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ABSTRACT SUPPLIED BY ORIGINATOR: The isotopic and elemental composition of sclerosponge skeletons are used to reconstruct paleoceanographic records. Yet few studies have systematically examined the natural variability in sclerosponge skeletal d18O, growth, and Sr/Ca, and how that may influence the interpretation of sclerosponge proxy records. Here, we analyzed short records in seven specimens of Acanthocheatetes wellsi (high-Mg calcite, 21 mol% Mg) from Palau, four A. wellsi (high-Mg calcite, 21 mol% Mg) from Saipan, and three Astroclera willeyana (aragonite) sclerosponges from Saipan, as well as one long record in an A. wellsi specimen from Palau spanning 1945-2001.5. In Saipan, species-specific and mineralogical effects appear to have a negligible effect on sclerosponge d18O, facilitating the direct comparison of d18O records between species at a given location. At both sites, A. wellsi d18O and growth rates were sensitive to environmental conditions, while Sr/Ca was not. High-resolution d18O analyses confirmed this finding as both A. wellsi and A. willeyana deposited their skeleton following the trends in isotopic equilibrium with seawater, though with a 0.27 pdf mil offset in the case of A. willeyana. In the high Mg-calcite species A. wellsi, Mg may be interfering with Sr incorporation into the skeleton. On multi-decadal timescales, A. wellsi sclerosponge d18O in Palau tracked the Southern Oscillation Index variability post-1977, but not pre-1977, coincident with the switch in the Pacific Decadal Oscillation (PDO) ~1976. This suggests that water mass circulation in the region is influenced by ENSO variability during positive PDO phases, but not during negative ones.</gco:CharacterString>
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