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    Volume 40 Issue 5
    May  2015
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    Article Navigation >  Earth Science  > 2015  >  40(5): 797-809
    Song Junjun, Gong Yiming, 2015. Ostracods from the Emuha Section of Devonian-Carboniferous Transitional in Western Junggar. Earth Science, 40(5): 797-809. doi: 10.3799/dqkx.2015.065
    Citation: Song Junjun, Gong Yiming, 2015. Ostracods from the Emuha Section of Devonian-Carboniferous Transitional in Western Junggar. Earth Science, 40(5): 797-809. doi: 10.3799/dqkx.2015.065
    shu

    Ostracods from the Emuha Section of Devonian-Carboniferous Transitional in Western Junggar

    doi: 10.3799/dqkx.2015.065

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

    • Received Date: 2014-09-21
    • Publish Date: 2015-05-15
      Abstract
    • To provide new evidences for the stratigraphic division of Devonian and Carboniferous as well as paleoenvironmental reconstruction of western Junggar, Xinjiang, NW China. The biostratigraphic data of Devonian-Carboniferous boundary (D-C) has been explored in this study by field sampling and laboratory analysis in western Junggar. 12 ostracod species (including 1 new species) from the Devonian-Carboniferous in the Emuha section of western Junggar are first described and presented. It is found that they belong to 9 genera, including Cavellina sublatiovata, C.cf. obesa, C. sp., Glyptopleura sp., Healdianella renalata, H. sp., Bairdiocypris vafra, Bairdia sp., Rectobairdia sp., Fabalicypris sp., Youngiella calvata, Coelonella xizhunensis sp. nov.. The stratigraphical distribution of ostracods in the Emuha section suggests that the Hongguleleng Formation should be Late Devonian to the Early Carboniferous in age. In terms of paleoecology, the retrieved ostracods indicate an off-shore environment during intermittent periods of volcanic activities in volcanic arc zone.

       

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    • 致谢: 中科院南京古生物研究所王尚启研究员在成文过程中给予了热情指导和帮助；中国地质大学(武汉)地球科学学院袁爱华博士在介形类鉴定过程中提供许多帮助；纵瑞文、王志宏、范若颖和蒋涛参加了野外工作，在此一并表示感谢！
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