王秋来,祁玉平,胡科毅,盛青怡,林巍

• 1:中国科学院资源地层学与古地理学重点实验室
• 2:中国科学院南京地质古生物研究所

摘要(Abstract)：

石炭系维宪阶-谢尔普霍夫阶全球界线层型尚未确立。由于石炭纪冰期效应显著,海平面升降频繁,造成沉积环境发生剧烈变化,给该界线的划分和对比带来了一定困难。罗悃剖面位于贵州省罗甸县西南,出露维宪阶上部至莫斯科阶上部的一套上斜坡相深水碳酸盐岩沉积,受水深影响较小,同时产丰富的牙形刺及有孔虫,可以较好地进行深、浅水相区的对比。本文通过对该剖面维宪阶—谢尔普霍夫阶界线层较为详细的采样分析,共发现牙形刺8属32种(含9亚种和1未定种),自下而上识别出两个牙形刺带,即Lochriea nodosa和L.ziegleri带,将谢尔普霍夫阶底界置于L.ziegleri的首现面,即罗悃剖面4.65m处;同时与同属华南的纳庆剖面以及全球其他地区重要剖面的牙形刺带或菊石带进行了对比。

关键词(KeyWords)： 生物地层;牙形刺;维宪阶;谢尔普霍夫阶;石炭纪;罗悃剖面;罗甸;贵州

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(No.41072009,41372023,41290260);; 科技部基础性项目(2013FY111000)资助

作者(Author): 王秋来,祁玉平,胡科毅,盛青怡,林巍

DOI: 10.19839/j.cnki.dcxzz.2014.03.003

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