“…We address these questions by testing the following hypotheses: (1) V c,max25 could vary across different vegetated biomes and life‐forms, with higher values in grasslands relative to shrublands and forests and in fast‐growing relative to slow‐growing species, because the former plant types usually have higher nutrient concentrations that are often related to more investment in photosynthetic apparatus (Ali et al, 2016; Kattge et al, 2009; Smith & Dukes, 2018); (2) V c,max25 could show a significant phylogenetic signal, given that V c,max25 has been connected previously with multiple biotic factors (i.e., RuBisCO kinetic parameters and photosynthesis‐associated leaf nutrient concentrations) that all display strong phylogenetic regulation (Galmes et al, 2015; Huang et al, 2022; Jump & Peñuelas, 2005; Liu et al, 2022; Sardans et al, 2021); and (3) the global patterns of V c,max25 could be regulated jointly by both current environmental factors and long‐term evolutionary history, with the latter being the dominant driver, because mounting evidence suggests a more important contribution of species identity information to the variability of photosynthesis‐associated leaf nutrient concentrations than environmental factors (Asner et al, 2014; Dahlin et al, 2013; Palacio et al, 2022; Sardans et al, 2021; Vallicrosa, Sardans, Maspons, & Peñuelas, 2022; Vallicrosa, Sardans, Maspons, Zuccarini, et al, 2022). To test these three hypotheses, we first collated a global dataset of field‐measured V c,max25 for C 3 plants with concurrent measurements of present‐day environmental factors (i.e., climate and soil variables), then integrated this unique global dataset with multiple statistical modelling analyses detailed below.…”