Responses of soil microbes and their interactions with plant community after nitrogen and phosphorus addition in a Tibetan alpine steppe

被引:23
作者
Dong, Junfu [1 ]
Wang, Shuping [2 ]
Niu, Haishan [2 ]
Cui, Xiaoyong [1 ,3 ]
Li, Linfeng [1 ]
Pang, Zhe [1 ]
Zhou, Shutong [1 ]
Wang, Kui [1 ]
机构
[1] Univ Chinese Acad Sci, Coll Life Sci, Beijing 101408, Peoples R China
[2] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 101408, Peoples R China
[3] Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China
基金
中国国家自然科学基金;
关键词
Microbial community; Nitrogen fertilization and phosphorus fertilization; PLFA; Tibetan alpine steppe; ARBUSCULAR MYCORRHIZAL FUNGI; LIMITING BACTERIAL-GROWTH; BELOW-GROUND COMMUNITIES; CLIMATE-CHANGE; GRASSLAND; BIOMASS; CARBON; FERTILIZATION; MICROORGANISMS; AVAILABILITY;
D O I
10.1007/s11368-020-02586-3
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Purpose Nitrogen (N) and phosphorus (P) additions are the widely used restoration management for degraded grasslands. However, soil microbial community responses to N and P additions are still not well understood, especially multiple levels or/and combined N and P additions in high-altitude grasslands. In this study, the single and interactive effects of N and P additions on the soil microbes were explored. Methods A field experiment with two factors (N 0, 7.5, and 15 g N m(-2) year(-1); P 0, 3.27, and 6.55 g P m(-2) year(-1)) was conducted by a completely randomized block design in a Tibetan plateau steppe. Total and specific microbial biomass (bacteria, fungi, G+/G- bacteria, saprotrophs, actinomycetes, and arbuscular mycorrhizal fungi) were analyzed by using phospholipid fatty acids (PLFAs). Additionally, based on their fixed weight composites, we used a composite variable (phenotype) to represent the microbial community. Results The results showed that N addition decreased the microbe phenotype, total microbial biomass, and specific microbial biomass (total bacteria, G+, and G- bacteria). P application and its interaction with N application all increased the microbial phenotype, total microbial biomass, and specific microbial biomass (total bacteria, G+, G-, saprotrophs, and actinomycetes). Besides, the microbial phenotype was positively correlated with P application rates and not correlated with N application rates. Conclusion In conclusion, P was the key limiting factor for soil microbes, and its interaction with N is also important for some specific microbes. In addition, long-term responses of soil microbes after N and P amendments need further investigation in the Tibetan alpine steppe.
引用
收藏
页码:2236 / 2247
页数:12
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