Bilby, R.E., Brian R. Fransen, and Peter A. Bisson. 1995. Incorporation of nitrogen and carbon from spawning coho salmon into the trophic system of small streams: evidence from stable isotopes. Can. J. Fish. Aquat. Sci. (In Press). Highest levels of enrichment of the stream biota with the heavier isotopes occurred in the early spring, shortly after carcasses had decomposed. Juvenile coho salmon exhibited a doubling in rate of growth and a 40% increase in condition factor following spawning. Age 0 cutthroat trout in a nearby stream without salmon exhibited no change in growth rate during the winter and condition factor did not improve until late winter. Proportion of nitrogen contributed by spawning salmon varied among trophic categories, ranging from about 17% in collector-gatherers to more than 30% in juvenile coho salmon. Carbon contributed by spawning salmon ranged from 0% in the foliage of riparian plants and shredders to 34% in juvenile coho salmon. Coho salmon, which usually spawn at lower densities than pink and sockeye salmon, are not known to represent an important vector of nutrient or organic matter transport from marine to freshwater ecosystems. But because low levels of primary and secondary productivity are characteristic of many headwater streams in the Pacific Northwest, even modest inputs of certain nutrients or organic matter of high nutritional values may be of consequence in maintaining trophic productivity. Differences in isotope ratios between the two sites increased during the winter, while carcasses were present in the stream and remained at high levels through early spring, shortly after the carcasses were fully decomposed and while salmon fry were emerging from the streambed gravel. Juvenile fish more than doubled in weight following the arrival of the adult salmon in the system, gaining 3.6 g during the winter of 1992- 1993 and 3.2 g during 1993-1994. Condition factor of the juvenile coho salmon in Grizzly Creek decreased between June and October, achieving the lowest values of the year at this time. Condition factor in December increased, corresponding with the presence of spawning salmon and continued to increase through March, the time of year when proportions of marine derived N and C are at peak levels in fish in the creek. Incorporation of marine-derived nutrients into the stream biota occurs while the nitrogen and carbon are in the organic form, prior to mineralization. Spawning salmon may be important in maintaining production regardless of the relative availability of nutrients from other sources. Larger size has been shown to substantially increase the over winter survival rate of juvenile coho salmon and larger smolt size has been related to increased marine survival in both coho salmon and Steelhead. Reductions in winter and marine survival will reduce the number of returning adult salmon and further suppress the productivity of the freshwater system, thus creating a feedback process which progressively depresses the capacity of the freshwater system to support fish. However, fewer returning salmon, and the nutrients they carry, also has consequences for the productivity of stream ecosystems. Large- scale declines of coho populations in many coastal watersheds may represent significant losses of trophic productivity and nutrient capital in headwater streams, and reduced export of nutrients and organic matter from these streams may impact production in aquatic ecosystems downstream from areas in which spawning occurs. The influence of spawning salmon on the trophic productivity of small headwater streams may be especially important since heavy shading limits autotrophic production throughout the year. Decreased productivity may be self-perpetuating if the capacity of a watershed to produce future generations of coho salmon is progressively diminished by fewer and fewer returning adults. Bilby, R.E. et al. 1995