

caddaense dinoflagellate cyst Oppel 

Zone. The macrofaunas refine this Early 

Bajocian age to the early Laeviuscula 

Chronozone. A belemnite from the 

Tusk-1 well has a strontium isotope 

( 87 Sr/ 86 Sr) ratio consistent with the biostratigraphical 

age. All the identifiable 

ammonites belong to Pseudotoites robiginosus 

(Crick). Pseudotoites is 

prominent in the Early Bajocian of the 

Indo-Pacific Realm, being known 

mainly from onshore Western Australia 

and the Southern Andes, together with 

rare occurrences in Irian Jaya (west New 

Guinea); somewhat surprisingly, it is 

also rarely present in southern Alaska. 

The palynofloras studied from the Tusk- 

1 and Tusk-2 wells contain abundant 

specimens of the marine dinoflagellate 

cyst Dissiliodinium caddaense, and are 

assigned to the Dissiliodinium caddaense 

Oppel Zone. The Athol Formation 

is a correlative of the Newmarracarra 

Limestone of the onshore Perth 

Basin, Western Australia; the distribution 

of both these units indicates a marine 

transgression onto the Australian 

block during the Early Bajocian. 

2010010566 

摩洛哥西南部塔法牙盆地赛诺曼期层 

序地层和海平面升降 = Cenomanian 

sequence stratigraphy and sea-level fluctuations 

in the Tarfaya Basin (SW Morocco). 

( 英文 ). Kuhnt W; Holbourn A; 

Gale A; Chellai El H; Kennedy W J. 

Geological Society of America Bulletin, 

2009, 121(11-12): 1695-1710 

We investigated the sequence architecture 

of two expanded Cenomanian 

successions along a depth transect in the 

Tarfaya Basin (SW Morocco) and correlated 

these successions to published records 

from northwest Europe and India. 

Changes in terrigenous material, carbonate 

and organic carbon content, carbonate 

microfacies and foraminiferal biofacies, 

as well as nondepositional and ero- 

175

sional surfaces were used to define depositional 

sequences and systems tracts. 

We identified two main transgressive 

cycles in the lower and middle-upper 

Cenomanian separated by a major regression 

at the early-middle Cenomanian 

transition (sequence boundary Ce 3). 

This regressive interval is characterized 

by lagoonal low-stand deposits indicating 

an overall sealevel fall of more than 

30 m. Superimposed on the two main 

transgressive cycles, there are 11 thirdorder 

depositional sequences that correlate 

to globally recognized sealevel fluctuations 

and appear to be paced by long 

eccentricity variations (400 Ka period). 

Positive carbon isotope excursions in the 

middle Cenomanian (96.0 Ma) and latest 

Cenomanian (94.0 Ma) following 

sealevel lowstands together with planktonic 

foraminiferal and ammonite datums 

provide a robust framework for 

stratigraphic correlation. We suggest that 

the onset of these excursions was triggered 

by eccentricity minima during periods 

of low variability in obliquity 

(nodes), which probably coincided with 

glacioeustatic lowstands. 

2010010567 

西藏日喀则恰布林地区晚白垩世和新 

生代相关碰撞砾岩的孢粉地层及其古 

环境发育的意义 = Palynological stratigraphy 

of the Late Cretaceous and Cenozoic 

collision-related conglomerates 

at Qiabulin, Xigaze, Xizang (Tibet) and 

its bearing on palaeoenvironmental development. 

( 英文 ). Li Jian-guo ;Guo 

Zhen-yu; Batten D J;Cai Hua-wei;Zhang 

Yi-yong;Li Jian-guo; Guo Zhen-yu;. 

Journal of Asian Earth Sciences, 2010, 

38(3-4): 86-95 

The stratigraphy, age, depositional 

environment and correlation of the collision-related 

variegated sandstone and 

conglomerate beds exposed along the 

southern side of the Gangdise Mountains 

to the north of the Yarlung Zangbo suture 

in the Xigaze region, Xizang (Tibet) 

have been much debated. Generally referred 

to as the Dagzhuka Formation, 

these beds of great thickness have, until 

recently, not been reported to contain 

any convincing fossils. Two distinctly 

different palynological assemblages, indicating 

Late Cretaceous and Oligocene–Early 

Miocene ages respectively, 

have now been recovered from 

lithologically distinguishable units of the 

sedimentary succession at Qiabulin to 

the west of the town of Xigaze. This 

means that instead of one stratigraphic 

unit, as has been generally accepted 

hitherto, at least two are represented. As 

a result, the Dagzhuga Formation is considered 

here to refer only to the Cenozoic 

deposits and the Qiabulin Formation, 

previously regarded as a synonym, 

is resurrected to accommodate the Cretaceous 

beds. These two formations 

were juxtaposed by tectonic movements. 

Our finding indicates that the stratigraphic 

successions on the southern 

Laurasian continental margin of Xizang 

reflect changes from a deep forearc basin 

through shallow littoral environments 

to a mountainous landscape during 

the Late Cretaceous and early Cenozoic. 

This interpretation compares well 

with those documented from the Gamba 

and Tingri districts to the south of the 

Yarlung Zangbo suture. 

2010010568 

云南罗平中三叠世大凹子剖面牙形石 

生物地层及其沉积环境研究 = Conodonts 

stratigraphy and sedimentary environment 

of the Middle Triassic at 

Daaozi section of Luoping County , 

Yunnan Province,south China. ( 中文 ). 

黄金元 ; 张克信 ; 张启跃 ; 吕涛 ; 周长勇 ; 白 

建科 . 微体古生物学报 , 2009, 26(3): 

211-224 3 图版 . 

罗平生物群产出于关岭组二段 , 该段 

大凹子精细剖面细致的沉积学描述记 

录显示 , 剖面岩性变化趋势为 : 从生物 

扰动灰岩到含硅质结核的条带泥晶灰 

岩 ( 钙屑浊积岩 ) 向白云岩演化。剖面 

详细的牙形石生物地层研究表明 , 

176

牙形石带属于 Nicoraella kockeli 带 , 同 

时该带可分两个亚带 , 即 N -icoraella 

kockeli type 1 亚带和 Nicoraella 

kockelitype 2 亚带。牙形石生物地层 

年代确定在 Anisian 期的 Pelsonian 亚 

期。通过大凹子剖面含牙形石段产出 

环境分析表明 : 深灰色具脉状层理含泥 

质灰岩的开阔台地相沉积环境牙形石 

产出较少且保存一般 , 而深黑色纹层状 

泥晶灰岩段台间盆地相沉积环境中牙 

形石产出丰富且保持完好。大凹子剖 

面沉积构造研究表明 : 罗平生物群产出 

于台间盆地相钙屑浊流沉积环境。 

2010010569 

从孢粉化石证据论冀北后城组的时代 

= On age of the Houcheng Formation in 

Hebei in the light of palynological evidence. 

( 中文 ). 张路锁 ; 张树胜 ; 赵克明 . 

地层学杂志 , 2009, 33(4): 407-412 3 图 

版 . 

