Seasonal and spatial variations in bacterial and picoplankton abundanc
es and bacterial production (thymidine incorporation rates) were deter
mined in the water column up to 150 m in several stations in the centr
al and eastern Arabian Sea. Higher bacterial densities of about 1 x 10
(9) cells L(-1) were observed during the intermonsoon periods of Septe
mber and April/May compared to the southwest monsoon period of July/Au
gust and the winter period of February/March Although primary producti
on was low during April/May, bacterial production was much higher duri
ng this period unlike July/August. it also showed an increase from the
northern to the southern Arabian Sea, suggesting the presence of high
amounts of dissolved organic carbon in this area. High picoplankton d
ensities, ranging up to 45 x 10(6) cells L(-1) were observed during Fe
bruary, particularly in the northern Arabian Sea. Rapid turnover of ba
cteria during the intermonsoon period of April/May suggests the predom
inance of a 'microbial loop' in the foodweb and a prevailing source of
dissolved organic carbon in the oceanic waters.