Microbiology and Enzimology Lab., Federal University of Agreste Pernambuco, Garanhuns, PE, 55292-270, Brazil.
Soil Quality Lab., Agricultural Science Center, Federal University of Piauí, Teresina, PI, 64049-550, Brazil.
Sci Rep. 2024 Feb 16;14(1):3919. doi: 10.1038/s41598-024-54221-7.
Soil fertility is key point to pastures systems and drives the microbial communities and their functionality. Therefore, an understanding of the interaction between soil fertility and microbial communities can increase our ability to manage pasturelands and maintain their soil functioning and productivity. This study probed the influence of soil fertility on microbial communities in tropical pastures in Brazil. Soil samples, gathered from the top 20 cm of twelve distinct areas with diverse fertility levels, were analyzed via 16S rRNA sequencing. The soils were subsequently classified into two categories, namely high fertility (HF) and low fertility (LF), using the K-Means clustering. The random forest analysis revealed that high fertility (HF) soils had more bacterial diversity, predominantly Proteobacteria, Nitrospira, Chloroflexi, and Bacteroidetes, while Acidobacteria increased in low fertility (LF) soils. High fertility (HF) soils exhibited more complex network interactions and an enrichment of nitrogen-cycling bacterial groups. Additionally, functional annotation based on 16S rRNA varied between clusters. Microbial groups in HF soil demonstrated enhanced functions such as nitrate reduction, aerobic ammonia oxidation, and aromatic compound degradation. In contrast, in the LF soil, the predominant processes were ureolysis, cellulolysis, methanol oxidation, and methanotrophy. Our findings expand our knowledge about how soil fertility drives bacterial communities in pastures.
土壤肥力是牧场系统的关键,它驱动着微生物群落及其功能。因此,了解土壤肥力与微生物群落之间的相互作用,可以提高我们管理牧场和维持土壤功能和生产力的能力。本研究探讨了土壤肥力对巴西热带牧场微生物群落的影响。从 12 个具有不同肥力水平的不同区域的表层 20 厘米处采集土壤样本,通过 16S rRNA 测序进行分析。随后,使用 K-Means 聚类将土壤分为高肥力 (HF) 和低肥力 (LF) 两类。随机森林分析表明,高肥力 (HF) 土壤的细菌多样性更高,主要有变形菌门、硝化螺旋菌门、绿弯菌门和拟杆菌门,而在低肥力 (LF) 土壤中,酸杆菌门增加。高肥力 (HF) 土壤表现出更复杂的网络相互作用和富集的氮循环细菌群。此外,基于 16S rRNA 的功能注释在聚类之间存在差异。HF 土壤中的微生物群表现出增强的功能,如硝酸盐还原、好氧氨氧化和芳香族化合物降解。相比之下,在 LF 土壤中,主要的过程是脲酶解、纤维素酶解、甲醇氧化和甲烷营养作用。我们的研究结果扩展了关于土壤肥力如何驱动牧场中细菌群落的知识。