文献类型：期刊文献

英文题名：Different Responses of Growing Season Ecosystem CO2 Fluxes to Rain Addition in a Desert Ecosystem

作者：Xu, Xiaotian[1,2] Wu, Bo[1,3] Bao, Fang[1,3] Gao, Ying[1,3] Li, Xinle[4,5] Cao, Yanli[1,3] Lu, Qi[1,3] Gao, Junliang[4,5] Xin, Zhiming[4,5] Liu, Minghu[4,5]

第一作者：Xu, Xiaotian

通信作者：Wu, B[1];Wu, B[2]

机构：[1]Chinese Acad Forestry, Inst Desertificat Studies, Beijing 100091, Peoples R China;[2]Beijing Acad Agr & Forestry Sci, Inst Forestry & Pomol, Beijing 100093, Peoples R China;[3]State Adm Forestry & Grassland, Key Lab Desert Ecosyst & Global Change, Beijing 100091, Peoples R China;[4]Chinese Acad Forestry, Expt Ctr Desert Forestry, Bayannur 015200, Peoples R China;[5]Dengkou Desert Ecosyst Res Stn Inner Mongolia, Bayannur 015200, Peoples R China

年份：2023

卷号：12

期号：5

外文期刊名：PLANTS-BASEL

收录：;Scopus(收录号：2-s2.0-85149924570);WOS:【SCI-EXPANDED(收录号:WOS:000947101500001)】；

语种：英文

外文关键词：desert ecosystem; rain addition; CO2 fluxes; CO2 sink; nonlinear response

摘要：Desert ecosystem CO2 exchange may play an important role in global carbon cycling. However, it is still not clear how the CO2 fluxes of shrub-dominated desert ecosystems respond to precipitation changes. We performed a 10-year long-term rain addition experiment in a Nitraria tangutorum desert ecosystem in northwestern China. In the growing seasons of 2016 and 2017, with three rain addition treatments (natural precipitation +0%, +50%, and +100% of annual average precipitation), gross ecosystem photosynthesis (GEP), ecosystem respiration (ER), and net ecosystem CO2 exchange (NEE) were measured. The GEP responded nonlinearly and the ER linearly to rain addition. The NEE presented a nonlinear response along the rain addition gradient, with a saturation threshold by rain addition between +50% and +100%. The growing season mean NEE ranged from -2.25 to -5.38 mu mol CO2 m(-2) s(-1), showing net CO2 uptake effect, with significant enhancement (more negative) under the rain addition treatments. Although natural rainfall fluctuated greatly in the growing seasons of 2016 and 2017, reaching 134.8% and 44.0% of the historical average, the NEE values remained stable. Our findings highlight that growing season CO2 sequestration in desert ecosystems will increase against the background of increasing precipitation levels. The different responses of GEP and ER of desert ecosystems under changing precipitation regimes should be considered in global change models.