Microzooplankton (heterotrophic microplankton and heterotrophic nanoflagellates) and their herbivorous activity were estimated from dilution experiments in August 1998 during two Lagrangian drift experiments that sampled contrasting conditions-an upwelling/relaxation event along the shelf edge and an oligotrophic offshore filament. During upwelling/relaxation, heterotrophic microplankton were present at mean surface concentrations between 15,000 and 48,000 cells l(-1). Heterotrophic nanoflagellate concentrations were between 200 and 700 cells ml(-1) and the most abundant component of the heterotrophic microplankton was the aloricate choreotrich ciliates which increased dramatically in concentration from 6,000 to 24,000 cells l(-1) during the first 4 days of the study. Total microzooplankton biomass reached a maximum of 39mgC.m(-3). In the filament, which developed from the upwelling, cell concentrations were lower and averaged 4,500 cells l(-1) for heterotrophic microplankton and 250 cells ml(-1) for heterotrophic nanoflagellates. Total microzooplankton biomass was about 10-12m-C.m(-3). Microzooplankton turned over between 40 and 85% of the phytoplankton standing stock, thereby consuming between 5 and 78mg phytoplankton carbon.m(-3) .d(-1). The magnitude of this activity was highest during upwelling/relaxation and was positively correlated to heterotrophic nanoflagellate biomass and chlorophyll-a concentration but not heterotrophic microplankton biomass. The proportion of primary production grazed decreased from 160 to 59% d(-1) during upwelling/relaxation and ranged between 60 and 90% d(-1) in the filament. Microzooplankton herbivory within the euphotic zone increased from 684 to >2000mgC.m(-2).d(-1) during upwelling/relaxation and was between 327 and 802mgC.m(-2).d(-1) in the filament. Although microzooplankton herbivory was lower and less variable during the filament study, microzooplankton consumed on average 60% of the phytoplankton standing stocks which was higher than found during upwelling/relaxation. Microzooplankton assimilation efficiency ranged between 3 and 33% during upwelling/relaxation and between 0 and 13% in the filament. Our data demonstrate a close coupling between phytoplankton growth and microzooplankton herbivory in surface waters off the Galician Coast and suggest that microzooplankton may have been a significant sink for phytogenic carbon during August 1998. (C) 2001 Elsevier Science Ltd. All rights reserved.