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Add your Dating event free of charge, using our Promotion Centre.It is not surprising that constraining last interglacial sea-level changes within uncertainties of less than 1–2 m remains controversial, considering sea-level variations recognised between reef sites in the Holocene, and observed geographical variation in isostatic or flexural adjustments.Fossil coral reefs on uplifting margins also provide clear evidence for MIS substages 5c and 5a, and those on Huon Peninsula indicate fluctuations related to Heinrich events (MIS 3).An elevation of 6 m has commonly been adopted when correcting tectonically active sites for uplift.Recent compilations suggest elevations up to 8–9 m, but incorporate few observations from reefs where the last interglacial is found below sea level.