Abstract
Different mixing schedules in marine microcosms were studied. Continuous mixing resulted in higher chlorophyll concentrations, lower nutrient concentrations and lower zooplankton [flagellates, rotifers and copepods] biomass than no mixing. No mixing caused water-column stratifications of chlorophyll and nutrients, as well as of organisms such as flagellates and rotifers adapted to low-mixing regimes. The most dramatic result was the low biomass of zooplankton in the continuously mixed microcosms and the high biomass of zooplankton in the unmixed microcosm.

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