Southern Ocean contribution to both steps in deglacial atmospheric CO2 rise

Abstract 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 CO2. Paleoceanographic reconstructions reveal evidence for the existence of CO2-rich waters in the mid to deep Southern Ocean. Th...

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Autores principales: Thomas A. Ronge, Matthias Frische, Jan Fietzke, Alyssa L. Stephens, Helen Bostock, Ralf Tiedemann
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/12b5a8cc9a0a4d93944c45c3278007b8
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