Ostracods from the Pingyi Basin (eastern China) and their significance for the K/Pg boundary

Author:

Wang He1ORCID,Du Shengxian234,Yu Tingting15ORCID,Li Sha1,Lu Huinan1,Zhang Haichun1,Cao Meizhen1,Horne David J.6ORCID

Affiliation:

1. State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, China

2. Shandong Institute of Geological Sciences, Jinan 250013, China

3. Key Laboratory of Gold Mineralization Processes and Resource Utilization Subordinated to the Ministry of Land and Resources, Jinan 250013, China

4. Key Laboratory of Metallogenic Geological Process and Resources Utilization in Shandong Province, Jinan 250013, China

5. University of Science and Technology of China, Hefei 230026, China

6. School of Geography, Queen Mary University of London, Mile End Road, London E1 4NS, UK

Abstract

AbstractThe Pingyi Basin is a late Mesozoic to Cenozoic fault basin in East China, containing a good record of Cretaceous to Paleogene non-marine carbonate and gypsum deposits. Abundant microfossils including gastropods, ostracods, charophytes and palynomorphs have been reported from this basin. A taxonomic study of ostracods from the Gejiazhuang section in the Pingyi Basin reveals a total of 17 species assigned to 11 genera. A further ostracod biostratigraphic correlation suggests the K/Pg boundary lies within Member 1 of the Bianqiao Formation in the Gejiazhuang section, which is supported by charophyte biostratigraphy.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference54 articles.

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4. A monograph of the marine and freshwater Ostracoda of the North Atlantic and of North Western Europe. I. Podocopa;The Scientific Transactions of the Royal Dublin Society Series 2,1889

5. The Ostracoda and Foraminifera of tidal rivers. Part I. Ostracoda;Annals and Magazine of Natural History, Series 4,1870

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