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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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| Publicado no: | Paleoceanography |
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| Main Authors: | , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
John Wiley and Sons Inc.
2016
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4950126/ https://ncbi.nlm.nih.gov/pubmed/27478302 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1002/2016PA002954 |
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