岷江上游河流氮分布及潜在沉积物微生物驱动过程
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1:中国科学院成都生物研究所,成都 610000 ,2:重庆师范大学地理与旅游学院,重庆 400047

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国家自然科学基金项目(32271676)和中国博士后科学基金项目(2023M733439)联合资助


Nitrogen distribution and potential microbial driving processes in the upper reaches of Minjiang River
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1:Chengdu Institute of Biology, Chinese Academy of Sciences, Chengdu 610000 , P.R.China ,2:School of Geography and Tourism, Chongqing Normal University, Chongqing 400047 , P.R.China

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    摘要:

    氮元素在自然界中的迁移转化是维持生态系统平衡的关键过程。在自然水体中,河流沉积物的氮功能菌在氮转化过程中起着至关重要的作用。为探究河流氮分布及沉积物微生物驱动过程,本文对岷江上游3个海拔河段的水体和沉积物进行氮分布研究,通过高通量测序分析沉积物微生物群落组成及其功能预测。结果表明:在岷江上游高海拔河段(>3000 m),沉积物铵盐含量较高,硝酸盐含量较低,水体亚硝酸盐浓度在2000~3000 m海拔河段显著高于其他海拔河段,同时氮组分分布受到pH、溶解氧、流速等环境因子的影响。岷江上游沉积物细菌群落主要受沉积物氮组分和可溶性有机碳的影响;古菌群落主要受海拔、沉积物氮组分和土壤有机碳的影响。岷江上游沉积物潜在氮转化微生物群落相似性在地理空间上呈显著衰减模式,且高海拔河段的潜在氮转化古菌群落具有显著差异性。其中,潜在硝化古菌是岷江上游的优势菌群,且潜在硝化古菌与潜在异化型硝酸盐还原古菌在高海拔河段显著高于较低海拔河段。对岷江上游不同氮转化过程而言, Nitrososphaerales 目、 Nitrososphaeraceae 科、 Nitrososphaeraceae 属是参与硝化过程的关键菌群,黄杆菌属( Flavobacterium )是硝酸盐还原过程的关键菌群,梭状芽胞杆菌属( Clostridium_sensu_stricto_ 1)和慢生根瘤菌属( Bradyrhizobium )是固氮过程的主要菌群,黄色杆菌属( Xanthobacter )、副球菌属( Paracoccus )和假单胞菌属( Pseudomonas )是反硝化过程的主要菌群。本文揭示了岷江上游高海拔河段的氮分布主要受到潜在沉积物氮转化古菌的驱动,该结论可为岷江上游河流生态管理策略提供一定理论支撑。

    Abstract:

    The migration and transformation of nitrogen (N) in nature is a key process to maintain the ecosystem balance. In natural water, N-transforming microorganisms in river sediments play a crucial role in the process of N conversion. In order to investigate N distribution in rivers and the sediment microorganism driving processes, this paper studied N distribution in the upper reaches of the Minjiang River, and the composition and function prediction of microbial communities in sediments. Results showed that the sediment ammonium salt was high while the sediment nitrate was lower in the upper reaches of the Minjiang River at high altitude (>3000 m), and the water nitrite was significantly higher in the 2000-3000 m altitude reaches than that in other altitude reaches. Meanwhile, the distribution of N components was affected by environmental factors such as pH, dissolved oxygen and flow velocity. The sediment bacterial communities were mainly affected by sediment-N components and dissolved organic carbon, while the archaea community was mainly affected by altitude, sediment-N composition and soil organic carbon. The similarity of potential nitrogen-transforming microbial communities showed a significant decline pattern in geographical space, and the potential N-transforming archaea communities in the high altitude reaches were significantly different. Among them, the potential nitrifying archaea were the dominant bacterial group in the upper reaches of the Minjiang River, and the potential nitrifying archaea and potential dissimilating nitrate reducing archaea were significantly higher in the high altitude reaches than in the low altitude reaches. For different processes,Nitrososphaerales, Nitrososphaeraceae and Nitrososphaeraceae are the dominant microorganisms in the nitrification process, andFlavobacteriumis the main group in the N reduction process.Clostridium_sensu_stricto_1andBradyrhizobiumare the main groups in N fixation.Xanthobacter ,Paracoccus and Pseudomonasare the main groups in denitrification. This paper reveals that nitrogen distribution in the upper reaches of the Minjiang River at high altitude is mainly driven by potential sediment-N transforming archaea, these results can provide theoretical support for the ecological management strategy of the upper reaches of the Minjiang River.

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杨早,李娜英,仲波,王晓锋,李贤祥,刘鑫,梅鑫瞳,何奕忻.岷江上游河流氮分布及潜在沉积物微生物驱动过程.湖泊科学,2025,37(4):1314-1326. DOI:10.18307/2025.0425

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  • 收稿日期:2024-08-02
  • 最后修改日期:2024-10-21
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  • 在线发布日期: 2025-07-04
  • 出版日期: 2025-07-06
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