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Understanding the Response of Nitrifying Communities to Disturbance in the McMurdo Dry Valleys Antarctica

机译:了解南极麦克默多干旱谷的硝化社区对干扰的响应

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摘要

Polar ecosystems are generally limited in nitrogen (N) nutrients, and the patchy availability of N is partly determined by biological pathways, such as nitrification, which are carried out by distinctive prokaryotic functional groups. The activity and diversity of microorganisms are generally strongly influenced by environmental conditions. However, we know little of the attributes that control the distribution and activity of specific microbial functional groups, such as nitrifiers, in extreme cold environments and how they may respond to change. To ascertain relationships between soil geochemistry and the ecology of nitrifying microbial communities, we carried out a laboratory-based manipulative experiment to test the selective effect of key geochemical variables on the activity and abundance of ammonia-oxidizing communities in soils from the McMurdo Dry Valleys of Antarctica. We hypothesized that nitrifying communities, adapted to different environmental conditions within the Dry Valleys, will have distinct responses when submitted to similar geochemical disturbances. In order to test this hypothesis, soils from two geographically distant and geochemically divergent locations, Miers and Beacon Valleys, were incubated over 2 months under increased conductivity, ammonia concentration, copper concentration, and organic matter content. Amplicon sequencing of the 16S rRNA gene and transcripts allowed comparison of the response of ammonia-oxidizing Archaea (AOA) and ammonia-oxidizing Bacteria (AOB) to each treatment over time. This approach was combined with measurements of NH oxidation rates using N isotopic additions. Our results showed a higher potential for nitrification in Miers Valley, where environmental conditions are milder relative to Beacon Valley. AOA exhibited better adaptability to geochemical changes compared to AOB, particularly to the increase in copper and conductivity. AOA were also the only nitrifying group found in Beacon Valley soils. This laboratorial manipulative experiment provided new knowledge on how nitrifying groups respond to changes on key geochemical variables of Antarctic desert soils, and we believe these results offer new insights on the dynamics of N cycling in these ecosystems.
机译:极地生态系统通常受氮(N)养分的限制,氮的斑块可用性部分取决于生物途径,例如硝化作用,而这是由独特的原核功能基团进行的。微生物的活性和多样性通常受到环境条件的强烈影响。但是,我们对极端寒冷环境中控制特定微生物功能基团(例如硝化剂)的分布和活性的属性知之甚少,以及它们如何响应变化。为了确定土壤地球化学与硝化微生物群落生态之间的关系,我们进行了一项基于实验室的操作实验,以测试关键地球化学变量对美国麦克默多干旱谷地区土壤中氨氧化群落的活性和丰度的选择性影响。南极洲。我们假设适应干旱谷内不同环境条件的硝化群落在遭受类似地球化学干扰时将具有不同的响应。为了检验该假设,将来自两个地理位置遥远且地球化学差异较大的地区(米尔斯和信标谷)的土壤在增加的电导率,氨浓度,铜浓度和有机质含量下培养了2个月。通过对16S rRNA基因和转录本的扩增子测序,可以比较随时间推移每种处理对氨氧化古细菌(AOA)和氨氧化细菌(AOB)的反应。该方法与使用N同位素添加法测量NH氧化速率相结合。我们的研究结果表明,在比尔肯山谷环境条件温和的米尔斯山谷,硝化潜力更高。与AOB相比,AOA对地球化学变化具有更好的适应性,特别是铜和电导率的增加。 AOA也是在信标谷土壤中发现的唯一硝化基团。这项实验室操作实验为硝化基团如何响应南极沙漠土壤关键地球化学变量的变化提供了新知识,我们相信这些结果为这些生态系统中氮循环的动力学提供了新见解。

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