“…The sharp decrease of gs found in mid-June could be explained by an asphyxia condition caused by soil flooding (as shown in the results section, a large amount of rainfall fell in May and June), in fact a reduction in oxygen concentration in the root zone could determine a rapid decline of gs (Smith et al, 1989;Barickman et al, 2019). Nevertheless, waterlogging could also affect the activity of photosynthetic enzymes, resulting in decreased Pn (Sharma et al, 2021b); during the above-mentioned period, as explained, a reduction of gs was recorded, but Pn had a peak, probably due to the optimal high temperatures recorded in the first part June and the rainfall occurred before the waterlogging; moreover, the negative effects of waterlogging might be manifested more gradually on Pn than gs (Yordanova and Popova, 2007), in fact, a sharp decline of Pn was observed at the end of June, when, on the other hand, gs had recovered, maybe due to high temperatures and no precipitations in the second part of June, resulting in evaporation of the water from the soil and then better conditions of the root system. However, based on the current knowledge it is not possible to determine with accuracy the temporal dynamics of the effects of waterlogging specifically on carob trees.…”