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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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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: Kubota, Kaoru, Yokoyama, Yusuke, Ishikawa, Tsuyoshi, Sagawa, Takuya, Ikehara, Minoru, Yamazaki, Toshitsugu
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2019
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Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC6761199/
https://ncbi.nlm.nih.gov/pubmed/31554821
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-019-49739-0
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