margin of the southwest Caribbean. ( 英 文 ).Rincón D A; Arenas J E; Cuartas C H; CárdenasA L; Stratigraphy, 2007, 4(4): 261-311Biostratigraphy in northern Colombia has traditionallybeen done using foraminifera. Quantitativebiostratigraphic techniquescould improvethe zonations that have been proposed for theregion. We analyze the biostratigraphic informationfrom 190planktonic foraminifera species,and 1961 ditch-cutting samples from 26 oil wellsin northern Colombia to produce a zonation fortheregion. A quantitative biostratigraphic techniqueknown as Constrained Optimization wasused to analyze the data.The proposed zonationrelies exclusively on last occurrences, which arereadily applied to petroleum exploration. It hasthirteenzones and eight subzones for the Eoceneto Pliocene interval. Three zones and two subzonesare defined for the Eocene, three zones forthe Oligocene, six zones and six subzones for theMiocene, and one zone for the Pliocene. Thezonation reveals three major unconformities:(1) a late Eocene - early Oligocene hiatus; (2) alate Oligocene - early Miocene hiatus; and (3) alate Miocene hiatus; the hiatusesare related tothe collision of the Caribbean with the SouthAmerican plate.2008040329中 国 南 方 埃 迪 卡 拉 生 物 群 中 的 八 射 螺 旋 状 生物 = Octoradiate Spiral Organisms in the Ediacaranof South China. ( 英 文 ). Tang Feng; YinChongyu; Bengtson S; Liu pengju; WangZiqiang; Gao Linzhi. Acta GeologicaSinica, 2008, 82(1): 27-34Shales of the Ediacaran Doushantuo Formationof South China contain a new disc-shapedmacrofossii, Eoandromeda octobrachiata, characterizedby eight spiral arms that were probablyhoused within an outer membrane.Although thepresence of eight radiating structures entails aresemblance to cnidarian octocorais as well as toctenophores,direct homologies with these extantgroups are unlikely.Instead we bring attention tothe helicospiral morphology of newly reportedembryos from the Doushantuo Formation,suggesti...古 杯 、 多 孔 及 腔 肠 动 物2008040330得 克 萨 斯 瓜 达 鲁 普 山 国 家 公 园 南 部 Bell Canyon组 Reef Trail 段 上 部 的 六 射 海 绵 和 伴 生 的其 他 海 绵 = Hexactinellid and associatedsponges from the upper Reef Trail Member ofthe Bell Canyon Formation, southern GuadalupeMountains National Park, Texas. ( 英 文 ). Rigby JK; Bell G L; Thompson K. Journal of Paleontology,2007, 81(6): 1241-1256 6 图 版 .A small faunule of silicified hexactinellidsponges and root tufts has been recovered fromthe upper Guadalupian Reef Trail Member of theBell Canyon Formation, from the Patterson Hills,in the southwestern part of the Guadalupe MountainsNational Park in western Texas. Somedemosponges from the type section of the ReefTrail Member, near the mouth of McKittrickCanyon on the front of the Guadalupe Mountainsin the park, have also been documented. Includedin the faunule from the Patterson Hillslocalities are the new amphidiscosid hexactinellidpelicasponge Trailospongia reischi n. gen.and sp., the questionable pelicaspongiid Hexirregularianana n. gen. and sp., and the dictyospongiidhexactinellids Microstaura doliolumFinks, 1960, and Microstaurella minima n. gen.and sp., and Microstaurella parva n. gen. and sp.They are associated with specimens of the lyssacinosidbrachiosponges Toomeyospongiellagigantia Rigby and Bell, 2005, Toomeyospongiamodica n. sp., and Toomeyospongia minuta n.gen. and sp., and fragments of three differenttypes of root tufts, termed Tufts 1, 3, and 4. Twospecimens of the new cylindrical demospongeMckittrickella pratti n. gen. and sp. are associatedwith Tuft 2 in the collection from the typesection of the Reef Trail Member, and a thirdspecimen was collected from the member in thePatterson Hills. These sponges from Localities1–7 are the youngest Permian sponges