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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...
Guardat en:
| Publicat a: | Sci Rep |
|---|---|
| Autors principals: | , , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2019
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| Matèries: | |
| Accés en línia: | 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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