A laboratory experiment was conducted to assess the effects of the freezing thawingcycles (FTCs) on soil microbial biomass carbon (MBC), and CO2 and CH4 emissions from wetland soils in the continuous permafrost zone (TQ) and seasonally frozen region (JC) of Northeast China. Soil samples were incubated at different frost intensities \[+5 (control), -5, and -15 ℃\] for 12 h respectively, and then thawed at +5 ℃ for 12 h. These freezethaw cycles were repeated for 0, 1, 5, 10, and 15 times. The results showed that the CO2 and CH4 emission rates and MBC of two types of soil decreased after the first freezethaw incubation, and presented an increase and then decrease pattern and then trended to be stable with the increases of cycling times. Compared with the control (5 ℃) and low frost intensity (-5 ℃) treatments, high frost intensity (-15 ℃) significantly promoted CO2 and CH4 emissions but did not significantly influence MBC. At -15 ℃, the cumulative CO2 emissions from TQ soil reached 679.99 mg·kg-1 after 15 FTCs, which was about 50% higher than that of JC soil (454.32 mg·kg-1). The highest cumulative CH4 emission from TQ soil was 334.49 μg·kg-1 at -5 ℃ after 15 FTCs, while this value was 600.07 μg·kg-1 at -15 ℃ for JC soil. The temperature sensitivities of methanogens might bedifferent between these two frozen soils during the freezingthawing cycles. Our results provide scientific data for the assessment of global climate change on soil carbon turnover in the mainpermafrost regions of Northeast China.