CH_4 emission from different stages of thermokarst formation in Central Yakutia, East Siberia(Environment)

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The present study was carried out to evaluate the effect of permafrost thawing on methane (CH_4) emission from different development stages of thermokarst formation in Central Yakutia, East Siberia. Four stages of thermokarst, "Bullar," "Dyede," "Tuumpu" and mature "Alas," differing in age, depth of depression and water presence, were selected for examination. The emission of CH_4 was measured at each thermokarst in forest, dry grassland, wet grassland and on the pond surface. The forest plots were CH_4 sinks and uptake ranged from -1 to -34μg C m^<-2> h^<-1>. The CH_4 fluxes from dry grasslands ranged from -5.4 to 0.9μg C m^<-2> h^<-1>, and in wet grasslands CH_4 fluxes substantially increased, ranging from 3.6 to 285μg C m^<-2> h^<-1>. Pond surfaces had the highest CH_4 emissions, ranging from 657 to 8.0×10^3μg C m^<-2> h^<-1>. The amount of CH_4 stored in the permafrost (up to a depth of 15m) was estimated to be approximately 0.259g C m^<-2>. This value was small compared with the current CH_4 emission from pond surfaces (4.3-16g C m^<-2> growing season^<-1>) in thermokarst depressions. Accordingly, the release of CH_4 trapped in the permafrost was not significant compared with the high CH_4 emission from the pond surface in young thermokarst depressions. The formation of thermokarst involving permafrost thawing could influence the regional CH_4 budget significantly by forming thermokarst wetlands that produce and emit CH_4 as a result of current microbial processes under anaerobic conditions.

CH_4 emission from different stages of thermokarst formation in Central Yakutia, East Siberia(Environment)

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