Not AvailableAreas of remarkably higher concentrations of zooplankton standing stock were encountered in the northeastern (12°46'-13° 30 N and 93°03'-93°35' E) and southern (08°30'-09°30'N and 92o00'-92o41'E) regions the Andaman and Nicobar seas. The NE monsoon (October-January) was the most productive season followed by the premonsoon (February-May). The zooplankton population occurred in high abundance when the surface waters were characterised by low temperature and salinity. Occurrence of eggs and larvae of finfishes, pelagic tunicates, euphausiids, copepods, amphipods, foraminifers and lucifers in profusion accounted for the NE monsoon maximum. SW monsoon (June-September) was the least productive season. Monthly variations di...