El Nino-Southern Oscillation variability, salinity, coral geochemistry
Digital Object Identifier (DOI)
Coral skeletal geochemistry offers the potential to reconstruct the sea surface salinity (SSS) history of the tropical oceans on seasonal to interannual and perhaps centennial timescales because of the strong link between variation in SSS and seawater delta(18)O in tropical regions. We explore this potential using a monthly resolved, 65-year record of skeletal delta(18)O and Sr/Ca variations in a Porites coral from Espiritu Santo, Vanuatu. We demonstrate that El Nino-Southern Oscillation-related climate variability strongly influences coral delta(18)O at Santo through local salinity changes associated with the position of the South Pacific Convergence Zone and the movement of its associated salinity front. Such a demonstration provides the "ground truth'' data that can be used to place paleoclimate variability estimated using existing fossil coral records from this region into a modern conceptual framework. We also evaluate different methods of combining coral delta(18)O and Sr/Ca to reconstruct SSS and conclude that the coral delta(18\)O anomaly time series provides the best fit to recent in situ SSS data at Santo.
Was this content written or created while at USF?
Citation / Publisher Attribution
Paleoceanography, v. 19, no. 4, article PA4002.
Scholar Commons Citation
Kilbourne, K. H.; Quinn, Terrence M.; Taylor, Frederick W.; Delcroix, Thierry; and Gouriou, Yves, "El Nino Southern Oscillation-Related Salinity Variations Recorded in the Skeletal Geochemistry of a Porites Coral from Espiritu Santo, Vanuatu" (2004). Marine Science Faculty Publications. 113.