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Abrupt sea surface pH change at the end of the Younger Dryas in the central sub-equatorial Pacific inferred from boron isotope abundance in corals (Porites)

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Authors

Douville, Eric
Paterne, Martine
Cabioch, Guy
Louvat, P.
Gaillardet, J.
Juillet-Leclerc, A.
Ayliffe, Linda

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Copernicus GmbH

Abstract

The "δ11B-pH" technique was applied to modern and ancient corals Porites from the sub-equatorial Pacific areas (Tahiti and Marquesas) spanning a time interval from 0 to 20.720 calendar years to determine the amplitude of pH changes between the Last Glaci

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Biogeosciences

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Restricted until

2037-12-31