Abstract

Elemental hyperaccumulation protects plants from many aboveground herbivores. Little is known about effects of hyperaccumulation on belowground herbivores or their ecological interactions. To examine effects of plant selenium (Se) hyperaccumulation on nematode root herbivory, we investigated spatial distribution and speciation of Se in hyperaccumulator roots using X-ray microprobe analysis, and effects of root Se concentration on root-associated nematode communities. Perennial hyperaccumulators Stanleya pinnata and Astragalus bisulcatus, collected from a natural seleniferous grassland contained 100–1500 mg Se kg−1 root dry weight (DW). Selenium was concentrated in the cortex and epidermis of hyperaccumulator roots, with lower levels in the stele. The accumulated Se consisted of organic (C-Se-C) compounds, indistinguishable from methyl-selenocysteine. The field-collected roots yielded 5–400 nematodes g−1 DW in Baermann funnel extraction, with no correlation between root Se concentration and nematode densities. Even roots containing > 1000 mg Se kg−1 DW yielded herbivorous nematodes. However, greenhouse-grown S. pinnata plants treated with Se had fewer total nematodes than those without Se. Thus, while root Se hyperaccumulation may protect plants from non-specialist herbivorous nematodes, Se-resistant nematode taxa appear to associate with hyperaccumulators in seleniferous habitats, and may utilize high-Se hyperaccumulator roots as food source. These findings give new insight into the ecological implications of plant Se (hyper)accumulation.

Highlights

  • Selenium (Se) is a trace element that naturally occurs in soils, at concentrations that vary with geology and climate

  • A. bisulcatus growing in this naturally seleniferous grassland; this heterogeneity is known from the literature [4,43]

  • The main focus of the study was the effect of root Se accumulation on the abundance of root-associated nematodes

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Summary

Introduction

Selenium (Se) is a trace element that naturally occurs in soils, at concentrations that vary with geology and climate. Across the Western United States, Se levels are typically high, sometimes in excess of 10 mg Se kg−1 soil [1]. Selenium is an essential element for these populations, but can be toxic at elevated concentration, with a narrow window between deficiency and toxicity [2,3]. Se is a beneficial element, but toxic to most plant species at tissue concentrations above 100 mg Se kg−1 dry weight (DW); for crop plants the toxicity threshold can be as low as 10 mg Se kg−1 DW [2,3]. Some plants, the so-called hyperaccumulator species, can accumulate Se to concentrations as high as 10,000 mg Se kg−1 DW, or

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