|Title||Convergence in the temperature response of leaf respiration across biomes and plant functional types|
|Publication Type||Journal Article|
|Year of Publication||2016|
|Authors||Heskel, Mary A., O'Sullivan Odhran S., Reich Peter B., Tjoelker Mark G., Weerasinghe Lasantha K., Penillard Aurore, Egerton John J., Creek Danielle, Bloomfield Keith J., Xiang Jen, Sinca Felipe, Stangl Zsofia R., de la Torre Alberto Martinez-, Griffin Kevin L., Huntingford Chris, Hurry Vaughan, Meir Patrick, Turnbull Matthew H., and Atkin Owen K.|
|Journal||Proceedings of the National Academy of Sciences|
|Keywords||carbon exchange, Climate models, plant respiration, Q10, temperature sensitivity, thermal response|
Plant respiration constitutes a massive carbon flux to the atmosphere, and a major control on the evolution of the global carbon cycle. It therefore has the potential to modulate levels of climate change due to the human burning of fossil fuels. Neither current physiological nor terrestrial biosphere models adequately describe its short-term tem- perature response, and even minor differences in the shape of the response curve can significantly impact estimates of ecosystem carbon release and/or storage. Given this, it is critical to establish whether there are predictable patterns in the shape of the respiration–temper- ature response curve, and thus in the intrinsic temperature sensitivity of respiration across the globe. Analyzing measurements in a compre- hensive database for 231 species spanning 7 biomes, we demonstrate that temperature-dependent increases in leaf respiration do not follow a commonly used exponential function. Instead, we find a decelerating function as leaves warm, reflecting a declining sensitivity to higher temperatures that is remarkably uniform across all biomes and plant functional types. Such convergence in the temperature sensitivity of leaf respiration suggests that there are universally applicable controls on the temperature response of plant energy metabolism, such that a single new function can predict the temperature dependence of leaf respiration for global vegetation. This simple function enables straight- forward description of plant respiration in the land-surface compo- nents of coupled earth system models. Our cross-biome analyses shows significant implications for such fluxes in cold climates, gener- ally projecting lower values compared with previous estimates.