Elevated [CO2] mitigates the effect of surface drought by stimulating root growth to access sub-soil water.

Through stimulation of root growth, increasing atmospheric CO2 concentration ([CO2]) may facilitate access of crops to sub-soil water, which could potentially prolong physiological activity in dryland environments, particularly because crops are more water use efficient under elevated [CO2] (e[CO2])...

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Main Authors: Shihab Uddin, Markus Löw, Shahnaj Parvin, Glenn J Fitzgerald, Sabine Tausz-Posch, Roger Armstrong, Garry O'Leary, Michael Tausz
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2018-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC6002051?pdf=render
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author Shihab Uddin
Markus Löw
Shahnaj Parvin
Glenn J Fitzgerald
Sabine Tausz-Posch
Roger Armstrong
Garry O'Leary
Michael Tausz
author_facet Shihab Uddin
Markus Löw
Shahnaj Parvin
Glenn J Fitzgerald
Sabine Tausz-Posch
Roger Armstrong
Garry O'Leary
Michael Tausz
author_sort Shihab Uddin
collection DOAJ
description Through stimulation of root growth, increasing atmospheric CO2 concentration ([CO2]) may facilitate access of crops to sub-soil water, which could potentially prolong physiological activity in dryland environments, particularly because crops are more water use efficient under elevated [CO2] (e[CO2]). This study investigated the effect of drought in shallow soil versus sub-soil on agronomic and physiological responses of wheat to e[CO2] in a glasshouse experiment. Wheat (Triticum aestivum L. cv. Yitpi) was grown in split-columns with the top (0-30 cm) and bottom (31-60 cm; 'sub-soil') soil layer hydraulically separated by a wax-coated, root-penetrable layer under ambient [CO2] (a[CO2], ∼400 μmol mol-1) or e[CO2] (∼700 μmol mol-1) [CO2]. Drought was imposed from stem-elongation in either the top or bottom soil layer or both by withholding 33% of the irrigation, resulting in four water treatments (WW, WD, DW, DD; D = drought, W = well-watered, letters denote water treatment in top and bottom soil layer, respectively). Leaf gas exchange was measured weekly from stem-elongation until anthesis. Above-and belowground biomass, grain yield and yield components were evaluated at three developmental stages (stem-elongation, anthesis and maturity). Compared with a[CO2], net assimilation rate was higher and stomatal conductance was lower under e[CO2], resulting in greater intrinsic water use efficiency. Elevated [CO2] stimulated both above- and belowground biomass as well as grain yield, however, this stimulation was greater under well-watered (WW) than drought (DD) throughout the whole soil profile. Imposition of drought in either or both soil layers decreased aboveground biomass and grain yield under both [CO2] compared to the well-watered treatment. However, the greatest 'CO2 fertilisation effect' was observed when drought was imposed in the top soil layer only (DW), and this was associated with e[CO2]-stimulation of root growth especially in the well-watered bottom layer. We suggest that stimulation of belowground biomass under e[CO2] will allow better access to sub-soil water during grain filling period, when additional water is converted into additional yield with high efficiency in Mediterranean-type dryland agro-ecosystems. If sufficient water is available in the sub-soil, e[CO2] may help mitigating the effect of drying surface soil.
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spelling doaj.art-7a91168dac5841219354569aa68de7512022-12-22T02:29:36ZengPublic Library of Science (PLoS)PLoS ONE1932-62032018-01-01136e019892810.1371/journal.pone.0198928Elevated [CO2] mitigates the effect of surface drought by stimulating root growth to access sub-soil water.Shihab UddinMarkus LöwShahnaj ParvinGlenn J FitzgeraldSabine Tausz-PoschRoger ArmstrongGarry O'LearyMichael TauszThrough stimulation of root growth, increasing atmospheric CO2 concentration ([CO2]) may facilitate access of crops to sub-soil water, which could potentially prolong physiological activity in dryland environments, particularly because crops are more water use efficient under elevated [CO2] (e[CO2]). This study investigated the effect of drought in shallow soil versus sub-soil on agronomic and physiological responses of wheat to e[CO2] in a glasshouse experiment. Wheat (Triticum aestivum L. cv. Yitpi) was grown in split-columns with the top (0-30 cm) and bottom (31-60 cm; 'sub-soil') soil layer hydraulically separated by a wax-coated, root-penetrable layer under ambient [CO2] (a[CO2], ∼400 μmol mol-1) or e[CO2] (∼700 μmol mol-1) [CO2]. Drought was imposed from stem-elongation in either the top or bottom soil layer or both by withholding 33% of the irrigation, resulting in four water treatments (WW, WD, DW, DD; D = drought, W = well-watered, letters denote water treatment in top and bottom soil layer, respectively). Leaf gas exchange was measured weekly from stem-elongation until anthesis. Above-and belowground biomass, grain yield and yield components were evaluated at three developmental stages (stem-elongation, anthesis and maturity). Compared with a[CO2], net assimilation rate was higher and stomatal conductance was lower under e[CO2], resulting in greater intrinsic water use efficiency. Elevated [CO2] stimulated both above- and belowground biomass as well as grain yield, however, this stimulation was greater under well-watered (WW) than drought (DD) throughout the whole soil profile. Imposition of drought in either or both soil layers decreased aboveground biomass and grain yield under both [CO2] compared to the well-watered treatment. However, the greatest 'CO2 fertilisation effect' was observed when drought was imposed in the top soil layer only (DW), and this was associated with e[CO2]-stimulation of root growth especially in the well-watered bottom layer. We suggest that stimulation of belowground biomass under e[CO2] will allow better access to sub-soil water during grain filling period, when additional water is converted into additional yield with high efficiency in Mediterranean-type dryland agro-ecosystems. If sufficient water is available in the sub-soil, e[CO2] may help mitigating the effect of drying surface soil.http://europepmc.org/articles/PMC6002051?pdf=render
spellingShingle Shihab Uddin
Markus Löw
Shahnaj Parvin
Glenn J Fitzgerald
Sabine Tausz-Posch
Roger Armstrong
Garry O'Leary
Michael Tausz
Elevated [CO2] mitigates the effect of surface drought by stimulating root growth to access sub-soil water.
PLoS ONE
title Elevated [CO2] mitigates the effect of surface drought by stimulating root growth to access sub-soil water.
title_full Elevated [CO2] mitigates the effect of surface drought by stimulating root growth to access sub-soil water.
title_fullStr Elevated [CO2] mitigates the effect of surface drought by stimulating root growth to access sub-soil water.
title_full_unstemmed Elevated [CO2] mitigates the effect of surface drought by stimulating root growth to access sub-soil water.
title_short Elevated [CO2] mitigates the effect of surface drought by stimulating root growth to access sub-soil water.
title_sort elevated co2 mitigates the effect of surface drought by stimulating root growth to access sub soil water
url http://europepmc.org/articles/PMC6002051?pdf=render
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