As the global climate warms, a key question is how increased leaf temperatures will affect tree physiology and the coupling between leaf and air temperatures in forests. To explore the impact of increasing temperatures on plant performance in open air, we warmed leaves in the canopy of two mature evergreen forests, a temperate Eucalyptus woodland and a tropical rainforest. The leaf heaters consistently maintained leaves at a target of 4°C above ambient leaf temperatures. Ambient leaf temperatures (Tleaf) were mostly coupled to air temperatures (Tair), but at times leaves could be 8-10°C warmer than ambient air temperatures especially in full sun. At both sites, Tleaf were warmer at higher air temperatures (Tair > 25 ℃), but cooler at lower Tair, contrary to the ‘leaf homeothermy hypothesis’. Warmed leaves showed significantly lower stomatal conductance (-0.05 mol m-2 s-1 or -43% across species) and net photosynthesis (-3.91 micro-mol m-2 s-1 or -39%), with similar rates in leaf respiration rates at a common temperature (no acclimation). Increased canopy leaf temperatures due to future warming should reduce carbon assimilation via reduction in photosynthesis in these forests, which could potentially weaken the land carbon sink in tropical and temperate forests. This dataset contains three .csv files - one with leaf temperatures from EUCFACE, one with leaf temperatures from the tropical site Daintree Research Observatory (DRO) and one file with physiological responses to warming. For further discussion or explanation of the data please contact Krstine Crous at k.crous@westernsydney.edu.au 0000-0001-9478-7593.