Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM

The Paleocene‐Eocene Thermal Maximum (PETM) is recognized globally by a negative excursion in stable carbon isotope ratios (δ(13)C) in sedimentary records, termed the carbon isotope excursion (CIE). Based on the CIE, the cause, duration, and mechanisms of recovery of the event have been assessed. He...

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Detalles Bibliográficos
Autores principales: Papadomanolaki, Nina M., Sluijs, Appy, Slomp, Caroline P.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9310739/
https://www.ncbi.nlm.nih.gov/pubmed/35910591
http://dx.doi.org/10.1029/2021PA004232

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9310739/
https://www.ncbi.nlm.nih.gov/pubmed/35910591
http://dx.doi.org/10.1029/2021PA004232

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