The contribution of arbuscular mycorrhizal fungi to ecosystem respiration and methane flux in an ephemeral plants-dominated desert

被引:9
|
作者
Yue, Ping [1 ,2 ,3 ]
Cui, Xiaoqing [4 ,5 ]
Zuo, Xiaoan [1 ,3 ]
Li, Kaihui [6 ]
Wang, Shaokun [1 ,3 ]
Jia, Yangyang [4 ]
Misselbrook, Tom [7 ]
Liu, Xuejun [4 ]
机构
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Urat Desert Grassland Res Stn, Lanzhou 730000, Peoples R China
[2] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Desert & Desertificat, Lanzhou, Peoples R China
[3] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Naiman Desertificat Res Stn, Lanzhou, Peoples R China
[4] China Agr Univ, Coll Resources & Environm Sci, Beijing, Peoples R China
[5] Peking Univ, Sino France Inst Earth Syst Sci, Coll Urban & Environm Sci, Lab Earth Surface Proc, Beijing, Peoples R China
[6] Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi, Peoples R China
[7] Rothamsted Res, Dept Sustainable Soils & Grassland Syst, Okehampton, Devon, England
基金
英国生物技术与生命科学研究理事会; 中国国家自然科学基金;
关键词
arbuscular mycorrhizal fungi; ecosystem respiration; ephemeral plants; methane flux; soil microorganisms; SOIL RESPIRATION; NITROGEN ADDITION; GURBANTUNGGUT DESERT; ATMOSPHERIC METHANE; TERRESTRIAL PLANTS; OXIDIZING BACTERIA; HERBACEOUS LAYER; CARBON; PRECIPITATION; RESPONSES;
D O I
10.1002/ldr.3838
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Arbuscular mycorrhizal fungi (AMF) can significantly influence the soil carbon cycle, however, their impacts on desert soils are still unclear. Here, a field control experiment, using in-growth mesocosms, was conducted to quantitatively assess the contribution of AMF and ephemeral plants to ecosystem respiration (R-e) and methane (CH4) flux in the Gurbantunggut Desert in China, from April to May 2017. Ephemeral plant biomass was significantly increased by AMF infection. R-e was significantly positively correlated with AMF infection rate, whereas CH4 flux was significantly negatively correlated. The contribution of AMF to R-e was up to 24%, comparable to the contribution of non-AMF microbial respiration, which accounted for up to 36%, whereas the respiration of ephemeral plants accounted for 40%. Variation in R-e was most strongly associated with soil organic carbon and soil available potassium concentrations and soil temperature. Non-AMF microorganisms accounted for most of the CH4 flux (up to 85%). In contrast, AMF only accounted for 15% of total CH4 flux. The CH4 flux was significantly influenced by soil NO3--N content, soil moisture, soil temperature and soil NH4+-N content. Overall, AMF significantly influenced R-e and CH4 flux, and also enhanced the growth of ephemeral plants, which have an important role in the carbon cycle in desert ecosystems.
引用
收藏
页码:1844 / 1853
页数:10
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