Climate warming and permafrost degradation will increase greenhouse gas emissions from the permafrost swamps. However, the fluxes of these trace gases have been scarcely quantified in cold temperate zone continuous permafrost region. The seasonal variation and the influence factors (temperature, water level, depth of thawing, and soil organic carbon and nitrogen content) of emission fluxes of greenhouse gas including CO₂, CH₄, and N₂O from seven kinds of natural swamps (Carex schmidtii marsh-C, Betula ovalifolia-C. schmidtii shrub swamp-G, Alnus sibirica-C. schmidtii swamp-M, B. platyphylla-C. schmidtii swamp-B, Larix gmelinii-C. schmidtii swamp-LT, Larix gmelinii-moss swamp-LX, and Larix gmelinii-Sphagnum spp. swamp-LN) were studied over a one-year period by static chamber-GC technique in continuous permafrost region at the Daxing'an Mountains, northeast China. The results showed that: (1) the CO₂ annual average emission flux (125.12-163.33 mg m^-2 h^-1) was similar. (2) CH₄ annual average emission flux (-0.007-0.400 mg m^-2 h^-1) exhibited a different trend in C greater than that of others (5.6-65.7 times greater than the others, P<0.01). (3) N₂O annual average emission flux (1.52-37.90 μg m^-2 h^-1) had significant differences among all the sites (M, B was 2.0-23.9 times higher than that of others, P<0.05, LT, LX and LN was 2.9-6.2 times greater than C and G, P<0.05); (4) The three greenhouse gases emissions from seven kinds of wetlands were controlled partly by soil temperature, water level, thaw depth, soil organic carbon and nitrogen content, carbon to nitrogen ratio, pH value, and water content. The CO₂ emissions were mainly controlled by soil temperature, and that of B, LT, LX, and LN were also controlled by the water level. The CH₄ emissions were mainly controlled by soil temperature and thaw depth. The N₂O emissions were controlled partly by soil temperature, water level, thaw depth, soil organic carbon and nitrogen content, carbon to nitrogen ratio, pH value, and water content. Above environmental factors can explain the variation of soil N₂O flux by 26%-99%. (5) The global warming potential (GWP) of the seven natural wetland soils were similar ranged in 11.05-15.37 t CO₂ hm^-2 a^-1, which all were dominated by CO₂. The C took CH₄ as the secondary position and forested wetlands took N₂O as the secondary position. Based on the results, it was found that these swamp soils in the permafrost region of Daxing'an Mountains are still in the low emission stage of CO₂, CH₄ and N₂O.