Articles | Volume 7, issue 8
16 Aug 2010
 | 16 Aug 2010

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)

E. Douville, M. Paterne, G. Cabioch, P. Louvat, J. Gaillardet, A. Juillet-Leclerc, and L. Ayliffe

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Cited articles

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Asami, R., Felis, T., Deschamps, P., Hanawa, K., Iryu, Y., Bard, E., Durand, M., and Murayama, M.: Evidence for tropical South Pacific climate change during the Younger Dryas and the Bølling-Allerød from geochemical records of fossil Tahiti corals, Earth Planet. Sc. Lett., 288, 96–107, 2009.
Bard, E., Hamelin, B., Arnold, M., Montaggioni, L., Cabioch, G., Faure, G., and Rougerie, F.: Deglacial sea-level record from Tahiti corals and the timing of global melt water discharge, Nature, 382, 241–244, 1996.
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Boiseau, M.: Etude de la variabilité climatique liée à l'ENSO dans l'Océan Pacifique Central Sud (Moorea) à partir de traceurs géochimiques contenus dans le squelette d'un Scleractiniaire à zooxanthelles (Porites Lutea), pH'D thesis, University of Paris VII, Paris, 202 pp., 1998.
Final-revised paper