Preprints
https://doi.org/10.5194/egusphere-2026-467
https://doi.org/10.5194/egusphere-2026-467
29 Jan 2026
 | 29 Jan 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Plant belowground traits indicate increased plant-mediated methane transport along a peatland permafrost thaw gradient

Tiia Määttä, Samantha Bosman, Jeffrey Chanton, Patrick Crill, Suzanne Hodgkins, Jalisha Theanutti Kallingal, Rachel Wilson, Ruth Varner, and Avni Malhotra

Abstract. Permafrost thaw in subarctic peatlands alters ecosystem methane (CH4) fluxes. Collapsing permafrost palsas change hydrology, interstitial oxygen availability, and vegetation composition, and each of these factors contribute to net CH4 flux by influencing CH4 production, consumption and transport. However, changes in plant-mediated CH4 fluxes have mostly been estimated using aboveground characteristics, such as biomass and leaf area, leaving belowground parts (roots and rhizomes) understudied despite their direct contact to depth-dependent CH4 flux processes. Here, we explored the potential of using root and rhizome traits as proxies for plant-mediated CH4 cycling along a peatland permafrost thaw gradient in subarctic Sweden. We investigated changes in root and rhizome biomass, surface area (SA), diameter, tissue density (TD), and specific root length (SRL) along the permafrost thaw gradient, and how these traits relate to early-, middle-, peak- and season median CH4 fluxes. We utilized chamber CH4 flux and pore water CH4 concentration and isotopic measurements during the productive season. Shrub SRL, diameter and isotopic data suggested increased plant-mediated carbon substrates available for acetoclastic methanogenesis across the thaw gradient. Root TD, proxy for root porosity, decreased with thaw and had negative correlations with CH4 fluxes throughout the season. Simultaneously, herbaceous rhizome SA-CH4 flux correlations were positive and pore water CH4 concentrations were lowest in the fully thawed stage. These results indicated increasing herbaceous plant-mediated transport of acetoclastically-produced CH4 with thaw. Our study demonstrates that integrating plant belowground traits with environmental and biogeochemical data can help improve CH4 flux predictions in thawing landscapes and revealed key mechanistic insights regarding the interplay between substrate availability for methanogenesis and gas transport.

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Tiia Määttä, Samantha Bosman, Jeffrey Chanton, Patrick Crill, Suzanne Hodgkins, Jalisha Theanutti Kallingal, Rachel Wilson, Ruth Varner, and Avni Malhotra

Status: open (until 12 Mar 2026)

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Tiia Määttä, Samantha Bosman, Jeffrey Chanton, Patrick Crill, Suzanne Hodgkins, Jalisha Theanutti Kallingal, Rachel Wilson, Ruth Varner, and Avni Malhotra

Data sets

Plant belowground trait and vegetation survey data from the Stordalen mire 2023 Tiia Määttä and Avni Malhotra https://doi.org/10.5281/zenodo.18269229

CH4 & DIC concentrations & δ13C from porewater at Stordalen Mire, July 2023 Rachel Wilson et al. https://doi.org/10.5281/zenodo.18363867

Tiia Määttä, Samantha Bosman, Jeffrey Chanton, Patrick Crill, Suzanne Hodgkins, Jalisha Theanutti Kallingal, Rachel Wilson, Ruth Varner, and Avni Malhotra

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Short summary
Permafrost thaw can lead to vegetation shifts and higher methane (CH4) emissions in peatlands. However, plant belowground controls of these emissions are uncertain. We investigated how plant roots and rhizomes contribute to CH4 emissions along a peatland permafrost thaw gradient. We found that low herbaceous plant root tissue density and high rhizome surface area were associated with higher CH4 emissions. This indicated increased plant-mediated CH4 transport with thaw.
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