An Update of Conodonts in the Induan-Olenekian Boundary Strata at West Pingdingshan Section,Chaohu,Anhui Province

被引:0
|
作者
赵来时 [1 ]
童金南 [1 ]
张素新 [1 ]
孙知民 [1 ]
机构
[1] State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Wuhan 430074, China
[2] Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
基金
中国国家自然科学基金;
关键词
conodont; Induan-Olenekian boundary; Lower Triassic; Chaohu;
D O I
暂无
中图分类号
Q915 [古动物学];
学科分类号
0709 ; 070903 ;
摘要
The Lower Triassic in Chaohu (巢湖) area, Anhui (安徽) Province, China, is well developed and its sequence is typical in South China. After a brief introduction of the Induan-Olenekian boundary of Chaohu, this article presents some new data on conodonts. More than ten times of conodont samplings and investigations have recovered thousands of conodont specimens, which are especially rich in the Induan-Olenekian boundary strata at the West Pingdingshan Section in Chaohu City, Anhui Province. The most distinctive forms are the conodonts of the Neospathodus dieneri group and N. waageni group. The first occurrence of N. waageni eowaageni, which is regarded as the indicator of the Induan-Olenekian boundary, is situated at 40.49 m above the base of Yinkeng (殷坑) Formation. Some key conodonts and seven new specimens are introduced.
引用
收藏
页码:207 / 216
页数:10
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