JXB Advance Access originally published online on February 26, 2009
Journal of Experimental Botany 2009 60(6):1633-1644; doi:10.1093/jxb/erp028
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© 2009 The Author(s).
This is an Open Access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/by-nc/2.0/uk/) which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.
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RESEARCH PAPER |
Water and nitrogen conditions affect the relationships of
13C and
18O to gas exchange and growth in durum wheat
1Unitat de Fisiologia Vegetal, Facultat de Biologia, Universitat de Barcelona, Barcelona, Spain
2International Maize and Wheat Improvement Center (CIMMYT), El Batán, Mexico
* To whom correspondence should be addressed. E-mail: j.araus{at}cgiar.org
Whereas the effects of water and nitrogen (N) on plant
13C have been reported previously, these factors have scarcely been studied for
18O. Here the combined effect of different water and N regimes on
13C,
18O, gas exchange, water-use efficiency (WUE), and growth of four genotypes of durum wheat [Triticum turgidum L. ssp. durum (Desf.) Husn.] cultured in pots was studied. Water and N supply significantly increased plant growth. However, a reduction in water supply did not lead to a significant decrease in gas exchange parameters, and consequently
13C was only slightly modified by water input. Conversely, N fertilizer significantly decreased
13C. On the other hand, water supply decreased
18O values, whereas N did not affect this parameter.
18O variation was mainly determined by the amount of transpired water throughout plant growth (Tcum), whereas
13C variation was explained in part by a combination of leaf N and stomatal conductance (gs). Even though the four genotypes showed significant differences in cumulative transpiration rates and biomass, this was not translated into significant differences in
18Os. However, genotypic differences in
13C were observed. Moreover,
80% of the variation in biomass across growing conditions and genotypes was explained by a combination of both isotopes, with
18O alone accounting for
50%. This illustrates the usefulness of combining
18O and
13C in order to assess differences in plant growth and total transpiration, and also to provide a time-integrated record of the photosynthetic and evaporative performance of the plant during the course of crop growth.
Key words:
13C and
18O, leaf gas exchange, water and nitrogen limitation, wheat, WUE
Received 4 October 2008; Revised 5 January 2009 Accepted 26 January 2009
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