Volume 45 Issue 3
Mar.  2020
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Article Navigation >  Earth Science  > 2020  >  45(3): 711-727
Bu Jianjun, He Weihong, Zhang Kexin, Yu Yang, Wang Jiaxuan, Wu Jun, 2020. Evolution of the Paleo-Asian Ocean: Evidences from Paleontology and Stratigraphy. Earth Science, 45(3): 711-727. doi: 10.3799/dqkx.2019.068
Citation: Bu Jianjun, He Weihong, Zhang Kexin, Yu Yang, Wang Jiaxuan, Wu Jun, 2020. Evolution of the Paleo-Asian Ocean: Evidences from Paleontology and Stratigraphy. Earth Science, 45(3): 711-727. doi: 10.3799/dqkx.2019.068
shu

Evolution of the Paleo-Asian Ocean: Evidences from Paleontology and Stratigraphy

doi: 10.3799/dqkx.2019.068
  • 1.

    Wuhan Center of China Geological Survey, Wuhan 430205, China

  • 2.

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

  • 3.

    Institute of Geological Survey, China University of Geosciences, Wuhan 430074, China

  • Received Date: 2019-01-05
  • Publish Date: 2020-03-15
    Abstract
  • The southern margin of the Paleo-Asian Ocean spanned Xinjiang, Gansu, Inner Mongolia, Heilongjiang and other places of China. This paper summarizes the history of Paleozoic tectonic evolution of Paleo-Asian Ocean and addresses the debates on the evolution. Based on the analysis of outcrops of the Upper Paleozoic and researches on paleontology (including brachiopods, radiolarians and plants) through the Paleo-Asian Ocean Domain in China, two conclusions are made. Firstly, during the Early Palaeozoic, the main basin of the Paleo-Asian Ocean might be located in the Tianshan area within western China and in the Airgin Sum-Hegenshan-Linxi-Heihe area within middle and eastern China. During the Late Paleozoic, the main basin of the Paleo-Asian Ocean might be located in the South Tianshan area within western China and in the Solonker-Ondor Sum-Xar Moron-Yanji area within middle and eastern China. Secondly, the west part of the Paleo-Asian Ocean might have been closed in the Early Carboniferous to the Middle Permian while the east part has been closed in the Late Permian. However, the north part of the ocean in Beishan area and the southwest part of the ocean in the South Tianshan persisted to the end-Permian at least. Additionally, this study proposes the potential application of palaeontology (i.e., radiolarians, fusulinids, corals) and of palaeoecology of benthic faunas in the evolution of Paleo-Asian Ocean.

     

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