华南寒武纪早期海水氧化还原状态对动物演化的影响

金承胜; 崔豪; 程猛; 张子虎; 常华进; 张弢; 曹正琦

doi:10.3799/dqkx.2023.142

Volume 49 Issue 10

Oct. 2024

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Article Navigation > Earth Science > 2024 > 49(10): 3674-3684

Jin Chengsheng, Cui Hao, Cheng Meng, Zhang Zihu, Chang Huajin, Zhang Tao, Cao Zhengqi, 2024. Impact of Marine Redox Conditions on Animal Evolution in Early Cambrian Nanhua Basin, South China. Earth Science, 49(10): 3674-3684. doi: 10.3799/dqkx.2023.142

Citation:

Jin Chengsheng, Cui Hao, Cheng Meng, Zhang Zihu, Chang Huajin, Zhang Tao, Cao Zhengqi, 2024. Impact of Marine Redox Conditions on Animal Evolution in Early Cambrian Nanhua Basin, South China. Earth Science, 49(10): 3674-3684. doi: 10.3799/dqkx.2023.142

Citation:

Jin Chengsheng, Cui Hao, Cheng Meng, Zhang Zihu, Chang Huajin, Zhang Tao, Cao Zhengqi, 2024. Impact of Marine Redox Conditions on Animal Evolution in Early Cambrian Nanhua Basin, South China. Earth Science, 49(10): 3674-3684. doi: 10.3799/dqkx.2023.142

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Impact of Marine Redox Conditions on Animal Evolution in Early Cambrian Nanhua Basin, South China

doi: 10.3799/dqkx.2023.142

1.
College of Resource Environment and Tourism, Hubei University of Arts and Science, Xiangyang 441053, China
2.
Changjiang River Scientific Research Institute of Changjiang Water Resources Commission, Wuhan 430010, China
3.
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2022-12-01
Available Online: 2024-11-08
Publish Date: 2024-10-25

Abstract

Abstract

Marine redox variations have been frequently used to explain the radiation and extinction of early animals during the Early Cambrian. However, this hypothesis remains unclear. Here, it conducted total organic carbon, iron speciation, major elements, and trace elements in the basinal Zhalagou Section. The new redox results were compared with published redox environments from the coeval other sections in South China and Siberian. The results suggest that oxic waters were intensively expanded during Cambrian Age 2-3, whereas the degree of oceanic anoxia was enhanced during Cambrian Age 4. Comparison of ocean redox states and fossils suggests that enhanced ocean oxygenation might play key roles in the radiation of early animals during Cambrian Age 2-3, but expanded ocean anoxia might have significant effects on the decreased diversification of early animals and extinction of archaeocyaths during Cambrian Age 4.
- iron speciation,
- trace element,
- anoxia,
- animal extinction,
- Yangtze Block,
- geochemistry

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References(50)

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Impact of Marine Redox Conditions on Animal Evolution in Early Cambrian Nanhua Basin, South China

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