Shaanxi Key Laboratory of Agricultural and Environmental Microbiology, Yangling, Shaanxi 712100, China; State Key Laboratory of Crop Stress Biology in Arid Areas, College of Life Sciences, Northwest A&F University, Yangling, Shaanxi 712100, China.
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, 712100 Yangling, Shaanxi, China; Institute of Soil and Water Conservation, Northwest A&F University, 712100 Yangling, Shaanxi, China.
Sci Total Environ. 2023 May 1;871:162063. doi: 10.1016/j.scitotenv.2023.162063. Epub 2023 Feb 4.
Deciphering the ecological role of soil communities in the maintenance of multiple ecosystem functions is pivotal for the conservation and sustainability of soil biodiversity. However, few studies have investigated niche differentiation of abundant and rare microbiota, as well as their contributions to multiple soil elemental cycles, particularly in agroecosystems that have received decades of intense fertilization. Here, we characterized the environmental thresholds and phylogenetic signals for the environmental adaptation of both abundant and rare microbial subcommunities via amplicon sequencing and metagenomic sequencing and explored their importance in sustaining soil multiple nutrient cycling in agricultural fields that were fertilized for two decades. The results showed that rare taxa exhibited narrower niche breadths and weaker phylogenetic signals than abundant species. The assembly of abundant subcommunity was shaped predominantly by dispersal limitation (explained 71.1 % of the variation in bacteria) and undominated processes (explained 75 % of the variation in fungi), whereas the assembly of rare subcommunity was dominated by homogeneous selection process (explained 100 % of the variation in bacteria and 60 % of the variation in fungi). Soil ammonia nitrogen was the leading factor mediating the balance between stochastic and deterministic processes in both abundant (R = 0.15, P < 0.001) and rare (R = 0.08, P < 0.001) bacterial communities. Notably, the rare biosphere largely contributed to key soil processes such as carbon (R = 0.03, P < 0.05; R = 0.05, P < 0.05) and nitrogen (R = 0.03, P < 0.05; R = 0.17, P < 0.001) cycling. Collectively, these findings facilitate our understanding of the maintenance of rhizosphere bacterial and fungal diversity in response to agricultural fertilization and highlight the key role of rare taxa in sustaining agricultural ecosystem functions.
解析土壤群落在维持多种生态系统功能中的生态作用对于保护和维持土壤生物多样性至关重要。然而,很少有研究调查丰富和稀有微生物群落的生态位分化,以及它们对多种土壤元素循环的贡献,特别是在接受了几十年高强度施肥的农业生态系统中。在这里,我们通过扩增子测序和宏基因组测序,描述了丰富和稀有微生物亚群落的环境阈值和系统发育信号,并探讨了它们在维持施肥 20 年的农业土壤中多种养分循环中的重要性。结果表明,稀有类群的生态位宽度比丰富类群窄,系统发育信号也弱。丰富亚群的组装主要受扩散限制(解释细菌变异的 71.1%)和非主导过程(解释真菌变异的 75%)的影响,而稀有亚群的组装主要受同质选择过程的影响(解释细菌变异的 100%和真菌变异的 60%)。土壤氨氮是调节丰富(R = 0.15,P < 0.001)和稀有(R = 0.08,P < 0.001)细菌群落中随机和确定性过程平衡的主要因素。值得注意的是,稀有生物群在关键土壤过程中(如碳(R = 0.03,P < 0.05;R = 0.05,P < 0.05)和氮(R = 0.03,P < 0.05;R = 0.17,P < 0.001)循环中)对土壤过程的贡献很大。总的来说,这些发现有助于我们理解根际细菌和真菌多样性对农业施肥的维持,并强调了稀有类群在维持农业生态系统功能中的关键作用。