贵州安顺长兴阶顶部三叶虫化石TRILOBITE FROM UPPERMOST CHANGHSINGIAN IN ANSHUN,GUIZHOU PROVINCE
冯凡斌,胡庆,冯庆来
摘要(Abstract):
三叶虫是二叠纪末生物集群灭绝中消失的生物门类之一,但是关于该门类生物化石在中国消失的确切层位未见报道。贵州安顺新民剖面大隆组顶部的三叶虫化石Pseudophillipsia sp.产于火山成因的黏土岩之炭质泥岩夹层中,相邻的泥灰岩结核中产牙形石化石Clarkina meishanensis。该黏土岩及炭质泥岩夹层可以与浙江长兴煤山D剖面的第25层对比,这说明三叶虫延续到了主灭绝事件层位,对研究二叠纪末生物集群灭绝的原因具有一定的意义。
关键词(KeyWords): 生物地层;三叶虫;灭绝;晚二叠世;华南
基金项目(Foundation): 国家自然科学基金项目(No.40839903);; “地质过程与矿产资源国家重点实验室”专项经费资助
作者(Author): 冯凡斌,胡庆,冯庆来
DOI: 10.19839/j.cnki.dcxzz.2011.03.009
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