摘要：We used a high-resolution oxygen isotope (δ(18)Ocoral), carbon isotope (δ(13)Ccoral) and Sr/Ca ratios measured in the skeleton of a reef-building coral, Porites sp., to reveal seasonal-scale upwelling events and their interannual variability in the Gulf of Oman. Our δ(13)Ccoral record shows sharp negative excursions in the summer, which correlate with known upwelling events. Using δ(13)Ccoral anomalies as a proxy for upwelling, we found 17 summer upwelling events occurred in the last 26 years. These anomalous negative excursions of δ(13)Ccoral result from upwelled water depleted in (13)C (dissolved inorganic carbon) and decreased water-column transparency. We reconstructed biweekly SSTs from coral Sr/Ca ratios and the oxygen isotopic composition of seawater (δ(18)OSW) by subtracting the reconstructed Sr/Ca-SST from δ(18)Ocoral. Significant δ(18)OSW anomalies occur during major upwelling events. Our results suggest δ(13)Ccoral anomalies can be used as a proxy for seasonal upwelling intensity in the Gulf of Oman, which, driven by the Indian/Arabian Summer Monsoon, is subject to interannual variability.
