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宁夏沙质河流湿地涨落带土壤细菌群落结构及多样性特征研究

Study on structure and diversity of soil bacterial communities in the hydro-fluctuation zone of sandy river wetlands in Ningxia

  • 摘要: 河流湿地涨落带属于典型的生态过渡带,养分循环及微生物功能变化较为活跃。宁夏黄沙古渡国家湿地公园是典型的沙质河流湿地类型,目前关于其涨落带微生物多样性的研究较少。于2022年8月,采集宁夏黄沙古渡国家湿地公园的沙质河流湿地涨落带4个区域(按水分条件分为干旱区域、近水区域、干湿交错区域、淹水区域)的土壤,采用高通量测序技术分析细菌群落结构及多样性特征,探究涨落带土壤理化因子与细菌群落结构和功能协同演变及影响因素。研究结果表明,宁夏黄沙古渡国家湿地公园沙质河流湿地涨落带土壤细菌隶属于42门120纲180目231科333属118种,主要细菌菌群包括变形菌门、放线菌门、厚壁菌门、酸杆菌门、绿弯菌门等11个菌门,其优势菌群为变形菌门和放线菌门,且相对丰度明显受研究区域水位条件影响;节杆菌属(Arthrobacter)为干旱区域、干湿交错区域和淹水区域最主要的属水平菌群,芽孢杆菌属(Bacillus)为近水区域最主要的属水平菌群;4个水分区域存在差异的前10个菌群中,相对丰度变化最显著的菌群为拟杆菌门,属水平上相对丰度变化最显著的是变形菌门的拜纳蒙纳斯属(Balneimonas)、微红微球菌属(Rubellimicrobium)及红噬细胞菌属(Rhodocytophaga)。近水区域土壤养分含量最高,但其细菌群落结构和物种组成较其他区域简单。不同水分土壤细菌功能丰富,在代谢、遗传信息处理和环境信息处理方面表现活跃,水分对沙质河流湿地土壤细菌群落代谢功能具有重要影响。沙质河流湿地土壤细菌群落结构对水分变化的响应较为敏感,部分菌群的相对丰度发生了显著变化,水分条件主要影响了湿地变形菌门的微生物。土壤含水量、有机质、pH、碱解氮和电导率是影响土壤细菌群落结构的主要影响因子,研究结果可以为沙质河流湿地保护和可持续利用提供重要参考依据。

     

    Abstract: The hydro-fluctuation zone of river wetlands is a typical ecological transition zone characterized by dynamic nutrient cycling and microbial functional shifts. As a representative sandy river wetland, Ningxia Huangshagudu National Wetland Park has received limited research attention regarding microbial diversity in its hydro-fluctuation zone. In August 2022, we investigated the microbial diversity in the hydro-fluctuation zone of the sandy river wetland at Huangshagudu Wetland Park, Ningxia. These regions were classified based on water conditions into the arid region (D), near-water area (NT), dry-wet interlacing area (DW), and flooded area (W). The Illumina MiSeq high-throughput sequencing was employed to analyze the bacterial community structure and diversity characteristics, and to explore the co-evolution and influencing factors of soil physicochemical properties and bacterial community structures and functions in the hydro-fluctuation zone.The results indicated that soil bacteria in the study area comprised 42 phyla, 120 classes, 180 orders, 231 families, 333 genera, and 118 species. The predominant bacterial groups detected across different water regions were Proteobacteria, Actinobacteria, Firmicutes, Acidobacteria, and Chloroflexi. Proteobacteria and Actinobacteria were present in all four regions, yet significant differences in abundances were observed among them. Arthrobacter was the most dominant genus in the D, DW, and W regions, while Bacillus dominated in the NT region. Among the top 10 distinct floras in the four regions, Bacteroidota exhibited the most notable change in relative abundance. At the genus level, Balneimonas, Rubellimicrobium, and Rhodocytophaga showed the most significant variations in relative abundance. Although the near-water area had the highest soil nutrient content under different water conditions, its bacterial community structure and species composition were simpler compared to other areas. Bacterial functions across different moisture conditions were rich, with high activity in metabolism, genetic information processing, and environmental information processing.Water has an important influence on the metabolic function of soil bacterial communities in sandy river wetlands.The soil bacterial community structure in sandy river wetland is sensitive to the response of water changes, and the relative abundance of some bacteria has changed significantly, and the water conditions mainly affect the microorganisms under Proteobacteria in wetlands.Soil volumetric water content, soil organic matter, pH, available nitrogen, and electrical conductivity are the main influencing factors affecting the soil bacterial community structure, so the results can provide an important reference for the protection and sustainable utilization of sandy river wetlands.

     

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