Atlantic Deep-water Response to the Early Pliocene Shoaling of the Central American Seaway

The early Pliocene shoaling of the Central American Seaway (CAS), ~4.7–4.2 million years ago (mega annum-Ma), is thought to have strengthened Atlantic Meridional Overturning Circulation (AMOC). The associated increase in northward flux of heat and moisture may have significantly influenced the evolu...

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Detalles Bibliográficos
Autores principales: Bell, David B., Jung, Simon J. A., Kroon, Dick, Hodell, David A., Lourens, Lucas J., Raymo, Maureen E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4507445/
https://www.ncbi.nlm.nih.gov/pubmed/26193070
http://dx.doi.org/10.1038/srep12252

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4507445/
https://www.ncbi.nlm.nih.gov/pubmed/26193070
http://dx.doi.org/10.1038/srep12252

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