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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...
| Autores principales: | , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2023
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| Materias: | |
| 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 |