巢湖十五里河不同河段沉积物古菌群落结构特征研究

Characteristics of Archaeal Community Structures in the Different River Reach Sediments in the Shiwuli River, Caohu Lake Basin

  • 摘要:
      目的  为了探究城市河流沉积物古菌群落结构特征及其环境指示意义,
      方法  应用高通量测序技术获取巢湖十五里河不同河段表层沉积物古菌群落组成,用冗余分析(RDA)和相关性分析等方法探究古菌群落结构特征与沉积物环境因子间的联系。
      结果  十五里河表层沉积物古菌的优势菌门和次优势菌门分别是广古菌和奇古菌与深古菌,其相对丰度分别为51.9% ~ 96.0%、3.2% ~ 42.5%和0.2% ~ 22.5%;下游表层沉积物广古菌相对丰度显著低于中游和上游,而奇古菌和深古菌相对丰度显著高于中游和上游(除与河道低坝隔开的样点C7);除圩西河与干流汇合处样点C3优势菌纲为Nitrososphaeria外,甲烷微菌纲是河流表层沉积物古菌的优势菌纲,其在下游表层沉积物中相对丰度显著低于中游和上游;除C7样点次优势菌纲为Thermococci外,甲烷杆菌纲是中游和上游表层沉积物古菌的次优势菌纲,而下游3个样点次优势菌纲各不一致;下游表层沉积物甲烷囊菌属和Rice_Cluster_I相对丰度显著高于其他河段,中游和上游表层沉积物甲烷鬃毛菌属和甲烷杆菌属相对丰度显著高于下游。不同河段表层沉积物古菌群落丰富度未有显著差异,但下游表层沉积物古菌多样性指数显著高于上游和中游。pH、总有机碳、速效钾、全磷、C/N和C/P是影响沉积物古菌群落结构的主要环境因子,而pH、全磷和C/P是影响沉积物古菌多样性的主要环境因子。
      结论  十五里河下游河段表层沉积物古菌群落结构特征和多样性与中游和上游具有显著差异,指示着营养盐含量较高和污染相对严重的中游和上游与营养盐含量较低和污染较轻的下游表层沉积物环境状况差异。

     

    Abstract:
      Objective  Archaea plays an important role in the biogeochemical cycle of elements in various environments. The aim of this study was to explore the relationship between the archaeal community structures and the environmental factors and to explore how the characteristics of archaeal community structures indicating sediment environments in urban river sediments.
      Method  16S rRNA gene-based Illumina MiSeq sequencing was used to investigate archaeal community structures in the different reaches in the Shiwuli River, and redundancy analysis (RDA) and correlation analysis between archaeal community indices and environmental factors were conducted to explore the driving factors affecting archaeal community structures and archaeal diversities.
      Result  The first dominant phylum (relative abundance 51.93% ~ 96.02%) was Euryarchaeota, and the second dominant phyla were Thaumarchaeota (relative abundance 3.22% ~ 42.47%) and Bathyarchaeota (relative abundance 0.17% ~ 22.49%) in all river surface sediments. The relative abundance of Euryarchaeota in the upstream and midstream was significantly higher than that in the downstream, while the relative abundance of Thaumarchaeota and Bathyarchaeota in the downstream was higher than that in the midstream and upstream, especially for the relative abundance of Bathyarchaeota (except for sampling site C7 separated from the river by lower dam). Except for Nitrososphaeria at class level at sampling site C3 at the confluence of Weixi River and Shiwuli River, the first dominant archaea were Mehtanomicrobia and their relative abundance was higher in the downstream than that in the midstream and upstream. Except for Thermococci at sampling site C7, the second dominant archaea in the midstream and upstream were Methanobacteria, while the dominate archaea were different among the three sampling sites in the downstream. At the genus level, the relative abundances of Methanocella and Rice_Cluster_I were significantly higher in the downstream than those in the other reaches, while those of Methanosaeta and Methanobacterium in the midstream and upstream were significantly higher than those in the downstream. There was no significant difference in the total abundance of archaea among different river reaches, but the archaeal diversities in the downstream were higher than those in the upstream and midstream. Soil pH, total organic carbon, available potassium, total phosphate, C/N and C/P were the environmental factors affecting the distribution of sediment archaeal community in the river, and pH, total phosphate and C/P were the important environmental factors affecting the sediment archaeal diversities.
      Conclusion  In general, the archaeal community structures and diversities in the different river reaches of Shiwuli River were significantly distinct, reflecting the difference in the surface sediment environment which owned high nutrient and pollution in the midstream/upstream, and low nutrient and pollution in the downstream.

     

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