Evidence for elevated alkalinity in the glacial Southern Ocean

Evidence for elevated alkalinity in the glacial Southern Ocean

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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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Bibliografische gegevens
Hoofdauteurs:	Rickaby, R, Elderfield, H, Roberts, N, Hillenbrand, C, Mackensen, A
Formaat:	Journal article
Taal:	English
Gepubliceerd in:	2010

Gelijkaardige items

Evidence for elevated alkalinity in the glacial Southern Ocean
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Gepubliceerd in: (2010)

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Benthic foraminiferal oxygen isotope offsets over the last glacial-interglacial cycle
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Deep ocean nutrients during the Last Glacial Maximum deduced from sponge silicon isotopic compositions (vol 292, pg 290, 2010)
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