Articles | Volume 37, issue 1
https://doi.org/10.5194/jm-37-257-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/jm-37-257-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Ostracods (Crustacea) as shelf to basin indicators: evidence from Late Devonian Yangdi and Nandong sections in Guangxi, South China
Junjun Song
State Key Laboratory of Biogeology and Environmental Geology, School
of Earth Sciences, China University of Geosciences, Wuhan 430074, China
Key Laboratory of Economic Stratigraphy and Palaeogeography,
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences,
Nanjing 210008, China
CR2P, MNHN-UPMC-CNRS, Sorbonne Universités, Université Pierre
et Marie Curie, T46-56, E.5, case 104, 75252 Paris CEDEX 05, France
Sylvie Crasquin
CR2P, MNHN-UPMC-CNRS, Sorbonne Universités, Université Pierre
et Marie Curie, T46-56, E.5, case 104, 75252 Paris CEDEX 05, France
Yiming Gong
CORRESPONDING AUTHOR
State Key Laboratory of Biogeology and Environmental Geology, School
of Earth Sciences, China University of Geosciences, Wuhan 430074, China
Related authors
No articles found.
Junjun Song and Yiming Gong
J. Micropalaeontol., 37, 341–346, https://doi.org/10.5194/jm-37-341-2018, https://doi.org/10.5194/jm-37-341-2018, 2018
Short summary
Short summary
Wangshangkia, a new genus of Ostracoda, is described from the Late Devonian in Dushan of Guizhou, South China. This genus belongs to the family Bairdiocyprididae Shaver, 1961 and includes two new species, i.e. Wangshangkia dushaniensis and W. bailouiensis. The new genus is characterized by a wide ventral carina with radial striae. It is reported from the Famennian of South China and disappeared just below the Devonian–Carboniferous boundary. Wangshangkia is essentially a benthic crawler.
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Short summary
Forty-eight ostracod species belonging to 28 genera from the Late Devonian of Guangxi in South China are described and figured. The ostracod assemblages can be attributed to the Late Devonian rhenana–linguiformis conodont zones. The ecological assemblages of ostracods from the Yangdi and Nandong sections are indicative of the carbonate platform to basin environment.
Forty-eight ostracod species belonging to 28 genera from the Late Devonian of Guangxi in South...