Abstract
Abstract Radiocarbon dates on corals taken from the upper landward and seaward surfaces of fringing reefs on the north coast of Viti Levu, Fiji (18°S, 178°E), indicate the probable course of Holocene sea-level change. Sea level apparently rose to c. 0.45 m above present level by 5300 years B.P. and has since declined at a constant rate. These observations are consistent with other data from Viti Levu.
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