Peak Cenozoic warmth enabled deep-sea sand deposition

The early Eocene (~ 56–48 million years ago) was marked by peak Cenozoic warmth and sea levels, high CO(2), and largely ice-free conditions. This time has been described as a period of increased continental erosion and silicate weathering. However, these conclusions are based largely on geochemical...

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Detalles Bibliográficos
Autores principales: Burton, Zachary F. M., McHargue, Tim, Kremer, Christopher H., Bloch, Roger B., Gooley, Jared T., Jaikla, Chayawan, Harrington, Jake, Graham, Stephan A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9908870/
https://www.ncbi.nlm.nih.gov/pubmed/36755039
http://dx.doi.org/10.1038/s41598-022-27138-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9908870/
https://www.ncbi.nlm.nih.gov/pubmed/36755039
http://dx.doi.org/10.1038/s41598-022-27138-2

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