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Volume 7, issue 8
Biogeosciences, 7, 2445–2459, 2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 7, 2445–2459, 2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

  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. Douville1, M. Paterne1, G. Cabioch2, P. Louvat3, J. Gaillardet3, A. Juillet-Leclerc1, and L. Ayliffe4 E. Douville et al.
  • 1Laboratoire des Sciences du Climat et de l'Environnement, Institut Pierre Simon Laplace (LSCE/IPSL) Domaine du CNRS, UMR 8212, Av. de la Terrasse, 91198 Gif/Yvette, France
  • 2Institut de Recherche pour le Développement (IRD), UMR IPSL/LOCEAN, UPMC/CNRS/IRD/MNHN, 32 avenue Henri Varagnat, 93143 Bondy CEDEX, France
  • 3Institut Physique du Globe de Paris (IPG-Paris), Laboratoire de Géochimie et de Cosmochimie, Place Jussieu, 75252 Paris, France
  • 4Research School of Earth Sciences, Australian National University, ACT 0200, Canberra, Australia

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 Glacial Period and the Holocene. Boron isotopes were measured by Multi-Collector – Inductively Coupled Plasma Mass Spectrometry (MC-ICPMS) with an external reproducibility of 0.25‰, allowing a precision of about ±0.03 pH-units for pH values between 8 and 8.3. The boron concentration [B] and isotopic composition of modern samples indicate that the temperature strongly controls the partition coefficient KD for different aragonite species. Modern coral δ11B values and the reconstructed sea surface pH values for different Pacific areas match the measured pH expressed on the seawater scale and confirm the calculation parameters that were previously determined by laboratory calibration exercises. Most ancient sea surface pH reconstructions near Marquesas are higher than modern values. These values range between 8.19 and 8.27 for the Holocene and reached 8.30 at the end of the last glacial period (20.7 kyr BP). At the end of the Younger Dryas (11.50±0.1 kyr BP), the central sub-equatorial Pacific experienced a dramatic drop of up to 0.2 pH-units from the average pH of 8.2 before and after this short event. Using the marine carbonate algorithms, we recalculated the aqueous pCO2 to be 440±25 ppmV at around 11.5 kyr BP for corals at Marquesas and ~500 ppmV near Tahiti where it was assumed that pCO2 in the atmosphere was 250 ppmV. Throughout the Holocene, the difference in pCO2 between the ocean and the atmosphere at Marquesas (ΔpCO2) indicates that the surface waters behave as a moderate CO2 sink or source (−53 to 20 ppmV) during El Niño-like conditions. By contrast, during the last glacial/interglacial transition, this area was a marked source of CO2 (21 to 92 ppmV) for the atmosphere, highlighting predominant La Niña-like conditions. Such conditions were particularly pronounced at the end of the Younger Dryas with a large amount of CO2 released with ΔpCO2 of +185±25 ppmV. This last finding provides further evidence of the marked changes in the surface water pH and temperature in the equatorial Pacific at the Younger Dryas-Holocene transition and the strong impact of oceanic dynamic on the atmospheric CO2 content.

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