Particulate organic carbon and particulate organic nitrogen show a dec
reasing trend towards the sea. Dissolved silica and phosphorus showed
an erratic variation in the Cauvery estuary. The delta C-13 shows a ma
rginal conservative behaviour in the Cauvery estuary. Reduction in the
dissolved P and Si concentrations are accompanied by enhanced levels
in particulates. Phosphorus in sediments occurred in all the size frac
tions and possibly exist as a ferric and/or calcium phosphate.