“…The importance of capturing the photosynthetic physiologies of C 3 and C 4 grass types, and their variation with CO 2 and climate, has long been recognized (Collatz, Berry, & Clark, ; Sellers et al, ; Still, Berry, et al, ). However, additional ecological and hydrological factors control C 3 and C 4 distributions and can interact in complex ways, producing offsetting effects driven by interactions with hydrological cycles (Griffith, Lehmann, et al, ) or by driving systems towards deterministically woody states (Bond, ; Moncrieff, Scheiter, Bond, & Higgins, ; Oliveras & Malhi, ). For example, in an experimental study conducted in a semi‐arid, mixed C 3 /C 4 grassland in North America, Morgan et al () showed that C 4 grasses were counterintuitively outperforming C 3 grasses owing to increases in water‐use efficiency driven by interacting effects of higher CO 2 and warming on soil moisture and plant physiological responses.…”