2001Europe PMC (PubMed Central)Requires access

Restudy of the conodont sequence across the Carboniferous-Permian boundary in South Guizhou

Wang ZH, Qi YP

Open publisher page 5 citations

Abstract

This paper describes in detail the conodont sequence across the Carboniferous Permian boundary in Luodian and Ziyun of South Guizhou. The following conodont zones can be recognized in descending order: Streptognathodus barskovi, S. constrictus, S. isolatus, S. wabaunsensis, S. tenuialveus and S. firmus zones. The first occurrence of Streptognathodus isolatus is considered as the base of the Permian. The correlation of the conodont sequences across the Carboniferous Permian boundary between China and Kazakhstan, as well as North America is discussed.

About this research paper

What this paper is about

This paper describes in detail the conodont sequence across the Carboniferous Permian boundary in Luodian and Ziyun of South Guizhou. The following conodont zones can be recognized in descending order: Streptognathodus barskovi, S. constrictus, S. isolatus, S. wabaunsensis, S. tenuialveus and S. firmus zones. The first occurrence of Streptognathodus isolatus is considered as the base of the Permian. The correlation of the conodont sequences across the Carboniferous Permian boundary between China and Kazakhstan, as well as North America is discussed.

Why it matters

OpenAlex reports 5 citations for this work. Citation counts describe recorded attention and do not establish research quality.

Key contribution

A contribution statement is not available in the OpenAlex record.

Method / approach

Method details are not available in the OpenAlex metadata.

Main findings

Findings are not separately available in the OpenAlex metadata.

Limitations

Limitations are not available in the OpenAlex metadata.

Applications

Application details are not available in the OpenAlex metadata.

Available abstract

This paper describes in detail the conodont sequence across the Carboniferous Permian boundary in Luodian and Ziyun of South Guizhou. The following conodont zones can be recognized in descending order: Streptognathodus barskovi, S. constrictus, S. isolatus, S. wabaunsensis, S. tenuialveus and S. firmus zones. The first occurrence of Streptognathodus isolatus is considered as the base of the Permian. The correlation of the conodont sequences across the Carboniferous Permian boundary between China and Kazakhstan, as well as North America is discussed.

Key concepts: Conodont, Permian, Carboniferous, Geology, Sequence (biology), Paleontology, Boundary (topology), Biostratigraphy

Related papers

Back to paper searchBrowse research topicsOriginal source
Restudy of the conodont sequence across the Carboniferous-Permian boundary in South Guizhou — Research Paper | ScholarLens