ABSTRACT: Phytoplankton growth and microzooplankton grazing were investigated during the IronEx II mesoscale enrichment experiment using the seawater dilution technique combined with group-specific pigment markers. Growth rate estimates for thephytoplankton community increased ≥2-fold, from 0.6 d^-1 in the ambient environment to 1.2-1.6 d^-1 in the iron-enhanced bloom. Grazing lagged growth, allowing phytoplankton biomass to accumulate at a high rate (~0.8 d^-1)initially. However, grazing mortality ultimately increased 3- to 4-fold to 1.2-1.4 d^-1, largely balancing growth by Day 6 of the experiment. Increased rates were broadly distributed among phytoplankton taxa, but they differed in timing. Whereaspicophytoplankton showed more of a steady balance between growth and grazing, increasing grazing pressure on diatoms followed a 3-5-fold increase in larger (>20 µm) heterotrophic dinoflagellates and ciliates, which grew in response to enhanced diatombiomass. In the ambient environment, phytoplankton production was 15 to 20 µg C l^-1 d^-1, with diatoms accounting for 17% of growth and 7% of grazing losses. Total phytoplankton production increased to 150-200 µg C l^-1d^-1 at the peak of the patch bloom, where 79% of growth and 55% of microzooplankton grazing involved diatoms. Phytoplankton grazing mortality was significantly correlated with grazer biovolume, and high carbon-specific grazing estimates at thebloom peak indicated growth rates ~1.0 d^-1 for the heterotrophic community and up to 1.4 d^-1 for >20 µm heterotrophs. During several days when high phytoplankton biomass was relatively constant in the patch bloom, the pennatediatom dominated the community and remained physiologically healthy and growing at a fast rate, even though nutrient conditions were suboptimal. Efficient cropping of diatoms by large protistan grazers and rapid remineralization of iron and biogenicsilica were required to maintain this dynamic balance. Contrary to expectations, the carbon export ratio did not increase with the iron-induced diatom bloom. Thus, mesoscale iron-enrichment of high-nutrient, low chlorophyll waters in the easternequatorial Pacific clearly demonstrated that phytoplankton growth rates and standing stocks were iron-limited. However, the food web also demonstrated a remarkable resiliency to environmental perturbation by establishing a new balance in which theessential features of a microzooplankton-dominated, low export system were maintained.