摘要
笔者在安徽南部贵池一东至地区上石炭统一下二叠统中首次发现丰富的有孔虫化石，经系统研究在上石炭统建立了两个组合，下二叠统建立了三个组合，并与国内相应地层有孔虫组合进行了对比。从而填补了该区晚石炭世一早二叠世有孔虫生物群的空白，丰富了生物群的内容，并讨论了隆林阶在该区的存在。
The authors discovered abundant forminifer fossils in the Upper Carboniferous-Lower Permi-an in southern Anhui.Through a systematic study,they established two assemblages in the UpperCarboniferous and three assernblages in the Lower Permian, thus filling in the gap in the LateCarboniferous-Early Permian foraminifer biotas in the area. There new assemblages have beencorrelated with those occurring in corresponding strata at home.
出处
《中国区域地质》
CSCD
1994年第2期160-160,共1页
Regional Geology of China
