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Fish proliferation and rare-earth deposition by topographically induced upwelling at the late Eocene cooling event
The deep-sea clay that covers wide areas of the pelagic ocean bottom provides key information about open-ocean environments but lacks age-diagnostic calcareous or siliceous microfossils. The marine osmium isotope record has varied in response to environmental changes and can therefore be a useful st...
| Autores principales: | , , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7303186/ https://www.ncbi.nlm.nih.gov/pubmed/32555233 http://dx.doi.org/10.1038/s41598-020-66835-8 |