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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...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
John Wiley and Sons Inc.
2022
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| Materias: | |
| 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 |