Evidence for elevated alkalinity in the glacial Southern Ocean

An increase in whole ocean alkalinity during glacial periods could account, in part, for the drawdown of atmospheric CO₂ into the ocean. Such an increase was inevitable due to the near elimination of shelf area for the burial of coral reef alkalinity. We present evidence, based on downcore measureme...

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Bibliografiske detaljer
Main Authors: Rickaby, R, Elderfield, H, Roberts, N, Hillenbrand, C, Mackensen, A
Format: Journal article
Sprog:English
Udgivet: American Geophysical Union 2010
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