主要分布于冀北地区的后城组是一 

套以河流相红色砂砾岩为主的地层 , 此 

前在不同地点的该岩组中曾发现中侏 

罗世晚期的叶肢介、瓣鳃类和爬行动 

物化石和晚侏罗世的介形类和孢粉等 

化石。新近在蔚县后城组发现的孢粉 

组合与此前在宣化堰家沟、万全渔儿 

山西侧后城组晚侏罗世孢粉化石组合 

面貌具有明显的差异 , 时代属中侏罗 

世。孢粉化石证据说明冀北的后城组 

系 — 套中 — 晚侏罗世沉积。 

2010010570 

鄂尔多斯盆地早白垩世剥蚀地层厚度 

恢复研究 = Denudation thickness restoration 

of Early Cretaceous strata in the 

Ordos Basin. ( 中文 ). 翁望飞 ; 刘池洋 ; 赵 

红格 ; 王建强 ; 张蓉蓉 ; 陈洪 ; 桂小军 . 地 

层学杂志 , 2009, 33(4): 373-381 

鄂尔多斯盆地下白垩统为中生代盆 

地演化末期最晚沉积的地层 , 也是自鄂 

尔多斯盆地发育以来后期遭受剥蚀改 

造最为强烈的地层 , 残存范围最小。通 

过对全盆八百二十余口钻井现存中生 

代地层厚度及岩性的统计 , 从中选取了 

313 口井读取声波时差值 , 采用声波时 

差和地层对比趋势法相结合进行剥蚀 

厚度估算 , 同时利用联井剖面对比法对 

整个盆地的恢复厚度进行对比验证。 

在此基础之上 , 恢复了早白垩世盆地原 

始沉积厚度 , 初步探讨了盆地原始沉积 

面貌 , 基本确定了盆地原始沉积边界 , 

从而进一步加深了对晚白垩世以来盆 

地强烈构造变动的认识 , 对多种能源矿 

产同盆共存富集规律的研究具一定的 

启示。 

2010010571 

基于高分辨率层序地层学的大庆长垣 

南部浅层气分布特征研究 = Shallow 

gas distribution character of the Heidimiao 

Reservoir in the southern Daqing 

placanticline based on high-resolution 

sequencestratigraphy. ( 中文 ). 刘宗堡 ; 吕 

延防 ; 杨志 ; 李秋影 ; 李迪 . 地层学杂 

志 , 2009, 33(4): 382-390 

松辽盆地大庆长垣南部黑帝庙油层 

具有良好的浅层气开发潜力。应用高 

分辨率层序地层学原理 , 通过对各级基 

准面旋回结构、叠加样式的沉积动力 

学分析 , 利用 1 164 口测井曲线和 6 口 

井岩芯资料 , 把松辽盆地大庆长垣南部 

黑帝庙油层划分为 1 个长期基准面旋 

回、4 个中期基准面旋回、25 短期基 

准面旋回 , 提出了研究区北部为后期构 

造抬升而缺失的层序地层新格架。短 

期基准面旋回内储层沉积特征及单砂 

体展布规律研究表明 : 黑帝庙油层为松 

辽盆地北部物源控制的湖盆逐渐萎缩 

背景下形成的河控缓坡三角洲前缘亚 

相沉积体系 , 微相类型以水下分流河 

道、河口坝和远砂坝为主。依据区域 

性湖侵成因的 9 套暗色泥岩盖层把黑 

帝庙油层垂向上划分为 9 套储盖组合 ; 

生储盖组合特征及动态资料综合分析 

表明浅层气主要分布于长期旋回下降 

早期的中期旋回下降晚期或上升早期 

储层砂体中 ; 单砂体展布规律与气源断 

层和构造的合理匹配是浅层气富集的 

177

主控因素 , 气藏类型主要为构造 — 岩 

性、断层 — 岩性圈闭 , 在以上研究的基 

础上应用气水解释模板在全区预测地 

质储量 , 其研究对指导整个松辽盆地北 

部浅层气勘探与开发具有重要理论意 

义和实际应用价值。 

2010010572 

突尼斯北部上侏罗统 — 白垩系最低部 

综合生物地层和区域对比 = Integrated 

biostratigraphy and regional correlations 

of Upper Jurassic - lowermost Cretaceous 

series in northern Tunisia. ( 英文 ). 

Boughdiri M; Sallouhi H; Haddad S; 

Cordey F; Soussi M. GFF, 2009, 131(1- 

2): 71-81 8 图版 . 

Integrated biostratigraphy and palaeogeographical 

interpretations of Upper 

Jurassic-Lower Cretaceous (Callovian- 

Berriasian) successions are synthesised 

on the basis of published data and our 

recent investigations of key sections 

from the "Tunisian Dorasale" (TD) and 

"Tunisian Trough" (TT) domains of 

northern Tunisia. After a revised biostratigraphy 

had been proposed for the 

"rosso ammonitico" series, bed-by-bed 

sampling led to a radiolarian-based first 

direct dating of the partly coeval biosiliceous 

series in the TT. Upward within 

the Jurassic column, an integrated biostratigraphy 

(ammonites, calpionellids 

and associated biomicrofacies) allowed 

precise biozonation for the Kimmeridgian-middle 

Berriasian interval. 

The heterogeneity of the Late Jurassic 

facies in northern Tunisia is the result of 

two main geodynamical and palaeogeographical 

events. The first corresponds 

to the fragmentation of the initial 

Early Jurassic platform linked to 

Tethyan rifting. The second event, coeval 

to the radiolarian-bearing series of 

the TT, is expressed by a significant 

deepening in north-west Tunisian palaeoenvironments. 

During Kimmeridgian-Tithonian 

times, previous 

troughs evolved back into carbonate 

platforms. Within the Maghrebian Belt, 

Upper Jurassic-lowermost Cretaceous 

series comprising three major facies 

groups are easily correlated; minor differences 

in age are interpreted as due to 

local tectonic control. Regional correlations 

confirm, on the one hand, a common 

geological history for the external 

segments of the African margin and, on 

the other hand, a distinct palaeogeographical 

evolution of the inner domain 

including the "Dorsales calcaires" 

and ancient massifs, both being separated 

by intermediate flysch zone segments. 

2010010573 

阿根廷巴通阶 - 卡洛维阶界线地层中一 

层火山灰的新锆石年龄 = A new U-Pb 

zircon age for an ash layer at the Bathonian-Callovian 

boundary, Argentina. ( 英 

文 ). Kamo S L; Riccardi AC. 

GFF, 2009, 131(1-2): 177-182 

A U-Pb zircon age of 164.64 +/- 0.2 

Ma (95% confidence level) is reported 

for an ash bed, at the Bathonian- 

Callovian (late Middle Jurassic) boundary, 

determined by isotope dilution 

thermal ionisation mass spectrometry 

from individual, chemically abraded 

grains. The volcanic ash layer occurs 

within the Chacay Melehue Formation, 

Chacay Melehue section, Neuquen Province, 

central west Argentina, above the 

last record of ammonites of the regional 

Lilloettia steinmanni Standard Zone, and, 

stratigraphically, where the first of those 

of the regional Eurycephalites vergarensis 

Standard Zone appears, generally referred 

to as the uppermost Bathonian 

and the lowermost Callovian, respectively. 

This ash layer represents the only 

known datable horizon worldwide that is 

directly related to a well-documented 

ammonite faunal succession at this 

boundary. The U-Pb zircon age is older 

than one previously reported for the 

same bed and closer to an estimation of 

164.7 +/- 4Ma for the boundary based 

on the scaling durations of ammonite 

zones to their subzones in the sub-boreal 

178

standard zonation. The new age agrees 

better with the age model for the Oxfordian 

through Bathonian M-sequence 

magnetic anomalies in the Pacific and 

contributes to the radioisotopic age calibration 

of the Jurassic time scale. 

