Production and accumulation of reef framework by calcifying corals and macroalgae on a remote Indian Ocean cay

Coral reefs face increasing pressures in response to unprecedented rates of environmental change at present. The coral reef physical framework is formed through the production of calcium carbonate (CaCO3) and maintained by marine organisms, primarily hermatypic corals, and calcifying algae. The northern part of Western Australia, known as the Kimberley, has largely escaped land-based anthropogenic impacts and this study provides important metabolic data on reef-building organisms from an undisturbed set of marine habitats. From the reef platform of Browse Island, located on the mid-shelf just inside the 200 m isobath off the Kimberley coast, specimens of the dominant coral (six species) and algal (five species) taxa were collected and incubated ex situ in light and dark shipboard experimental mesocosms for 4 h to measure rates of calcification and production patterns of oxygen. During experimental light and dark incubations, all algae were net autotrophic producing 6 to 111 mmolO(2)m(-2)d(-1). In contrast, most corals were net consumers of O2 with average net fluxes ranging from -42 to 47 mmolO(2)m(-2)d(-1). The net change in pH was generally negative for corals and calcifying algae (-0.01 to -0.08 h(-1)). Resulting net calcification rates (1.9 to 9.9 gCaCO(3)m(-2)d(-1)) for corals and calcifying algae (Halimeda and Galaxura) were all positive and were strongly correlated with net O-2 production. In intertidal habitats around Browse Island, estimated relative contributions of coral and Halimeda to the reef production of CaCO3 were similar at around 600 to 840 gm(-2)yr(-1). The low reef platform had very low coral cover of < 3 % which made a smaller contribution to calcification of similar to 240 gCaCO(3)m(-2)yr(-1). Calcification on the subtidal reef slope was predominantly from corals, producing similar to 1540 gCaCO(3)m(-2)yr(-1), twice that of Halimeda. These data provide the first measures of community metabolism from the offshore reef systems of the Kimberley. The relative contributions of the main reef builders, in these undisturbed areas, to net community metabolism and CaCO3 production is important to understand exclusively climate-driven negative effects on tropical reefs.