Microbial communities at soil-stream interfaces may be particularly importa
nt in regulating amounts and forms of nutrients that leave upland soils and
enter stream ecosystems. While microbial communities are thought to be res
ponsible for key nutrient transformations within near-stream sediments, the
re is relatively little mechanistic information on factors that control mic
robial activities in these areas. In this study, we examine the roles of di
ssolved organic carbon (DOC) vs. particulate organic carbon (POC) as potent
ial controls on rates of bacterial productivity (measured as incorporation
of [H-3]thymidine into bacterial DNA) and amounts of bacterial biomass (mea
sured as fatty acid yield) in sediments along a transect perpendicular to a
soil-stream interface. We hypothesized that spatial patterns in bacterial
productivity would vary in response to strong and persistent patterns in po
re-water concentrations of DOC that were observed along a soil-stream trans
ect throughout a 2-year period, Our results did not support the existence o
f such a link between pore-water DOC and bacterial productivity. In contras
t, we found bacterial productivity and biomass were related to small-scale
spatial variations in sediment POC on 3 of 4 sample dates. While our result
s indicate that total bacterial productivity in near-stream sediments is no
t consistently linked to spatial variations in pore-water DOG, it is likely
that DOC and POC are not mutually exclusive and the relative contribution
of DOC and POC to sedimentary microbes varies temporally and spatially in d
ifferent riparian habitats.