Back to the roots: Characterizing root exudates of dominant tundra plants to improve the understanding of plant-soil interactions in a changing arctic

Global warming increases the vegetation cover and leads to shifts in vegetation types in the Arctic. An increase in the vegetation cover might substantially enhance carbon dioxide (CO 2 ) emissions from northern permafrost soils, since root exudation of labile carbon and nitrogen can stimulate soil organic matter (SOM) decomposition via the rhizosphere priming effect. The current understanding of Arctic rhizosphere priming largely rests on soil incubation studies that simulate root exudation by adding various organic substrates in varying concentrations to soils. How the specific exudates of different plants influence rhizosphere priming is unclear as Arctic plant root exudate release rates and composition are largely unknown. Using targeted and non-targeted liquid chromatography–mass spectrometry, we compared the exudate composition and exudation rates of total organic carbon, 7 organic acids, 14 amino acids and 9 carbohydrates from three abundant and functionally different tundra plants ( Betula glandulosa , Alnus viridis and Eriophorum vaginatum ). While organic carbon and primary metabolites exudation were similar among the studied plants despite their different nitrogen acquisition strategies, distinct differences between the plant species were found in the overall root exudate composition. Between 80 to 94% of the root exudate metabolome was not shared among the three plants. Our findings indicate that a change in vegetation types across the Arctic will primarily alter the release of secondary plant metabolites into the soil and thereby could alter soil microbial processes. Our observations further suggest that previous laboratory experiments studying priming frequently oversaturated microorganisms with labile substrates compared to natural conditions; this highlights the need for more realistic priming studies. Our data on root exudation provide critical background information for improving laboratory experiments. • Total exuded carbon and primary metabolites were not different between plant species • The overall root exudate metabolome was different between plant species • Metabolome diversity is likely related to nitrogen uptake strategies • Previous incubation studies use substrate additions equalling several growing seasons • Mechanistic priming studies could be improved by observational root exudation data

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Publication Details

Journal
Soil Biology and Biochemistry
Published
2025-06-24
DOI
https://doi.org/10.1016/j.soilbio.2025.109897
Citations
9
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
11.71
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article

Back to the roots: Characterizing root exudates of dominant tundra plants to improve the understanding of plant-soil interactions in a changing arctic

A. F. Carter, Sylvain Monteux, Rica Wegner, Merle Plassmann et al.
9 citations
Soil Biology and Biochemistry
Climate change and permafrost
11.71
article

Back to the roots: Characterizing root exudates of dominant tundra plants to improve the understanding of plant-soil interactions in a changing arctic

A. F. Carter, Sylvain Monteux, Rica Wegner, Merle Plassmann, Birgit Wild, Lewis Sauerland, Eva Oburger
article en
9 citations

Abstract

Global warming increases the vegetation cover and leads to shifts in vegetation types in the Arctic. An increase in the vegetation cover might substantially enhance carbon dioxide (CO 2 ) emissions from northern permafrost soils, since root exudation of labile carbon and nitrogen can stimulate soil organic matter (SOM) decomposition via the rhizosphere priming effect. The current understanding of Arctic rhizosphere priming largely rests on soil incubation studies that simulate root exudation by adding various organic substrates in varying concentrations to soils. How the specific exudates of different plants influence rhizosphere priming is unclear as Arctic plant root exudate release rates and composition are largely unknown. Using targeted and non-targeted liquid chromatography–mass spectrometry, we compared the exudate composition and exudation rates of total organic carbon, 7 organic acids, 14 amino acids and 9 carbohydrates from three abundant and functionally different tundra plants ( Betula glandulosa , Alnus viridis and Eriophorum vaginatum ). While organic carbon and primary metabolites exudation were similar among the studied plants despite their different nitrogen acquisition strategies, distinct differences between the plant species were found in the overall root exudate composition. Between 80 to 94% of the root exudate metabolome was not shared among the three plants. Our findings indicate that a change in vegetation types across the Arctic will primarily alter the release of secondary plant metabolites into the soil and thereby could alter soil microbial processes. Our observations further suggest that previous laboratory experiments studying priming frequently oversaturated microorganisms with labile substrates compared to natural conditions; this highlights the need for more realistic priming studies. Our data on root exudation provide critical background information for improving laboratory experiments. • Total exuded carbon and primary metabolites were not different between plant species • The overall root exudate metabolome was different between plant species • Metabolome diversity is likely related to nitrogen uptake strategies • Previous incubation studies use substrate additions equalling several growing seasons • Mechanistic priming studies could be improved by observational root exudation data

Soil Biology and BiochemistryVol. 209
Stockholm University (SE), Bolin Centre for Climate Research (SE), UiT The Arctic University of Norway (NO), BOKU University (AT)
Zero hunger
Openalex Percentile: Top 1%
Climate change and permafrost
11.71
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