文献类型：期刊文献

英文题名：Divergent responses of CO(2 )and CH(4 )fluxes to changes in the precipitation regime on the Tibetan Plateau: Evidence from soil enzyme activities and microbial communities

作者：Zhang, Kerou[] Yan, Zhongqing[] Li, Meng[] Kang, Enze[] Li, Yong[] Yan, Liang[] Zhang, Xiaodong[] Wang, Jinzhi[] Kang, Xiaoming[1]

第一作者：张克柔

通信作者：Kang, XM[1]

机构：[1]Chinese Acad Forestry, Inst Wetland Res, Beijing 100091, Peoples R China; Beijing Key Lab Wetland Serv & Restorat, Beijing 100091, Peoples R China; Sichuan Zoige Wetland Ecosystem Res Stn, Beijing 624500, Sichuan, Peoples R China

年份：2021

卷号：801

外文期刊名：SCIENCE OF THE TOTAL ENVIRONMENT

收录：;WOS:【SCI-EXPANDED(收录号:WOS:000701725600007)】；

基金：This paper was supported by the National Nonprofit Institute Research Grant (No. CAFYBB2019SY038), and the Second Tibetan Plateau Scientific Expedition and Research Program (STEP) (Grant No 2019 QZKK0304). Data used in this study is available via https://doi.org/10.5281/zenodo.4964790.

语种：英文

外文关键词：Manipulate field experiment; Precipitation regime; Carbon flux; Tibetan alpine meadow; Extracellular enzyme activity; Microbial community

摘要：Carbon fluxes (CO2 and CH4) are important indicators of the response of alpine meadow ecosystems to global climate change. Alpine meadows on the Qinghai-Tibet Plateau are sensitive to climate change. Although the temporal allocation of precipitation can vary, its intensity is expected to increase, and its frequency is expected to decrease in the future. In this study, a manipulative field experiment was conducted to investigate how carbon fluxes are altered in response to moderate and severe changes in the precipitation regime. Fluctuations in CH4 flux were large under a severely altered precipitation regime (range of -0.048-0.038 mg m-2 h-1). Severe changes in the precipitation regime significantly reduced soil CH4 uptake by approximately 54.3%. This was probably affected by the decrease in the dissolved organic carbon concentration and changes in the microbial community (mainly Gammaproteobacteria), which were induced by variation in soil water conditions under various precipitation regimes. Under moderate changes in the precipitation regime, the average value of CO2 fluxes (ecosystem respiration) was 698.21 +/- 35.19 mg m-2 h-1, which was significantly decreased by 20.7% compared with the control. This likely stems from the suppression of enzyme activity (particularly alpha-1,4-glucosidase and beta-1,4-glucosidase) and the alteration of microbial community structure in this treatment, which led to a decrease in organic matter breakdown and a reduction in the release of CO2 to the atmosphere. However, CO2 fluxes were slightly (i.e., not significantly) decreased under the severely altered precipitation regime. Such different responses of CO2 flux are probably driven by differences in microbial strategies. This study not only increases our understanding of the mechanisms underlying the adaptation of alpine meadow ecosystems to global climate change but also provides new insight into the carbon source/sink functions of alpine meadows. (c) 2021 Elsevier B.V. All rights reserved.