Skeletal faunas from the Qiongzhusian of southern Shaanxi: biodiversity and lithofacies-biofacies links in the Lower Cambrian carbonate settings
Skeletal faunas from the Qiongzhusian of southern Shaanxi:biodiversity and lithofacies-biofacies links in the Lower Cambrian carbonate settings作者机构:13355 Berlin Ackerstrasse 71~76 Germany Technische Universitt Berlin Sekr.ACK 14
出 版 物:《Progress in Natural Science:Materials International》 (自然科学进展·国际材料(英文))
年 卷 期:2004年第14卷第1期
页 面:92-97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]
基 金:SupportedbytheNationalNaturalScienceFoundationofChina (GrantNos.40 172 0 0 2and 40 2 3 2 020) theMajorStateBasicResearchDevelopmentProgramofChina(GrantNo.G2 0 0 0 0 7770 0) ChineseAcademyofSciences(KZCX2116) andDeutscheForschungsgesellschaft(Er96/3 2 1)
主 题:skeletal fauna Xihaoping Member Shuijingtuo Formation Lower Cambrian Shaanxi
摘 要:The Xiaoyang section, located in Zhenba County of Shaanxi Province, is important both for documenting the biodiversity of the Qiongzhusian Stage (Lower Cambrian) and for analyzing lithofacies biofacies links in carbonate depositing environments on the Yangtze Platform. The skeletal fossils from the Xihaoping Member, including linguloid valves, cambroclavid and chancelloriid sclerites, genal and occipital spines of polymerid trilobites, and tubular fossils, are described here as the Eoobolus Cambroclavus fauna, which mainly occurred in peritidal environments. The fossils from the argillaceous limestones of the lower Shuijingtuo Formation, containing lingulate brachiopods, eodiscoid trilobites, bivalved arthropods, microdictyoniid sclerites and siliceous sponge spicules, are regarded as the Palaeobolus Hupeidiscus Kunmingella fauna, which presumably lived in subtidal or deeper water environments. The faunal diversity in the Xihaoping Member is lower than that in the lower Shuijingtuo Formation. The investigations of the skeletal fossil assemblages from carbonate lithofacies in southern Shaanxi will significantly contribute to a detailed documentation of the biodiversity during the Qiongzhusian interval on the Yangtze Platform and add new knowledge on the Cambrian bioradiation.