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At Urelapa island, Vanuatu, sea-level rise and a tectonic uplift of ~3mmyr -1 have controlled water depth and the colonization and reef development on a substrate from 23 until 6calkyr BP. Analysis of coralgal assemblages offers insights on the mode of reef growth and on water depth over the reef for the studied period. Those assemblages, precisely dated by the 230 Th/...