2010010574 

西班牙东北部伊比利亚山脉东部侏罗 

纪 ( 下基米里支阶 ) 含菊石 

Ataxioceras 沉积的生物地层学新资料 

= Updated biostratigraphy of Jurassic 

(lower Kimmeridgian) deposits containing 

the ammonite Ataxioceras from the 

eastern Iberian Range, northeastern 

Spain. ( 英文 ). Moliner L; Oloriz F. 

GFF, 2009, 131(1-2): 195-203 3 图版 . 

Ammonite biostratigraphy and its correlation 

potential are evaluated for Ataxioceras-bearing 

deposits in the eastern 

Iberian Range, E-NE Spain. The 

Chronostratigraphic Standard Hypselocyclum 

Zone of sub-Mediterranean areas 

is analysed. Correlation of the new 

Ataxioceras lothari Biozone is proposed 

utilising first appearance datum (FAD)- 

based biostratigraphy, resulting from a 

review of ammonite (Ataxioceratinae) 

systematics. The lower boundary of the 

A. lothari Biozone and its chronostratigraphic 

equivalent Lothari Chronozone 

are defined by the FAD of Ataxioceras 

Fontannes s.s., and their upper boundaries 

by the FAD of Crussoliceras Enay. 

Distinction of the sub-biozones (subzones) 

A. hippolytense and A. lothari is 

confirmed, but these units are slightly 

reinterpreted. No ammonite subdivisions 

are defined for the A. hippolytense subzone, 

although two informal "intrasubzone 

biodivisions" (A. lothari and 

Geyericeras aragoniense) are recognised 

within the A. lothari subzone, the latter 

defined for the first time. The correlation 

potential of the proposed biostratigraphic 

scheme (zone and intra-zone 

levels using Ataxioceratinae) is high for 

marine successions from both epicontinental 

and oceanic-fringe environments 

under Tethyan influence (southern 

Europe and north-western Africa). The 

potential for correlation at the intra-zone 

level is higher for epicontinental than for 

oceanic-fringe areas; yet the precise correlation 

of some biostratigraphic 

boundaries is difficult at the "intrasubzone 

biodivision" level between the 

eastern Iberian Range and SE France. 

Updated identification and subdivision 

of the equivalent Metahaploceras strombecki 

Biozone in oceanic-fringe sections 

are presented, together with this unit's 

correlation potential with respect to the 

proposed A. lothari Biozone. 

2010010575 

侏罗纪 : 科学扩张的前沿阵地 = The 

Jurassic: In the forefront of science outreach. 

( 英文 ). Vajda V; Turner S. 

GFF, 2009, 131(1-2): 1-3 

2010010576 

侏罗纪斯堪迪纳维亚以及相关地区近 

岸沉积 = Onshore Jurassic of Scandinavia 

and related areas. ( 英文 ). Vajda V; 

Wigforss-Lange J. GFF, 2009, 131(1-2): 

5-23 

Jurassic strata are extensively distributed 

in offshore areas of Scandinavia, 

but onshore exposures are mostly restricted 

to southern Sweden (Skane), the 

Danish island of Bornholm, East 

Greenland, northern Norway (Andoya) 

and Svalbard. The latest Triassic and 

Jurassic saw active tectonism in Scandinavia 

associated with the break-up of 

Pangaea and rifting in the North Atlantic 

region and the North Sea. Rifting and 

the gradual rise in sea level controlled 

the structural and sedimentological architecture 

of Scandinavian basins 

throughout the Jurassic. The Upper Triassic 

is represented by continental red 

beds (claystones and arkosic conglomerates) 

indicative of arid conditions (until 

the Norian) and by coal measures characteristic 

of humid conditions (in the 

Rhaetian). Early Jurassic sedimentation 

179

in the region was dominated by fluvialestuarine 

systems. Basin subsidence 

combined with the supply of huge volumes 

of sediments led to the accumulation 

of thick sand units on vast coastal 

plains in the Early and Middle Jurassic. 

During the Late Jurassic, transgressions 

led to deposition of extensive marine 

mud, although sandstones are locally 

preserved. Paralic depositional environments 

prevailed during the Late Jurassic 

and into the Early Cretaceous in southern 

Scandinavia. Scandinavia hosts a 

rich Jurassic palaeontological record including 

fossil plants, sharks, dinosaur 

footprints, ammonites, belemnites, ichthyosaurs 

and pliosaurs. Miospores provide 

the primary tool for biostratigraphic 

subdivision and correlation of the continental 

Jurassic sediments, whereas ammonites, 

dinoflagellates and foraminifera 

are the main groups employed for 

marine biostratigraphy. However, much 

work remains to be completed to 

achieve a highly resolved zonation 

scheme that integrates both marine and 

terrestrial indices. 

2010010577 

澳大利亚侏罗纪沉积学和化石序列 : 

目前海相和非海相对比和未来预测 = 

Australian Jurassic sedimentary and fossil 

successions: current work and future 

prospects for marine and non-marine 

correlation. ( 英文 ). Turner S; Bean L B; 

Dettmann M; McKellar J L; McLoughlin 

S; Thulborn T. GFF, 2009, 131(1-2): 

49-70 6 图版 . 

Strata of Jurassic age occur extensively 

across onshore Australia, but they 

are predominantly of non-marine origin. 

Marine Jurassic strata have only limited 

onshore exposure in northwestern and 

central-western Australia, with thick marine 

sequences lying offshore on the 

North West Shelf. The richest petroleum 

province in Australia is located at the 

shelf's southern end, where the Dingo 

Claystone represents an important 

source rock for oil and gas. By and large, 

non-marine deposits, including economic 

coals, are distributed in the eastern 

states. Jurassic stage boundaries, in 

the main, are poorly constrained with 

respect to the Australian sedimentary 

succession. New work on microfossils, 

plants, fish, and zircon dating is providing 

a basis for improved correlation 

across Australian basins, with overseas 

successions, and recent international 

IUGS geologic timescales. 

2010010578 

四足动物群落差异和东欧早三叠世生 

物事件若干方面 = Differentiation of 

tetrapod communities and some aspects 

of biotic events in the early triassic of 

Eastern Europe. ( 英文 ). Shishkin M A; 

Sennikov A G; Novikov I V; Ilyina N V. 

Paleontological Journal, 2006, 40(1): 1- 

10 1 图版 . 

The patterns of spatial differentiation 

of the Early Mesozoic terrestrial biota in 

Eastern Europe and Australia-Tasmania 

demonstrate that the tetrapod faunal recovery 

following the Permian extinction 

was characterized by both global and 

regional heterogeneity. Local distinctions 

observed in the development of 

Early Triassic tetrapod assemblages of 

European Russia allow the recognition 

of the following realms: (1) the central 

and northern regions of the East European 

Platform (Moscow-Mezen Syncline) 

and the Timan-North Ural Region; 

(2) the southern Fore-Urals, including 

the Obshchii Syrt Plateau; and (3) the 

southern regions of the East European 

Platform (the slope of the Voronezh Anticline). 

