litic biozones lower than their FAD in shallowerwater facies on the Yangtze Platform. Later inthe late Floian, these genera became major componentsof the Sinorthis fauna that flourishedover much of the Yangtze Platform, suggesting amigration of the benthic shelly fauna from slopeto platform facies during the Floian radiation inSouth China. Compared to the platform fauna,the deep-water brachiopod fauna of the Sanduarea has a lower level of richness, diversity, andcommunity organization. Three brachiopod associationsare recognized: the Paralenorthis-Nereidella, the Palaeoglossa longa, and the Lingulella-Protoskenidioidesassociations. An upsectiondecrease in shell size, faunal richness,and species diversity in the Tonggao Formationindicate a deteriorating environment towardshypersalinity in the Sandu area, resulting in theultimate disappearance of the deep-waterbrachiopod fauna.2008040343环 境 对 加 拿 大 东 部 安 提 库 斯 塔 岛 早 志 留 世 五房 贝 腕 足 动 物 群 落 时 空 变 化 的 控 制 = Environmentalcontrol on temporal and spatial differentiationof Early Silurian pentameride brachiopodcommunities, Anticosti Island, eastern Canada.( 英 文 ). Jin Jisuo. Canadian Journal ofEarth Sciences, 2008, 45(2): 159-187The Early Silurian carbonate succession ofAnticosti Island, eastern Canada, contains a richand diverse pentameride brachiopod fauna. Multivariateanalyses of 91 samples (total 17 230specimens) confirm a high degree of temporalsegregation but only moderate spatial differentiationof the Virgiana, Pentamerus, Stricklandia,Ehlersella, Microcardinalia, and Clorindacommunities. Most pentameride communitiesshow a wider range of water depth than previouslybelieved. The V. barrandei Communityoccupied a substrate setting from lower BA2 toupper BA3, whereas the V. mayvillensis Communitylived mainly in BA4. The P. oblongusCommunity preferred a BA3 setting, comparableto the classic Pentamerus Community, but the P.palaformis Community was predominantly BA4.The stricklandiid communities have a high βdiversity, dominated by various species ofStricklandia, Ehlersella, Microcardinalia, andKulumbella, and occurred most commonly inBA4, but could extend to BA3 environments.The Clorinda Community of Anticosti Islandpreferred deep and quiet water settings, comparableto its widely accepted BA5 assignmentelsewhere. At the generic level, the Virgiana,Pentamerus, and the stricklandiid communitieshave a largely overlapping BA range, but a clearstratigraphical separation. Thus, their temporalalternations were not likely controlled by waterdepth, water turbulence, or substrate conditions,but by fluctuating ocean water temperature, assuggested by chemostratigraphical and paleobiogeographicalevidence.2008040344加 拿 大 东 部 安 提 库 斯 塔 岛 早 志 留 世 兰 多 维 列统 正 形 贝 腕 足 动 物 组 合 = Llandovery (EarlySilurian) orthide brachiopod associations fromAnticosti Island, eastern Canada. ( 英 文 ). LiRong-Yu; Allen T. Canadian Journal of EarthSciences, 2008, 45(2): 189-201Five Llandovery orthide brachiopod associations,through cluster analysis, are delineated onAnticosti Island. The Levenea-Dicoelosia Association(A), occurring in the Goéland andRichardson members of the lower Jupiter Formation,represents a deep-water setting aroundor below the maximum storm wave base. TheFlabellitesia-Dalejina Association (B), appearingin the Cybèle, Ferrum, and Pavillon membersof the upper Jupiter Formation, indicateswater depth in between the maximum and normalstorm wave bases. The Isorthis (Ovalella)Association (C 1 ), present in the Fox Point Memberof Becscie Formation, corresponds to theshallower water setting around the normal stormwave base. The Mendacella bleikeriensis Association(C 2 ), occurring in the Innommée, Sandtop,and Macgilvray members of Gun RiverFormation, characterizes the water depth slightlybelow the normal storm wave base. The Mendacellaudauberis Association (D), appearing inthe Merrimack Formation, signifies a waterdepth around the maximum storm wave base.The water depth indication of these associationsmay bear potential as future reference for otherregions, but attention should be paid to the specieslevel as some congeneric species can belongto different associations of different depth. Thecluster analysis on orthide collections based onbinary data demonstrates that statistical methods,Jaccard coefficient and Ward's method of clustering,are practical and effective to delineatelarge brachiopod collections on Anticosti Island.2008040345华 南 早 三 叠 世 腕 足 动 物 舌 形 贝 类 新 属 和 新 种= New Early Triassic Lingulidae (Brachiopoda)genera and species from South China. ( 英 文 ).Peng Yuanqiao; Shi Guangrong. Alcheringa,2008, 32(2): 149 - 170Two new genera, Sinolingularia gen. nov. andSinoglottidia gen. nov., together with three newspecies, Sinolingularia huananensis gen. et sp.nov., Sinolingularia yini gen. et sp. nov. andSinoglottidia archboldi gen. et sp. nov., are describedon the basis of a large collection of wellpreservedspecimens from several sectionsstraddling the Permian - Triassic boundary inSouth China.110
