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    中国百强科技报刊

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    Volume 34 Issue 5
    Sep.  2009
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    Article Contents
    ZHAO Lai-shi, WU Yuan-bao, HU Zhao-chu, ZHOU Lian, LIU Yong-sheng, SHI Yu-fang, ZHANG Su-xin, TONG Jin-nan, YUAN Peng, 2009. Trace Element Compositions in Conodont Phosphates Responses to Biotic Extinction Event: A Case Study for Main Act of Global Boundary Stratotype Section and Point of the Permian-Triassic. Earth Science, 34(5): 725-732.
    Citation: ZHAO Lai-shi, WU Yuan-bao, HU Zhao-chu, ZHOU Lian, LIU Yong-sheng, SHI Yu-fang, ZHANG Su-xin, TONG Jin-nan, YUAN Peng, 2009. Trace Element Compositions in Conodont Phosphates Responses to Biotic Extinction Event: A Case Study for Main Act of Global Boundary Stratotype Section and Point of the Permian-Triassic. Earth Science, 34(5): 725-732.

    Trace Element Compositions in Conodont Phosphates Responses to Biotic Extinction Event: A Case Study for Main Act of Global Boundary Stratotype Section and Point of the Permian-Triassic

    • Received Date: 2009-02-10
    • Publish Date: 2009-09-25
    • Trace element compositions in Upper Permian conodonts with low color alteration index were measured in situ by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) from a stratigraphic section of the Meishan in Changxing, Zhejiang Province.The results show that the Ce anomalies and rare earth element (REE) concentrations are characterized by fast fluctuation.These features indicate highly fluctuating environmental conditions including redox and instable ecosystem conditions during the P/T transition.The element compositions couple well with the paleo-oceanic environment and the biotic crisis.The study effective defines and offers new approach for the key issues to the biotic extinction and recovery process, time limit, paleo-ocean chemistry and paleoecology at the end of the Permian.

       

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