Climatic conditions at the initial 

stage of the development of local communities 

were characterized by an increase 

in aridity and seasonal contrasts 

of climate. Therefore, terrestrial assemblages 

mostly concentrated in the 

aquatic and coastal biotopes. Accordingly, 

vertebrate assemblages of the region 

were dominated everywhere by 

aquatic amphibians and semiaquatic reptiles, 

while the accompanying palyno- 

180

morph assemblages show the predominance 

of hygrophilous vegetation indicative 

of swampy mangrove setting. With 

respect to amphibians, a peak of local 

biogeographic differentiation falls on the 

onset of the Early Triassic and, in the 

case of reptiles, on the end of this time 

span. This change conforms to the increasing 

role of reptiles in the overall 

taxonomic diversity with time. Among 

the three main biogeographic units of 

the region, the Southern Fore-Ural 

Realm is distinguished by the maintenance 

of distinct faunal links with 

Gondwanan regions. The Southern 

Realm shows a connection with the 

Germanic Basin and more western 

Euramerican areas, which is documented 

for the Late Olenekian and occurred under 

influence of coastal marine conditions. 

新生界 

2010010579 

高纬度地区的冷气候或暖期红矾土 ? 

= Cool-Climate or Warm-Spike Lateritic 

Bauxites at High Latitudes?. ( 英文 ). Retallack 

G J. Journal of Geology, 2009, 

116(6): 558-570 

Laterites and bauxites and their associated 

Ultisols and Oxisols are widespread 

in warm-wet climates today, and 

their spread to high latitudes has been 

attributed to episodes of past global 

warming. Bauxitic paleosols from the 

Early Eocene Monaro Volcanics of 

southeastern Australia have been 

claimed as exceptions formed in a coolwet 

climate. Re-examination and chemical 

analysis of a sequence of intrabasaltic 

paleosols in the Bega no. 7 core of 

radiometrically dated Monaro Volcanics 

now show highly variable paleotemperature 

and precipitation. The core includes 

53 successive paleosols, mostly nonbauxitic, 

but bauxitic paleosols reveal 

local spikes in warmth and precipitation 

coincident with early Eocene (55-, 52-, 

51-, and 48-Ma) global spikes of warmth, 

precipitation, and high atmospheric CO2. 

These bauxitic paleosols thus formed in 

warm-wet, not cool-dry, climates, and 

their poleward spread coincided with 

global greenhouse spikes. 

2010010580 

推断大洋时期的年龄分布 : 来自太平 

洋地区的经验 = Extrapolating Oceanic 

Age Distributions: Lessons from the Pacific 

Region. ( 英文 ). Rowley D B. Journal 

of Geology, 2009, 116(6): 587-598 

Extrapolation of the age distribution 

of oceanic lithosphere has played a significant 

role in assessments of variations 

in global mean spreading rate, global 

mean ocean basin depth, and implications 

for global mean sea level. Subduction 

has already removed 50% of oceanic 

lithosphere younger than 55.7 Ma, 

making some level of extrapolation a 

necessary part of global plate reconstructions. 

An area equal in size to the 

Pacific Basin oceanic lithosphere must 

be extrapolated for ages older than 29.1 

Ma. Three modes of extrapolation are 

identified. Mode 1 extrapolation uses the 

preserved history as recorded on one 

plate to infer the history of the previously 

adjacent plate. This mode of extrapolation 

is exemplified by the inferred 

history of the Farallon, Vancouver, 

Nazca, and Cocos plates relative to the 

Pacific Plate, on which this record is 

preserved. Mode 2 involves extrapolation 

beyond the preserved age extent of 

a given ridge system. No observable 

data exist that directly constrain the motions 

beyond the youngest magnetic reversal-dated 

oceanic lithosphere along 

such a boundary. This mode has, for example, 

been employed to extrapolate the 

age distribution resulting from spreading 

along the Izanagi-Pacific ridge system 

for as much as 60 m.yr. beyond the last 

directly determined record preserved on 

the Pacific Plate. Mode 3 is extrapolation 

of age distributions of entirely subducted 

ocean basins where no information 

explicitly constrains the relativemotion 

history of such basins. The age 

181

distributions in various neo-Tethyan basins 

require mode 3 extrapolation. This 

article examines extrapolations specifically 

using modes 2 and 3, employing 

the known spreading histories of the Pacific-Farallon/Vancouver 

and Pacific- 

Phoenix plate systems and the Tasman 

Sea as case studies. These tests demonstrate 

that extrapolated distributions of 

ages do not match preserved ages. Important 

events recorded in the preserved 

oceanic lithosphere, including both initiation 

and extinction of spreading ridges, 

cannot be inferred from the extrapolations 

and yet constitute important events 

that control aspects of the preserved 

oceanic lithosphere age distribution. 

Hence, reconstructed age distributions 

that require significant mode 2 and 3 extrapolations 

cannot provide a rigorous 

basis for testing hypotheses related to 

global histories of ridge production, 

mean age, mean depth, or other potentially 

correlated phenomena. This may 

appear to be an obvious result, and 

hence not worth publishing, but the persistent 

use of extrapolated age distributions 

in the published literature suggests 

that problems with extrapolation have 

not been appreciated by all. 

2010010581 

中国西北新疆北部阿尔泰山南缘库卫 

铁镁质岩体的年代学及地球化学 : 印 

度 - 欧亚碰撞的远距离影响证据 = 

Geochronology and geochemistry of the 

Kuwei mafic intrusion, southern margin 

of the Altai Mountains, northern Xinjiang, 

northwest China: Evidence for distant 

effects of the Indo-Eurasia collision. 

( 英文 ). Zhang Z C; Kusky T; Mao J W; 

Zhao L; Yan S H; Chen B L; Zhou G; 

Chai F M. Journal of Geology, 2008, 

116(2): 119-133 

The Kuwei mafic intrusion, consisting 

of hornblende gabbro, gabbro, gabbro 

norite, and olivine norite, lies in the 

southern Altai Mountains, northern Xinjiang. 

A combined field, geochronological, 

and geochemical study of the Kuwei 

intrusion is reported here. This study 

provides the first reliable SHRIMP U-Pb 

zircon dating results for the intrusion, 

and these yielded an age of 47 +/- 1 Ma, 

which is the first documented report of 

Eocene magmatism in the region. The 

chondrite-normalized rare earth element 

patterns for the Eocene intrusions are 

flat, and most of the incompatible elements 

are comparably depleted. Thus, 

geochemical data suggest that the Kuwei 

mafic intrusion was produced by partial 

melting of asthenospheric mantle that 

was slightly contaminated by lithospheric 

material. We interpret the 47-Ma 

magmatism to result from asthenospheric 

mantle upwelling following the 

progressive India-Eurasian collision. Although 

the Kuwei intrusion is laterally 

beyond the limit of Eocene deformation 

normally attributed to the India-Asia 

collision, the timing of magmatism in 

the intrusion suggests that lateral extension 

may have initially affected a wider 

region than the area later thickened by 

convergence in the Tibetan Plateau. The 

Kuwei intrusion and other plutons likely 

related to it may have been emplaced 

into dilational jogs in fault systems activated 

by the India-Asia collision. The 

emplacement depth is estimated to be 

similar to 6 km, based on geobarometric 

determinations. Erosion was imperceptible 

before 25 Ma but has worn away an 

average of 0.024 cm of uplift every year 

since 25 Ma. The 6 km of exhumation 

since the late Oligocene is also attributed 

to far-field effects of the India-Asia 

collision. 