knownfrom the region, and possibly from North America.2008040331英 格 兰 和 法 国 侏 罗 纪 微 壳 管 状 蠕 虫 = Microconchidtubeworms from the Jurassic of Englandand France. ( 英 文 ). Vinn O; Taylor P D. Actapalaeontologica Polonica, 2007, 52(2): 391-399The Bajocian tubeworm Spirorbis midfordensis,previously regarded as a spirorbid polychaete,is reinterpreted as a microconchid andassigned to Punctaconchus gen. nov. along withtwo new species, Punctaconchus ampliporus sp.nov., the type species of the new genus, andPunctaconchus palmeri sp. nov.. Microconchidsare a mostly Palaeozoic group of tubeworms thatare probably more closely related to modern lophophoratephyla than they are to polychaetes.2008040332帕 米 尔 山 脉 中 三 叠 世 似 六 射 珊 瑚 Furcophyllia= The Middle Triassic scleractinia-like coralFurcohyllia from the Pamir Mountains. ( 英 文 ).Melnikova G K; Roniewicz E. Acta palaeontologicaPolonica, 2007, 52(2): 401-406Furcophyllia is an unusual coral with septaregularly splitting into branching sets called septalbrooms. This pattern of septal apparatus is soalien to scleractinians, that, despite a trabecular106
microstructure of septa resembling that of theScleractinia, the genus was originally ascribed toa rare group of corals informally referred to assleractiniamorphs, previously known from theOrdovician and Permian. Here, we report Furcophylliashaitanica sp. nov. from limestoneboulders found in the volcano-clastic deposits ofthe upper Ladinian Sajtan suite of the SouthEastern Pamirs. A new species of Furcophylliasignifies that the genus was a faunal elementwidely distributed in the Tethys.2008040333中 国 早 寒 武 世 澄 江 地 层 Palaeoscolecid 蠕 虫Cricocosmia 和 Tabelliscolex 属 的 躯 干 纹 饰 =Trunk ornament on the palaeoscolecid wormsCricocosmia and Tabelliscoles from the EarlyCambrian Chengjiang deposits of China. ( 英 文 ).Han Jian; Liu Jianni; Zhang Zhifei; ZhangXingliang; Shu Degan. Acta palaeontologicaPolonica, 2007, 52(2): 423-431New observation reveals that the ventral trunkbears an additional set of ventral sclerites whilethe lateral sclerited display a tubercle-bearing(inner surface) and net-like (outer surface) microstructuresimilar to that of Tabelliscolexhaxagonus. (1) Cricocosmia shows a dorsoventraland antero-posterior differentiation intrunk ornament; (2) as seen from the microstructure,Cricocosmia is close to Tabelliscolexhexagonus, supporting the idea that lobopodiansand arthropods, both of which show an uppercapping layer in the outer sclerites, are moreclosely related than the palaeoscolecidans; and(3) the similarities among the scalids, pharyngealteeth and the trunk spines of palaeoscolecidansare superficial. Tabelliscolex maanshanensis sp.nov., characterized by an inner concentric circletof laminae in each tubercle of the lateral trunkplate, is proposed herein. Element mapping revealthat four known pathways of preservationcan be found co-occurring in a single specimenof Cricocosmia or Tabelliscolex, which shedsnew light on the preservation of the Chengjiangfossils.2008040334加 拿 大 Manitoba 南 部 上 奥 陶 统 床 板 珊 瑚Manipora 的 形 态 特 征 = Morphometrics ofManipora (tabulata: Upper Ordovician: southernManitoba, Canada). ( 英 文 ). Bae B-Y; Elias R J;Lee D-J. Journal of Paleontology, 2008, 82(1):78-90 1 图 版 .Multivariate morphometric analysis was appliedfor differentiation of closely related speciesand evaluation of intra- and interspecific variationin Manipora from the Selkirk Member, RedRiver Formation, in southern Manitoba. Sevenmorphological characters were quantified intransverse thin sections of 46 coralla and statisticallytested for selecting effective characters indiscriminating species. Cluster analysis was performedon a raw data matrix coordinated with 46coralla