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...

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Detalles Bibliográficos
Autores principales: Ohta, Junichiro, Yasukawa, Kazutaka, Nozaki, Tatsuo, Takaya, Yutaro, Mimura, Kazuhide, Fujinaga, Koichiro, Nakamura, Kentaro, Usui, Yoichi, Kimura, Jun-Ichi, Chang, Qing, Kato, Yasuhiro
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
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

Internet

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

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