We examined the impact of exposing natural populations of marine bacteria (from seawater collected near Woods Hole, Massachusetts, USA) to multiple nitrogen and carbon sources in a series of batch growth experiments conducted from 1989 through 1990. The substrate C:N ratio (C:N(S)) was varied from 1.5:1 to 10:1 either with equal amounts of NH4+ and different amino acids or an amino acid mixture, all supplemented with glucose to maintain the C:N(S) ratio equal to that of the respective amino acid, or with combinations of glucose and NH4+ alone. A common feature of the experiments involving amino acids was the concurrent uptake of NH4+ and amino acids that persisted as long as a readily assimilable carbon source (glucose in our case) was taken up. There was no net regeneration of NH4+, even though catabolism of amino acids occurred. Regeneration of NH4+ was evident only after glucose was completely utilized, which usually occurred at the end of exponential growth. The contribution of (NH4+)-N-15 to total nitrogen uptake by the end of exponential growth varied from approximately 60 to 80% when individual amino acids were present and down to approximately 24% when the amino acid mixture was added. These estimates are conservative because we did not account for possible isotope dilution effects resulting from amino acid catabolism. When NH4+ and glucose were the sole nitrogen and carbon sources, there was a stoichiometric balance between glucose and NH4+ uptake over a wide range of C:N(S) ratios, leading to a constant bacterial biomass C:N ratio (C:N(B)) of approximately 4.5:1. As a result NH4+ usage varied from 50% when the C:N(S) ratio was 3.6:1, to 100% when the C:N(S) ratio was 10:1. Gross growth efficiency varied from approximately 60% when NH4+ plus glucose were added alone or with the amino acid mixture, to 47% when the individual amino acids were used in place of the mixture. It is thus evident that actively growing bacteria will act as sinks for nitrogen when a carbon source that can be assimilated easily is available to balance NH4+ uptake, even when amino acids are available and are being co-metabolized.