2010010582 

伊朗东部 Sahlabad 省下始新统的海 

侵层序 , 生物地层学与微相分析意义 

= Lower Eocene transgressive successions 

of Sahlabad province, eastern Iran, 

implication of biostratigraphy and microfacies 

analysis. ( 英文 ). Babazadeh S. 

Revue de Paleobiologie, 2008, 27(2): 

449-459 

182

The Sahlabad province was characterized 

by deep resedimented deposits, radiolarian 

chert and shallow water marine sediments 

containing benthic foraminifera. The foraminiferal 

assemblage containing orthophragminids, 

small Nummulites, rotaliids such 

as Lockhartia conditi (Nuttall), Lockhartia 

haimei (Davies), Cuvillierina vallensis (Ruiz 

de Gaona), alveolinids and miliolids was 

dominantly deposited in shallow/protected 

subtidal to deeper/open subtidal. The microfacies 

analysis of carbonate rocks were carried 

out with respect to the distribution of depositional 

components and biota. Two main faunal 

assemblages are determined : Miliolinadominated 

assemblage (composed Opertorbitolites, 

Alveolina and miliolids) and orthophragminid-dominated 

assemblage (characterized 

by Discocyclina, Assilina and Asterocyclina). 

The ophiolitic mélanges which derived 

from the subduction zone in this province 

are covered by the Early Eocene transgressive 

conglomerates. 

2010010583 

全球古近纪 - 新近纪全球层型剖面和点 

位 ,Dababiya 采石场剖面的有孔虫指 

标 = Foraminiferal criteria for the Dababiya 

Quarry Beds, the Paleocene/Eocene 

Global Stratotype Sections 

and Point. ( 英文 ). Galal G. Revue de 

Paleobiologie, 2008, 27(2): 475-510 

One hundred eighty-one foraminiferal species 

(58 planktic & 123 benthic) were identified 

across the Dababiya Quarry Beds (DQBs 

1- 5, about 3.75 m thick) at the Paleocene/Eocene 

Global Stratotype Sections and 

Point (the Dababiya Quarry Section, Dababiya, 

Luxor, Egypt). The identified planktic species 

(5 serial & 53 spiral, recorded only within the 

size fractions 63-375 μm) are related to 10 

genera (2 serial & 8 spiral : 7 trochospiral & 1 

planispiral), which are classified into 7 families, 

3 superfamilies and one suborder. Meanwhile, 

the identified benthic species (31 agglutinated 

& 92 calcareous : 2 porcellaneous & 

90 hyaline) are related to 63 genera, 42 families, 

23 superfamilies and 6 suborders, which 

are found only within the size fractions 63-500 

μm. Thirteen distinctive biostratigraphic intervals 

(from Pre-DQBa to Post-DQB) were recognized 

within the Dababiya Quarry succession, 

on the basis of variation in foraminiferal 

frequency and species number. This necessitates 

the differentiation of the residue of each 

of the studied samples into five size fractions. 

Various frequencies of each of the recorded 

taxonomic groups were traced along the studied 

succession within different size fraction 

reflecting the importance of individual faunal 

size in further refinement of the studied stratotype. 

2010010584 

伊洛瓦底江流入印度洋的河流沉积通 

量 : 对 19 世纪原数据的再研究 = The 

Irrawaddy River sediment flux to the 

Indian Ocean: The original nineteenthcentury 

data revisited. ( 英文 ). Robinson 

R A J; Bird M I; Oo N W; Hoey T B; 

Aye M M; Higgitt D L; Lu X X; Swe A; 

Tun T; Win S L. Journal of Geology, 

2007, 115(6): 629-640 

The Irrawaddy (Ayeyarwady) River 

of Myanmar is ranked as having the 

fifth-largest suspended load and the 

fourth-highest total dissolved load of the 

world's rivers, and the combined Irrawaddy 

and Salween (Thanlwin) system 

is regarded as contributing 20% of 

the total flux of material from the Himalayan-Tibetan 

orogen. The estimates for 

the Irrawaddy are taken from published 

quotations of a nineteenth-century data 

set, and there are no available published 

data for the Myanmar reaches of the 

Salween. Apart from our own field studies 

in 2005 and 2006, no recent research 

documenting the sediment load of these 

important large rivers has been conducted, 

although their contribution to 

biogeochemical cycles and ocean geochemistry 

is clearly significant. We present 

a reanalysis of the Irrawaddy data 

from the original 550-page report of 

Gordon covering 10 yr of discharge 

( 1869-1879) and 1 yr of sediment concentration 

measurements ( 1877-1878). 

We describe Gordon's methodologies, 

evaluate his measurements and calculations 

and the adjustments he made to his 

data set, and present our revised interpretation 

of nineteenth-century discharge 

and sediment load with an estimate 

of uncertainty. The 10-yr average 

of annual suspended sediment load cur- 

183

ently cited in the literature is assessed 

as being underestimated by 27% on the 

basis of our sediment rating curve of the 

nineteenth-century data. On the basis of 

our sampling of suspended load, the 

nineteenth-century concentrations are 

interpreted to be missing about 18% of 

their total mass, which is the proportion 

of sediment recovered by a 0.45-mm filter. 

The new annual Irrawaddy suspended 

sediment load is MT. Our revised 

estimate of the annual sediment 

load 364 +/- 60 from the Irrawaddy- 

Salween system for the nineteenth century 

( 600 MT) represents more than half 

the present-day Ganges-Brahmaputra 

flux to the Indian Ocean. Since major 

Chinese rivers have reduced their load 

due to damming, the Irrawaddy is likely 

the third-largest contributor of sediment 

load in the world. 

2010010585 

现代珊瑚礁自然形态的统计 = The statistics 

of natural shapes in modern coral 

reef landscapes. ( 英文 ). Purkis S J; Kohler 

K E; Riegl B M; Rohmann S O. 


508 

Spatial heterogeneity is a fundamental 

characteristic of modern and ancient depositional 

settings, and the scaling of 

many carbonate environments has been 

shown to follow power function distributions. 

The difficulty in obtaining information 

on the horizontal persistence 

of sedimentary lithotopes at the basin 

scale has, however, hampered evaluation 

of this fact over larger geographic areas. 

In recent years, large-scale maps of reef 

facies derived from remotely sensed data 

have become widely available, allowing 

for an analysis of reef-scale map products 

from 26 sites spread through four 

reef provinces, covering > 7000 km(2) 

of shallow-water habitat in the U. S. territorial 

Pacific. For each site, facies 

maps were decomposed to polygons describing 

the perimeter of patches of differing 

sedimentologic/ benthic character. 

A suite of geospatial metrics quantifying 

unit shape, fractal dimension, and frequency-area 

relations was applied to investigate 

the intra- and intersite variability. 

The spatial architecture of these reef 

sites displays robust fractal properties 

over an extended range of scales with 

remarkable consistency between provinces. 

These results indicate the possibility 

of extrapolating information from 

large to small scales in various depositional 

environments. 

2010010586 

印度库茂恩和加尔瓦的小喜马拉雅 : 

第一部分构造和地层 = The Kumaun 

and Garwhal Lesser Himalaya, India: 

Part 1. Structure and stratigraphy. ( 英文 ). 

