“…In the past, responses of leaf respiration to short-term shifts in (measurement) temperature were generally described via temperature-insensitive Q 10 (i.e., often setting Q 10 = 2.0 in Earth System Models), or via classical Arrhenius kinetics where activation energy is constant (reviewed by Atkin et al, 2005). However, it has become increasingly apparent that overall activation energy of leaf respiration (or Q 10 ) is not constant across measurement temperatures (Atkin and Tjoelker, 2003;Noguchi et al, 2015;Heskel et al, 2016a;Adams et al, 2016;Atkin et al, 2017). In an extended, Arrhenius-type description, the temperature-dependency of activation energy is captured by the exponent parameter δ R (Kruse et al, 2016(Kruse et al, , 2017.…”