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...
Autori principali: | Cliff, E, Khatiwala, S, Schmittner, A |
---|---|
Natura: | Journal article |
Lingua: | English |
Pubblicazione: |
Nature Research
2021
|
Documenti analoghi
-
Air-sea disequilibrium enhances ocean carbon storage during glacial periods
di: Khatiwala, S, et al.
Pubblicazione: (2019) -
Mechanisms driving glacial deep ocean deoxygenation
di: Cliff, E
Pubblicazione: (2022) -
Estimates of anthropogenic carbon in the Indian Ocean with allowance for mixing and time-varying air-sea CO2 disequilibrium
di: Hall, T, et al.
Pubblicazione: (2004) -
Eutrophication-Driven Deoxygenation in the Coastal Ocean
di: Nancy N. Rabalais, et al.
Pubblicazione: (2014-03-01) -
Deoxygenation in Marginal Seas of the Indian Ocean
di: S. Wajih A. Naqvi
Pubblicazione: (2021-02-01)