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Evolution and paleogeography of Eospirifer(Spiriferida,Brachiopoda) in Late Ordovician and Silurian

Evolution and paleogeography of Eospirifer(Spiriferida,Brachiopoda) in Late Ordovician and Silurian

作     者:ZHAN RenBin JIN JiSuo LIANG Yan MENG LingKai 

作者机构:State Key Laboratory of Palaeobiology and StratigraphyNanjing Institute of Geology and PalaeontologyChinese Academy of SciencesNanjing 210008China Department of Earth SciencesUniversity of Western OntarioLondonON N6A 5B7Canada 

出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))

年 卷 期:2012年第55卷第9期

页      面:1427-1444页

核心收录:

学科分类:070903[理学-古生物学与地层学(含:古人类学)] 0709[理学-地质学] 07[理学] 0708[理学-地球物理学] 0704[理学-天文学] 

基  金:supported by Chinese Academy of Sciences (Grant No. KZCX2-YW-Q05-01) National Natural Science Foundation of China(Grant No. 40825006) the CAS/SAFEA International Partnership Program for Creative Research Teams and the State Key Laboratory of Paleobiology and Stratigraphy 

主  题:古地理环境 腕足动物门 奥陶系 志留系 物种多样性 演化 宏观进化 中国南方 

摘      要:Eospirifer,the oldest known genus of the spiriferide group(Brachiopoda),first appeared on the Zhe-Gan Platform of South China paleoplate during late Katian(Late Ordovician) represented by *** survived the end-Ordovician mass extinction,and reappeared on the Upper Yangtze Platform of South China paleoplate by the end of Ordovician near the upper part of the Normalograptus persculptus *** from the beginning of Silurian,Eospirifer experienced some morphological innovations and expanded its geographical distribution *** reached its species diversity acme and the widest geographic distribution in Wenlock(middle Silurian),with the diversity hotspots in Laurentia,Avalonia,and *** shell size frequency curves of *** under different paleogeographic settings suggest that this pioneer species of Eospirifer,with several macroevolutionary novelties,adopted a range of life strategies to adapt to the changing environments during early spiriferide *** are also some morphological macroevolutionary trends during the evolutionary history of Eospirifer from Late Ordovician to the end of Silurian,such as the ever enlarging shell sizes and the width/length ratios from late Katian to Wenlock,but decreasing apparently of both parameters from Wenlock to Pridoli.

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