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文 ). Lian O B; Mathewes R W; Hicock S R. Canadian Journal of Earth Sciences, 2001, 38(6): 943-952 New palynological data from peaty sediments deposited during the Port Moody Interstade, at about 18 000 14 C years, indicate that the environment in the western Fraser Lowland of British Columbia consisted of subalpine forest and parkland with abundant fir and spruce that grew under a temperate and moist climate, similar to the wetter subzones of the present-day Engelmann Spruce – Subalpine Fir biogeoclimatic zone. The moist conditions interpreted for the Port Moody Interstade are consistent with recent computer modelling and earlier palynological data from unglaciated western Washington State, but appear to contradict regional Cooperative Holocene Mapping Project (COHMAP) reconstructions and some earlier palaeoenvironmental studies that support dry conditions. Strong seasonality is suggested as part of the explanation, with Pacific storms in summer following the southern margin of the last Cordilleran ice sheet, bringing abundant moisture to the study area during the growing season, but probably not in winter, when storm tracks were displaced to the south. The cold and dry anticyclonic winds postulated by COHMAP were probably also relatively weak in summer, resulting in stronger expression of moist Pacific air masses than previously thought. The timing of the Port Moody Interstade coincides with that of a short climatic fluctuation reported from several other sites in both the northern and southern hemispheres. These events, if causally related, suggest a rapidly propagated atmospheric– oceanic signal. 2009020067 阿根廷圣胡安省 Volcan 山脉泥盆纪 Chigua 组和石炭纪 Maliman 组孢粉 , 第二部分 : 带气囊、假气囊和赤道周壁环带孢子 = Palynology of the Chigua (Devonian) and Maliman (Carboniferous) formations in the Volcan Range, San Juan Province, Argentina. Part II. Cavate, pseudosaccate and cingulizonate spores. ( 法文 ). Amenabar C R; Di Pasquo M; Carrizo H A; Azcuy C L. Ameghiniana, 2007, 44(3): 547-564 Palynological analysis of the Chigua and Maliman formations of Middle Devonian and Mississippian age respectively, is presented. They crop out in the Del Volcan Range at the Rio Blanco Basin in western Argentina. In this second part, 40 indigenous species of cavate, pseudosaccate and cingulizonate spores from both units are illustrated. The species Geminospora sp. cf. G. tuberculata var. tuberculata McGregor is recorded in the Middle Devonian of South America for the first time. The following species are also recorded in the Mississippian of South America for the first time as Crassispora invicta Playford, Densosporites asperus Braman and Hills, Densosporites gracilis Smith and Butterworth, Densosporites secundus Playford and Satterthwait, Densosporites sp. cf. D. triangularis Kosanke, Gorgonispora sp. cf. G. crassa (Winslow) Higgs et al., Lophozonotriletes dentatus Hughes and Playford, Spelaeotriletes echinatus (Hacquebard) Utting, Velamisporites perinatus (Hughes and Playford) Playford. Some possibly reworked species (scolecodonts, paleomicroplankton and spores) from the Maliman Formation are illustrated and some of them are also described 2009020068 俄罗斯 Timan 南部 Balneologicheskaya-1 参照钻孔剖面中吉维特期 - 弗拉期孢粉特征 = Palynological characterization of Givetian- Frasnian deposits in the reference Borehole section 1-Balneologicheskaya (Southern Timan). ( 英文 ). Tel’nova O P. Stratigraphy and Geological Correlation, 2008, 16(2): 143- 161 A succession of seven palynological assemblages characterizing the Yuzhnyi Timan, Taman, Ust-Yarega, Domanik, and Vetlosyan formations of the southern Timan is established in the Givetian-Frasnian deposits recovered by Borehole 1-Balneologicheskaya and studied in detail. Five individual zones, which are distinguished within stratigraphic range of the optivus-krestovnicovii miospore zone, can be of basic importance for a highresolution stratigraphic subdivision of the sedimentation stage under consideration. Phytostratigraphic boundary corresponding to the Frasnian Stage base in the East European platform is substantiated in palynological aspect. 2009020069 美国阿拉巴马州和密西西比州古新世 - 始新世 paratropical 沼泽和边缘海花粉植物群的对比 = Comparisons between Palaeocene– Eocene paratropical swamp and marginal marine pollen floras from Alabama and 22
