Article ID Journal Published Year Pages File Type
4687773 Journal of China University of Geosciences 2008 10 Pages PDF
Abstract
The Lower Triassic in Chaohu area, Anhui 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 Formation. Some key conodonts and seven new specimens are introduced.
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
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