李思儒,巩恩普,张永利,王立芙,杨臻元

• 1:东北大学资源与土木工程学院

摘要(Abstract)：

黔南紫云宗地乡高寨发育早二叠世萨克马尔期中晚期珊瑚层,是该时期中国南方报道较少的生物建造类型,具有较高的研究价值。珊瑚层由单体四射珊瑚提曼珊瑚(Timania)和沟珊瑚(Bothrophyllum)建造而成。珊瑚层内生物种类丰富,包括群体珊瑚Antheria、棘皮类、有孔虫、钙藻、Tubiphytes、腕足类等。本文对珊瑚层岩石进行微相研究,划分出了珊瑚障积岩、有孔虫生屑泥粒灰岩、钙藻-有孔虫生屑泥粒灰岩、似球粒泥粒灰岩-颗粒灰岩、生屑粒泥灰岩和白云质生屑泥粒灰岩等6种微相类型。晚古生代冰川作用导致的高频率海平面变化控制珊瑚层的形成和消失。珊瑚层发育于早二叠世“冰室地球”到“温室地球”这一转折发生的关键时期,其发现为华南地区对晚古生代冰川作用的响应提供了证据。

关键词(KeyWords)： 萨克马尔期;珊瑚层;海平面变化;晚古生代冰期;黔南

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金(41972002、42272008)资助

作者(Author): 李思儒,巩恩普,张永利,王立芙,杨臻元

DOI: 10.19839/j.cnki.dcxzz.2023.0013

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