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. Forty-eight ostracod species belonging to 28 genera from the Late Devonian ofGuangxi in South China are described and figured. The ostracod assemblagefrom the Nandong section can be attributed to therhenana–linguiformis conodont zones. The ecological assemblages ofostracods from the Yangdi section correspond to a smooth-podocopidassociation accompanied by some pelagic entomozoids. This mixed assemblage isindicative of an environment of carbonate platform to slope during an ongoingregression. The ostracod faunas from the Nandong section are on the contrarycomposed of both pelagic and benthic ostracods and pelagic forms dominate innumber of specimens suggesting a basin environment.

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