The Crisis of Forest Methane Absorption Capacity Due to Increased Anaerobic Stress in High-CO2 Environments: Mitigation Measures

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Abstract
Methane (CH4) is the second most important greenhouse gas after carbon dioxide (CO2), and its atmospheric concentration is on the rise. Soil CH4 consumption (=absorption) capacity is declining due to reduced forests and green spaces, as well as other environmental factors and anaerobic stresses. Environmental and stand structure parameters were cross-referenced with publicly available international ecosystem databases, such as FLUXNET, ICOS, NEON, AmeriFlux, the TRY plant trait database and the Oak Ridge FACE site. Searches were conducted using keywords such as region, water level, and stand density. The data indicate that under high-CO2 conditions, the increase of forest canopy density leads to increased litter accumulation on the forest floor and reduced sunlight penetration, creating anaerobic conditions. This can cause forests to shift from CH4 consumption to CH4 release. Based on these findings, we discussed methods to maintain and enhance the CH4-absorbing capacity of forest soils. This can be achieved through management practices that improve environmental conditions and increase soil fauna’s activity, such as those associated with thinning operations in overmature forest stands across various regions. This ecological manipulation through thinning practices promotes ground-level temperature increases and the activities of soil fauna, as well as maintaining aerobic conditions near the soil surface.

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