Felsic volcanism as a factor driving the end-Permian mass extinction

The Siberian Traps large igneous province (STLIP) is commonly invoked as the primary driver of global environmental changes that triggered the end-Permian mass extinction (EPME). Here, we explore the contributions of coeval felsic volcanism to end-Permian environmental changes. We report evidence of...

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Detalles Bibliográficos
Autores principales: Zhang, Hua, Zhang, Feifei, Chen, Jiu-bin, Erwin, Douglas H., Syverson, Drew D., Ni, Pei, Rampino, Michael, Chi, Zhe, Cai, Yao-feng, Xiang, Lei, Li, Wei-qiang, Liu, Sheng-Ao, Wang, Ru-cheng, Wang, Xiang-dong, Feng, Zhuo, Li, Hou-min, Zhang, Ting, Cai, Hong-ming, Zheng, Wang, Cui, Ying, Zhu, Xiang-kun, Hou, Zeng-qian, Wu, Fu-yuan, Xu, Yi-gang, Planavsky, Noah, Shen, Shu-zhong
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2021
Materias:
Earth, Environmental, Ecological, and Space Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8597993/
https://www.ncbi.nlm.nih.gov/pubmed/34788084
http://dx.doi.org/10.1126/sciadv.abh1390

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8597993/
https://www.ncbi.nlm.nih.gov/pubmed/34788084
http://dx.doi.org/10.1126/sciadv.abh1390

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