Equatorial Pacific seawater pCO(2) variability since the last glacial period

The ocean may have played a central role in the atmospheric pCO(2) rise during the last deglaciation. However, evidence on where carbon was exchanged between the ocean and the atmosphere in this period is still lacking, hampering our understanding of global carbon cycle on glacial–interglacial times...

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Detalles Bibliográficos
Autores principales: Kubota, Kaoru, Yokoyama, Yusuke, Ishikawa, Tsuyoshi, Sagawa, Takuya, Ikehara, Minoru, Yamazaki, Toshitsugu
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6761199/
https://www.ncbi.nlm.nih.gov/pubmed/31554821
http://dx.doi.org/10.1038/s41598-019-49739-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6761199/
https://www.ncbi.nlm.nih.gov/pubmed/31554821
http://dx.doi.org/10.1038/s41598-019-49739-0

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