广东连州长兴期含煤地层THE CHANGHSINGIAN COAL-BEARING FORMATION OF LIANZHOU,GUANGDONG
姚兆奇,陈楚震,芮琳,刘陆军
摘要(Abstract):
九陂组(亚田煤组)是粤北和湘南晚二叠世重要的含煤地层,其下伏"梅田灰岩"的涵义和化石Galloway-inella meitienensis的层位问题曾长期未得澄清。通过对梅田组剖面的详细工作,建立了下部的Gallowayinella组合和上部的Nanlingella jiaozishanica-Sphaerulina subrotunda组合。位于麻田组与梅田组之间的九陂组(亚田煤组)上界还达不到长兴阶的顶部,其下限则高于Gallowayinella组合,但不低于Palaeofusulina sinensis亚带的中上部。这样,九陂组(亚田煤组)的时代应定格在P.sinensis亚带的上部,但不包括该亚带的顶部。九陂组不能称作是华南二叠纪层位最高的含煤地层。同时对类Gallowayinella和植物"Ullmannia cf.bronnii"的时代分布等问题作了简要的讨论。
关键词(KeyWords): 类;生物地层;九陂组(亚田煤组);晚二叠世;连州;广东
基金项目(Foundation): 中国科学院知识创新工程重要方向性项目(KZCX2-YW-105)资助
作者(Author): 姚兆奇,陈楚震,芮琳,刘陆军
DOI: 10.19839/j.cnki.dcxzz.2011.01.007
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