Early Eocene deep-sea benthic foraminiferal faunas: Recovery from the Paleocene Eocene Thermal Maximum extinction in a greenhouse world

The early Eocene greenhouse world was marked by multiple transient hyperthermal events. The most extreme was the Paleocene-Eocene Thermal Maximum (PETM, ~56 Ma), linked to the extinction of the globally recognised deep-sea benthic foraminiferal Velasco fauna, which led to the development of early Eo...

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Detalles Bibliográficos
Autores principales: Arreguín-Rodríguez, Gabriela J., Thomas, Ellen, D’haenens, Simon, Speijer, Robert P., Alegret, Laia
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2018
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5825042/
https://www.ncbi.nlm.nih.gov/pubmed/29474429
http://dx.doi.org/10.1371/journal.pone.0193167

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5825042/
https://www.ncbi.nlm.nih.gov/pubmed/29474429
http://dx.doi.org/10.1371/journal.pone.0193167

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