Effect of Dry-Wet Cycling on Methanotrophs in Wetland Soils

Wetlands occupy a mere 6% of Earth's land surface, yet they contribute 25-45% of global natural methane (CH₄) emissions. A key contradiction emerges here: it is the soil of these wetlands that serves as the host for methane-trophic microorganisms, which can oxidize the vast majority of the methane they produce under specific conditions (for example, the aerobic interface). A wetland's role as either a net source or sink for atmospheric CH₄ is therefore a primary driver of hydrological variability. This research synthesis current understandings of how wet-dry cycles regulate methanotrophic communities and their CH₄ consumption capacity. Shifts in the water table directly modulate methanotroph physiology, community structure, and metabolic activity. These hydrological effects are further amplified or attenuated by nitrogen availability, plant-derived exudates, and edaphic properties. Herein, key knowledge gaps concerning the adaptive responses of methanotrophs to hydrological change are identified, and targeted research priorities improving predictions of wetland CH₄ fluxes under contrasting moisture regimes are accordingly outlined. This review synthesizes recent advances to highlight the mechanistic understanding essential for guiding wetland management strategies.