Abstract

The soybean (Glycine max L. merr) genotype Fiskeby III is highly resistant to a multitude of abiotic stresses, including iron deficiency, incurring only mild yield loss during stress conditions. Conversely, Mandarin (Ottawa) is highly susceptible to disease and suffers severe phenotypic damage and yield loss when exposed to abiotic stresses such as iron deficiency, a major challenge to soybean production in the northern Midwestern United States. Using RNA-seq, we characterize the transcriptional response to iron deficiency in both Fiskeby III and Mandarin (Ottawa) to better understand abiotic stress tolerance. Previous work by our group identified a quantitative trait locus (QTL) on chromosome 5 associated with Fiskeby III iron efficiency, indicating Fiskeby III utilizes iron deficiency stress mechanisms not previously characterized in soybean. We targeted 10 of the potential candidate genes in the Williams 82 genome sequence associated with the QTL using virus-induced gene silencing. Coupling virus-induced gene silencing with RNA-seq, we identified a single high priority candidate gene with a significant impact on iron deficiency response pathways. Characterization of the Fiskeby III responses to iron stress and the genes underlying the chromosome 5 QTL provides novel targets for improved abiotic stress tolerance in soybean.

Highlights

  • Fiskeby III is reported to be more tolerant to a variety of abiotic stresses than most soybean germplasm [24,25,26,27,28]

  • There were no statistical difference in soil-plant analysis development (SPAD) chlorophyll readings between Fiskeby III and Mandarin

  • While the precise role Glyma.05G001700 plays in conferring tolerance to FeD stress remains unknown, our analyses confirm its importance in the Fiskeby III iron stress response

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Summary

Introduction

Iron deficiency chlorosis (IDC) is a major issue in most non-graminaceous crop species around the world. Though iron (Fe) is prevalent in all soils, a variety of factors, including soil composition, moisture, and pH levels, can render Fe2+ biologically unavailable. Two different strategies have been identified for iron uptake in plant species [1]. Dicot species, including soybean, utilize the strategy I system where protons are secreted into the rhizosphere by ARABIDOPSIS H+ ATPase 2 (AHA2) [2] to acidify the soil. This releases iron from various cofactors, and it is reduced into the biologically available Fe2+ by FERRIC

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