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《Acta Scientiarum Naturalium Universitatis Pekinensis》 2008-02
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Lower Ordovician Reefs in the Honghuayuan Formation at Dongzhi,Anhui:Microbial Reefs Just Prior to the Ordovician Biodiversification

CAO Jun1,LIU Jianbo 1,2,EZAKI Yoichi3,ADACHI Natsuko4 1School of Earth and Space Sciences,Peking University,Beijing 100871;2Key Laboratory of Orogenic Belts and Crustal Evolution,Ministry of Education,Beijing 100871;3Department of Geosciences,Osaka City University,Osaka 558-8585;4Japan Society for the Promotion of Science Fellow/Department of Geology,Miyagi University of Education,Miyagi 980-0845  
Morphological and ecological diversity of organisms increased during the global Great Biodiversification Event from the late Early Ordovician.Those changes were accompanied with a marked declines in microbial reefs in the subtidal settings.The reefs were built by benthic microbes,Calathium,and lithistid sponges in the middle Early Ordovician Honghuayuan Formation of Jianxin,Anhui Province.The reefs exhibit three main rock types:1)massive skeletal grainstones,2)lithistid sponge Calathium-microbial bindstones,and 3)microbial boundstones.Girvanella,one of representative calcimicrobes,is classified into four categories in the reefs:1)dispersed,2)encrusting,3)forming into intraclasts,and 4)infilling within sponges.These types of Girvanella play a significant frame-building role in the Calathium/lithistid sponge-microbial reefs of the Honghuayuan Formation.Such kind of microbial reefs commonly occur in the Yangtze Platform and elsewhere in the world just prior to the first acme of the Ordovician biodiversification.Metazoan competitions with microbes might be closely related to marked declines in microbial sediments decline after the deposition of the microbial reefs of the Honghuayuan Formation.
【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);; 日本科学促进会科学研究基金(17540444);; 日本学术振兴会特别研究员奖励费资助项目
【CateGory Index】: Q913
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