We report a novel form of xylem dysfunction in angiosperms: reversible collapse of the xylem conduits of the smallest vein orders that demarcate and intrusively irrigate the areoles of red oak (Quercus rubra) leaves. Cryo-scanning electron microscopy revealed gradual increases in collapse from approximately 22 MPa down to 23 MPa, saturating thereafter (to 24 MPa). Over this range, cavitation remained negligible in these veins. Imaging of rehydration experiments showed spatially variable recovery from collapse within 20 s and complete recovery after 2 min. More broadly, the patterns of deformation induced by desiccation in both mesophyll and xylem suggest that cell wall collapse is unlikely to depend solely on individual wall properties, as mechanical constraints imposed by neighbors appear to be important. From the perspective of equilibrium leaf water potentials, petioles, whose vessels extend into the major veins, showed a vulnerability to cavitation that overlapped in the water potential domain with both minor vein collapse and buckling (turgor loss) of the living cells. However, models of transpiration transients showed that minor vein collapse and mesophyll capacitance could effectively buffer major veins from cavitation over time scales relevant to the rectification of stomatal wrong-way responses. We suggest that, for angiosperms, whose subsidiary cells give up large volumes to allow large stomatal apertures at the cost of potentially large wrong-way responses, vein collapse could make an important contribution to these plants' ability to transpire near the brink of cavitation-inducing water potentials.Terrestrial photosynthesis is inextricably linked with water loss. Plants expose hydrated cells to the atmosphere to obtain CO 2 , with evaporation an inevitable consequence. Vascular plants meet this challenge by replacing water lost via transpiration with water pulled from the soil. What allows this is the xylem: a system of stiff-walled conduits capable of remaining water filled at negative pressures low enough to extract water from micrometer-to nanometer-scale soil capillaries and to drive flow through the 10-to 100-mm-diameter xylem conduits that extend from the roots to the leaves (Tyree and Zimmermann, 2002). To deliver water at rates equal to transpiration, the pressure in the xylem must fall far below the vapor pressure of water, such that water transport through the xylem occurs in a metastable state (i.e. at kinetic, but not thermodynamic, equilibrium) and thus at risk of cavitation (Stroock et al., 2014). How many plants seemingly operate with little to no safety margin against cavitation Brodribb and Holbrook, 2004;Meinzer et al., 2009;Choat et al., 2012) remains an important and unsolved question.Cavitation occurs when metastable liquid water is replaced by water vapor due to the expansion of a gas bubble nucleus, forming an embolism or air blockage: embolism disrupts water transport because tensions cannot be transmitted through gas. The most probable origin of such nuclei is thought to be g...