盛青怡,王秋来,祁玉平,廖卓庭

• 1:中国科学院南京地质古生物研究所现代古生物学和地层学国家重点实验室

摘要(Abstract)：

贵州罗甸纳庆剖面是竞争谢尔普霍夫阶底界全球界线层型剖面和点位的最有力候选剖面之一。纳饶剖面紧邻纳庆剖面,是其辅助剖面。纳饶剖面维宪阶-谢尔普霍夫阶(Viséan-Serpukhovian)界线层段的牙形刺生物地层已经初步建立,可与纳庆剖面直接对比。纳饶剖面V/S界线位于41.8 m处,是以牙形刺演化谱系L. nodosa-L.ziegleri中L. ziegleri的首现来定义的。本研究报道了这一界线层段的有孔虫化石。界线附近共识别出有孔虫23属28种,建立了两个有孔虫带,自下而上分别是Asteroarchaediscus rugosus带和Janischewskina delicata带。A.rugosus带是维宪最晚期的有孔虫带。J. delicata带是谢尔普霍夫初期的有孔虫带,以44 m处J. delicata的首现为标志。纳饶剖面V/S界线2.2m内同时出现了谢尔普霍夫阶底界标志性的牙形刺和有孔虫,为该界线附近牙形刺和有孔虫的对比提供了重要依据。

关键词(KeyWords)： 有孔虫;纳饶剖面;石炭系;维宪阶-谢尔普霍夫阶;金钉子;贵州

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金(41702016、41630101);; 江苏省自然科学基金(BK20171102);; 现代古生物学和地层学国家重点实验室(20172109);; 中国科学院战略性先导专项(XDB18000000、XDB26000000)共同资助

作者(Author): 盛青怡,王秋来,祁玉平,廖卓庭

DOI: 10.19839/j.cnki.dcxzz.2021.0005

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