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第 4 卷第 4 期古生物学文摘 ( 网络版 )目录2008 年 12 月古生物学综论 ………………………(1)遗迹化石 …………………(4)分子古生物学 ……………(5)古生态学 …………………(6)微体古生物学综论 ………………………(14)孢粉 ………………………(15)疑源类 ……………………(22)牙形石 ……………………(22)小壳化石 …………………(23)古植物学综论 ………………………(24)藻类 ………………………(27)真菌 ………………………(33)蕨类植物 ( 广义 )………(34)早期种子植物 ……………(36)裸子植物 …………………(38)被子植物 …………………(41)古无脊椎动物学综论 ………………………(42)原生动物 …………………(44)古杯、多孔及腔肠动物 …(105)苔藓动物 …………………(106)腕足动物 …………………(107)软体动物 …………………(111)节肢动物 …………………(116)棘皮动物 …………………(122)笔石动物 …………………(123)分类位置不明 ……………(123)古脊椎动物学综论 ………………………(126)鱼类 ………………………(126)两栖类 ……………………(128)爬行类 ……………………(128)鸟类 ………………………(140)哺乳类 ……………………(141)古人类学古人类学 …………………(145)历史地质学、地层学综论 ………………………(147)古地理学、古气候学 ……(151)前古生界 …………………(151)古生界 ……………………(153)中生界 ……………………(160)新生界 ……………………(171)
第 4 卷第 4 期古生物学文摘 ( 网络版 )2008 年 12 月古生物学综论2008040001动物的最早化石记录及其意义 = The earliestfossil record of the animals and its significance.( 英文 ). Budd1 G E. Philosophical Transactionsof the Royal Society B: Biological Sciences,2008, 363(1496): 1425-1434The fossil record of the earliest animals hasbeen enlivened in recent years by a series ofspectacular discoveries, including embryos, fromthe Ediacaran to the Cambrian, but many issues,not least of dating and interpretation, remaincontroversial. In particular, aspects of taphonomyof the earliest fossils require careful considerationbefore pronouncements about their affinities.Nevertheless, a reasonable case can nowbe made for the extension of the fossil record ofat least basal animals (sponges and perhaps cnidarians)to a period of time significantly beforethe beginning of the Cambrian. The Cambrianexplosion itself still seems to represent the arrivalof the bilaterians, and many new fossils inrecent years have added significant data on theorigin of the three major bilaterian clades. Whyanimals appear so late in the fossil record is stillunclear, but the recent trend to embrace risingoxygen levels as being the proximate cause remainsunproven and may even involve a degreeof circularity2008040002化石记录中全球温度与生物多样性、起源及灭绝之间的长期对应关系 = A long-term associationbetween global temperature and biodiversity,origination and extinction in the fossilrecord. ( 英文 ). Mayhew P J; Jenkins G B; BentonT G. Proceedings of the Royal Society B:Biological Sciences, 2008, 275(1630): 47-53The past relationship between global temperatureand levels of biological diversity is of increasingconcern due to anthropogenic climatewarming. However, no consistent link betweenthese variables has yet been demonstrated. Weanalysed the fossil record for the last 520Myragainst estimates of low latitude sea surfacetemperature for the same period. We found thatglobal biodiversity (the richness of families andgenera) is related to temperature and has beenrelatively low during warm ‘greenhouse’ phases,while during the same phases extinction andorigination rates of taxonomic lineages havebeen relatively high. These findings are consistentfor terrestrial and marine environments andare robust to a number of alternative assumptionsand potential biases. Our results providethe first clear evidence that global climate mayexplain substantial variation in the fossil recordin a simple and consistent manner. Our findingsmay have implications for extinction and biodiversitychange under future climate warming.2008040003地史时期最大规模集群灭绝后的复苏 = Recoveryfrom the most profound mass extinctionof all time. ( 英文 ). Sahney S; Benton M J. Proceedingsof the Royal Society B: Biological Sciences,2008, 275(1636): 759-765The end-Permian mass extinction, 251 millionyears (Myr) ago, was the most devastating ecologicalevent of all time, and it was exacerbatedby two earlier events at the beginning and end ofthe Guadalupian, 270 and 260Myr ago. Ecosystemswere destroyed worldwide, communitieswere restructured and organisms were left strugglingto recover. Disaster taxa, such as Lystrosaurus,insinuated themselves into almost everycorner of the sparsely populated landscape in theearliest Triassic, and a quick taxonomic recoveryapparently occurred on a global scale. However,close study of ecosystem evolution shows thattrue ecological recovery was slower. After theend-Guadalupian event, faunas began rebuildingcomplex trophic structures and refilling guilds,but were hit again by the end-Permian event.Taxonomic diversity at the alpha (community)level did not recover to pre-extinction levels; itreached only a low plateau after each pulse andcontinued low into the Late Triassic. Our datashowed that though there was an initial rise incosmopolitanism after the extinction pulses,large drops subsequently occurred and, counterintuitively,a surprisingly low level of cosmopolitanismwas sustained through the Early andMiddle Triassic.2008040004第七届国际侏罗系大会 (2006 年 9 月 6-18 日于波兰克拉科夫 ) = VII International Congresson the Jurassic System (September 6–18,2006, Krakow, Poland). ( 英文 ). Zakharov V A;Rogov M A. Stratigraphy and Geological Correlation,2007, 15(2): 236-2382008040005时间信息、化石记录和系统发育 = Temporalinformation, fossil record and phylogeny. ( 法文 ).Lelièvre H; Bagils R Z; Rouget I. Comptes RendusPalevol, 2008, 7(1): 27-361
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-
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schackoinids, indicating that the e
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( 英文 ). Nomaki H; Yamaoka A; S
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新西兰 Otago 南海岸全
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Scotland. ( 英文 ). Murray J W.