by three selected characters. Two majorclusters on the resulting dendrogram were regardedas morphospecies, following comparativeexamination of the coralla using serial sections.Cluster analyses were also conducted on principalcomponent score matrices obtained from theraw data set coordinated with 46 coralla by allseven characters, and from an experimental dataset including the 46 coralla plus two replicates ofeach and six of the characters. The results agreeclosely with the first cluster analysis, but discriminationof morphospecies was slightly degraded.The validity of two morphospecies recognizedin the first cluster analysis was verifiedby discriminant analyses, descriptive statistics,and bivariate plots. The results show that tabulariumarea is the most meaningful character fordistinguishing these morphospecies; ranges ofvariations of the other six characters overlapbetween morphospecies. Another cluster analysislike the first was performed, but with the additionof 11 type specimens and reference corallaof Manipora species from the Upper Ordovicianof southern and northern Manitoba and Texas.Based on this analysis, together with comparativeexamination of thin sections, the two morphospeciesare identified as valid species: M.amicarum Sinclair, 1955 and M. manitoba(Sokolov, 1955). Manipora magna Flower, 1961is considered to be a synonym of M. amicarum,while M. trapezoidalis Flower, 1961 and M. garsonensisCaramanica, 1992 are considered to besynonyms of M. manitoba, and the hypotypes ofM. amicarum of Nelson (1963) are assigned toM. manitoba.2008040335贵 州 北 部 晚 奥 陶 世 四 射 珊 瑚 动 物 群 组 合 特征 、 古 生 物 地 理 亲 缘 关 系 及 群 体 灭 亡 = CombinationFeatures,paleobiogeographic affinityand mass extinction of the Latest Ordovician(Hirnantian)rugosan fauna from northernGuizhou,China. ( 英 文 ). He Xinyi; Chen Jianqiang;Xiao Jingyi. Acta Geologica Sinica, 2007,81(1): 23-41The rugosan fauna from the Guanyinqiao Bed(latest Ordovician, Hirnantian) of northernGuizhou, China is known to belong to the coldor cool-water type corals. The components of thefauna are solitary corals only, and corallite septaare generally strongly dilated, especially thestreptelasmatid corals are dominant comprising98% of the whole fauna. The Guanyinqiao Bedis rich in rugosans of 18 genera, which are streptelasmatidStreptelasma (=Helicelasma),107
- Page 2 and 3:
第 4 卷 第 4 期古 生 物 学
- Page 4:
Fossils, i.e. remains of living org
- Page 8 and 9:
nus, a new ichnospecies of Fuersich
- Page 10 and 11:
以 松 柏 类 和 盾 籽 类 为
- Page 12 and 13:
Island, Papua New Guinea. ( 英 文
- Page 14 and 15:
A C. Canadian Journal of Earth Scie
- Page 16 and 17:
mated depositional interval of 10 t
- Page 18 and 19:
北 海 古 近 纪 一 种 新 型
- Page 20 and 21:
scabrate-verrucate, and rugulate mi
- Page 22 and 23:
the Tetori Group in the Kuzuryu are
- Page 24 and 25:
during the Late Pleistocene are rec
- Page 26 and 27:
ane have been previously reported f
- Page 28 and 29:
Albian-early Paleocene in the Anady
- Page 30 and 31:
Poaceae and Plantago lancelata. shr
- Page 32 and 33:
the eastern segment of its southern
- Page 34 and 35:
member of the La Despedida Formatio
- Page 36 and 37:
lembaye (Maastricht region) and fro
- Page 38 and 39:
tion the ontogenetic stage of the p
- Page 40 and 41:
早 期 种 子 植 物2008040123
- Page 42 and 43:
中 国 内 蒙 古 东 北 部 晚
- Page 44 and 45:
2008040137辽 西 北 票 中 侏
- Page 46 and 47:
综 论2008040144低 PH 值 对 Amm
- Page 48 and 49:
ut poorly studied. Dimorphism (or t
- Page 50 and 51:
and migration towards the sediment-
- Page 52 and 53:
schackoinids, indicating that the e
- Page 54 and 55:
( 英 文 ). Nomaki H; Yamaoka A; S
- Page 56 and 57:
新 西 兰 Otago 南 海 岸 全
- Page 58 and 59: Scotland. ( 英 文 ). Murray J W.
