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Do biomolecular condensates regulate the transcriptional and post-transcriptional responses of plant roots to water deficit?

Published online by Cambridge University Press:  12 November 2025

Coralie Masson
Affiliation:
Institute for Plant Sciences of Montpellier (IPSiM), Univ Montpellier, CNRS, INRAE, Institut Agro, Montpellier, France
Hanzhang Yu
Affiliation:
Institut de biologie moléculaire des plantes (IBMP), CNRS, Université de Strasbourg, Strasbourg, France
Fabrice Bauget
Affiliation:
Institute for Plant Sciences of Montpellier (IPSiM), Univ Montpellier, CNRS, INRAE, Institut Agro, Montpellier, France UMR AGAP Institut, Univ Montpellier, CIRAD, INRAE, Institut Agro, Montpellier, France CIRAD, UMR AGAP Institut, F-34398 Montpellier, France
Dominique Gagliardi
Affiliation:
Institut de biologie moléculaire des plantes (IBMP), CNRS, Université de Strasbourg, Strasbourg, France
Yann Boursiac*
Affiliation:
Institute for Plant Sciences of Montpellier (IPSiM), Univ Montpellier, CNRS, INRAE, Institut Agro, Montpellier, France
*
Corresponding author: Yann Boursiac; Email: yann.boursiac@inrae.fr

Abstract

Water deficit at the plant cell level can be assimilated to a reduction in turgor pressure and an increase in osmotic pressure. In a previous work, we showed that the mRNA abundance of some genes displays a quantitative relationship to these physicochemical parameters. Biomolecular condensates have been shown to depend on the physicochemical environment and are known to regulate mRNA fate. In this review, we present recent work about the implication of biomolecular condensates in mRNA regulation of plants under water deficit and question the biophysical origin of their dynamics. Data in the literature suggest that while the perception of mild water deficit may have been overlooked, biomolecular condensates are clear candidates to sense and transduce severe water deficit in plant cells.

Information

Type
Review
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2025. Published by Cambridge University Press in association with John Innes Centre
Figure 0

Figure 1. Key examples of biomolecular condensates regulating mRNA fate in plants under osmotic stress conditions. Note: In addition to their role in mRNA sequestration, biomolecular condensates are involved at various steps of the mRNA life cycle in plants confronted with osmotic stresses. For example, SEU, a transcription regulator, and STM form nuclear condensates under osmotic stress to facilitate transcriptional responses (Cao et al., 2023; Wang et al., 2022). OsFKBP20-1b colocalizes with UBP1b in stress granules and with SR45, a protein involved in splicing (Park et al., 2020). DCP5, meanwhile, exhibits rapid assembly dynamics that are dependent on osmolarity to regulate the transcriptome (Wang et al., 2024b). CBC, cap binding complex; Pol II, RNA polymerase II; PABPN, nuclear poly(A) binding protein; PABPC, cytoplasmic poly(A) binding protein; eIF4E, eukaryotic translation initiation factor 4E.

Figure 1

Figure 2. Schematic turgor pressure (black line, left axis) and osmotic pressure (green line, right axis) versus water potential of cells during a hyper-osmotic shock. Greyed zone represents the turgid state of the cell, beyond this zone, the cell is plasmolyzed, the turgor pressure is zero and the water potential is equal to –Π. Horizontal segments and points represent osmotic shock ranges or values found for plant cells in the literature (cf main text). P and Π were calculated using ϵ = 2.23MPa and an initial turgor pressure of 0.41MPa. The initial osmotic pressure was set equal to the initial P. Π was calculated using the mass balance into the cell, where the relative variation of solute concentration, and so the relative osmotic pressure variation, is the inverse of the relative volume variation. P is calculated from the elastic modulus definition, and $\varPsi =P\hbox{--} \varPi$. Note that some observations were made in the root apical meristem, which could lose turgor at higher osmotic treatments. For more information, see Supplementary Material S1.

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