We examined how the spatially and temporally predictable disturbance caused
by a spawning run of native sockeye salmon Oncorhynchus nerka temporarily
affected benthic and invertebrate drift communities of two small streams in
southwestern Alaska. Surface gravel size temporarily increased as a conseq
uence of this mechanical disturbance, and periphyton biomass decreased in o
ne stream. The postspawning rise in periphyton biomass in Bear Creek (large
r sockeye salmon run) likely reflects nutrient release by decomposing socke
ye salmon. Total benthic invertebrate and larval chironomid density decreas
ed during spawning in one stream, but most invertebrate taxa in both stream
s did not exhibit clear spawning-related impacts. In contrast, invertebrate
drift almost always increased during daylight hours when sockeye salmon we
re present, but it was difficult to separate mechanical effects of sockeye
salmon acting via redd construction versus swimming. Total daytime drift de
nsity during spawning was four times greater in Bear Creek (4 sockeye salmo
n/m stream) and 2.5 times greater in Whitefish Creek (0.5 sockeye salmon/m
stream), compared with pre- and postspawning values. In experimental enclos
ures, total drift and drift by Ephemeroptera (mayflies), Hydracarina (water
mites), and Plecoptera (stoneflies) were also significantly higher in the
presence of swimming sockeye salmon. Juvenile coho salmon Oncorhynchus kisu
tch consumed significantly more chironomid larvae during spawning in Whitef
ish Creek, apparently capitalizing on the increased chironomid drift caused
by the spawning-run disturbance. Results are discussed in terms of the imp
ortance of salmonids to the stream ecosystems in which they spawn, with ref
erence to benthic community structure and increased access to invertebrates
in the drift by resident fishes.