Abstract. Heterotrophic microbes play key roles in regulating fluxes of
energy and nutrients, which are increasingly affected by globally changing
environmental conditions such as warming and nutrient enrichment. While the
effects of temperature and nutrients on microbial mineralization of carbon
have been studied in some detail, much less attention has been given to how
these factors are altering uptake rates of nutrients. We used laboratory
experiments to simultaneously evaluate the temperature dependence of soluble
reactive phosphorus (SRP) uptake and respiration by leaf-litter-associated
microbial communities from temperate headwater streams. Additionally, we
evaluated the influence of the initial concentration of SRP on the
temperature dependence of P uptake. Finally, we used simple simulation
models to extrapolate our results and estimate the effect of warming and P
availability on cumulative gross uptake. We found that the temperature
dependence of P uptake was lower than that of respiration (0.48 vs. 1.02 eV). Further, the temperature dependence of P uptake increased with the
initial concentration of SRP supplied, ranging from 0.12 to 0.48 eV over an
11 to 212 µg L−1 gradient in initial SRP concentration.
Finally, despite our laboratory experiments showing increases in
mass-specific rates of gross P uptake with temperature, our simulation
models predict declines in cumulative P uptake with warming, because the
increased rates of respiration at warmer temperatures more rapidly depleted
benthic carbon substrates and consequently reduced the biomass of the
benthic microbial community. Thus, even though mass-specific rates of P uptake were higher at the warmer temperatures, cumulative P uptake was lower
over the residence time of a pulsed input of organic carbon. Our results
highlight the need to consider the combined effects of warming, nutrient
availability, and resource availability and/or magnitude on carbon processing as
important controls of nutrient processing in heterotrophic ecosystems.