The middle Permian Cryptospirifer fauna(brachiopod) has hitherto been found in morethan 30 localities in the Yangtze Platform,SouthChina.Examination of data from various localitiesshows that it occurs stratigraphically in threeintervals in the range from the upper Kungurianto Wordian.In the Baoshan block in westernYunnan the fauna occurs in the basal part of theDaaozi Formation and is of possibly an earlyWordian age.Outside China the Cryptospiriferfauna has been reported from central and northwestI...2008040352智 利 北 部 科 顿 迪 里 拉 奥 陶 纪 腕 足 动 物 和 笔 石的 首 次 记 录 = First record of Ordovicianbrachiopods and graptolites from Cordon de Lila(Puna de Atacama),Northern Chile. ( 英 文 ).Benedetto J L; Niemeyer H; Gonzalez J; BrussaE D. Ameghiniana, 2008, 45(1): 3-12Brachiopods and graptolites are reported forthe first time from the Quebrada Grande Formationexposed at Cordon de Lila, south of theSalar de Atacama. The stratigraphic succession,over 1000m thick, consists of conglomeratesinterbedded with sandstones and shales. Thecalcareous microconglomerates and calcareniteslaying near the base of the unit have yielded thebrachiopods Paralenorthis sp., Monorthis transversaBenedetto, and Mollesella? sp. The threetaxa have been recorded elsewhere in the Sierrade Famatina, western Argentina, from beds ofwell-constrained Arenig age (O.. evae -B. navisconodont zones). The graptolite fauna recoveredc. 300 m above the brachiopod levels consists ofTetragraptus sp. and Cryptograptus? sp., suggestinga Yapeenian-early Darriwilian age (approximatelylate Arenig-early Llanvirn of theBritish Series). This discovery is significant as itconstitutes the westernmost occurrence of Ordovicianmarine faunas in the Argentine-ChileanPuna region, and supports a paleogeographicconnection between the western Puna Basin andthe Famatina volcaniclastic belt.软 体 动 物2008040353种 - 属 比 率 反 映 海 洋 双 壳 类 范 围 扩 张 和 生 物 多样 性 的 全 球 历 史 = Species–genus ratios reflecta global history of diversification and range expansionin marine bivalves. ( 英 文 ). Krug A Z;Jablonski D; Valentine J W. Proceedings of theRoyal Society B: Biological Sciences, 2008,275(1639): 1117-1123The distribution of marine bivalve speciesamong genera and higher taxa takes the form ofthe classic hollow curve, wherein few lineagesare species rich and many are species poor. Thedistribution of species among genera (S/G ratio)varies with latitude, with temperate S/G's fallingwithin the null expectation, and tropical and polarS/G's exceeding it. Here, we test several hypothesesfor this polar overdominance in thespecies richness of small numbers of genera. Wefind a significant positive correlation betweenthe latitudinal range of a genus and its speciesrichness, both globally and within regions. Genusage and species richness are also positivelyrelated, but this relationship breaks down whenthe analysis is limited to genera endemic to climatezones or with narrow latitudinal ranges.The data suggest a link between speciation andrange-expansion, with genera expanding out ofthe tropical latitudinal bins tending to speciatemore prolifically, both globally and regionally.These genera contain more species within climatezones than taxa endemic to that zone.Range expansion thus appears to be fundamentallycoupled with speciation, producing theskewed distribution of species among genera,both globally and regionally, whereas clade longevityis achieved through extinction—resistance conferred by broad geographicalranges2008040354克 里 米 亚 山 Berriasian 期 菊 石 亚 纲 新 考 米 菊石 科 Malbosiceras 属 和 Pomeliceras 属 的 代表 = Representatives of genera Malbosiceras andPomeliceras (Neocomitidae, Ammonoidea) fromthe Berriasian of the Crimean Mountains. ( 英 文 ).Arkad’ev V V; Bogdanova T N; Lysenko N I.Stratigraphy and Geological Correlation, 2007,15(3): 277-296The revised representatives of ammonite generaMalbosiceras and Pomeliceras from the Berriasianof the Crimean Mountains are classedwith seven species, four of the first genus [M.malbosi (Pictet), M. chaperi (Pictet), M. broussei(Mazenot), M. pictetiforme Tavera] and three ofthe second one [P. aff. boisseti Nikolov, P. breveti(Pomel), P. (?) funduklense Lysenko etArkadiev sp. nov.]. The identified species aredescribed. The genus Mazenoticeras is consideredas synonym of Malbosiceras. The abovespecies prove that all the Berriasian zones(jacobi, occitanica and boissieri) are characteristicof corresponding deposits in the CrimeanMountains.2008040355克 里 米 亚 山 Berriasian 阶 上 带 标 志 菊 石 化 石Fauriella boissieri = Ammonite Fauriella boissieri(Pictet), the index species of the Berriasianupper zone from the Crimean Mountains. ( 英 文 ).Arkad’ev V V. Stratigraphy and GeologicalCorrelation, 2007, 15(2): 185-192112
Ammonite Fauriella boissieri (Pictet), theindex species of the Berriasian upper zone, isdescribed for the first time as taxon occurring inthe Crimean Mountains. In the Berriasian sectionsof the central Crimea and Chatyr-Dag massif,species F. boissieri are encountered only inassociation with upper Berriasian ammonites.The Berriasian-Valanginian boundary has notbeen identified based on ammonites in the CrimeanMountains. Consequently, there is no reasonto include the otopeta Zone into the boissieriZone in the rank of its upper subzone.2008040356俄 罗 斯 中 部 下 白 垩 统 Ryazanian 阶 底 层 菊 石组 合 = Ammonite assemblages from basal layersof the Ryazanian Stage (Lower Cretaceous)of Central Russia. ( 英 文 ). Mitta V V. Stratigraphyand Geological Correlation, 2007, 15(2):193-205Five successive ammonite assemblages aredistinguished in the basal part (Riasanitesrjasanensis Zone s. l.) of the Ryazanian Stage ofthe East European platform. These are (from thebase upward) (1) Hectoroceras tolijense; (2)Hectoroceras kochi; (3) Riasanites swistowianus;(4) Riasanites rjasanensis; and (5) Transcaspiitestransfigurabilis assemblages. Twolower