Abstract. The degradation of organic matter to CH 4 and CO 2 was investigated in three different boreal peatland systems in Finland, a mesotrophic fen (MES), an oligotrophic fen (OLI), and an ombrotrophic peat (OMB). MES had similar production rates of CO 2 and CH 4 , but the two nutrientpoor peatlands (OLI and OMB) produced in general more CO 2 than CH 4 . δ 13 C analysis of CH 4 and CO 2 in the presence and absence methyl fluoride (CH 3 F), an inhibitor of acetoclastic methanogenesis, showed that CH 4 was predominantly produced by hydrogenotrophic methanogenesis and that acetoclastic methanogenesis only played an important role in MES. These results, together with our observations concerning the collective inhibition of CH 4 and CO 2 production rates by CH 3 F, indicate that organic matter was degraded through different paths in the mesotrophic and the nutrient-poor peatlands. In the mesotrophic fen, the major process is canonical fermentation followed by acetoclastic and hydrogenotrophic methanogenesis, while in the nutrient-poor peat, organic matter was apparently degraded to a large extent by a different path which finally involved hydrogenotrophic methanogenesis. Our data suggest that degradation of organic substances in the oligotrophic environments was incomplete and involved the use of organic compounds as oxidants.