VARIATION IN PHYTOPLANKTON COMPOSITION WITHIN LARGER RIVERS: STABLE ISOTOPIC APPROACH Anita J. Kumar and Michael D. Delong Large River Studies Center, Biology Department, Winona State University, Winona, MN 55987 A number of recent studies have indicated that autochthonous primary production, particularly phytoplankton, are a major food source in floodplain ecosystems. Previous studies have also shown phytoplankton concentrations change overtime as a function of biological, chemical, and physical attributes of the river ecosystems. This study examined the carbon and nitrogen stable isotope ratios phytoplankton both main channel and backwater habitats on four separate dates (June-August). The study was conducted in Reaches 5 and 6 of the Upper Mississippi River. Standard techniques used in past studies were employed for collection and processing of TOM samples. Algal and detrital fractions were separated using colloidal silica centrifugation. TOM was divided in the field and laboratory into fine TOM (FTOM; 1000-100 ?m) and ultrafine (UTOM; 100-1 ?m). Samples were shipped to Kansas State University for determination of carbon and nitrogen stable isotope ratios. Carbon isotope ratios of phytoplankton in both the main channel and backwaters increased during the course of the study. Nitrogen stable isotope ratios decreased in both habitats over the course of the study, with ?15N of backwater phytoplankton decreasing more than observed in the main channel. This study indicates that the inorganic carbon and nitrogen sources used by phytoplankton change as hydrological retention time in main channel and backwater habitats increases. The decrease in ?15N reflects a likely shift from biogenic inorganic nitrogen to atmospheric nitrogen. The findings of this study suggest that hydrological retention time is also important in shaping system function in the main channel. Keywords: transport organic matter, Upper Mississippi River, phytoplankton, backwater, main channel, hydrology, stable isotope