HOLOCENE INITIATION AND DEVELOPMENT OF NEW-CALEDONIAN FRINGING REEFS,SW PACIFIC

The analysis of 8 selected cores through fringing reefs in New Caledon ia reveals that accretion in the Holocene has been less than 6 m. The cores exhibit three main facies: branching coral (Acropora, dominantly ), massive coral heads (Porites, mainly) and coral sand/rubble, princi pally made up of acroporid fragments, Subordinate facies are composed of coralline algae and alcyonarian spiculite. The initiation of growth varies according to location. The southern reefs (i.e. early settled reefs) generally began to grow first, prior to 5000 y BP. The northern structures (i.e. more recently settled reefs) are younger, occurring after 4200 y BP. This retardation could be ascribed to differences in local physical conditions (nature of substrate, wave energy). Vertical accretion rates were generally higher in areas of lower energy (3.25- 6.4 mm . y(-1)) versus those exposed to higher energy conditions (1.4- 3.1 mm . y(-1)). Vertical development through time was accompanied by changes in composition of biological assemblages which reflect changes in hydrodynamics. The basal Acropora-dominated facies was replaced up wards by a Porites-dominated framework. The New Caledonian fringing re efs reached the sea surface generally between 5000 and 2500y BP after the stabilization of sea level. Hence all of these reefs can be classi fied as catch-up reefs.