- Page 60 and 61: A three-year sediment trap experime
- Page 62 and 63: a habitat disturbance and is nearly
- Page 64 and 65: Pitted surfaces associated with wal
- Page 66 and 67: Saanich than exists today sedimento
- Page 68 and 69: 2008040208大 堡 礁 区 域 绿
- Page 70 and 71: was pulsed, with major declines usu
- Page 72 and 73: mycelium, was observed where reticu
- Page 74 and 75: suggest that reticulopodia are self
- Page 76 and 77: to OIS 3, compared to the more stab
- Page 78 and 79: Patterson R T. Journal of Foraminif
- Page 80 and 81: known xenophyophore species grouped
- Page 82 and 83: aminiferal Research, 2001, 31(4): 2
- Page 84 and 85: arctic environment over this critic
- Page 86 and 87: Semeniuk T A. Journal of Foraminife
- Page 88 and 89: sible to make production calculatio
- Page 90 and 91: arcellacean strains from within the
- Page 92 and 93: annual flux rates is calculated and
- Page 94 and 95: corded in the Colli Berici (type lo
- Page 96 and 97: most complete OAE 2 sections. While
- Page 98 and 99: oceanic plate stratigraphy from gra
- Page 100 and 101: A series of layers rich in organic
- Page 102 and 103: lowermost Danian planktonic foramin
- Page 104 and 105: characters shows that only one geno
- Page 106 and 107: able for regional palaco-environmen
- Page 110 and 111: Brachyelasma, Amplexobrachyelasma,
- Page 112 and 113: litic biozones lower than their FAD
- Page 114 and 115: The middle Permian Cryptospirifer f
- Page 116 and 117: 石 科 = Ammonoid faunas from the
- Page 118 and 119: Buchiid bivalves are geographically
- Page 120 and 121: velopment of both the sedimentary a
- Page 122 and 123: China. ( 英 文 ). Huang Diying; N
- Page 124 and 125: 德 国 南 部 上 侏 罗 统 (Ox
- Page 126 and 127: shelf basin off the northern coast
- Page 128 and 129: like base referred to Primocandelab
- Page 130 and 131: 鱼 类2008040413大 西 洋 鳕
- Page 132 and 133: long as the humerus plus radius, ve
- Page 134 and 135: members in both size and abundance
- Page 136 and 137: ple's Republic of China. ( 英 文
- Page 138 and 139: K-P transition in Brazil. ( 英 文
- Page 140 and 141: wide tooth crowns, a sub-rectangula
- Page 142 and 143: 2008040459罗 马 尼 亚 特 兰
- Page 144 and 145: logical descriptions of all availab
- Page 146 and 147: 东 副 特 提 斯 晚 萨 马 期
- Page 148 and 149: S; Vaiani S C. Rivista Italiana di
- Page 150 and 151: adiocarbon dating the arrival of th
- Page 152 and 153: able problems, particularly differe
- Page 154 and 155: done with glyphs on paper. In this
- Page 156 and 157: obtained through extensive field-ba
- Page 158 and 159:
noli G; Maletz J; Stouge S. Canadia
- Page 160 and 161:
法 国 蒙 塔 格 尼 努 尔 中
- Page 162 and 163:
presence of well-rounded, coarse-sa
- Page 164 and 165:
缅 甸 北 部 Hukawng 峡 谷 琥
- Page 166 and 167:
graphy and Geological Correlation,
- Page 168 and 169:
plex,northwestern Iran. ( 英 文 )
- Page 170 and 171:
松 辽 盆 地 晚 白 垩 世 青
- Page 172 and 173:
ous nannoplankton) points of view.O
- Page 174 and 175:
the"Yanshan Movement".During the Mi
- Page 176 and 177:
geochemical approach discussed in t
- Page 178 and 179:
sediments from the northern shelf o
- Page 180 and 181:
意 大 利 北 亚 平 宁 Lamone
- Page 182 and 183:
nano record further into the early
- Page 184:
lankovitch-scale frequency. Analyse