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A three-year sediment trap experime
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a habitat disturbance and is nearly
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Pitted surfaces associated with wal
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Saanich than exists today sedimento
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2008040208大堡礁区域绿
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was pulsed, with major declines usu
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mycelium, was observed where reticu
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suggest that reticulopodia are self
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to OIS 3, compared to the more stab
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Patterson R T. Journal of Foraminif
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known xenophyophore species grouped
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aminiferal Research, 2001, 31(4): 2
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arctic environment over this critic
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Semeniuk T A. Journal of Foraminife
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sible to make production calculatio
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arcellacean strains from within the
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annual flux rates is calculated and
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corded in the Colli Berici (type lo
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most complete OAE 2 sections. While
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oceanic plate stratigraphy from gra
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A series of layers rich in organic
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lowermost Danian planktonic foramin
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characters shows that only one geno
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able for regional palaco-environmen
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margin of the southwest Caribbean.
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Brachyelasma, Amplexobrachyelasma,
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litic biozones lower than their FAD
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The middle Permian Cryptospirifer f
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石科 = Ammonoid faunas from the
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Buchiid bivalves are geographically
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velopment of both the sedimentary a
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China. ( 英文 ). Huang Diying; N
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德国南部上侏罗统 (Ox
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shelf basin off the northern coast
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like base referred to Primocandelab
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鱼类2008040413大西洋鳕
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long as the humerus plus radius, ve
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members in both size and abundance
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ple's Republic of China. ( 英文
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K-P transition in Brazil. ( 英文
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wide tooth crowns, a sub-rectangula
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2008040459罗马尼亚特兰
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logical descriptions of all availab
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东副特提斯晚萨马期
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S; Vaiani S C. Rivista Italiana di
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adiocarbon dating the arrival of th
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able problems, particularly differe
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done with glyphs on paper. In this
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obtained through extensive field-ba
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noli G; Maletz J; Stouge S. Canadia
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法国蒙塔格尼努尔中
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presence of well-rounded, coarse-sa
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缅甸北部 Hukawng 峡谷琥
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graphy and Geological Correlation,
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plex,northwestern Iran. ( 英文 )
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松辽盆地晚白垩世青
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ous nannoplankton) points of view.O
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the"Yanshan Movement".During the Mi
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geochemical approach discussed in t
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sediments from the northern shelf o
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意大利北亚平宁 Lamone
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nano record further into the early
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lankovitch-scale frequency. Analyse
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