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...

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Detalles Bibliográficos
Autores principales: Ronge, Thomas A., Frische, Matthias, Fietzke, Jan, Stephens, Alyssa L., Bostock, Helen, Tiedemann, Ralf
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
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

Internet

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

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