Abstract

Silicon is reported to reduce the toxic effects of Al on root elongation but the in planta mechanism by which this occurs remains unclear. Using seedlings of soybean (Glycine max) and sorghum (Sorghum bicolor), we examined the effect of up to 2 mM Si on root elongation rate (RER) in Al-toxic nutrient solutions. Synchrotron-based low energy X-ray fluorescence (LEXRF) was then used for the in situ examination of the distribution of Al and Si within cross-sections cut from the apical tissues of sorghum roots. The addition of Si potentially increased RER in Al-toxic solutions, with RER being up to ca. 0.3 mm h-1 (14%) higher for soybean and ca. 0.2 mm h-1 (17%) higher for sorghum relative to solutions without added Si. This improvement in RER could not be attributed to a change in Al-chemistry of the bulk nutrient solution, nor was it due to a change in the concentration of Al within the apical (0–10 mm) root tissues. Using LEXRF to examine sorghum, it was demonstrated that in roots exposed to both Al and Si, much of the Al was co-located with Si in the mucigel and outer apoplast. These observations suggest that Si reduces the toxicity of Al in planta through formation of Al–Si complexes in mucigel and outer cellular tissues, thereby decreasing the binding of Al to the cell wall where it is known to inhibit wall loosening as required for cell elongation.

Highlights

  • Aluminum (Al) is the most common metallic element in the earth’s soils (Lindsay, 1979), but at neutral and near-neutral pH values, Al-containing minerals are of low solubility and are not toxic

  • The addition of Si partially alleviated the reduction of root elongation in Al-toxic solutions (Figures 1A,B, 2), this improvement in growth could not be attributed to a decrease in soluble Al in the bulk nutrient solution (Figure 2)

  • In accordance with previous studies, we have found that Si can potentially increase root elongation rate (RER) in Al-toxic solutions, with the magnitude of the effect increasing with the concentration of Si

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Summary

Introduction

Aluminum (Al) is the most common metallic element in the earth’s soils (Lindsay, 1979), but at neutral and near-neutral pH values, Al-containing minerals are of low solubility and are not toxic. An estimated 30–40% of all arable soils worldwide are acid (von Uexküll and Mutert, 1995; Eswaran et al, 1997), with the solubility of Al being elevated in these acid soils. Despite being the most studied trace element in the field of phytotoxicity, much remains unknown regarding the toxic effects of Al. Silicon, the second most abundant element in the earth’s crust, is regarded as a beneficial element for plant growth (Broadley et al, 2012). It has been proposed that this increased resistance is due to a physical effect, with Si forming a layer which impedes penetration

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