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sitivity to temporal and intercolonial variations in skeletal growth rate (Hayashi et al., 2013). Testing these results requires environmental reconstruction from corals located along the periphery of their habitable range. Well-developed Porites colonies persist near the northerly limit of hermatypic corals at Ushibuka, Japan in the Amakusanada, east of the East China Sea (32°N, 130°E), where they experience large seasonal SST variations (the average amplitude is 11.7°C) and winter minima of approximately 14°C (Omata et al., 2006). This results in very low growth rates at this location (Fallon et al., 1999), as opposed to corals from similar latitudes in Bermuda (32°N) and Western Australia (29°S), the sites of the paleoceanographic mid-latitude hermatypic coral reconstructions reported to date, where winter temperatures remain above 18°C (Kuhnert et al., 1999, 2005). Here, we compare new, high-resolution Sr/Ca data, measured along the growth axes of Porites from Ushibuka, to previously published δ18O data from the same specimens (Omata et al., 2006).

Coral growth-rate insensitive Sr/Ca as a robust temperature recorder at the extreme latitudinal limits of Porites