Célérier J; Harrison T M; Webb A A G; 

Yin An. Geological Society of America 

Bulletin, 2009, 121(9-10): 1262-1280 

Our understanding of the geologic 

evolution of the Himalaya remains incomplete, 

particularly in regard to structural 

and geochronologic details of the 

Proterozoic-Paleozoic Lesser Himalayan 

Sequence. We conducted an integrated 

field mapping, geochronological study, 

and geochemical analysis of the Lesser 

Himalayan Sequence strata in the Kumaun 

and Garwhal Himalaya of NW India 

(78°00'–80°30'E). Structural observations 

reveal a systematic change in 

deformation styles from lower to higher 

structural levels in the Main Central 

Thrust footwall. In the south, and at 

lower structural levels, the Main Central 

Thrust foot-wall is characterized by parallel 

folding and sparse development of 

axial cleavage. Quartz microstructures 

indicate that deformation occurred at 

temperatures below 350 °C. In contrast, 

in the north and at higher structural levels 

close to the Main Central Thrust, deformation 

is characterized by replacement 

of original bedding, the development 

of penetrative cleavage, and schistosity 

locally. Folds are tight, in places 

isoclinal and overturned. The corresponding 

quartz microstructures indicate 

184

that deformation occurred above 350 °C. 

Dating of detrital zircons from Lesser 

Himalayan Sequence metasedimentary 

units, and igneous zircons from schistose 

gneisses throughout the Lesser Himalayan 

Sequence allow refinements to 

the stratigraphic framework. First, unlike 

what has been observed in western Nepal 

immediately west of our study area, 

U-Pb zircon dating suggests the absence 

of Paleoproterozoic strata in the 

Ramgarh Thrust hanging wall. This suggests 

that the thrust cuts upsection laterally 

along strike. Second, U-Pb detrital 

zircon dating suggests that metasedimentary 

strata in the Ramgarh Thrust hanging 

wall are correlative with basal units 

of the Outer Lesser Himalayan Sequence, 

removing the necessity that the 

Ramgarh Thrust hanging wall was allochthonous 

with respect to its footwall 

Lesser Himalayan Sequence units. 

Schistose gneisses with U-Pb ages of ca. 

1850 Ma are older than Lesser Himalayan 

Sequence units in the area, suggesting 

that they are Lesser Himalayan Sequence 

basement. We conclude that the 

Ramgarh Thrust is an out-of-sequence 

thrust postdating a folding event in its 

footwall. The earlier proposal that Neoproterozoic-Cambrian 

Lesser Himalayan 

Sequence strata are the southern extension 

of the Tethyan Himalayan Sequence 

requires that the Tons Thrust, which 

separates the distal and proximal facies 

of the Lesser Himalayan Sequence, be a 

major, south-directed structure with a 

slip magnitude of >50–100 km. 

2010010587 

德国南部中新世 Sandelzhausen 化石 

层的研究史 , 地质学 , 动物群和时代 = 

The fossil lagerstatte Sandelzhausen 

(Miocene; southern Germany): history 

of investigation, geology, fauna, and age. 

( 英文 ). Moser M; Rossner G E; Gohlich 

U B; Bohme M; Fahlbusch V. Palaeontologische 

Zeitschrift, 2009, 83(1): 7-23 

Sandelzhausen in southern Germany 

ranks among the most important Neogene 

fossil terrestrial localities in Europe, 

due to its exceptional record of both 

macro- and microvertebrates as well as 

invertebrates. From its discovery in 

1959 until its final closure in 2001, the 

site has been the subject of two longterm, 

systemaic digging campaigns as 

well as occasional collecting by the 

Ludwig-Maximilians Universitat together 

with the Bayerische Staatssammlung 

fur palaontologie und Geologie. 

In addition to a few plant remains a 

fossil fauna comprising more than 200 

taxa and 50,000 identifiable specimens 

has been collected including ostracods, 

molluscs, and, especially, vertebrates of 

all groups, with an emphasis on mammals. 

2010010588 

希腊 Pindus 山脉冰川历史 = The glacial 

history of the Pindus Mountains, 

Greece. ( 英文 ). Hughes P D; Woodward 

J C; Gibbard P L; Macklin M G; Gilmour 

M A; Smith G R. Journal of Geology, 

2006, 114(4): 413-434 

Geomorphological evidence for Pleistocene 

glaciation has been mapped in 

the Pindus Mountains of northwest 

Greece, and the chronology of glaciation 

in this area has been established through 

soil profile analysis and U-series dating 

of secondary carbonates (calcite) formed 

within glacial deposits. Three glacial 

stages are evident in the sedimentological 

and geomorphological records. The 

earliest and most extensive recorded 

glaciation predates 350,000 yr B. P. and 

was characterized by extensive valley 

glaciers and ice fields. A more recent 

glaciation occurred before the last interglacial 

and was characterized by glaciers 

that reached midvalley positions. The 

last phase of glaciation in Greece is recorded 

by small cirque glacier moraines 

and relict periglacial rock glaciers. The 

glacial and periglacial sequence on 

Mount Tymphi has been used in conjunction 

with a reference parastratotype, 

the long lacustrine sequence at Ioannina, 

185

to provide a chronostratigraphical 

framework for cold-stage deposits in 

Greece. The three glacial stages are formally 

defined: the Skamnellian Stage, 

equivalent to the Elsterian Stage of 

northern Europe and marine isotope 

stage (MIS) 12; the Vlasian Stage, 

equivalent to the late Saalian Stage of 

northern Europe and MIS 6; and the 

Tymphian Stage, which is equivalent to 

the Weichselian/Wurmian stages of 

northern Europe and the Alps, respectively, 

and MIS 5d-2. This is the first 

formalized chronostratigraphical framework 

based on the glacial record to be 

established for cold stages in the Mediterranean 

and provides a new platform 

for paleoclimatological investigations in 

the region. 

2010010589 

犹他州更新世 Bonneville 湖石灰华形 

成的控制因素 = Controls of tufa development 

in Pleistocene Lake Bonneville, 

Utah. ( 英文 ). Felton A; Jewell P W; 

Chan M; Currey D. Journal of Geology, 

2006, 114(3): 377-389 

Prominent tufa localities along the 

Provo level (similar to 14,000 C-14 yr B. 

P.) shoreline in Pleistocene Lake Bonneville 

have been characterized in detail. 

Three types of tufa are recognized: capping 

tufa, beachrock, and capping tufa 

over beachrock. Capping tufa and 

beachrock are end members of a continuum 

based on variable clastic content. 

All three types typically occur on headland 

environments that had stable substrate 

and little sediment input. Tufa development 

correlates with bedrock exposure 

and landform orientation, which 

in turn are correlated (R-2 = 0.89) with 

the longest fetch directions in the basin. 

Tufa also tends to be located at major 

subbasin divides and in the western portion 

of the basin. 

2010010590 

西西里海峡裂缝水下火山作用的岩石 

学和地球化学 = Petrology and geochemistry 

of submarine volcanism in the 

Sicily Channel Rift. ( 英文 ). Rotolo S G; 

Castorina F; Cellura D; Pompilio M. 


