“…In moist soils, these pressures are moderate, typically above 22 MPa, but during drought, they decrease considerably, as plants are forced to extract water from drying soil, which reduces the stability of the water column. Below a specific pressure threshold, cavitation events occur when airwater menisci located at pores between xylem conduits break (Tyree, 1997;Cochard et al, 2009;Mayr et al, 2014), vaporizing sap, reducing xylem conductance, and eventually leading to plant death by desiccation (Brodribb et al, 2010;Urli et al, 2013). The xylem pressure at which cavitation occurs, leading to 50% loss of hydraulic function (P 50 ), is a trait that varies widely across species (Delzon et al, 2010;Bouche et al, 2014) and links with climate: xeric species are more resistant to cavitation than species that occupy more mesic habitats (Brodribb and Hill, 1999;Maherali et al, 2004;Choat et al, 2012;Pittermann et al, 2012).…”