Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/53772
Title: Comparative performance of the stable isotope signatures of carbon, nitrogen and oxygen in assessing early vigour and grain yield in durum wheat
Author: Bort Pie, Jordi
Makram, B.
Kawther, K.
Zakaria, K.
Araus Ortega, José Luis
Keywords: Cereals
Blat
Isòtops estables en ecologia
Millorament selectiu de plantes
Isòtops de carboni
Oxigen
Nitrogen
Cereals
Wheat
Stable isotopes in ecological research
Plant breeding
Carbon isotopes
Oxygen
Nitrogen
Issue Date: Jun-2014
Publisher: Cambridge University Press
Abstract: The present paper studied the performance of the stable isotope signatures of carbon (δ13C), nitrogen (δ15N) and oxygen (δ18O) in plants when used to assess early vigour and grain yield (GY) in durum wheat growing under mild and moderate Mediterranean stress conditions. A collection of 114 recombinant inbred lines was grown under rainfed (RF) and supplementary irrigation (IR) conditions. Broad sense heritabilities (H2) for GY and harvest index (HI) were higher under RF conditions than under IR. Broad sense heritabilities for δ13C were always above 0·60, regardless of the plant part studied, with similar values for IR and RF trials. Some of the largest genetic correlations with GY were those shown by the δ13C content of the flag leaf blade and mature grains. Under both water treatments, mature grains showed the highest negative correlations between δ13C and GY across genotypes. Flag leaf δ13C was negatively correlated with GY only under RF conditions. The δ13C in seedlings was negatively correlated, under IR conditions only, with GY but also with early vigour. The sources of variation in early vigour were studied by stepwise analysis using the stable isotope signatures measured in seedlings. The δ13C was able to explain almost 0·20 of this variation under RF, but up to 0·30 under IR. In addition, nitrogen concentration in seedlings accounted for another 0·05 of variation, increasing the amount explained to 0·35. The sources of variation in GY were also studied through stable isotope signatures and biomass of different plant parts: δ13C was always the first parameter to appear in the models for both water conditions, explaining c. 0·20 of the variation. The second parameter (δ15N or N concentration of grain, or biomass at maturity) depended on the water conditions and the plant tissue being analysed. Oxygen isotope composition (δ18O) was only able to explain a small amount of the variation in GY. In this regard, despite the known and previously described value of δ13C as a tool in breeding, δ15N is confirmed as an additional tool in the present study. Oxygen isotope composition does not seem to offer any potential, at least under the conditions of the present study.
Note: Reproducció del document publicat a: http://dx.doi.org/10.1017/S0021859613000269
It is part of: Journal of Agricultural Science, 2014, vol. 152, num. 3, p. 408-426
Related resource: http://dx.doi.org/10.1017/S0021859613000269
URI: http://hdl.handle.net/2445/53772
ISSN: 0021-8596
Appears in Collections:Articles publicats en revistes (Biologia Evolutiva, Ecologia i Ciències Ambientals)

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