URBAN, N. R., and EISENREICH, S. J. 1988. Nitrogen cycling in a forested Minnesota bog. Can. J. Bot. 66: 435-449.The nitrogen cycle of a small, forested, Sphagnum peatland in northern Minnesota was studied for 4 years. Hydrologic inputs and outputs (atmospheric deposition, upland runoff, streamflow) were monitored for 4 years, and annual uptake of N by vegetation was measured over a 3-year period. Microbe-mediated processes of nitrogen fixation and mineralization were measured in the laboratory and field, and accumulation rates of N within the peatland were measured in dated peat cores. Aerobic heterotrophs appear to be the dominant agents of N fixation at this site. Rates of N fixation decrease rapidly below the surface. Perhaps limited by moisture and low pH, N fixation (0.5 -0.7 kg. ha-I . year-') is a minor input to the bog relative to the input from atmospheric deposition (10.4 kg. hg-' . year-I). The bog is a large sink for N with approximately 65 % of inputs retained. Annual turnover of N (66 kg, ha-I) is much larger than the total input (14.6 kg. ha-I). This large turnover is achieved by rapidly cycling a relatively small pool of N in the aerobic layers of peat. Plant uptake is closely coupled to mineralization such that losses from the system in runoff are small. However, 7 to 12 kg N . ha-I . year-I is buried in anaerobic peat and rendered unavailable to the biota.