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中国长江沿岸泥滩和农业土壤中氨氧化菌的生态位分离

Niche Separation of Ammonia Oxidizers in Mudflat and Agricultural Soils Along the Yangtze River, China.

作者信息

Zhou Xue, Li Bolun, Guo Zhiying, Wang Zhiyuan, Luo Jian, Lu Chunhui

机构信息

State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing, China.

School of Geographic Sciences, Nanjing University of Information Science and Technology, Nanjing, China.

出版信息

Front Microbiol. 2018 Dec 18;9:3122. doi: 10.3389/fmicb.2018.03122. eCollection 2018.

Abstract

Nitrification driven by ammonia oxidizers is a key step of nitrogen removal in estuarine environments. Spatial distribution characteristics of ammonia-oxidizers have been well understood in mudflats, but less studied in the agricultural soils next to mudflats, which also play an important role in nitrogen cycling of the estuarine ecosystem. In the present research, we investigated ammonia oxidizers' distributions along the Yangtze River estuary in Jiangsu Province, China, sampling soils right next to the estuary (mudflats) and the agricultural soils 100 m away. We determined the relationship between the abundance of genes of ammonia-oxidizing archaea (AOA) and ammonia-oxidizing bacteria (AOB) and the potential nitrification rates of the mudflats and agricultural soils. We also identified the environmental variables that correlated with the composition of the ammonia oxidizers' communities by 16S rRNA gene pyrosequencing. Results indicated that agricultural soils have significantly higher potential nitrification rates as well as the AOA abundance, and resulted in strong phylogenetic clustering only in AOA communities. The ammonia oxidizers' community compositions differed dramatically among the mudflat and agricultural sites, and stochasticity played a dominant role. The AOA communities were dominated by the Group 1.1a cluster at the mudflat, whereas the 54D9 and 29i4 clusters were dominant in agriculture soils. The dominant AOB communities in the mudflat were closely related to the lineage, whereas the agricultural soils were dominated by the lineage. Soil organic matter and salinity were correlated with the ammonia oxidizers' community compositions.

摘要

由氨氧化菌驱动的硝化作用是河口环境中氮去除的关键步骤。氨氧化菌的空间分布特征在泥滩中已得到充分了解,但在泥滩附近的农业土壤中研究较少,而这些农业土壤在河口生态系统的氮循环中也起着重要作用。在本研究中,我们调查了中国江苏省长江河口沿线氨氧化菌的分布情况,对紧邻河口的土壤(泥滩)和距离河口100米处的农业土壤进行了采样。我们确定了氨氧化古菌(AOA)和氨氧化细菌(AOB)基因丰度与泥滩和农业土壤潜在硝化速率之间的关系。我们还通过16S rRNA基因焦磷酸测序确定了与氨氧化菌群落组成相关的环境变量。结果表明,农业土壤具有显著更高的潜在硝化速率以及AOA丰度,并且仅在AOA群落中导致强烈的系统发育聚类。泥滩和农业地点之间氨氧化菌的群落组成差异很大,随机性起主导作用。泥滩的AOA群落以1.1a组聚类为主,而农业土壤中54D9和29i4聚类占主导。泥滩中占主导的AOB群落与该谱系密切相关,而农业土壤则以该谱系为主导。土壤有机质和盐度与氨氧化菌的群落组成相关。

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