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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2008-02
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Microbialites in the Middle Cambrian Qinjiamiao Group in Xingshan,Hubei Province:Implication for Paleoenvironmental Reconstruction

DANG Haowen 1,3,LIU Jianbo 1,2,YUAN Xinpeng1 1School of Earth and Space Sciences,Peking University,Beijing 100871;2Key Laboratory of Orogenic Belts and Crustal Evolution,Ministry of Education,Beijing 100871;3School of Ocean and Earth Sciences,Tongji University,Shanghai 200092  
Abundant microbialites,from the Middle Cambrian Qinjiamiao Group in the Gudongkou section near Xingshan County of Hubei Province,south China,were studied and described in detail by macro-and microscopic observations.The microbialites in the Qinjiamiao Group consist of a great amount of stromatolites and minor thrombolites,and contain some distinguishable filamentous fossils of Girvanella.The relationship between Girvanella filaments and sediment particles strongly suggests that the microbialites in the Qinjiamiao Group were formed by microbial mats trapping and binding of carbonate sediment and the calcification of Girvanella filaments.The detailed morphology and structure of the microbialites as well as sedimentary features in the Qinjiamiao Group argue that the microbialites were deposited in deep to shallow subtidal settings.The Middle Cambrian Microbialites Resurgence Event,distinguished from the Qinjiamiao Group in Yangtze Platform and elsewhere in the world,might be controlled by virtually barren of metazoan,and could be recognized as a performance of the unique stutter-step transitional interval from Proterozoic stromatolitic-thrombolitic reefs to Phanerozoic metazoan-dominated reefs.
【Fund】: 国家重点基础研究发展计划(2006CB806402 G200077700);; 国家自然科学基金(49902003 40472008)资助项目
【CateGory Index】: Q913
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