Abstract

Iron (Fe) is an essential mineral that has low solubility in alkaline soils, where its deficiency results in chlorosis. Whether low Fe supply and alkaline pH stress are equivalent is unclear, as they have not been treated as separate variables in molecular physiological studies. Additionally, molecular responses to these stresses have not been studied in leaf and root tissues simultaneously. We tested how plants with the Strategy I Fe uptake system respond to Fe deficiency at mildly acidic and alkaline pH by measuring root ferric chelate reductase (FCR) activity and expression of selected Fe uptake genes and riboflavin synthesis genes. Alkaline pH increased cucumber (Cucumis sativus L.) root FCR activity at full Fe supply, but alkaline stress abolished FCR response to low Fe supply. Alkaline pH or low Fe supply resulted in increased expression of Fe uptake genes, but riboflavin synthesis genes responded to Fe deficiency but not alkalinity. Iron deficiency increased expression of some common genes in roots and leaves, but alkaline stress blocked up-regulation of these genes in Fe-deficient leaves. In roots of the melon (Cucumis melo L.) fefe mutant, in which Fe uptake responses are blocked upstream of Fe uptake genes, alkaline stress or Fe deficiency up-regulation of certain Fe uptake and riboflavin synthesis genes was inhibited, indicating a central role for the FeFe protein. These results suggest a model implicating shoot-to-root signaling of Fe status to induce Fe uptake gene expression in roots.

Highlights

  • Iron (Fe) is an important micronutrient that plays crucial roles in plant growth, development, and reproduction (Walker and Waters, 2011; Kobayashi and Nishizawa, 2012; Vigani et al, 2013)

  • While low Fe supply and alkaline stress both resulted in elevated ferric chelate reductase (FCR) activity in cucumber roots, the patterns were quite different

  • We obtained similar chlorophyll and FCR activity results with another variety of cucumber (Miniature White; Supplementary Fig. S2). These results indicated that alkaline stress elevated the root FCR activity relative to Fe-replete plants, but abolished the normal response to Fe supply

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Summary

Introduction

Iron (Fe) is an important micronutrient that plays crucial roles in plant growth, development, and reproduction (Walker and Waters, 2011; Kobayashi and Nishizawa, 2012; Vigani et al, 2013). Iron uptake into roots of graminaceous plant species (known as Strategy II) is characterized by production and secretion of phytosiderophores that chelate Fe(III) for uptake (Kobayashi and Nishizawa, 2012). Iron uptake by non-graminaceous angiosperm species (known as Strategy I) is characterized by rhizosphere acidification by H+-ATPase proteins, reduction of Fe(III) to Fe(II) by ferric chelate reductase (FCR) proteins, and uptake of Fe(II) by iron transporter proteins (Kobayashi and Nishizawa, 2012). The activity of these Fe uptake proteins is up-regulated in Fe-deficient roots.

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