2008040346腕 足 动 物 Yingtangella 属 和 Rhipidothyris 属之 间 的 亲 缘 关 系 = The relationship between thebrachiopod genera Yingtangella Bai & Ying,1978 and Rhipidothyris Cooper & Williams,1935. ( 英 文 ). Chen Xiuqin; Qiao Li. Alcheringa,2008, 32(2): 191 - 198The brachiopod genus Yingtangella Bai &Ying, 1978 from the early Middle Devonian(Eifelian) of Guangxi, China, was originally assignedto the Rhynchonellida. An examination oftopotype material indicates that it is a terebratulidand a junior synonym of Rhipidothyris Cooper& Williams, 19352008040347Mummpikia ( 新 属 , 新 种 ) 及 方 解 石 壳 体 腕足 类 的 起 源 = Mummpikia gen. nov. and theorigin of calcitic-shelled brachiopods. ( 英 文 ).Balthasar U. Palaeontology, 2008, 51(2): 263-279Phosphatised limestone-hosted and shalehostedspecimens of the obolellid Mummpikianuda gen. et comb. nov. and two further unidentifiedobolellids from the Early Cambrian MuralFormation (Jasper National Park, CanadianRocky Mountains) provide novel insights intothe shell microstructure of obolellids and thenature of their pedicle. The shell was penetratedby abundant canals of a sub-μm diameter and theanterior tip of the delthyrium forms a projectioninto the body cavity that is penetrated by a thincanal. It is argued that both shell microstructureand posterior margin are linguliformean charactersand that obolellids hold a position basal inthe rhynchonelliform stem-group.2008040348浙 江 省 ( 中 国 东 南 地 区 ) 西 部 淳 安 晚 奥 陶 世Katian 期 晚 期 长 武 组 扭 月 贝 科 腕 足 类 = StrophomenideBrachiopods from the ChangwuFormation (Late Katian, Late Ordovician) ofChun'an, Western Zhejiang, South-East China.( 英 文 ). Zhan Renbin; Jin Jisuo; Rong Jiayu;Chen Pengfei; Yu Guohua. Palaeontology, 2008,51(3): 737-766Late Ordovician strophomenide brachiopods(superfamilies Strophomenoidea and Plectambonitoidea)from the upper Changwu Formation(mid Ashgill, late Katian) of Jianglütang,Chun'an County, western Zhejiang Province,consist of ten genera and 12 species. Five newspecies of three new genera are recognized:Chunanomena triporcata, Chunanomena sembellina,Cheramomena subsolana, Lateriseptomenamodesta, and Lateriseptomena rugosa. The strophomenidebrachiopods from the upper Katianstrata described in this study and those from theborder region of Zhejiang and Jiangxi provincesreported in previous work contain 16 strophomenoidand 12 plectambonitoid genera, andmost of the strophomenoids are endemic toSouth China. Numerical analysis of welldocumentedlate Katian strophomenide brachiopodfaunas indicates a strong provincialism,characterized by the highly distinct NorthAmerican province (Laurentia), the SouthChina-Kazakhstan province, and the Avalonia-Baltica province (Wales, Belgium and Sweden).Surprisingly, the Girvan district of Scotland,which was a peri-Laurentian terrane during theOrdovician, contains a late Katian brachiopodfauna that is more closely related to the contemporaneousbrachiopods of Avalonia-Baltica thanto those of North America.2008040349华 南 早 三 叠 世 腕 足 动 物 舌 形 贝 科 新 属 种 =New Early Triassic Lingulidae (Brachiopoda)genera and species from South China. ( 英 文 ).Peng Yuanqiao; Shi Guangrong. Alcheringa,2008, 32(2): 149 - 170Two new genera, Sinolingularia gen. nov. andSinoglottidia gen. nov., together with three newspecies, Sinolingularia huananensis gen. et sp.nov., Sinolingularia yini gen. et sp. nov. andSinoglottidia archboldi gen. et sp. nov., are describedon the basis of a large collection of wellpreservedspecimens from several sectionsstraddling the Permian - Triassic boundary inSouth China.2008040350腕 足 动 物 Yingtangella 属 和 Rhipidothyris 属之 间 的 亲 缘 关 系 = The relationship between thebrachiopod genera Yingtangella Bai & Ying,1978 and Rhipidothyris Cooper & Williams,1935. ( 英 文 ). Chen Xiuqin; Qiao Li. Alcheringa,2008, 32(2): 191 - 198The brachiopod genus Yingtangella Bai &Ying, 1978 from the early Middle Devonian(Eifelian) of Guangxi, China, was originally assignedto the Rhynchonellida. An examination oftopotype material indicates that it is a terebratulidand a junior synonym of Rhipidothyris Cooper& Williams, 1935.2008040351古 地 中 海 地 区 隐 石 燕 动 物 群 ( 中 二 叠 世 腕 足类 ) 在 空 间 和 时 间 上 的 分 布 及 其 古 地 理 意 义= Spatial and Temporal Distribution of theCryptospirifer Fauna(Middle Permian Brachiopods)in the Tethyan Realm and Its PaleogeographicImplications. ( 英 文 ). Jin Xiaochi;Zhan Lipei. Acta Geologica Sinica, 2008, 82(1):1-16111
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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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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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lankovitch-scale frequency. Analyse