“…For most species, especially the nondesert ones, g min rates tend to show small variations at temperatures from 15 to 35°C, while temperatures above 35° induce a drastic increase in cuticle permeability and, consequently, in water loss (Schreiber, ; Schuster et al, ). This abrupt increase in g min rates under a certain temperature threshold, also known as transition temperature (Schuster et al, ), can have a catastrophic effect on plants exposed to heat waves, especially under drought conditions, since the increase in water loss can significantly increase the tension in xylem vessels, which can result in a reduction in the time to HF (Cochard, ). However, despite the great impact that the increase in atmospheric temperature can have on g min rates (Bueno et al, ; Schuster et al, ) and, thus, on plant survival (Cochard, ), key questions regarding this topic remain.…”