Volume 43 Issue 11
Nov.  2018
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Wang Han, Xiao Yifan, Zhang Ning, Jiang Yang, Sun Xi, He Weihong, 2018. End-Permian Radiolarian Fauna from North Part of Nanpanjiang Basin and Implications of Paleo-Water Depths. Earth Science, 43(11): 3901-3909. doi: 10.3799/dqkx.2018.257
Citation: Wang Han, Xiao Yifan, Zhang Ning, Jiang Yang, Sun Xi, He Weihong, 2018. End-Permian Radiolarian Fauna from North Part of Nanpanjiang Basin and Implications of Paleo-Water Depths. Earth Science, 43(11): 3901-3909. doi: 10.3799/dqkx.2018.257
shu

End-Permian Radiolarian Fauna from North Part of Nanpanjiang Basin and Implications of Paleo-Water Depths

doi: 10.3799/dqkx.2018.257
  • 1.

    School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

  • 2.

    State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China

  • Received Date: 2018-03-11
  • Publish Date: 2018-11-15
    Abstract
  • The process of the Paleozoic-Mesozoic mass extinction in different paleogeographic settings is different. The research on radiolarian fauna provides not only important information for the study of paleogeographic settings but also basic information for the study of biodiversity evolution. The research on the radiolarians in the basinal facies of the Permian-Triassic transition is of great significance to reveal the mass extinction among different sedimentary facies and the paleoenvironmental evolution. The Permian-Triassic boundary section of Kejiao, Guizhou Province is located in the northern margin of the Nanpanjiang basin, which is in the basinal facies. In this paper, the preliminary statistics and taxonomy composition of the radiolarians from the Talung Formation and the basal part of Daye Formation in the Kejiao Section Were analyzed. And then the paleo-water depths of the late Changhsingian were studied in detail, based on the statistics and analysis of radiolarians and the preservation of the radiolarians. It is concluded that Talung Formation to basal Daye Formation were deposited below the wave base, and the paleo-water depths are generally considered as shallower than 150 meters. The paleo-water depths during the maximum transgression in the latest Changshingian (equivalent to the uppermost of the Talung Formation) are about/or deeper than 200 meters.

     

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