Aquatic Plant Roots May Quietly Devour Up to 81% of Their Methane Before It Reaches the Air

Freshwater ecosystems are among the planet’s most important natural sources of methane, a greenhouse gas that packs roughly eighty times the warming power of carbon dioxide over a twenty-year horizon. Wetlands, lakes, and ponds fringed with dense vegetation have long been recognized as methane hotspots, yet the exact magnitude of their emissions remains stubbornly difficult to pin down. A new study published in the journal Biogeochemistry by Charlotte Grasset of Uppsala University in Sweden now reveals that a hidden biological filter operating in the muddy root zone of aquatic plants may explain much of that variability, and the findings could reshape how scientists model methane emissions from vegetated inland waters around the world.

The central puzzle the study addresses is deceptively simple. Aquatic plants are equipped with internal air channels, known as aerenchyma, that shuttle oxygen down to their waterlogged roots while allowing gases produced in the sediment to escape upward and out into the atmosphere. This plumbing system makes plants the primary conduit through which methane, generated by microbes decomposing organic matter in oxygen-starved sediments, reaches the air. But the same root zone also hosts methanotrophic bacteria, methane-consuming microbes that thrive where oxygen leaking from roots meets methane rising from below. The question has always been how much methane these bacteria intercept before it ever enters the plant’s internal gas highway.

Previous measurements of this process, called rhizospheric oxidation, had been carried out on only a handful of species in natural settings, leaving scientists with little idea of how the phenomenon varies across the enormous diversity of aquatic plants. Some species move gases with remarkable efficiency, using pressure-driven convective bulk flow that can ventilate their tissues rapidly, while others rely on slower molecular diffusion. Grasset reasoned that this variation in transport efficiency might hold the key to understanding why some vegetated habitats emit far more methane than others, and she designed an experiment to test the idea across an unusually broad range of species.

The study examined eleven different aquatic plant species spanning a spectrum of gas transport capabilities. To quantify both methane oxidation and methane transport simultaneously and in situ, Grasset employed a dual stable isotope approach, a technique that tracks the fate of methane molecules by measuring how their isotopic signatures shift as they move through the plant-soil system. Because methanotrophic bacteria preferentially consume lighter isotopes of methane, the residual methane that survives oxidation and reaches the atmosphere carries a distinctive heavy isotopic fingerprint. By reading these fingerprints in the field, the researcher could calculate what fraction of the methane produced in the sediment was being oxidized in the rhizosphere of each species before release.

The results were striking. For plants that transport gases efficiently, up to eighty-one percent of the methane produced in the surrounding sediment was oxidized before it could escape through the plant tissues. In other words, in the most effective gas movers, more than four out of every five methane molecules generated by methanogenic archaea in the anoxic sediment never made it to the atmosphere at all. They were instead converted to carbon dioxide by methane-oxidizing bacteria in the thin oxygenated halo surrounding the roots, a transformation that drastically reduces the climate impact of the carbon leaving the sediment.

Perhaps even more consequential was the pattern that emerged across species. The fraction of methane oxidized was negatively correlated with the amount of methane each plant released. Efficient gas transporters, despite their powerful internal ventilation systems that might be expected to flush methane out rapidly, ended up emitting less methane than their slower-breathing counterparts. This counterintuitive relationship suggests that the very plants best equipped to move gases are also the ones that deliver the most oxygen to their rhizospheres, fueling the methanotrophic bacteria that consume the methane before it can be vented. The efficient plumbing, in effect, feeds the biological filter that neutralizes the gas.

Grasset is careful to note that the correlation, while compelling, does not yet establish causality. It remains possible that other factors, such as sediment chemistry, root architecture, or differences in methane production rates among the studied habitats, contribute to the observed pattern. Further experimental studies will be needed to confirm that high gas transport efficiency directly drives higher rhizospheric oxidation. Even so, the magnitude of the oxidation fractions measured, and their consistent relationship with plant-mediated methane release across eleven species, represents a major advance over the sparse species-level data that existed before.

The implications for global climate science are considerable. Methane emissions from vegetated freshwater habitats are among the most uncertain terms in global greenhouse gas budgets, in large part because emission models struggle to account for the enormous variability observed between different plant communities and species. Current approaches often treat aquatic vegetation as a single functional group, or rely on crude proxies for plant-mediated transport. If rhizospheric oxidation varies systematically with species traits such as gas transport efficiency, as this study suggests, then incorporating that trait into emission models could dramatically reduce the uncertainty in methane budgets for wetlands, lake margins, and other vegetated inland waters.

The study also points toward a practical framework for classifying aquatic plants by their climate behavior. Grasset argues that a mechanistic understanding of how plants release methane is necessary to define aquatic plant functional types with contrasting methane emissions, analogous to the plant functional types long used in terrestrial vegetation models. Species with high gas transport efficiency and high rhizospheric oxidation would fall into one category, emitting relatively little methane per unit of production, while species with sluggish internal ventilation and weak oxidation would form another. Mapping which types dominate which ecosystems could allow Earth system models to generate far more accurate predictions of how freshwater methane emissions will respond to climate change, permafrost thaw, and shifting vegetation distributions.

As researchers work to refine these models, the study stands as a vivid reminder that some of the most important climate regulation on the planet happens at scales invisible to the naked eye, in the oxygenated microzone hugging the roots of a water lily or a reed. The dual isotope technique deployed here offers a template for future in situ measurements across other ecosystems and climates, from boreal fens to tropical floodplains. If the relationship between transport efficiency and oxidation holds up under further scrutiny, the humble root zone of aquatic plants may prove to be one of nature’s most underappreciated methane filters, quietly scrubbing the majority of a potent greenhouse gas from the flux that would otherwise escape into a warming atmosphere.

Subject of Research: Methane rhizospheric oxidation by aquatic plants and its role in regulating freshwater methane emissions

Article Title: Methane rhizospheric oxidation and its ecosystem significance across different aquatic plant species

Article References: Grasset, C. (2026). Methane rhizospheric oxidation and its ecosystem significance across different aquatic plant species. Biogeochemistry. https://doi.org/10.1007/s10533-026-01374-4

Image Credits: AI Generated

DOI: 10.1007/s10533-026-01374-4

Keywords: methane, aquatic plants, rhizosphere, methanotrophy, aerenchyma, greenhouse gas, stable isotopes, wetlands, biogeochemistry, plant-mediated transport, freshwater emissions, climate