assemblages consist entirely of boreal taxa,which occur in association with diverse ammonitesof the Tethyan origin higher in the section.The data obtained show that three upper assemblagesare correlative with the Berriasian Dalmasicerastauricum, Riasanites rjasanensis-Spiticeras cautleyi, and Euthymiceras euthymisubzones of the northern Caucasus. The successionof five–six ammonite assemblages establishedin the East European platform above thetop of the Craspedites nodiger Zone may correspondto the same number of ammonite assemblagescharacterizing lower subzones of thestandard Berriasian. Berriasella rulevae Mitta,sp. nov. from the upper part of the Riasanitesrjasanensis Zone (transfigurabilis biohorizon) isdescribed.2008040357对 中 古 生 代 游 泳 生 物 的 不 成 功 捕 食 : 泥 盆 纪dacryoconarid 竹 节 石 的 壳 体 损 伤 和 异 常 情 况= Unsuccessful predation on Middle Paleozoicplankton: Shell injury and anomalies in Devoniandacryoconarid tentaculites. ( 英 文 ). BerkyovaS; Fryda J; Lukes P. Acta palaeontologicaPolonica, 2007, 52(2): 407-412Anomalous development of shell ornamentationand repaired shell injury in the Early Devoniandacryoconarid tentaculites are documentedand interpreted as either a repaired injury of theshell, or as a result of an anomalous function ofthe mantle, caused by injury of the soft body.The manner of shell repair, which resembles theway that some modern marine animals, such asmollusks, repair their shells, is discussed. Theissue of phylogenetic affinities of tentaculiteshas been also outlined. These findings representthe first documentation of unsuccessful predationon the Middle Paleozoic plankton.2008040358中 侏 罗 世 菊 石 的 灭 绝 模 式 、 假 灭 绝 和 分 布 :专 业 术 语 = Modes of extinction, pseudoextinctionand distribution in Middle Jurassicammonites: terminology. ( 英 文 ). Westermann GE. Canadian Journal of Earth Sciences, 2001,38(2): 187-195Mid-Jurassic Ammonitina (Cephalopoda,Mollusca) provide good examples of true andapparent "extinctions" (i.e., taxon or clade disappearances)at the local, regional, and globalscales. A terminology is presented. Extinction isthe termination of a phylogenetic lineage or entireclade (not of local demes or regional populations).Extinction was often preceded by progressiverange contraction that resulted in diachronousregional disappearance ("extirpation")and occurred with the elimination of the last refuge.Other range contractions, however, werenot terminal, but were followed by renewed expansions,resulting in temporary absence of thelineage over part of its known range only, due topseudo-extinction. Some lineages, called Lazarustaxa, apparently disappeared entirely forshort or extended periods by pseudotermination(causing a "phylogenetic hiatus"). This is an extremeform of pseudo-extinction with unknownrefuge due to small size and (or) unsuitable faciesand location. Lineage or clade reappearancemay be in the form of new species, whose relationshipto ancestral taxa has been problematic.Some disappearances can be explained with displacivecompetition, where the replacementtaxon is either of endemic origin or an immigrant.Recent research in previously underexploredfield areas has closed some of the gaps ofdocumentation by finding the refuges. Rangecontractions and expansions, together with theirregional disappearances and pseudo-extinctions,including pseudotermination, were often causallyrelated to sea-level changes, especiallyeustasy. Most true extinctions, however, cannotbe identified precisely, because they occurred insmall populations and (or) refuges. Extinctionspresumably did not coincide with global geoevents.2008040359加 拿 大 艾 伯 塔 上 白 垩 统 土 仑 阶 - 康 尼 亚 克 阶Cardium 组 和 相 邻 单 位 菊 石 动 物 群 :I. 船 菊113
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第 4 卷 第 4 期古 生 物 学
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Fossils, i.e. remains of living org
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nus, a new ichnospecies of Fuersich
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以 松 柏 类 和 盾 籽 类 为
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Island, Papua New Guinea. ( 英 文
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A C. Canadian Journal of Earth Scie
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mated depositional interval of 10 t
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北 海 古 近 纪 一 种 新 型
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scabrate-verrucate, and rugulate mi
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the Tetori Group in the Kuzuryu are
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during the Late Pleistocene are rec
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ane have been previously reported f
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Albian-early Paleocene in the Anady
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Poaceae and Plantago lancelata. shr
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the eastern segment of its southern
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member of the La Despedida Formatio
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lembaye (Maastricht region) and fro
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tion the ontogenetic stage of the p
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早 期 种 子 植 物2008040123
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中 国 内 蒙 古 东 北 部 晚
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2008040137辽 西 北 票 中 侏
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综 论2008040144低 PH 值 对 Amm
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ut poorly studied. Dimorphism (or t
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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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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