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    Volume 43 Issue 11
    Nov.  2018
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    Chu Daoliang, Miao Xue, Wu Yuyang, Guo Wenwei, Shu Wenchao, Tong Jinnan, 2018. Conchostracans from the Permian-Triassic Transition in Weibei Area of Shaanxi Province and Its Biostratigraphic. Earth Science, 43(11): 3910-3921. doi: 10.3799/dqkx.2018.104
    Citation: Chu Daoliang, Miao Xue, Wu Yuyang, Guo Wenwei, Shu Wenchao, Tong Jinnan, 2018. Conchostracans from the Permian-Triassic Transition in Weibei Area of Shaanxi Province and Its Biostratigraphic. Earth Science, 43(11): 3910-3921. doi: 10.3799/dqkx.2018.104

    Conchostracans from the Permian-Triassic Transition in Weibei Area of Shaanxi Province and Its Biostratigraphic

    doi: 10.3799/dqkx.2018.104
    • Received Date: 2018-04-17
    • Publish Date: 2018-11-15
    • As global challenging key issues of paleontology and stratigraphy, the terrestrial Permian-Triassic (P-Tr) stratigraphic subdivision and correlation have great significance for a comprehensive understanding of the nature of the global biotic and environmental event. Here, we try to establish the biostratigraphic correlation framework of the terrestrial depositions, and further explore the correlation between the marine and terrestrial P-Tr depositions, based on the P-Tr transitional mixed marine-terrestrial biota in Weibei area of Shaanxi Province. The present study focuses on the taxonomy, evolutionary lineage and stratigraphy of P-Tr transitional conchostracans (clam shrimps, spinicaudatans) in the terrestrial and terrestrial-marine siliciclastic facies, which are regarded as an intermediate link for biostratigraphic correlation between terrestrial and marine sequences. A total of eight species in four genus and three species in two genus conchostracans were identified in the Shichuanhe Section and Houzhougong miao Section, respectively. Accordingly, in the study it proposes that the conchostracans fauna may be subdivided into three assemblages including the latest Permian Pseudestheria minuta-Pseudestheria xinjiangensis assemblage, the P-Tr transitional Euestheria gutta-Palaeolimnadiopsis vilujensis assemblage and the earliest Triassic Magniestheria subcircularis-Cornia germari assemblage. Especially, the Euestheria gutta-Palaeolimnadiopsis vilujensis assemblage is proposed as marker of the P-Tr transitional beds of the terrestrial strata among various regions.

       

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