Glacial deep ocean deoxygenation driven by biologically-mediated air-sea disequilibrium

Glacial deep ocean deoxygenation driven by biologically-mediated air-sea disequilibrium

Deep ocean deoxygenation inferred from proxies has been used to support the hypothesis that a lower atmospheric carbon dioxide during glacial times was due to an increase in the strength of the ocean’s biological pump. This relies on the assumption that surface ocean oxygen (O2) is equilibrated with...

Disgrifiad llawn

Manylion Llyfryddiaeth
Prif Awduron:	Cliff, E, Khatiwala, S, Schmittner, A
Fformat:	Journal article
Iaith:	English
Cyhoeddwyd:	Nature Research 2021

Eitemau Tebyg

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