Untargeted metabolomics reveals anion and organ-specific biochemistry of salinity tolerance in willow
Sas, E.; Fremont, A.; Gonzalez, E. J. B.; Sarrazin, M.; Barnabe, S.; Labrecque, M.; Brereton, n. J. B.; Pitre, F. E.
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1Willows can alleviate soil salinisation while generating sustainable feedstock for biorefinery, yet the metabolomic adaptations underlying their salt tolerance remain poorly understood. Testing two environmentally abundant salts, the response of Salix miyabeana was assessed after treatment with a moderate concentration of NaCl, and both moderate and high concentrations of Na2SO4 in a 12-week pot trial. Willows tolerated salts across all treatments (up to 9.1dS m-1 soil ECe), maintaining photosynthesis and biomass while selectively partitioning ions, confining Na+ to roots and accumulating Cl- and SO 2- in the canopy, and adapting to osmotic stress via reduced stomatal conductance. Untargeted LC-MS/MS captured over 5,000 putative compounds, characterising the baseline willow metabolome, including 278 core compounds constitutively produced across organs. Comparative statistical analyses revealed widespread metabolic reprogramming in response to soil salinity, altering 28% of the overall metabolome, and highlighting organ-tailored regulation. Comparing both salt forms at equimolar sodium, generalised salinity responses were limited to 3% of the metabolome, predominantly in roots. Anion-specific metabolomic responses were more extensive, with NaCl reducing carbohydrates and TCA intermediates, thereby exerting pressure on carbon and energy resources, alongside the accumulation of root structuring compounds, antioxidants flavonoids, and fatty acids. In contrast, Na2SO4 salinity triggered accumulation of sulphur-containing larger peptides, suggesting that excess sulphate incorporation leverage ion toxicity to produce specialized salt-tolerance associated metabolites. This high-depth picture of the willow metabolome underscores the importance of capturing plant adaptations to salt stress at organ-scale and considering ion-specific contributions to soil salinity.
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