详细信息
Plant and Soil Enzyme Activities Regulate CO2 Efflux in Alpine Peatlands After 5 Years of Simulated Extreme Drought ( SCI-EXPANDED收录) 被引量:13
文献类型:期刊文献
英文题名:Plant and Soil Enzyme Activities Regulate CO2 Efflux in Alpine Peatlands After 5 Years of Simulated Extreme Drought
作者:Yan, Zhongqing[1,2] Kang, Enze[1,2] Zhang, Kerou[1,2] Li, Yong[1,2] Hao, Yanbin[3] Wu, Haidong[4] Li, Meng[1,2] Zhang, Xiaodong[1,2] Wang, Jinzhi[1,2] Yan, Liang[1,2] Kang, Xiaoming[1,2]
第一作者:Yan, Zhongqing;闫钟清
通信作者:Kang, XM[1];Kang, XM[2]
机构:[1]Chinese Acad Forestry, Inst Wetland Res, Beijing Key Lab Wetland Serv & Restorat, Beijing, Peoples R China;[2]Tibetan Autonomous Prefecture Aba, Sichuan Zoige Wetland Ecosyst Res Stn, Zoige, Peoples R China;[3]Univ Chinese Acad Sci, Beijing, Peoples R China;[4]Minist Ecol & Environm, Informat Ctr, Beijing, Peoples R China
年份:2021
卷号:12
外文期刊名:FRONTIERS IN PLANT SCIENCE
收录:;WOS:【SCI-EXPANDED(收录号:WOS:000715221000001)】;
基金:This study was supported by the National Non-profit Institute Research Grant (CAFYBB2019SY030), the National Natural Science Foundation of China (32171597 and 42041005), and the National Non-profit Institute Research Grant (CAFYBB2020ZA004).
语种:英文
外文关键词:alpine peatland; extreme drought; ecosystem respiration; soil respiration; extracellular enzyme activities
摘要:Increasing attention has been given to the impact of extreme drought stress on ecosystem ecological processes. Ecosystem respiration (Re) and soil respiration (Rs) play a significant role in the regulation of the carbon (C) balance because they are two of the largest terrestrial C fluxes in the atmosphere. However, the responses of Re and Rs to extreme drought in alpine regions are still unclear, particularly with respect to the driver mechanism in plant and soil extracellular enzyme activities. In this study, we imposed three periods of extreme drought events based on field experiments on an alpine peatland: (1) early drought, in which the early stage of plant growth occurred from June 18 to July 20; (2) midterm drought, in which the peak growth period occurred from July 20 to August 23; and (3) late drought, in which the wilting period of plants occurred from August 23 to September 25. After 5 years of continuous extreme drought events, Re exhibited a consistent decreasing trend under the three periods of extreme drought, while Rs exhibited a non-significant decreasing trend in the early and midterm drought but increased significantly by 58.48% (p < 0.05) during the late drought compared with the ambient control. Plant coverage significantly increased by 79.3% (p < 0.05) in the early drought, and standing biomass significantly decreased by 18.33% (p < 0.05) in the midterm drought. Alkaline phosphatase, polyphenol oxidase, and peroxidase increased significantly by 76.46, 77.66, and 109.60% (p < 0.05), respectively, under late drought. Structural equation models demonstrated that soil water content (SWC), pH, plant coverage, plant standing biomass, soil beta-D-cellobiosidase, and beta-1,4-N-acetyl-glucosaminidase were crucial impact factors that eventually led to a decreasing trend in Re, and SWC, pH, beta-1,4-glucosidase (BG), beta-1,4-xylosidase (BX), polyphenol oxidase, soil organic carbon, microbial biomass carbon, and dissolved organic carbon were crucial impact factors that resulted in changes in Rs. Our results emphasize the key roles of plant and soil extracellular enzyme activities in regulating the different responses of Re and Rs under extreme drought events occurring at different plant growth stages.
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