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


     


Plant Physiology 83:316-322 (1987)
© 1987 American Society of Plant Biologists

This Article
Right arrow Full Text (PDF)
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
Right arrow Citing Articles via Web of Science (36)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Guehl, J.-M.
Right arrow Articles by Aussenac, G.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Guehl, J.-M.
Right arrow Articles by Aussenac, G.
Agricola
Right arrow Articles by Guehl, J.-M.
Right arrow Articles by Aussenac, G.
Environmental and Stress Physiology

Photosynthesis Decrease and Stomatal Control of Gas Exchange in Abies alba Mill. in Response to Vapor Pressure Difference

Jean-Marc Guehl and Gilbert Aussenac

Station de Sylviculture et de Production, Institut National de la Recherche Agronomique, Champenoux, 54280 Seichamps, France, Centre de Recherches Forestières de Nancy, Champenoux, 54280 Seichamps, France

The responses of steady state CO2 assimilation rate (A), transpiration rate (E), and stomatal conductance (gs) to changes in leaf-to-air vapor pressure difference ({Delta}W) were examined on different dates in shoots from Abies alba trees growing outside. In Ecouves, a provenance representative of wet oceanic conditions in Northern France, both A and gs decreased when {Delta}W was increased from 4.6 to 14.5 Pa KPa–1. In Nebias, which represented the dry end of the natural range of A. alba in southern France, A and gs decreased only after reaching peak levels at 9.0 and 7.0 Pa KPa–1, respectively. The representation of the data in assimilation rate (A) versus intercellular CO2 partial pressure (Ci) graphs allowed us to determine how stomata and mesophyll photosynthesis interacted when {Delta}W was increased. Changes in A were primarily due to alterations in mesophyll photosynthesis. At high {Delta}W, and especially in Ecouves when soil water deficit prevailed, A declined, while Ci remained approximately constant, which may be interpreted as an adjustment of gs to changes in mesophyll photosynthesis. Such a stomatal control of gas exchange appeared as an alternative to the classical feedforward interpretation of E versus {Delta}W responses with a peak rate of E. The gas exchange response to {Delta}W was also characterized by considerable deviations from the optimization theory of IR Cowan and GD Farquhar (1977 Symp Soc Exp Biol 31: 471-505).








HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
ASPB Publications PLANT PHYSIOLOGY® THE PLANT CELL
Copyright © 1987 by the American Society of Plant Biologists