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Abstract

As the global mean surface temperature increases, changes in biogeochemical cycling have the potential to have cascading effects on plant and invertebrate interactions. Previous warming studies have primarily been conducted in recently glaciated, more fertile soils, and the response of plant and invertebrate interactions to warming is unclear in lower latitude, less fertile soils of the Georgia Piedmont. In this study, I examined leaf and soil chemistry (%N, C:N) and herbivore damage (% area consumed) from understory tree seedlings of the Georgia Piedmont. There were species-level foliar carbon and nitrogen content responses to warming, but no warming-induced response of herbivory. Overall, warming did not have an indirect effect on plant-herbivore interactions, which is likely due to Piedmont soils containing less available nitrogen. However, species-level variation in foliar chemistry response to warming has implications for forest composition changes and impacts on nutrients.

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