Abstract
A warmer climate is generally expected to favour smaller organisms and steeper body-mass–abundance scaling through food webs. Results from across a stream temperature gradient now show that this effect can be offset by increasing nutrient supply. Natural ecosystems typically consist of many small and few large organisms1,2,3,4. The scaling of this negative relationship between body mass and abundance has important implications for resource partitioning and energy usage5,6,7. Global warming over the next century is predicted to favour smaller organisms8,9,10,11,12, producing steeper mass–abundance scaling13 and a less efficient transfer of biomass through the food web5. Here, we show that the opposite effect occurs in a natural warming experiment involving 13 whole-stream ecosystems within the same catchment, which span a temperature gradient of 5–25 °C. We introduce a mechanistic model that shows how the temperature dependence of basal resource carrying capacity can account for these previously unexpected results. If nutrient supply increases with temperature to offset the rising metabolic demand of primary producers, there will be sufficient resources to sustain larger consumers at higher trophic levels. These new data and the model that explains them highlight important exceptions to some commonly assumed ‘rules’ about responses to warming in natural ecosystems.
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