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Volume 30 Issue 5
Oct 2019
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Journal of Earth Science  > 2019  >  30(5): 1059-1074.
Bo Yang, Hanxiao Li, Paul B. Wignall, Haishui Jiang, Zhijun Niu, Qian Ye, Qiong Wu, Xulong Lai. Latest Wuchiapingian to Earliest Triassic Conodont Zones and δ13Ccarb Isotope Excursions from Deep-Water Sections in Western Hubei Province, South China. Journal of Earth Science, 2019, 30(5): 1059-1074. doi: 10.1007/s12583-019-1018-2
Citation: Bo Yang, Hanxiao Li, Paul B. Wignall, Haishui Jiang, Zhijun Niu, Qian Ye, Qiong Wu, Xulong Lai. Latest Wuchiapingian to Earliest Triassic Conodont Zones and δ13Ccarb Isotope Excursions from Deep-Water Sections in Western Hubei Province, South China. Journal of Earth Science, 2019, 30(5): 1059-1074. doi: 10.1007/s12583-019-1018-2
shu

Latest Wuchiapingian to Earliest Triassic Conodont Zones and δ13Ccarb Isotope Excursions from Deep-Water Sections in Western Hubei Province, South China

doi: 10.1007/s12583-019-1018-2
  • 1.

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

  • 2.

    Wuhan Center of Geological Survey, Wuhan 430205, China

  • 3.

    School of Earth & Environment, University of Leeds, Leeds LS2 9JT, UK

  • 4.

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

  • 5.

    Non-ferrous Metals Geological Exploration Bureau of Zhejiang Province, Shaoxing 312000, China

  • 6.

    State Laboratory of Paleontology and Stratigraphy, Nanjing Institute of Geology and Paleontology, Nanjing 210008, China

More Information
  • Corresponding author: Xulong Lai
  • Received Date: 22 Dec 2018
  • Accepted Date: 23 May 2019
  • Publish Date: 01 Oct 2019
    Abstract
  • Deep-water facies sections have advantages of recording complete information across the Permian-Triassic boundary (PTB). Here we present a detailed study on the conodont biostratigraphy and carbon isotope profile ranges from the Wuchiapingian-Changhsingian boundary (WCB) to the PTB of two deep-water facies sections at Zhuqiao and Shiligou in the Middle Yangtze region, western Hubei, South China. Fifteen species and three genera are identified. Eight conodont zones are recog-nized which in ascending order are the Clarkina orientalis, C. wangi, C. subcarinata, C. changxingensis, C. yini, C. meishanensis, Hindeodus parvus and Isarcicella isarcica zones. The onset of deposition of the deep-water siliceous strata of Dalong Formation in western Hubei began in the Late Wuchiapingian and persisted to the Late Changhsingian. Carbon isotope negative excursions occur near both the WCB and PTB in both sections. The WCB δ13Ccarb negative excursion is in the C. orientalis and C. wangi zones. The PTB δ13Ccarb negative excursion began in the C. yini Zone and extended to the I. isarcica Zone. The absence of several Changhsingian zones may indicate the difficulty of extracting conodonts from siliceous strata or the presence of an intra-Changhsingian hiatus.

     

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