摘要
湖北郧西地区石炭纪地层中 蜓竹 类化石丰富。西方记述的 蜓竹 类共 5 3个种 ,其中包括 6个新种 ,主要属种都附有照相图版。这些 蜓竹 类化石是该地区石炭纪年代地层划分最重要的依据。
The stratigraphic sequence of Carboniferous Period were developed well in Yunxi,Hubei.The fossils which are described in this paper are 53 species, including 6 new species. The main speeies among them are enclosed here with photo plates. These Fusulinida fossils are important for dividing chronostratigraphic sequence of Carboniferous Period.
出处
《湖北地矿》
2003年第4期3-10,共8页
Hubei Geology & Mineral Resources
