Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China; School of Geographical Science, Fujian Normal University, Fuzhou 350007, 00China.
Key Laboratory for Humid Subtropical Eco-geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350007, China; School of Geographical Science, Fujian Normal University, Fuzhou 350007, 00China.
Sci Total Environ. 2021 Feb 10;755(Pt 1):142449. doi: 10.1016/j.scitotenv.2020.142449. Epub 2020 Sep 22.
China has experienced a widespread increase in N deposition due to intensive anthropogenic activities, particularly in the subtropical regions. However, the effects of long-term N deposition on soil bacterial and fungal abundance, diversity, and community composition remain largely unclear. We assessed the effects of N deposition on soil microbial communities in summer and winter, using quantitative polymerase chain reaction and Illumina Miseq sequencing of bacterial 16S rRNA and fungal ITS genes from subtropical natural forest soils. The abundance of both soil bacteria and fungi exhibited a decreasing pattern with increasing N deposition rates. Nitrogen deposition increased bacterial diversity in both summer and winter, whereas fungal diversity was significantly decreased in summer, but greatly increased under the highest level of N deposition (150 kg N ha yr) in winter. Nitrogen deposition significantly increased the relative abundance of bacterial phyla Actinobacteria, Chloroflexi, and WPS-2, but decreased that of Acidobacteria and Verrucomicrobia. In addition, N deposition significantly decreased the relative abundance of Ascomycetes, but did not exert any significant effect on Basidiomycetes. The bacterial and fungal community compositions were greatly influenced by N deposition, with soil N availability and soil pH identified as the two most influential soil properties. This study demonstrates that the fungal community was more sensitive than the bacterial community to N deposition, and further emphasizes the importance of simultaneously evaluating soil bacterial and fungal communities in response to global environmental changes.
由于人类活动的强烈影响,中国经历了广泛的氮沉降增加,尤其是在亚热带地区。然而,长期氮沉降对土壤细菌和真菌丰度、多样性和群落组成的影响在很大程度上仍不清楚。我们评估了氮沉降对亚热带天然林土壤微生物群落的影响,在夏季和冬季分别使用定量聚合酶链反应和 Illumina Miseq 测序技术对细菌 16S rRNA 和真菌 ITS 基因进行了分析。随着氮沉降率的增加,土壤细菌和真菌的丰度均呈下降趋势。氮沉降增加了夏季和冬季的细菌多样性,而真菌多样性在夏季显著降低,但在冬季最高氮沉降(150kgN ha yr)下显著增加。氮沉降显著增加了放线菌门、绿弯菌门和 WPS-2 的相对丰度,但降低了酸杆菌门和疣微菌门的相对丰度。此外,氮沉降显著降低了子囊菌门的相对丰度,但对担子菌门没有任何显著影响。氮沉降对细菌和真菌群落组成有很大影响,土壤氮有效性和土壤 pH 被确定为两个最具影响力的土壤性质。本研究表明,真菌群落对氮沉降比细菌群落更为敏感,进一步强调了在评估土壤细菌和真菌群落对全球环境变化的响应时,同时评估这两个群落的重要性。