This paper focuses on the distribution of an important micronutrient element, phosphorus in the various coral reef sedimentary environments of the Lakshadweep Archipelago, in the Indian Ocean. One of the salient features observed is the high concentration of organic and residual phosphorous compared to inorganic phosphorous. This is particularly evident at stations characterised by higher total phosphorous concentrations. The concentrations of total phosphorous decrease with depth because of the upward migration of phosphate produced by mineralization of organic phosphorous and also as a result of the reduction of iron oxides to which phosphate is adsorbed. Among the inorganic forms, the major contribution towards total phosphorous pool was from calcium bound phosphorous. Sedimentary pH was not found to be a decisive factor in the distributional features of phosphorous forms in the surficial stations as well as in the core profile. In this study, organic carbon displayed co-variability with silty clay or fine sandy texture of the sediment. In most of the stations, organic carbon showed poor co-variance with organic and residual phosphorous form. This shows that major contribution towards organic and residual phosphorous form is from the residual fraction comprising biologically resistant or nonavailable phosphorous form composed of refractory materials.