“…Methane can be emitted via several pathways: simple molecular diffusion, ebullition (in the form of bubbles released from oversaturated sediments), plant-mediated flux (Bastviken et al, 2004), but also through so far neglected pathways including aeration, emissions from dry/drying sediments, or dredged organic material (Kosten et al, 2020). Among all, ebullition is considered the dominant pathway (van Bergen et al, 2019;Kosten et al, 2020), which can contribute 50-96 % (Casper et al, 2000;Xiao et al, 2017;van Bergen et al, 2019;Yang et al, 2020;Zhao et al, 2021) to the total CH4 flux. Along with the second important pathwaymolecular diffusion, both exhibit high spatiotemporal variability due to various physical and biological factors acting on very short time scales, for instance, temperature (van Bergen et al, 2019), eutrophication (Zhang et al, 2021), water depth (DelSontro et al, 2016), CH4 production rates (Zhou et al, 2019), CH4 oxidation rates (Sanseverino et al, 2013), dissolved oxygen concentration (Xiao et al, 2017), management regime (Yang et al, 2019), or the quality of organic matter in the sediment (Schmiedeskamp et al, 2021).…”