I/Ca in epifaunal benthic foraminifera: A semi-quantitative proxy for bottom water oxygen in a multi-proxy compilation for glacial ocean deoxygenation

I/Ca in epifaunal benthic foraminifera: A semi-quantitative proxy for bottom water oxygen in a multi-proxy compilation for glacial ocean deoxygenation

The decline in dissolved oxygen in global oceans (ocean deoxygenation) is a potential consequence of global warming which may have important impacts on ocean biogeochemistry and marine ecosystems. Current climate models do not agree on the trajectory of future deoxygenation on different timescales,...

Podrobná bibliografie
Hlavní autoři:	Lu, W, Rickaby, REM, Hoogakker, BAA, Rathburn, AE, Burkett, AM, Dickson, AJ, Martinez-Mendez, G, Hillenbrand, C-D, Zhou, X, Thomas, E, Lu, Z
Médium:	Journal article
Jazyk:	English
Vydáno:	Elsevier 2020

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