365 

Submarine magmatism in the Sicily 

Channel Rift began in the early Pliocene 

and lasted until almost 200 yr ago. We 

present here petrological and geochemical 

data on volcanic rocks dredged from 

Graham and Nameless banks and 

Pantelleria seamounts in the Pelagian 

sector of the Sicily Channel Rift. 

Petrological evidence suggests that the 

ascent of magmas to the surface was 

relatively rapid, probably through channels 

superimposed over the major tectonic 

discontinuities of the Rift. Major 

and trace element data indicate an ocean 

island basalt affinity for Graham and 

Nameless bank alkaline lavas and a depleted 

tholeiitic signature for one 

Pantelleria seamount, which had a shallower 

mantle source. Sr-Nd-Pb isotopic 

compositions suggest a heterogeneous 

mantle source involving both focus zone 

( FOZO) and high- mu( HIMU) components. 

Lead isotopic compositions are 

slightly less radiogenic in the tholeiitic 

basalt and more radiogenic ( closer to 

HIMU) in the alkaline lavas. We hypothesize 

that a decompressional melting 

mechanism affected the mantle beneath 

the Sicily Channel at different levels. 

Our data fit in a regional scenario 

characterized by the presence of HIMU 

or FOZO components in alkaline and 

calc-alkaline volcanics all around Sicily. 

The explanation for the common isotopic 

composition could lie in a ( fossil) 

plume head that variably contributed to 

magmatogenesis in response to variable 

lithospheric stretching. 

2010010591 

夏威夷第四纪冰期 - 间冰期气候旋回 = 

Quaternary glacial-interglacial climate 

186

cycles in Hawaii. ( 英文 ). Sheldon N D. 


376 

The upper kilometer of the Hawaiian 

Scientific Drilling Program core consists 

of lavas that were emplaced subaerially, 

burying paleosols. These paleosols were 

preserved with minimal alteration and 

are used to construct a similar to 330-kyr 

Quaternary climate record. Within the 

temporal resolution of this record, there 

appears to be a similar to 100-kyr climate 

oscillation between cool-dry and 

warm-wet conditions, indicating that 

tropical regions such as Hawaii have responded 

to the same global climate forcings 

as have higher-latitude areas during 

at least the past three glacial-interglacial 

cycles. It is also suggested that Hawaiian 

climate may have become progressively 

warmer and wetter over the same period. 

2010010592 

墨西哥 Guanajuato 地区 San Miguel 

de Allende 地堑中新世 - 上新世火山灰 

沉积中硅酸岩浆的对比 = Contrasting 

silicic magma series in Miocene- 

Pliocene ash deposits in the San Miguel 

de Allende Graben, Guanajuato, Mexico. 

( 英文 ). Adams A J; Christiansen E H; 

Kowallis B J; Carranza-Castaneda O; 

Miller W E. Journal of Geology, 2006, 

114(2): 247-266 

The San Miguel de Allende graben, 

Guanajuato, Mexico, contains numerous 

rhyolitic volcanic ash beds. Electron microprobe 

and x-ray fluorescence analyses 

of glass shards from 14 localities, 

combined with mineralogic, stratigraphic, 

radiometric, and paleomagnetic 

data, allow us to correlate the ash beds 

( and the intervening sedimentary strata 

and fossils), understand the timing of 

volcanism, date the age of extension, 

and better understand the tectonic and 

volcanic evolution of central Mexico. 

Our analyses reveal that at least six 

separate eruptions of rhyolitic ash occurred 

during the Late Miocene and 

Pliocene (5-3 Ma) while the San Miguel 

Allende basin was subsiding. The fallout 

ash beds can be distinguished by 

phenocryst mineralogy, inferred eruption 

temperatures, and differences in 

major and trace element compositions. 

Two magma series ( medium K and high 

K) are represented in the rhyolitic tephra 

deposits. The high-K series is marginally 

peralkaline, reduced ( indicated by 

high Fe/Mg ratios), dry ( paucity of hydrous 

silicates), hot (

水涛 ; 李中轩 ; 范超 ; 章森桂 . 地层学杂 

志 , 2009, 33(4): 413-419 

通过对江苏境内全新世典型考古遗 

址文化间歇层成因及其灾变事件信息 

的提取和时间序列的建立 , 结合与自 

然沉积地层和现代洪水沉积物以及已 

知海相地层的对比分析 , 是了解该区 

全新世以来考古地层揭示的海侵、海 

啸、古洪水、黄泛与淮泛等灾变事件 

过程和环境质量变化历史的重要手段 ; 

探讨全新世灾变事件的确切年代及其 

考古地层学可靠的判定依据和特征 , 

探索微体古生物学在本区新石器时代 

遗址海侵层调查中的应用是今后江苏 

及我国沿海地区全新世环境考古研究 

的努力方向 . 

2010010594 

苏北梁王城遗址黄泛层初步研究 = A 

preliminary study on the strata of Yellow 

River overflow in the Liangwangcheng 

site in northern Jiangsu. ( 中文 ). 

黄铿 ; 朱诚 ; 马春梅 ; 林留根 . 地层学杂 

志 , 2009, 33(4): 389-406 1 图版 . 

基于黄河下游流域考古遗址中第一 

次发现的黄泛地层 , 对苏北梁王城遗址 

T3902 探方南壁剖面上部自然淤积层 

采样 , 结合考古断代 , 并参照历史资料 , 

通过分析重砂矿物和粒度两方面的实 

验结果 , 揭示出考古遗址中黄泛地层的 

沉积物特征。旨在为今后环境考古中 

对黄泛地层的判别和对比提供可靠的 

科学依据 , 特别是为在黄河下游洪泛区 

考古遗址中疑似黄泛层的确认提供依 

据。 

2010010595 

天津地区黄骅坳陷全新世沉积环境及 

其变化特征 = Depositional environment 

of the Holocene in the Huanghua 

depression of Tianjin area. ( 中文 ). 李利 

波 ; 翟子梅 ; 周志勇 ; 田树信 . 地层学杂 

志 , 2009, 33(4): 420-424 

在岩芯观察的基础上 , 通过对钻井 

沉积环境的分析 , 结合其岩性剖面和 

沉积构造等资料 , 详细分析了天津地 

区黄骅坳陷全新世的沉积环境特征、 

类型及其展布 ; 认为该区主要有冲 

积、湖沼沉积、河口湾沉积、滨浅海 

沉积等 4 种主要沉积环境。全新世为 

一套松散堆积层 , 其岩性组合和生物 

化石组合特征及其变化 , 反映了天津 

地区黄骅坳陷全新世以来沉积环境由 

滨海 — 近岸浅海至河口湾、潟湖、滨 

海平原再至冲积平原的演变。 

2010010596 

瑞典中部和北部泥炭地地层 : 全新世 

气候改变的证据和泥炭沉积 = Stratigraphy 

of peatlands in central and northern 

Sweden: evidence of Holocene climatic 

change and peat accumulation. ( 英 

文 ). Rundgren M. GFF, 2008, 130(2): 

95-107 

Early peat surveys demonstrated the 

potential to detect Holocene climatic 

changes in southern Sweden through 

analysis of the degree of decomposition 

of Sphagnum peat and motivated systematic 

collection of peat-strati graphic 

information during subsequent geological 

mappings in central and northern 

Sweden. The resulting (published and 

unpublished) data was compiled and reanalysed, 

taking into account unpublished 

radiocarbon data and developments 

in radiocarbon calibration and 

pollen-stratigraphic dating. Data from 61 

carefully selected sites indicate a peat 

initiation maximum centred in the north 

9500-8000 cal. BP and interpreted to 

primarily reflect climatic change. The 

cause for a secondary maximum 6000- 

5500 cal. BP centred further south is less 

clear. Peat deposition data show a continuous 

increase in the period 10 500- 

2000 cal. BP, with almost constant values 

during recent millennia, indicating 

that peatlands in the region acted as a 

long-term Holocene carbon sink and increasingly 

so until c. 2000 years ago. 

