Aims: Poorly drained arctic ecosystems are potential large emitters of methane (CH₄) due to their high soil organic carbon content and low oxygen availability. In wetlands, aerenchymatous plants transport CH₄ from the soil to the atmosphere, but concurrently transport O₂ to the rhizosphere, which may lead to oxidation of CH₄. The importance of the latter process is largely unknown for arctic plant species and ecosystems. Here, we aim to quantify the subsurface oxidation of CH₄ in a waterlogged arctic ecosystem dominated by Carex aquatilis ssp. stans and Eriophorum angustifolium, and evaluate the overall effect of these plants on the CH₄ budget. Methods: A mesocosms study was established based on the upper 20 cm of an organic soil profile with intact plants retrieved from a peatland in West Greenland (69°N). We measured dissolved concentrations and emissions of ¹³CO₂ and ¹³CH₄ from mesocosms during three weeks after addition of ¹³C-enriched CH₄ below the mesocosm. Results: Most of the recovered ¹³C label (>98 %) escaped the ecosystem as CH₄, while less than 2 % was oxidized to ¹³CO₂. Conclusions: It is concluded that aerenchymatous plants control the overall CH₄ emissions but, as a transport system for oxygen, are too inefficient to markedly reduce CH₄ emissions.