Urea uptake rates of Thalassiusiru pseudonana (clone 3H) were determined using [14C]urea,[15N]urea, and by measuring disappearance of dissolved urea from the medium after adding 10 lg-atoms urea-N liter-'. In nitrate-sufficient cultures, the average [14C]urea uptake rate was 60% of the urea disappearance rate. Nitrate uptake continued in the presence of urea at a reduced rate, and only 15% of the urea N taken up was retained by the phytoplankton.The increase in PON during incubation was roughly equal to the total NO, and urea N taken up. Average urea uptake rates measured by all methods in 24-h nitrate-starved cultures were in excellent agreement with the rate of increase in PON during a l-h incubation. Uptake rate of [14C]urea and disappearance rate of urea were constant and equal. In neither nitrate-sufficient nor nitrate-starved cultures were [15N]urea uptake rates constant, with maximal rates measured 5.-l 5 min after the addition of urea.Ammonium was released by T. pseudonana following uptake of urea and was then taken up. A model of urea uptake and assimilation by T. pseudonana that involves efflux of urea N as NH, and its rapid reabsorption is proposed. These results can explain previous observations and have implications for utilization and cycling of urea N by phytoplankton in nature.Radioactive ( 14C) and stable (l 5N) isotope tracers of urea are used to measure urea uptake rates of phytoplankton in the laboratory and in nature, but uptake rates determined with these two isotopes are not always equal. Harrison et al. (1985) found that [ 14C]urea uptake rates were greater than [15N]urea uptake rates in the eastern Canadian Arctic, and Price and Harrison (in prep.) obtained similar results for urea uptake by Sargasso Sea plankton. In the Sargasso Sea, the time-courses of uptake of both labeled substrates were also different:[15N]urea incorporation by phytoplankton was roughly constant during a 24-h incubation period, while [ 14C]urea uptake was most rapid over the first 6 h of the incubation. Discrepancy between [14C]urea uptake and the change in the concentration of dissolved urea in seawater has also been re-L Present address: R. M. Parsons Laboratory, Bldg. 48-2 13,