摘要
首次在安徽宿松地区中二叠统中发现古代上升流沉积典型实例。通过对上升流层序岩相的分析,将研究区上升流岩相划分为硅质团块、硅质条带、硅质细层、硅质结核、硅质岩、硅质泥岩和泥晶灰岩7种类型,并发现发育有上升流沉积典型层理——微细层理;根据不同上升流沉积层序中岩相的有规律的组合特征,将其岩相组合划分为2种类型,即陆棚缓坡相和陆棚盆地相组合;分析了上升流对生物古生态特征的控制作用,认为上升流的发育强度和生物群落的丰度成正相关,而与分异度多成负相关。
引文
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