Distinct responses of soil carbon-degrading enzyme activities to warming in two alpine meadow ecosystems on the Qinghai-Tibet Plateau
Xinran Wu , Yuanrui Peng , Tao Wang , Noman Ahmad , Xuesong Bai , Ruiying Chang
Soil Ecology Letters ›› 2025, Vol. 7 ›› Issue (2) : 240291
Distinct responses of soil carbon-degrading enzyme activities to warming in two alpine meadow ecosystems on the Qinghai-Tibet Plateau
Soil extracellular enzymes play a central role in regulating soil organic carbon (SOC) dynamics. However, the effects of varying warming magnitudes and duration on permafrost soil carbon-degrading enzyme activities remain poorly understood. Here, we investigated warming effects on three representative carbon-degrading enzymes (β-1,4-glucosidase (BG), peroxidase (PER), phenol oxidase (POX)) in alpine and swamp meadows on the Qinghai-Tibet Plateau. The warming experiments were conducted using Open-top chambers at different warming magnitudes (+2.4 and +4.9 °C) and duration (3 and 6 years) in both meadows. The activity of BG increased with warming duration in alpine meadows regardless of the warming magnitude (69% and 45% for lower and higher warming treatments, respectively), although the effect was significant (p<0.05) only under 6-year warming. In contrast, warming did not significantly (p>0.05) alter BG activity in swamp meadows. Warming decreased POX activity in both alpine (62%) and swamp meadows (81%), but the effect was significant only under 6-year higher warming. Moreover, PER activity was not significantly influenced by warming in either meadow. Dissolved organic carbon and above-ground biomass were the primary factors influencing soil enzyme activities under warming in alpine meadow, while soil water content in swamp meadow. Noticeably, a negative correlation (p<0.05) was observed between SOC and oxidase/hydrolase activity in alpine meadow, suggesting the suppression of oxidase activity may benefit SOC storage under warming. Noticeably, a negative correlation (p<0.05) between SOC and oxidase/hydrolase activity was found in alpine meadow but not in swamp meadow, which was due to the difference in above-ground biomass. These findings highlight the need to consider the time-cumulative warming effects on plant growth and enzyme ratios in carbon models to improve the accuracy of model predicting of soil carbon dynamics in permafrost regions.
soil extracellular enzyme / soil organic carbon / warming magnitude / warming duration / alpine meadows / swamp meadows
| ● Soil C-acquiring enzyme activities of alpine and swamp meadows were examined under warming. | |
| ● BG activity increased with warming duration in alpine meadow but not in swamp meadows. | |
| ● Warming tended to decrease POX activity in both alpine and swamp meadows. | |
| ● SOC was negatively correlated with the ratio of oxidase to hydrolase activity in alpine meadows. |
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Higher Education Press
Supplementary files
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