西藏色龙西山二叠系-三叠系界线剖面稳定碳同位素特征

安显银; 张予杰; 朱同兴; 张以春; 袁东勋

doi:10.3799/dqkx.2018.103

Volume 43 Issue 8

Aug. 2018

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An Xianyin, Zhang Yujie, Zhu Tongxing, Zhang Yichun, Yuan Dongxun, 2018. Stable Carbon Isotope Characteristics of Permian-Triassic Boundary at the Selong Xishan Section. Earth Science, 43(8): 2848-2857. doi: 10.3799/dqkx.2018.103

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An Xianyin, Zhang Yujie, Zhu Tongxing, Zhang Yichun, Yuan Dongxun, 2018. Stable Carbon Isotope Characteristics of Permian-Triassic Boundary at the Selong Xishan Section. Earth Science, 43(8): 2848-2857. doi: 10.3799/dqkx.2018.103

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Stable Carbon Isotope Characteristics of Permian-Triassic Boundary at the Selong Xishan Section

doi: 10.3799/dqkx.2018.103

1.
Chengdu Center of China Geological Survey, Chengdu 610081, China
2.
State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Nanjing 210008, China

Received Date: 2018-03-17
Publish Date: 2018-08-15

Abstract

Abstract

The process and cause about the mass extinction event across the Paleozoic-Mesozoic transition have always been one of the key paleontological issues in the past few decades. The conodont zoning of the Selong Xishan section has made important progress, providing new evidence for understanding the stratigraphic sequence and sedimentary history of the area. Carbon isotope analyses of bulk samples in this study indicate that there are negative shifts across the Changshingian-Induan Boundary, which are comparable to South China. Newly identified carbon isotope negative shift at earliest Olenekian, base of Neospathodus waageni zone and the following positive shift coincide with the pattern recognized in South China and other places, implying the multi-phase extinction-recovery processes in Early Triassic.
- carbon isotope,
- Permian-Triassic,
- conodont,
- Selong Xishan,
- biostratigraphy,
- geochemistry,
- stratigraphy

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References

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Stable Carbon Isotope Characteristics of Permian-Triassic Boundary at the Selong Xishan Section

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