4.8 Article

Reversible Leaf Xylem Collapse: A Potential Circuit Breaker against Cavitation

期刊

PLANT PHYSIOLOGY
卷 172, 期 4, 页码 2261-2274

出版社

OXFORD UNIV PRESS INC
DOI: 10.1104/pp.16.01191

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资金

  1. National Science Foundation [IOS 1456836, DMR 14-20570]
  2. Air Force Office [FA9550-09-1-0188]
  3. William F. Milton Fund
  4. Sustainability Science Program at the Kennedy School of Government
  5. GSAS Research Scholars Initiative of Harvard University

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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 -2 MPa down to -3 MPa, saturating thereafter (to -4 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.

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