Sphagnum peat decomposition data display 

a long-term trend towards wetter 

188

conditions after 5000 cal. BP interpreted 

to primarily reflect progressively 

stronger westerly airflow and an accompanying 

increase in precipitation. These 

data also show that wet shifts occurred 

more frequently across the region 

around 3300, 2500-2100 and 1300 cal. 

BP. The timing of peak frequencies of 

wet shifts is similar to that of supposedly 

climate-related wet shifts identified in 

southern Sweden. Variability in frequency 

of wet shifts is most strongly 

pronounced in the south-west, with an 

apparent periodicity of 800-1000 years 

believed to reflect regular changes in 

westerly airflow during the mid and late 

Holocene. 

2010010597 

太平洋西南部早古近纪温度演化 = 

Early Palaeogene temperature evolution 

of the southwest Pacific Ocean. ( 英文 ). 

Bijl P K; Schouten S; Sluijs A; Reichart 

J G; Zachos J C; Brinkhuis H. Nature, 

2009, 461(7265): 776-779 

Relative to the present day, meridional 

temperature gradients in the Early 

Eocene age (56–53 Myr ago) were unusually 

low, with slightly warmer equatorial 

regions but with much warmer 

subtropical Arctic and mid-latitude climates. 

By the end of the Eocene epoch 

(34 Myr ago), the first major Antarctic 

ice sheets had appeared, suggesting that 

major cooling had taken place. Yet the 

global transition into this icehouse climate 

remains poorly constrained, as 

only a few temperature records are 

available portraying the Cenozoic climatic 

evolution of the high southern latitudes. 

Here we present a uniquely continuous 

and chronostratigraphically 

well-calibrated TEX 86 record of sea surface 

temperature (SST) from an ocean 

sediment core in the East Tasman Plateau 

(palaeolatitude 65° S). We show 

that southwest Pacific SSTs rose above 

present-day tropical values (to 34 °C) 

during the Early Eocene age (53 Myr 

ago) and had gradually decreased to 

about 21 °C by the early Late Eocene 

age (36 Myr ago). Our results imply that 

there was almost no latitudinal SST gradient 

between subequatorial and subpolar 

regions during the Early Eocene age 

(55–50 Myr ago). Thereafter, the latitudinal 

gradient markedly increased. In 

theory, if Eocene cooling was largely 

driven by a decrease in atmospheric 

greenhouse gas concentration, additional 

processes are required to explain the 

relative stability of tropical SSTs given 

that there was more significant cooling 

at higher latitudes. 

2010010598 

柴达木盆地察尔汗古湖泊晚更新世沉 

积地球化学与环境的变化 = Sedimentation 

geochemistry and environmental 

changes during the late Pleistocene of 

paleolake Qarhan in the Qaidam basin. 

( 英文 ). Chang F Q; Zhang H C; Yue C; 

Yang M S; Jie N; Fan H F; Lei G L; 

Zhang W X; Lei B; Yang L Q. Journal 

of China university of geosciences, 2008, 

19(1): 1-8 

On the basis of the analyses of TOC, 

CaCO3, delta C-13(org) delta O-18, and 

delta C-13 of the shell bar section in the 

Qaidam basin, and compared with grain 

size data, the environmental change history 

of the high water level of paleolake 

Qarhan was reconstructed and it could 

be divided into five stages. From 39.7 to 

35.8 kaBP was the development period 

of high paleolake level. From 35.8 to 

33.6 kaBP and 33.6 to 27.2 kaBP, TOC 

and CaCO3 contents and delta O-18 

values were high, whereas, delta C- 

13(org) values and median size content 

were low, reflecting a warm-humid climate 

and high lake level. During 27.2- 

22.3 kaBP and 22.3-17.5 kaBP, both 

temperature and the lake level were 

lower than those in the previous stages, 

but the climate was still warmer and 

more humid than that of today. The lake 

level decreased between 32.4 and 32.2 

kaBP, 30.4 and 29.8 kaBP, and 28.4 and 

27.2 kaBP. Generally, the climate was 

189

warm and humid in Qaidam basin and 

the high lake level sustained between 

39.7 and 17.5 kaBP. The lake retreated 

abruptly at 17.5 kaBP, with a very 

strong increase in evaporation, which 

resulted in salt formation and the extinction 

of Corbicula. 

2010010599 

南黄海 NT1 号岩芯沉积物源及沉积物 

的地球化学特征 = Geochemistry characteristics 

of sediment and provenance 

relations of sediments in Core NT1 of 

the South Yellow Sea. ( 英文 ). Wang H 

X; Zhang X J ; Lan X H; Zhang Z X; 

Lin Z H; Zhao G T. Journal of China 


287-298 

The contribution of substance from 

Yellow River, Yangtze River, and Korean 

rivers to the sedimentation of Yellow 

Sea is studied through geochemical 

analysis and through characterization of 

the source of the substance about sediment 

from Core NT1 among the lutaceous 

area in Central South Yellow Sea. 

The research finds out that the sediment 

in Core NT1 mainly comes from Yangtze 

River and Yellow River, the sediment 

between 0-7.70 m in upper Core 

NT1 mainly belongs to Yangtze River 

source; the sediments between 7.70- 

16.60 m and 42.0-54.80 m in middle 

Core NT1 are mainly from Yellow River, 

the 26 m thick sediment interlayer in it 

mainly comes from Yangtze River; and 

the sediment between 54.80-69.76 m in 

the bottom of Core NT1 is mainly from 

Yangtze River. The results demonstrate 

that Yangtze River has been playing a 

main role in the lutaceous area in the 

Central South Yellow Sea since early 

Late Pleistocene, and Yellow River 

started to influence the continental 

sedimentation of Yellow Sea from early 

Warm Glaciation of late Late Pleistocene. 

2010010600 

阿尔泰山旧石器时代早期 Karama 遗 

址最早期沉积的化石孢粉植物群、地 

质年代和气候地层 = The fossil palynoflora, 

geological age, and climatostratigraphy 

of the earliest deposits of 

the Karama site (Early Paleolithic, Altai 

Mountains). ( 英文 ). Bolikhovskaya N S; 

Derevyanko A P; Shun’kov M V. Paleontological 

Journal, 2006, 40 (Supplement 

5): S558-S566 3 图版 . 

The results of palynological analysis 

of the Early Paleolithic Karama site 

(northeastern Altai Mountains) are presented. 

The Karama site is among the 

most unique and ancient archeological 

sites of Eurasia. Detailed palynological 

study has refined the geological age of 

the sediments that enclose pebble industry 

artifacts. The landscape and climatic 

conditions of Early Paleolithic man are 

reconstructed. A detailed characterization 

of the changes in the flora and vegetation 

that occurred during the most ancient 

Neo-Pleistocene interglacials and 

glacials is provided. 

190

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