Pliocene cooling enhanced by flow of low-salinity Bering Sea water to the Arctic Ocean

Warming of high northern latitudes in the Pliocene (5.33–2.58 Myr ago) has been linked to the closure of the Central American Seaway and intensification of North Atlantic Deep Water. Subsequent cooling in the late Pliocene may be related to the effects of freshwater input from the Arctic Ocean via t...

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Detalles Bibliográficos
Autores principales: Horikawa, Keiji, Martin, Ellen E., Basak, Chandranath, Onodera, Jonaotaro, Seki, Osamu, Sakamoto, Tatsuhiko, Ikehara, Minoru, Sakai, Saburo, Kawamura, Kimitaka
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Pub. Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4491831/
https://www.ncbi.nlm.nih.gov/pubmed/26119338
http://dx.doi.org/10.1038/ncomms8587

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4491831/
https://www.ncbi.nlm.nih.gov/pubmed/26119338
http://dx.doi.org/10.1038/ncomms8587

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