Marine siliceous ecosystem decline led to sustained anomalous Early Triassic warmth

In the wake of rapid CO(2) release tied to the emplacement of the Siberian Traps, elevated temperatures were maintained for over five million years during the end-Permian biotic crisis. This protracted recovery defies our current understanding of climate regulation via the silicate weathering feedba...

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Detalles Bibliográficos
Autores principales: Isson, Terry T., Zhang, Shuang, Lau, Kimberly V., Rauzi, Sofia, Tosca, Nicholas J., Penman, Donald E., Planavsky, Noah J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9206662/
https://www.ncbi.nlm.nih.gov/pubmed/35717338
http://dx.doi.org/10.1038/s41467-022-31128-3

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9206662/
https://www.ncbi.nlm.nih.gov/pubmed/35717338
http://dx.doi.org/10.1038/s41467-022-31128-3

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