Abstract:
Based on the determination of the oxygen isotopic analysis of the skeleton of living
Porites lutea in Shalao fringing reef, Hainan Island, we obtained a coral δ
18O record for an 11 year period(1992-2002). We have assessed the characteristics of coral δ
18O signals responding to environmental conditions by comparing coral δ
18O variation with a local record of sea surface temperature (SST) and sea surface salinity (SSS), respectively. We conclude from our comparison that the annual variation of δ
18O is controlled by SST, whereas the seasonal variation of it by SSS.