A massive magmatic degassing event drove the Late Smithian Thermal Maximum and Smithian–Spathian boundary mass extinction

Global and Planetary Change - Tập 215 - Trang 103878 - 2022
Yong Du1, Huyue Song1, Thomas J. Algeo1,2,3, Haijun Song1, Li Tian1, Daoliang Chu1, Wei Shi1, Chao Li4,5, Jinnan Tong1
1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
2State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3Department of Geology, University of Cincinnati, Cincinnati, OH 45221-0013, USA
4State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China
5Key Laboratory of Deep-time Geography and Environment Reconstruction and Applications of Ministry of Natural Resources, Chengdu University of Technology, Chengdu 610059, China

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Global and Planetary Change

Tập 215

103878

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