Ayling, BridgetMcCulloch, MalcolmGagan, MichaelStirling, Claudine HAndersen, MortenBlake, Steve2015-12-070012-821Xhttp://hdl.handle.net/1885/18581Past changes in the seasonal distribution of insolation across the Earth's surface are thought to play a critical role in Quaternary climate cycles. In this study we use Sr/Ca and δ18O as geochemical proxies in the skeleton of a fossil Porites coral to rKeywords: Fossil coral; Geochemical proxies; Insolation forcing; Sea surface temperature (SST); Seasonality; Atmospheric temperature; Climatology; Geochemistry; Geochronology; Oceanography; Reefs; Glacial geology; interglacial; marine isotope stage; sea surface tem ?18O; fossil coral; insolation forcing; seasonality; southeast Pacific; Sr/Ca; SST; U/Ca200610.1016/j.epsl.2006.06.0092015-12-07