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Larger CO(2) source at the equatorial Pacific during the last deglaciation
While biogeochemical and physical processes in the Southern Ocean are thought to be central to atmospheric CO(2) rise during the last deglaciation, the role of the equatorial Pacific, where the largest CO(2) source exists at present, remains largely unconstrained. Here we present seawater pH and pCO...
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| Autors principals: | , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group
2014
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4052749/ https://ncbi.nlm.nih.gov/pubmed/24918354 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep05261 |
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