MIS 7 interglacial sea-surface temperature and salinity reconstructions from a southwestern subtropical Pacific coral

We generated a 5.5-yr snapshot of biweekly-to-monthly resolved time series of carbon and oxygen isotope composition (delta C-13 and delta O-18) and Sr/Ca and Mg/Ca from annually banded aragonite skeleton of a similar to 197 ka pristine Porites coral collected at Niue Island (19 degrees 00'S, 169 degrees 50'W) in the southwestern subtropical Pacific Ocean. This report is the first of a high-resolution coral-based paleoclimate archive during the Marine Isotope Stage (MIS) 7 interglacial. Statistical results suggest that annual averages of sea-surface temperature (SST) and salinity (SSS) at similar to 197 ka were not significantly different from and similar to 1.2 higher than at present, respectively. Monthly mean variations showed increased SSS at similar to 197 ka that was higher (1.4-1.9 relative to today) in the austral summer than in the austral winter. Monthly SST and SSS anomalies at similar to 197 ka indicated smaller amplitudes by similar to 0.3 degrees C (11%) and similar to 0.3 (24%) relative to the present possibly suggesting less influence of interannual climate variability around Niue. Our results, taken together with other climate proxy records, imply seasonal and interannual modulation of thermal and hydrological conditions, different from today, in the southwestern subtropical Pacific Ocean associated with the Western Pacific Warm Pool and the South Pacific Convergence Zone variability during the MIS 7 interglacial. (C) 2013 University of Washington. Published by Elsevier Inc All rights reserved.