晚二叠世全球海洋生态系统逐步坍塌与缺氧的可能联系

何卫红; 吴攸攸; 张克信; 铃木纪毅; 肖异凡; 杨廷禄; 吴琛; 黄亚飞

doi:10.3799/dqkx.2024.140

Volume 50 Issue 3

Mar. 2025

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Article Navigation > Earth Science > 2025 > 50(3): 983-999

He Weihong, Wu Youyou, Zhang Kexin, Suzuki Noritoshi, Xiao Yifan, Yang Tinglu, Wu Chen, Huang Yafei, 2025. Gradual Collapse of Global Marine Ecosystem in the Late Permian and Its Link to the Anoxia. Earth Science, 50(3): 983-999. doi: 10.3799/dqkx.2024.140

Citation:

He Weihong, Wu Youyou, Zhang Kexin, Suzuki Noritoshi, Xiao Yifan, Yang Tinglu, Wu Chen, Huang Yafei, 2025. Gradual Collapse of Global Marine Ecosystem in the Late Permian and Its Link to the Anoxia. Earth Science, 50(3): 983-999. doi: 10.3799/dqkx.2024.140

Citation:

He Weihong, Wu Youyou, Zhang Kexin, Suzuki Noritoshi, Xiao Yifan, Yang Tinglu, Wu Chen, Huang Yafei, 2025. Gradual Collapse of Global Marine Ecosystem in the Late Permian and Its Link to the Anoxia. Earth Science, 50(3): 983-999. doi: 10.3799/dqkx.2024.140

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Gradual Collapse of Global Marine Ecosystem in the Late Permian and Its Link to the Anoxia

doi: 10.3799/dqkx.2024.140

1.
School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China
2.
State Key Laboratory of Geomicrobiology and Environmental Changes, China University of Geosciences (Wuhan), Wuhan 430078, China
3.
Department of Earth Science, Graduate School of Science, Tohoku University, Sendai 980‒8578, Japan
4.
School of Earth Sciences, East China University of Technology, Nanchang 330013, China
5.
Wuhan Center of China Geological Survey, Wuhan 430205, China

Received Date: 2024-11-29
Publish Date: 2025-03-25

Abstract

Abstract

The duration for the End-Permian mass extinction has been estimated as about 30 to 60 kyr. However, an ever-expanding body of papers has revealed that the evolution of Late Permian ecosystems possibly involved some yet under-studied 'early warning signals' prior to the End-Permian mass extinction. The study on the pre-extinction 'warning signals' is still limited. In order to understand the process of marine ecosystem collapse specifically the 'early warning signals' pointing to the approaching of a global ecosystem regime shift (tipping point), 30 marine Permian-Triassic Boundary sections from different palaeogeographic settings were selected globally to investigate the spatiotemporal biodiversity changes of different taxa and the spatiotemporal redox conditions. The results reveal that: (1) The marine ecosystem collapsed first in deep waters and then in shallow waters (first in offshore pelagic settings, then in moderately deep waters and deep-water basins and shelves and finally in shallow water environments); (2) in the same environments (in deep or moderately deep waters), a similar differential temporal pattern is also apparent in that the planktonic ecosystems were devastated earlier than benthic ecosystems. To account for the spatiotemporal and ecological (taxonomic) differences in extinction timing, we propose that the formation and expansion of an OMZ (oxygen minimum zone) and the related anoxia (or oxygen depletion), were most likely responsible for the differential temporal patterns of marine ecosystem collapses between deep and shallow waters, and between planktonic and benthic communities during the Late Permian.
- collapse of marine ecosystem,
- oxygen minimum zone,
- anoxia,
- Late Permian,
- stratigraphy,
- environmental impact

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References(96)

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Gradual Collapse of Global Marine Ecosystem in the Late Permian and Its Link to the Anoxia

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