Plant Physiol. email content delivery
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


First published online July 29, 2009; 10.1104/pp.109.138305

Plant Physiology 151:949-954 (2009)
© 2009 American Society of Plant Biologists

This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow All Versions of this Article:
151/2/949    most recent
pp.109.138305v1
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in Web of Science
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via CrossRef
Google Scholar
Right arrow Articles by Cochard, H.
Right arrow Articles by Mencuccini, M.
PubMed
Right arrow PubMed Citation
Right arrow Articles by Cochard, H.
Right arrow Articles by Mencuccini, M.
Agricola
Right arrow Articles by Cochard, H.
Right arrow Articles by Mencuccini, M.
WHOLE PLANT AND ECOPHYSIOLOGY

New Insights into the Mechanisms of Water-Stress-Induced Cavitation in Conifers

Hervé Cochard*, Teemu Hölttä, Stéphane Herbette, Sylvain Delzon and Maurizio Mencuccini

INRA, UMR 547 PIAF, F–63100 Clermont-Ferrand, France (H.C., S.H.); University Blaise Pascal, UMR 547 PIAF, F–63177 Aubière, France (H.C., S.H.); Department of Forest Ecology, University of Helsinki, Helsinki FIN–00014, Finland (T.H.); University of Bordeaux, UMR BIOGECO, F–33405 Talence, France (S.D.); and School of GeoSciences, University of Edinburgh, Edinburgh EH9 3JN, United Kingdom (M.M.)

Cavitation resistance is a key parameter to understand tree drought tolerance but little is known about the mechanisms of air entry into xylem conduits. For conifers three mechanisms have been proposed: (1) a rupture of pit margo microfibrils, (2) a displacement of the pit torus from its normal sealing position over the pit aperture, and (3) a rupture of an air-water menisci in a pore of the pit margo. In this article, we report experimental results on three coniferous species suggesting additional mechanisms. First, when xylem segments were injected with a fluid at a pressure sufficient to aspirate pit tori and well above the pressure for cavitation induction we failed to detect the increase in sample conductance that should have been caused by torus displacement from blocking the pit aperture or by membrane rupture. Second, by injecting xylem samples with different surfactant solutions, we found a linear relation between sample vulnerability to cavitation and fluid surface tension. This suggests that cavitation in conifers could also be provoked by the capillary failure of an air-water meniscus in coherence with the prediction of Young-Laplace's equation. Within the bordered pit membrane, the exact position of this capillary seeding is unknown. The possible Achilles' heel could be the seal between tori and pit walls or holes in the torus. The mechanism of water-stress-induced cavitation in conifers could then be relatively similar to the one currently proposed for angiosperms.


The author responsible for distribution of materials integral to the findings presented in this article in accordance with the policy described in the Instructions for Authors (www.plantphysiol.org) is: Herve Cochard (cochard{at}clermont.inra.fr).

www.plantphysiol.org/cgi/doi/10.1104/pp.109.138305

* Corresponding author; e-mail cochard{at}clermont.inra.fr.

Received March 9, 2009; accepted July 28, 2009; published July 29, 2009.







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
ASPB Publications PLANT PHYSIOLOGY® THE PLANT CELL
Copyright © 2009 by the American Society of Plant Biologists