The relative importance of phytoplankton and heterotrophlc bacteria in the ut~lization of ammonium in a temperate coastal pelaglc environment (Long Island Sound. New York, USA) was examined uslng the short-lived radioisotope, I3N Uptake of ' 3~~: Into different slze fractions under simulated in situ temperature and light condihons was compared to size fractionations of bacterial abundance, chlorophyll, and uptake of tritlated thymidme and 14C-b~carbonate In January and Apnl, little ' 3~ entered the bactenal slze fract~on, but when bacteria were more metabolically a c t~v e in May and July, about '/3 of the total I3N uptake appeared in the size fraction conta~ning most of the bactena but httle of the chlorophyll (0 2 to 0 6 ,pm) Exposure to up to 8 mC1 I-' of I3N radioactivity d~d not ~n h~b~t bacterial or phytoplankton activity, and hlled controls showed virtually no uptake Ammonium uptake rates measured by I3N were comparable to those measured by the stable isotope 15N in 2 of 3 experiments The size fract~onation results were consistent wlth estimates of bactenal and phytoplankton demand tor nitrogen for growth Turnover rates for the dissolved a m m o n~u m pool ranged from 0 6 % h-' in April to 116 O/ O h-' in July In separate experiments .r\~th mlxed seawater cultures of bactena, the half-saturation constant (K,) for ammonium uptake was 1 0 1 uM, and ammonium uptake was reduced more by additions (100 to 1000 nM) of glutamine than by glutamate or othel ainlno a c~d s suggesting that glutamlne is directly ~nvolved in a m m o n~u m uptake In these bacteria