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Volume 29 Issue 4
Jul 2018
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Ke Zhang, Aihua Yuan, Qinglai Feng. The Upper Ordovician Microfossil Assemblages from the Pagoda Formation in Zigui, Hubei Province. Journal of Earth Science, 2018, 29(4): 900-911. doi: 10.1007/s12583-017-0958-7
Citation: Ke Zhang, Aihua Yuan, Qinglai Feng. The Upper Ordovician Microfossil Assemblages from the Pagoda Formation in Zigui, Hubei Province. Journal of Earth Science, 2018, 29(4): 900-911. doi: 10.1007/s12583-017-0958-7

The Upper Ordovician Microfossil Assemblages from the Pagoda Formation in Zigui, Hubei Province

doi: 10.1007/s12583-017-0958-7
Funds:

NSFC 41430101

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  • Corresponding author: Aihua Yuan
  • Received Date: 15 Jun 2017
  • Accepted Date: 23 Sep 2017
  • Publish Date: 01 Aug 2018
  • The Pagoda Formation is a lithologically and biologically distinctive unit among the Upper Ordovician. The strata are characterized by a nodular limestone, which yields fossil assemblages of high diversity. Conodonts of 14 genera 20 species (6 undetermined species) and ostracods of 14 genera 26 species (16 undetermined species) are identified. In addition, spherical radiolarians and minute-walled foraminifers were first reported from this formation in South China. The conodont assemblage is attributed to the Hamarous europaeus Zone, which indicates the Early Katian Age. The conodont HDS biofacies, along with thin-shelled ostracods, spherical radiolarians and foraminifers, suggest relatively deep and quiet water depositional environment. Accordingly, these fossil materials not only enrich the diversity of the Pagoda biota, but also provide evidence for discussions of depositional environments and stratigraphic correlations for the Pagoda Formation.

     

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