The enigma of Oligocene climate and global surface temperature evolution

Falling atmospheric CO(2) levels led to cooling through the Eocene and the expansion of Antarctic ice sheets close to their modern size near the beginning of the Oligocene, a period of poorly documented climate. Here, we present a record of climate evolution across the entire Oligocene (33.9 to 23.0...

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Detalles Bibliográficos
Autores principales: O’Brien, Charlotte L., Huber, Matthew, Thomas, Ellen, Pagani, Mark, Super, James R., Elder, Leanne E., Hull, Pincelli M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2020
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7568263/
https://www.ncbi.nlm.nih.gov/pubmed/32989142
http://dx.doi.org/10.1073/pnas.2003914117

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7568263/
https://www.ncbi.nlm.nih.gov/pubmed/32989142
http://dx.doi.org/10.1073/pnas.2003914117

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