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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Detalles Bibliográficos
Autores principales: Kubota, Kaoru, Yokoyama, Yusuke, Ishikawa, Tsuyoshi, Obrochta, Stephen, Suzuki, Atsushi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4052749/
https://www.ncbi.nlm.nih.gov/pubmed/24918354
http://dx.doi.org/10.1038/srep05261

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4052749/
https://www.ncbi.nlm.nih.gov/pubmed/24918354
http://dx.doi.org/10.1038/srep05261

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