Pliocene‐Pleistocene evolution of sea surface and intermediate water temperatures from the southwest Pacific

Over the last 5 million years, the global climate system has evolved toward a colder mean state, marked by large‐amplitude oscillations in continental ice volume. Equatorward expansion of polar waters and strengthening temperature gradients have been detected. However, the response of the mid latitu...

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Detalles Bibliográficos
Autores principales: McClymont, Erin L., Elmore, Aurora C., Kender, Sev, Leng, Melanie J., Greaves, Mervyn, Elderfield, Henry
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2016
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4950126/
https://www.ncbi.nlm.nih.gov/pubmed/27478302
http://dx.doi.org/10.1002/2016PA002954

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4950126/
https://www.ncbi.nlm.nih.gov/pubmed/27478302
http://dx.doi.org/10.1002/2016PA002954

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