Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth

During the Late Cretaceous and early Cenozoic the Earth experienced prolonged climatic cooling most likely caused by decreasing volcanic activity and atmospheric CO(2) levels. However, the causes and mechanisms of subsequent major global warming culminating in the late Paleocene to Eocene greenhouse...

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Detalles Bibliográficos
Autores principales: Batenburg, S. J., Voigt, S., Friedrich, O., Osborne, A. H., Bornemann, A., Klein, T., Pérez-Díaz, L., Frank, M.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6251870/
https://www.ncbi.nlm.nih.gov/pubmed/30470783
http://dx.doi.org/10.1038/s41467-018-07457-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6251870/
https://www.ncbi.nlm.nih.gov/pubmed/30470783
http://dx.doi.org/10.1038/s41467-018-07457-7

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