Wang Ying, Ji Hongfei, Hu Yaxian, Wang Rui, Rui Junpeng, Guo Shengli
State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Northwest A&F University, Yangling, China.
Environmental Microbiology Key Laboratory of Sichuan Province, Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu, China.
Front Microbiol. 2018 Oct 31;9:2613. doi: 10.3389/fmicb.2018.02613. eCollection 2018.
Fertilizer application has contributed substantially to increasing crop yield. Despite the important role of soil fungi in agricultural production, we still have limited understanding of the complex responses of fungal taxonomic and functional groups to organic and mineral fertilization in long term. Here we report the responses of the fungal communities in an alkaline soil to 30-year application of mineral fertilizer (NP), organic manure (M) and combined fertilizer (NPM) by the Illumina HiSeq sequencing and quantitative real-time PCR to target fungal internal transcribed spacer (ITS) genes. The results show: (1) compared to the unfertilized soil, fertilizer application increased fungal diversity and ITS gene copy numbers, and shifted fungal community structure. Such changes were more pronounced in the M and NPM soils than in the NP soil (except for fungal diversity), which can be largely attributed to the manure induced greater increases in soil total organic C, total N and available P. (2) Compared to the unfertilized soil, the NP and NPM soils reduced the proportion of saprotrophs by 40%, the predominant taxa of which may potentially affect cellulose decomposition. (3) Indicator species analysis suggested that the indicator operational taxonomic units (OTUs) in the M soil occupied 25.6% of its total community, but that only accounted for 0.9% in the NP soil. Our findings suggest that fertilization-induced changes of total fungal community were more responsive to organic manure than mineral fertilizer. The reduced proportion of cellulose decomposition-related saprotrophs in mineral fertilizer treatments may potentially contribute to increasing their soil C stocks.
施肥对提高作物产量做出了重大贡献。尽管土壤真菌在农业生产中发挥着重要作用,但我们对真菌分类群和功能群对有机和矿物肥料的长期复杂响应仍了解有限。在此,我们通过Illumina HiSeq测序和针对真菌内转录间隔区(ITS)基因的定量实时PCR,报告了碱性土壤中真菌群落对30年矿物肥料(NP)、有机肥(M)和复合肥(NPM)施用的响应。结果表明:(1)与未施肥土壤相比,施肥增加了真菌多样性和ITS基因拷贝数,并改变了真菌群落结构。这种变化在M和NPM土壤中比在NP土壤中更明显(除真菌多样性外),这在很大程度上可归因于粪肥导致土壤总有机碳、总氮和有效磷的更大增加。(2)与未施肥土壤相比,NP和NPM土壤使腐生菌的比例降低了40%,其主要分类群可能会影响纤维素分解。(3)指示物种分析表明,M土壤中的指示操作分类单元(OTU)占其总群落的25.6%,但在NP土壤中仅占0.9%。我们的研究结果表明,施肥引起的真菌群落总体变化对有机肥的响应比对矿物肥料的响应更大。矿物肥料处理中与纤维素分解相关的腐生菌比例降低可能有助于增加土壤碳储量。