Abstract

Phosphate is a major plant macronutrient and low phosphate availability severely limits global crop productivity. In Arabidopsis, a key regulator of the transcriptional response to low phosphate, phosphate starvation response 1 (PHR1), is modulated by a class of signaling molecules called inositol pyrophosphates (PP-InsPs). Two closely related diphosphoinositol pentakisphosphate enzymes (AtVIP1 and AtVIP2) are responsible for the synthesis and turnover of InsP8, the most implicated molecule. This study is focused on characterizing Arabidopsis vip1/vip2 double mutants and their response to low phosphate. We present evidence that both local and systemic responses to phosphate limitation are dampened in the vip1/vip2 mutants as compared to wild-type plants. Specifically, we demonstrate that under Pi-limiting conditions, the vip1/vip2 mutants have shorter root hairs and lateral roots, less accumulation of anthocyanin and less accumulation of sulfolipids and galactolipids. However, phosphate starvation response (PSR) gene expression is unaffected. Interestingly, many of these phenotypes are opposite to those exhibited by other mutants with defects in the PP-InsP synthesis pathway. Our results provide insight on the nexus between inositol phosphates and pyrophosphates involved in complex regulatory mechanisms underpinning phosphate homeostasis in plants.

Highlights

  • Inorganic phosphate (Pi) is a critical macronutrient required for optimal plant growth and development

  • To determine if the changes in these vip mutants were associated with alterations in PP-inositol phosphates (InsPs), we focused on the vip1-2/vip2-2 double mutant, and quantified PP-InsPs by radiolabeling with 3 H-myo-inositol using our previously described methods [27]

  • In this paper we characterize novel vip double mutants and compare their responses to limited Pi. We show that both local (RSA) and systemic responses to low phosphate are dampened/reduced in the vip mutants compared to wild type

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Summary

Introduction

Inorganic phosphate (Pi) is a critical macronutrient required for optimal plant growth and development. Pi uptake by plants is a major limit to crop productivity, and modern agriculture relies heavily on the use of phosphate fertilizers. This practice is unsustainable from both geopolitical and environmental perspectives. Manufacture of phosphatic fertilizers is dependent on mined rock phosphate and economically viable sources of these minerals are estimated to be depleted within the 100 years [1]. Compounding this problem, phosphate fertilizers are poorly bioavailable and over-application causes significant ecological damage to fresh and marine waterways. To meet increasing food demand, global agricultural practices must undergo “sustainable intensification” [2]

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