Mississippi, USA. ( 英文 ). Harrington G J. Palaeontology, 2008, 51(3): 611-622 Climate warming at the Palaeocene/Eocene boundary (c. 55.8 Ma) had significant permanent affects on paratropical and warmadapted vegetation types. Pollen and spore records which document vegetation turnover from the eastern US Gulf Coast have all been taken from sediments of marginal marine depositional environments. Pollen and spores (sporomorphs) are preserved excellently in these marginal marine depositional environments but these assemblages contain grains transported from many different vegetation types and over huge geographic distances. Currently it is unclear whether the turnover from important paratropical areas like the US Gulf Coast is a reflection on actual vegetation change in the local region or from source areas far away in the continental interior. Sporomorph data from 20 former swamps (lignites) from the Nanafalia, Tuscahoma and Hatchetigbee formations in Mississippi and Alabama, USA, are used to test the fidelity of the marine sporomorph record across the Palaeocene – Eocene transition. Data show that extinction is noted in the swamp record ( ≥ 7 per cent of Palaeocene taxa) and that swamps were susceptible to immigration in the Early Eocene with the first occurrences of Brosipollis spp. (Burseraceae), Dicolpopollis spp. (Palmae), Nuxpollenites psilatus (Loranthaceae) and Platycarya spp. (Juglandaceae). Swamps have higher withinsample diversity in the Eocene but higher among-sample diversity in latest Palaeocene–earliest Eocene samples, which parallels exactly diversity trends estimated from marine sporomorph assemblages. Palms also increase in abundance in the Eocene. The swamp data demonstrate that the flora growing in these ancient paratropical forests was diverse (c. 120 taxonomic groups) but incorporated an unusual admixture of plants with modern tropical affinities together with those that now live in modern temperate to subtropical North America. 2009020070 俄罗斯加里宁格勒地区 Sambian 半岛西部上白垩统和古近纪沉积的孢粉特征 , 第一部分 = Palynological characteristics of Upper Cretaceous and Paleogene deposits on the west of the Sambian Peninsula (Kaliningrad region), Part 1. ( 英文 ). Aleksandrova G A; Zaporozhets N I. Stratigraphy and Geological Correlation, 2008, 16(3): 295-316 The results of studying dinocysts in the Upper Cretaceous-Lower Paleogene succession of the Kaliningrad region are considered. Distinguished in the succession are seven biostratigraphic units in the rank of the Palaeohystrichophora infusorioides, Chatangiella vnigrii, Cerodinium diebelii, Alisocysta margarita, Deflandrea oebisfeldensis, Areosphaeridium diktyoplokum, and Rhombodinium perforatum beds and one Charlesdowniea clathrata angulosa Zone. 2009020071 阿根廷布宜诺斯艾利斯省南方山脉宾夕法尼亚期 - 乌拉尔世 Sauce Grande 组的首次孢粉记录 = The first palynological record of the Sauce Grande Formation (Pennsylvanian- Cisuralian) at the Australes range, Buenos Aires Province, Argentine. ( 其他 ). Di Pasquo M; Martinez MA; Freije H. Ameghiniana, 2008, 45(1): 69-81 The first palynological assemblage recovered from a sample of the Middle Member of the Sauce Grande Formation is presented. Palynomorphs are small (among 20 mu m - 50 mu m) and poorly preserved. Exines are fragmented, highly carbonized (dark gray or black in colour) and affected by framboidal pyrite. Eleven species of palynomorphs are described and illustrated: nine trilete spores (Apiculiretusispora sp., Cyclogranisporites sp., Granulatisporites austroamericanus Archangelsky and Gamerro, Lophotriletes sp., Horriditriletes sp. cf. H. gondwanensis (Tiwari and Moiz) Foster, Horriditriletes sp. cf. H. ramosus (Balme and Hennelly) Bharadwaj and Salujha, Raistrickia sp., Lundbladispora sp., Cristatisporites sp.), one pollen grain and one acritarch. The assemblage is referred to the Late Pennsylvanian -Cisuralian based on the stratigraphic range of the species recognized that additionally are widely distributed in Gondwana (e.g., Chacoparana, Parana, Paganzo, Karroo). The dominance of spores, and the presence of framboidal pyrite and an acritarch suggest a marine littoral palaeoenvironment for the assemblage. 2009020072 阿根廷圣克鲁斯省下白垩统 Punta del Barco 组的孢粉研究 — 系统描述 I: 单缝孢、光面孢和具环三缝孢 = Palynological study of the Punta del Barco Formation, 23
Page 2 and 3: 第 5 卷第 2 期古生物学
Page 4 and 5: calcite in 38% sulphuric acid. The
Page 6 and 7: 2009020010 细胞过度生长
Page 8 and 9: edistribution of continents, orogen
Page 10 and 11: Turner E C; Burdige D J. Geology, 2
Page 12 and 13: 遗迹化石 2009020028 美国
Page 14 and 15: trackways from Fumanya (south-east
Page 16 and 17: 华盛顿奥林匹克半岛
Page 18 and 19: sequenced and analysed the genome o
Page 20 and 21: estuarine sediments: Chezzetcook In
Page 22 and 23: preserved in the gypsum crystals of
Page 26 and 27: Lower Cretaceous of Santa Cruz prov
Page 28 and 29: sediments of the Zhuravka and Abros
Page 30 and 31: Flores Formation is exposed along t
Page 32 and 33: egion in Late Permian times was pro
Page 34 and 35: Chlorogloeaopsis contexta, Obruchev
Page 36 and 37: deposition of organic-rich, low-oxy
Page 38 and 39: 东攀剖面二叠纪末期
Page 40 and 41: econcile with Ediacaran trace and b
Page 42 and 43: 2009020121 中国西北兰州
Page 44 and 45: Paleontologica Argentina, 2008, 45(
Page 46 and 47: 始新世至中始新世早
Page 48 and 49: assemblage is highly dominated by m
Page 50 and 51: Creek Limestone of the Molong High.
