TEMPORAL AND SPATIAL VARIATION IN ZOOPLANKTON FLUX RATES IN THE OHIO RIVER. Debbie L. Guelda 1,2, Richard W. Koch 3,2, Jeff D. Jack 2, and Paul A. Bukaveckas 2. 1 Bemidji State University, Bemidji, MN 56601. 2 Department of Biology and Center for Watershed Research, University of Louisville, Louisville, KY 40292. 3 North Central Research Station, USDA Forestry Service, Grand Rapids MN 55744. We conducted a 3 year survey in the lower Ohio River (RKM 854-1500) assessing physiochemical and biological parameters such as zooplankton flux rates. The portion of the Ohio River in the study receives inputs from five major tributaries which have unique chemical and biological properties reflective of their watersheds. For 1998-2000, zooplankton species richness was inversely correlated with discharge and the tributaries differed in zooplankton species structure. Zooplankton flux rates (as individuals second-1 or grams carbon second-1) also varied with discharge. Budgets of zooplankton carbon provided input contribution of zooplankton from the upper Ohio River and tributaries. Inputs from the upper Ohio River provided 38% of zooplankton carbon and were not correlated with discharge. Tributaries provided 63% of zooplankton inputs; the importance of which varied seasonally and temporally. The most important tributaries contributing zooplankton carbon to the Ohio River were those draining reservoirs (Cumberland and Tennessee Rivers). Zooplankton showed no relationship with chlorophyll a or POC. The Ohio River acted as a net source of zooplankton carbon during 4 of our sampling times for groups such as Ceriodaphnia, Diphanosoma, and rotifers and often acted as a sink for Bosmina. Zooplankton flux differed depending on position in the basin; the upstream portion of the study area was a 'source' of zooplankton, while the downstream area upstream of the Ohio River's confluence with the Mississippi River acted as a 'sink' to zooplankton. Keywords: zooplankton, Ohio River, budget, flux rates, discharge