Duprey N., Lazareth Claire E., Corrège T., Le Cornec Florence, Maes Christophe, Pujol N., Mandeng Yogo Magloire, Caquineau Sandrine, Derome C. S., Cabioch Guy. (2012). Early mid-Holocene SST variability and surface-ocean water balance in the southwest Pacific. Paleoceanography, 27, p. PA4207. ISSN 0883-8305.
Titre du document
Early mid-Holocene SST variability and surface-ocean water balance in the southwest Pacific
Duprey N., Lazareth Claire E., Corrège T., Le Cornec Florence, Maes Christophe, Pujol N., Mandeng Yogo Magloire, Caquineau Sandrine, Derome C. S., Cabioch Guy
Source
Paleoceanography, 2012,
27, p. PA4207 ISSN 0883-8305
We present early mid-Holocene records of Sr/Ca, delta O-18 and delta(18)Osw from marine archives collected in Vanuatu: two Porites sp. corals (6.7- 6.5 ka BP) and a Tridacna maxima giant clam (6.2-6.0 ka BP). Sr/Ca, delta O-18, and delta O-18(sw) were used as proxies for sea surface temperature (SST) and sea surface salinity (SSS). The fossil geochemical records were compared to modern Porites sp. and T. maxima records. Reconstructed mean SSTs from the two fossil Porites sp. and from the modern coral are similar, implying that the Western Pacific Warm Pool (WPWP)' southern edge had reached its modern location by 6.7- 6.5 ka BP. The post-glacial SST rise in the Southwest Pacific was thus completed by the early mid-Holocene. The two early mid-Holocene corals and the giant clam recorded saltier conditions than modern related to 1) a decoupling between the precipitation regime and the SPCZ due to a northerly position of this climatic feature and 2) an increase of the moisture transport to the extra-tropics, driven by a strengthened or extended Hadley cell. The longest delta O-18 coral profile displays an El Nino Southern Oscillation (ENSO) signal reduced by 20-30% compared to the period 1928-1992, in concordance with the reduced ENSO variability observed in the Pacific area during the first half of the Holocene. However, the decoupling between the SPCZ and the precipitation regime may have also contributed to the weak ENSO signal recorded in the early mid-Holocene coral delta O-18 profile.
