Expanded oxygen minimum zones during the late Paleocene‐early Eocene: Hints from multiproxy comparison and ocean modeling

Anthropogenic warming could well drive depletion of oceanic oxygen in the future. Important insight into the relationship between deoxygenation and warming can be gleaned from the geological record, but evidence is limited because few ocean oxygenation records are available for past greenhouse clima...

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Veröffentlicht in:	Paleoceanography 2016-12, Vol.31 (12), p.1532-1546
Hauptverfasser:	Zhou, X., Thomas, E., Winguth, A. M. E., Ridgwell, A., Scher, H., Hoogakker, B. A. A., Rickaby, R. E. M., Lu, Z.
Format:	Artikel
Sprache:	eng
Schlagworte:	Anthropogenic factors benthic Bottom water Boundary conditions Climate models Climate system Climatic conditions Dissolved oxygen Eocene foraminifera I/Ca Intermediate water Iodine Marine Oceanography Oceans Oxygen Oxygenation Paleocene Paleoclimate science Pore water Seawater Speciation
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