Analysis of platinum-group elements in drill core samples from the Meishan Permian-Triassic boundary section, China
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  • 作者:Lin Xu (1)
    Yangting Lin (2)
  • 关键词:Permian ; Triassic boundary event ; platinum ; group element ; mass extinction ; extraterrestrial impact ; basaltic volcanic eruption
  • 刊名:Chinese Journal of Geochemistry
  • 出版年:2014
  • 出版时间:December 2014
  • 年:2014
  • 卷:33
  • 期:4
  • 页码:365-373
  • 全文大小:830 KB
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  • 作者单位:Lin Xu (1)
    Yangting Lin (2)

    1. Key Laboratory of Lunar and Deep Space Exploration, National Astronomical Observatories, Chinese Academy of Sciences, Beijing, 100012, China
    2. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China
  • ISSN:1993-0364
文摘
There is a long-standing controversy of what triggered the extinction at the Permian-Triassic boundary, the most severe mass extinction in the geologic record, including flood basaltic volcanism and/or bolide impact hypothesis. In order to clarify various pieces of evidence for the mass extinction event at the Permian-Triassic boundary, some researchers from some laboratories throughout the world have made a comprehensive study on a group of samples from the Meishan area of China. Some fresh core samples from the Permian-Triassic boundary in the Meishan area were analyzed in this study. The results showed that there is no Ir anomaly. Moreover, the PGEs patterns of those samples show obvious differentiation characteristics, that is different from the case encountered in meteorites. So no evidence supports the hypothesis of extraterrestrial impact. In contrast, the PGEs patterns are similar to those of Siberian and Emeishan basalts, which indicates that those PGEs are derived mainly from the basalts, lending a support to the correlation between mass extinction at the Permian-Triassic boundary and flood basaltic volcanism. This study has also confirmed the results for samples from section C prior to the analysis of the samples.

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