罗苏阶——上石炭统底部一个新的年代地层单位
芮琳 ,王志浩 ,张遴信
摘要(Abstract):
<正> 1983年在西班牙马德里召开第十届国际石炭纪地层及地质大会期间,石炭系中间界线特别委员会向国际地科联石炭系分会推荐了一个确定石炭系中间界线的最后修正的方案。内容可概括成如下三点: 1.下石炭统与上石炭统的国际界线应大致相当于菊石Eumgrphoceras带演变到Homoceras带的一转折期,界线选定在Eumorphoceras至Homoceras带的过渡处,但因Homoceras的地理分布相当局限,所以它不可能成为识别全球界线的合适分子。 2.基于上述原因,另一个分布很广的类群——牙形刺可以用以识别石炭系中间界线。
关键词(KeyWords):
基金项目(Foundation):
作者(Author): 芮琳 ,王志浩 ,张遴信
DOI: 10.19839/j.cnki.dcxzz.1987.02.003
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