1.Anoxia/high temperature double whammy during the Permian-Triassic marine crisis and its aftermath

作　　者：Haijun Song ;Paul B. Wignall ;Daoliang Chu 等

出　　处：Scientific Reports. 2014 ;4.doi:10.1038/srep04132

出版社：Springer Nature

文章 ID：110531453

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2.Mercury Spikes Indicate a Volcanic Trigger for the Late Ordovician Mass Extinction Event: An Example from a Deep Shelf of the Peri-Baltic Region

作　　者：Justyna Smolarek-Lach ;Leszek Marynowski ;Wiesław Trela 等

出　　处：Scientific Reports. 2019 ;9(1):1-11.doi:10.1038/s41598-019-39333-9

出版社：Springer Nature

文章 ID：235846129

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3.Anoxia/high temperature double whammy during the Permian-Triassic marine crisis and its aftermath

作　　者：Haijun Song ;Paul B. Wignall ;Daoliang Chu 等

出　　处：Scientific Reports. 2015 ;4(1).doi:10.1038/srep04132

出版社：Springer Nature

文章 ID：235838843

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4.Flat latitudinal diversity gradient caused by the Permian–Triassic mass extinction

作　　者：Haijun Song ;Shan Huang ;Enhao Jia 等

出　　处：Proceedings of the National Academy of Sciences. 2020 ;117(30):17578-17583.doi:10.1073/pnas.1918953117

出版社：The National Academy of Sciences of the United States of America

文章 ID：260995425

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5.Volcanically driven lacustrine ecosystem changes during the Carnian Pluvial Episode (Late Triassic)

作　　者：Jing Lu ;Peixin Zhang ;Jacopo Dal Corso 等

出　　处：Proceedings of the National Academy of Sciences. 2021 ;118(40).doi:10.1073/pnas.2109895118

出版社：The National Academy of Sciences of the United States of America

文章 ID：1036033123

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