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...

书目详细资料
Main Authors:	Cliff, E, Khatiwala, S, Schmittner, A
格式:	Journal article
语言:	English
出版:	Nature Research 2021

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