The productive capacity of aquatic systems often is equated with the '
chemical richness' of the water. A primary objective of the present st
udy was to relate macroinvertebrate benthos and drift to a streams' pr
oductive capacity as indicated by absolute levels of alkalinity. We te
sted this relationship in six 2nd-3rd order tributaries of the Salmon
River, Idaho that ranged in alkalinity from 50 to 360 mg 1(-1). Benthi
c density and biomass, drift biomass, and benthic organic matter incre
ased with increasing levels of alkalinity, although not all relationsh
ips were significant. The proportion of drift biomass to benthic bioma
ss was similar among study streams suggesting that drift was primarily
passive during the study period. The data suggest that spatial variat
ions in landscape-scale geology may indirectly affect spatial patterns
of macroinvertebrate benthic and drift standing crops among streams w
ithin a single river basin by mediating lotic chemical richness as fou
nd among tributaries of the Salmon River basin.