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Southern Ocean contribution to both steps in deglacial atmospheric CO(2) rise
The transfer of vast amounts of carbon from a deep oceanic reservoir to the atmosphere is considered to be a dominant driver of the deglacial rise in atmospheric CO(2). Paleoceanographic reconstructions reveal evidence for the existence of CO(2)-rich waters in the mid to deep Southern Ocean. These w...
| Autores principales: | , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8585946/ https://www.ncbi.nlm.nih.gov/pubmed/34764385 http://dx.doi.org/10.1038/s41598-021-01657-w |