Page 52 and 53: 木属的 3 个同名 Cyclostig
Page 54 and 55: Ceratopteris are from the Eocene of
Page 56 and 57: covering of the spore mass. Ultrast
Page 58 and 59: Southern Floristic Province. It imp
Page 60 and 61: An anatomically preserved mature st
Page 62 and 63: and predation between the two ocean
Page 64 and 65: endemic or Andean forms and others
Page 66 and 67: islands" (Taylor and Wilson, 2003)
Page 68 and 69: analysis, SHE Community Structure I
Page 70 and 71: 2009020208 安第斯火地岛
Page 72 and 73: Miolepidocyclina, Nephrolepidina, E
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alaskensis n. gen. and sp., Virgula
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y the fissispongiid Fissispongia ja
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to a revival of Kiderlen's (1937) h
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gentle and slow extinction speed an
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Two new bryozoan species are descri
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onset of Lopingian recovery/radiati
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ut also found in the paterinates. I
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is reinstated as the reference for
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three species are widespread in the
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Caenogastropoda displayed considera
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Western Canada Province of the Old
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originally referred to Cypraea cont
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the Late Triassic mass extinction b
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of septal folding is still, however
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subspecies originally referred to a
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persisting in the Dry Valleys until
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Great Estuarine Group (Jurassic) of
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have been extended as a result of t
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Otekaike Limestone an inner shelf e
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arthropods (Notostraca and Insecta:
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with a lichenocrinid holdfast, and
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Gotland, in Homerian (upper Wenlock
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terms of growth and development. Gr
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characterises the genus Ditrupa and
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Middle-Late Devonian. A new onychod
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hachirhinchus. Here, we describe ne
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segmented pectoral fin. The small u
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两栖类离片椎类中褶
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南非卡洛下三叠统 Kat
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Formation (Lower - Middle Campanian
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traits evolved in Theropoda. Our re
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2009020428 联合王国威尔
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vestigial or absent 'A' horn-cores,
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anterior dorsal vertebrae and proba
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2009020449 谢佩岛下始新
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Ka BP. Canids in this assemblage in
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collaboration avec le regrett é Pr
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Eucyon remains from the Pliocene Ar
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Megatheriidae) from the Arroyo Chas
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The trilophodont gomphothere group
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oldest representative of Eobaatar i
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ugose, almost spongy aspect; suture
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Neues Jahrbuch fur Geologie u. Pala
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ca 500 kyr toward the precessional
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subdivided in detail in Russia shou
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sediments were deposited in an intr
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Group 1 gneiss-migmatitic rocks (ca
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and implies that these two continen
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1.6 Ma, that is to say, the isotopi
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millipede remains. A review of the
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Kimmeridgian-early Tithonian, Titho
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2009020548 藏东南特提斯
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events and their induced harsh envi
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esearchers, here we suggest that th
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adjacent paleosols that differ in t
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generally consistent northeast tren
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Palaeoclimatology Palaeoecology, 20
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stratigraphic context. Nevertheless
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esponsible for fossil orientation:
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sulfide assemblages in them, of Cen
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south of the island. The occurrence
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ecords in the Jiuquan Basin, northw
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Myr younger than hitherto considere
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