王成源,王平,杨光华,谢伟

• 1:中国科学院南京地质古生物研究所
• 2:长安大学地球科学与国土资源学院

摘要(Abstract)：

首次在稗子田剖面发现Caudicriodus woschmidti并确认Pterospathodus eopennatus带的存在;以前报道的本剖面的Ozarkodinacrispa和Ozarkodina eosteinhornensis经4次样品分析,仍得不到确认。稗子田剖面的普里道利统(Pridoli)的沉积可能不全,不宜建阶。志留系与泥盆系之间可能为假整合。进一步讨论了牙形刺分带以及志留系内部统间的界线。认为金淳泰等(2005)依据稗子田剖面命名的6个新阶名,不宜使用。

关键词(KeyWords)： C.woschmidti带;假整合;普里道利统;志留系;盐边;四川

Abstract:

Keywords:

基金项目(Foundation): 全国地层委员会“中国主要断代地层建阶研究”项目的资助

作者(Author): 王成源,王平,杨光华,谢伟

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