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Does hydrogenotrophic methanogenesis occur in seagrass beds? Insights from whole-ecosystem stable isotope labelling
Journal article   Open access   Peer reviewed

Does hydrogenotrophic methanogenesis occur in seagrass beds? Insights from whole-ecosystem stable isotope labelling

Mona Abouhaidar Andskog, Ana Sierra Padilla, Tijs Joling, Damien T Maher, James Z. Sippo, Jack Middelburg, Bradley D. Eyre and Joanne M Oakes
Environmental research letters, Vol.21(14), pp.1-27
22/07/2026
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Abstract

seagrass methane stable isotopes blue carbon methanogenesis
Seagrass beds are blue carbon ecosystems; however, they release methane (CH<sub>4</sub> ), a potent greenhouse gas. Although likely important, the influence of primary production on methanogenic pathways remains understudied. We labelled intact seagrass-sediment cores and in situ seagrass beds with 13 C-dissolved inorganic carbon ( <sup>13</sup> C-DIC) to trace the transfer to <sup>13</sup> C-CH<sub>4</sub> over a short (<24 hours) and long (35 days) time frame. Labelled carbon was transferred from DIC to CH<sub>4</sub> in the absence of primary production, indicating hydrogenotrophic methanogenesis or mixotrophy. Longer-term persistent in situ <sup>13</sup> C-CH<sub>4</sub> release suggests that CH<sub>4</sub> was also produced from <sup>13</sup> C-labelled organic substrates. The transformation rate of <sup>13</sup> C-DIC to 13 C-CH<sub>4</sub> was reduced by 50% in the light, indicating interactions with primary production via CH<sub>4</sub> oxidation, oxidative stress, or substrate competition. Additionally, dark CH<sub>4</sub> fluxes (5.1 ± 0.7 μmol m -2 d -1 ) were 16% higher than light CH<sub>4</sub> fluxes (4.3 ± 0.4 μmol m -2 d -1 ) in seagrass beds under in situ conditions. These findings highlight the role of plant-sediment interactions in governing methanogenic pathways, with implications for seagrass beds as carbon-sequestering hotspots and CH<sub>4</sub> sources.

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