Surface ocean warming and acidification driven by rapid carbon release precedes Paleocene-Eocene Thermal Maximum

The Paleocene-Eocene Thermal Maximum (PETM) is recognized by a major negative carbon isotope (δ(13)C) excursion (CIE) signifying an injection of isotopically light carbon into exogenic reservoirs, the mass, source, and tempo of which continue to be debated. Evidence of a transient precursor carbon r...

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Detalles Bibliográficos
Autores principales: Babila, Tali L., Penman, Donald E., Standish, Christopher D., Doubrawa, Monika, Bralower, Timothy J., Robinson, Marci M., Self-Trail, Jean M., Speijer, Robert P., Stassen, Peter, Foster, Gavin L., Zachos, James C.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2022
Materias:
Earth, Environmental, Ecological, and Space Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8926327/
https://www.ncbi.nlm.nih.gov/pubmed/35294237
http://dx.doi.org/10.1126/sciadv.abg1025

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8926327/
https://www.ncbi.nlm.nih.gov/pubmed/35294237
http://dx.doi.org/10.1126/sciadv.abg1025

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