Six-fold increase of atmospheric pCO(2) during the Permian–Triassic mass extinction

The Permian–Triassic mass extinction was marked by a massive release of carbon into the ocean-atmosphere system, evidenced by a sharp negative carbon isotope excursion. Large carbon emissions would have increased atmospheric pCO(2) and caused global warming. However, the magnitude of pCO(2) changes...

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Detalles Bibliográficos
Autores principales: Wu, Yuyang, Chu, Daoliang, Tong, Jinnan, Song, Haijun, Dal Corso, Jacopo, Wignall, Paul B., Song, Huyue, Du, Yong, Cui, Ying
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8035180/
https://www.ncbi.nlm.nih.gov/pubmed/33837195
http://dx.doi.org/10.1038/s41467-021-22298-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8035180/
https://www.ncbi.nlm.nih.gov/pubmed/33837195
http://dx.doi.org/10.1038/s41467-021-22298-7

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