[1] Rates of net production, net calcification, and nutrient uptake were measured in a coral-dominated reef flat community on Ningaloo Reef in northwestern Australia under seasonally minimum and maximum light levels. Daily integrated light decreased twofold while water temperatures remained relatively constant increasing by only 1 C on average from summer to winter. Rates of daily community gross primary production (GPP) were only 33% AE 9% higher in summer than in winter (1400 AE 70 versus 1050 , respectively), despite evidence of sporadically high nitrate uptake in both seasons. In summer, rates of hourly net calcification (g net ) were linearly correlated with diurnal changes in net production, pH, and aragonite saturation state (W ar ); and were mostly correlated with light except at mid-day under heavy cloud cover. However, in winter, g net was independent of diurnal changes in light, net production, pH, and W ar indicating that the reef flat community had possibly reached a threshold above which rates of net calcification were insensitive to diurnal changes in their environment.

This study investigated the variation of bioerosional processes in relation to disturbances of reefal communities due to eutrophication. La Saline fringing reef (Reunion Island) is subjected to nutrient inputs from the adjacent land. Bioerosion by grazers, microborers, and macroborers was measured using experimental substrata exposed for 1 year in three sites characterized by different levels of nutrient input and benthic community response. The relationship between bioerosion and epilithic algal cover of hard substrata and the interactions between the various agents of bioerosion were analyzed with parametric statistics. Significant variations in bioerosion were found among sites, ranging from 1.63 to 3.52 kg CaCO 3 m -2 year -1 for grazing rates, from 6.73 to 32.25 g m -2 year -1 for macroboring rates, and from 43.78 to 67.56 g m -2 year -1 for microboring rates. One of the major factors controlling these variations appeared to be changes in the epilithic algal cover on substrata in response to changes in reefal water chemistry. In low nutrient areas, where dead corals were colonized mainly by algal turfs, erosion by microorganisms was low (43.78 g m -2 year -1 ) due to intense grazing (3.52 kg m -2 year -1 ). In reef zones receiving high nutrient inputs, the development of encrusting calcareous algae and macroalgae was associated with the lowest grazing (1.63 kg m -2 year -1 ) and macroboring (6.73 g m -2 year -1 ) rates recorded among sites. In contrast, high microboring rates (57.54 and 67.56 g m -2 year -1 ) were found in enriched areas in association with high macroalgal cover.

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