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The structure of the zooplankton community in Itapeva Lake was formed by four groups and more than 127 zooplankton species, in which microplankton was the predominant size structure. The largest richness recorded was of the protists group and in autumn seasonal campaign. Protists were characteristic of the lake, regarding density, except during spring at the Center point (copepods) and autumn at the South point (rotifers). The seasonal distribution revealed that during summer, mean density increased in the zooplankton community, exactly the opposite of phytoplankton (that blooms during the cold season). However, the maximum density was recorded during autumn. High density was recorded for the ciliate Codonella sp. at all points and during all seasons. The abundance of the tecamoeba Difflugia tuberculata was strongly associated with the maximum effects of fetch in the lake. Rotifers were generally the second most representative groups in terms of density. Rotifers and Cladocera were more abundant in summer, whereas copepods were in spring and winter/98. The Shannon–Wiener index showed that the smallest zooplankton diversity average occurred during the winter/98 (H=1.44), while in autumn the largest zooplankton diversity average (H=2.36) was observed. Correlations (r-Pearson, p<0.05) with wind velocity were significant for zooplankton density (groups and/or abundant species), diversity, and richness. The analysis of variance (ANOVA) showed a seasonally significant spatial-temporal variation for the factors sampling point, day and shift (p<0.01). Temporal alterations in density, diversity and richness were closely dependent on the hydrodynamic action induced by the wind on the spatial distribution of the zooplankton community in the Itapeva Lake. [ABSTRACT FROM AUTHOR]