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...
| Päätekijät: | , , , , |
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| Aineistotyyppi: | Journal article |
| Kieli: | English |
| Julkaistu: |
American Geophysical Union
2010
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| Aiheet: |
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