Articles | Volume 37, issue 1
https://doi.org/10.5194/jm-37-257-2018
https://doi.org/10.5194/jm-37-257-2018
Research article
 | 
05 Feb 2018
Research article |  | 05 Feb 2018

Ostracods (Crustacea) as shelf to basin indicators: evidence from Late Devonian Yangdi and Nandong sections in Guangxi, South China

Junjun Song, Sylvie Crasquin, and Yiming Gong

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Cited articles

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Adamczak, F.: Nomenclatorial notes on some Devonian ostracod taxa from Poland, Senckenbergiana lethaea, 58, p. 515, 1978. 
Bai, S. L., Bai, Z. Q., Ma, X. P., Wang, D. R., and Sun, Y. L.: Devonian events and biostratigraphy of South China, Peking University Press, Beijing, 1–303, 1994. 
Bandel, K. and Beker, G.: Ostracoden aus paläozoischen pelagischen Kalken der Karnischen Alpen (Silurium bis Unterkarbon), Senckenbergiana lethaea, 56, 1–84, 1975. 
Becker, G.: Progress in mid Palaeozoic palaeoceanographical studies from Ostracoda – from local to global importance (a review), Senckenbergiana lethaea, 80, 555–566, 2000. 
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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.