Dissolved organic matter (DOM) is the largest component of the organic matter pool in lotic ecosystems (1, 2). The concentrations and compositions of DOM vary spatially and temporally (3-5), which in turn affects the productivity of stream food webs (6, 7). Heterotrophic bacteria are major consumers of DOM (8, 9), and thus, DOM influences bacterial community composition (i.e., structure) and abundance (10-12).The processing and fate of organic carbon (C) is fundamentally and synergistically linked to the nitrogen (N) cycle (13,14). Despite this linkage between the C and N cycles, many studies focus solely on C dynamics (15)(16)(17) or N dynamics (18-20) rather than their interrelationship. In streams, specifically, C and N are tightly linked (21), and C availability strongly influences N dynamics (22, 23), yet our knowledge of how specific properties of DOM influence N dynamics is limited.Nitrogen is an important component of DOM (24), and a major fraction (often more than 50%) of the total dissolved N pool is dissolved organic nitrogen (DON) (25-27). The DON pool is composed of a continuum of compounds ranging from high-molecular-weight polymers, like polypeptides, to low-molecularweight monomers, like amino acids and urea (28,29). DON is also derived from different sources (e.g., allochthonous versus autochthonous), which influence the composition and lability (30,31).Allochthonous sources contribute the majority of refractory DON to streams (32), whereas alga-derived DON is more labile (33,34). DON utilization by heterotrophic bacteria varies; the labile fraction is readily utilized (35-38), while the recalcitrant fraction is utilized with the aid of extracellular enzymes (39).Reliance on organic versus inorganic forms of N depends on N availability. The ability to take up dissolved inorganic nitrogen (DIN) in the form of nitrate or ammonia is widespread among bacteria; ammonia uptake is energetically favorable, but often nitrate is more available (40, 41). Although DON serves as a potential N (and C) source for microbial communities (28,29,42), bacterial metabolism of DON is influenced by inorganic N concentrations (43). High DIN concentrations inhibit the production of enzymes that scavenge N from DON (44) and reduce extracellular hydrolysis of refractory DON (44,45).DOM serves as a substrate for bacterial growth (46), which in turn increases the demand for assimilation of nitrogen (21). DON serves, potentially, as both a C and an N source. The ability of DON to meet the metabolic demand for organic C likely influences the assimilative demand for N and whether, energetically, that demand is best met by N from DON or DIN. To empirically examine the impact of labile DOM on the responses of bacteria to DON and DIN, bacterial abundance and community composition (based on terminal restriction fragment length polymorphisms [T-RFLP] of 16S rRNA genes) (47) were examined in controlled laboratory microcosms subjected to various dissolved organic carbon (DOC), DON, and DIN treatments. Bacterial communities that had c...