The temporal distributions of pigment on biogenic calcareous and terrigenic reef sediments, chlorophyll a, chlorophyll b, chlorophyll c, fucoxanthin, and porphine concentrations were measured monthly in two sediment columns (0 -15 cm) for one year. Pigment concentrations increased significantly during winter (November-April) in both sediment types particularly in the upper layers of the sediments. Phytoplankton contributions to organic matter were found to be 8 ± 3 and 6 ± 2% in calcareous and terrigenous sediments respectively. The accumulation and the successive degradation of phytoplankton detritus to inorganic nutrients in calcareous sand may partly sustain the productivity of the coral reef communities which live in nutrient-poor environments.