Distribution Characteristics and Driving Factors of the Bacterial Community Structure in the Soil Profile of a Discontinuous Permafrost Region

• Published in: Forests 2024-08, Vol.15 (8), p.1456
• Main Authors: Liu, Qilong, Song, Liquan, Zou, Siyuan, Wu, Xiaodong, Zang, Shuying
• Format: Article
• Language: English
• Subjects: Acidic soils; Bacteria; bacterial community; bacterial diversity; Carbon cycle; Carbon sequestration; Chloroflexi; Climate change; Community structure; Data processing; Depth profiling; Distribution; Electrical conductivity; Electrical resistivity; Environmental aspects; Environmental information; Frozen ground; Genes; Global warming; Identification and classification; Infectious diseases; Information processing; Measurement; Metabolism; Microbiomes; Microorganisms; Moisture content; Mountains; Nitrogen; Peatlands; Permafrost; Physiological aspects; prediction of gene functions; Soil analysis; Soil bacteria; Soil layers; Soil microbiology; Soil microorganisms; Soil nutrients; soil profile; Soil profiles; Soil properties; Soil structure; Soil surfaces; Soil temperature; Soil water; Statistical analysis; Surface layers; Temperature; Testing; Transition layers; Variance analysis; Water content
• ISSN: 1999-4907; 1999-4907
• DOI: 10.3390/f15081456

Global warming leads to the melting of permafrost, affects changes in soil microbial community structures and related functions, and contributes to the soil carbon cycle in permafrost areas. Located at the southern edge of Eurasia’s permafrost region, the Greater Khingan Mountains are very sensitive to climate change. Therefore, by analyzing the bacterial community structure, diversity characteristics, and driving factors of soil profiles (active surface layer, active deep layer, transition layer, and permafrost layer) in this discontinuous permafrost region, this research provides support for the study of the carbon cycling process in permafrost regions. The results show that the microbial diversity (Shannon index (4.81)) was the highest at 0–20 cm, and the Shannon index of the surface soil of the active layer was significantly higher than that of the other soil layers. Acidobacteria and Proteobacteria were the dominant bacteria in the active layer soil of the permafrost area, and Chloroflexi , Actinobacteria , and Firmicutes were the dominant bacteria in the permafrost layer. Chloroflexi made the greatest contribution to the bacterial community in the permafrost soil, and Bacteroidota made the greatest contribution to the bacterial community in the active surface soil. The structure, richness, and diversity of the soil bacterial community significantly differed between the active layer and the permafrost layer. The number of bacterial species was the highest in the active layer surface soil and the active layer bottom soil. The difference in the structure of the bacterial community in the permafrost soil was mainly caused by changes in electrical conductivity and soil–water content, while that in the active layer soil was mainly affected by pH and soil nutrient indices. Soil temperature, NO[sub.3] [sup.−] -N, and pH had significant effects on the structure of the bacterial community. The active layer and permafrost soils were susceptible to environmental information processing and genetic information processing. Infectious disease: the number of bacterial species was significantly higher in the surface and permafrost layers than in the other layers of the soil. In conclusion, changes in the microbial community structure in soil profiles in discontinuous permafrost areas sensitive to climate change are the key to soil carbon cycle research.