In general, soil respiration rates correlated exponentially with soil temperature (R varied between 0.85-0.95). Q10 calculated varied between 3~3.7 for each treatments. As expected, soil respiration was 10~20% higher in the tulip poplar treatment than in the beech treatment (P<0.05). Hovewer, plots amended with beech leaves were more sensitive to temperature change: Q10 was higher by 0.2 (P<0.05). Soil respiration was about 5~10% higher in earthworm addition plots than in earthworm removal plots (P<0.05). Soil respiration in the earthworm manipulation plots was generally higher in the mature forest than successional forest (P<0.001) whereas in control plots the patten is opposite (P<0.001) . We found significant interactions between leaf litter and forest stage (P<0.001), earthworm and forest stage (P<0.001), but not between leaf litter and earthworms. Our results indicated that forest age and tree composition play an important role since both quality and quantity of lea litter input is different in young and old forests. Our results also suggested that earthworm can directly or indirectly increase C turnover, but these effects are confounded by other factors.