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了解南极麦克默多干谷硝化群落对干扰的响应。

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

作者信息

Monteiro Maria, S Baptista Mafalda, Séneca Joana, Torgo Luís, K Lee Charles, Cary S Craig, Magalhães Catarina

机构信息

School of Science, University of Waikato, 3240 Hamilton, New Zealand.

International Centre for Terrestrial Antarctic Research, University of Waikato, 3240 Hamilton, New Zealand.

出版信息

Microorganisms. 2020 Mar 13;8(3):404. doi: 10.3390/microorganisms8030404.

Abstract

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.

摘要

极地生态系统的氮(N)养分通常有限,氮的斑块状可利用性部分由生物途径决定,如硝化作用,这是由独特的原核生物功能群进行的。微生物的活性和多样性通常受到环境条件的强烈影响。然而,我们对控制特定微生物功能群(如硝化细菌)在极端寒冷环境中的分布和活性的属性以及它们如何响应变化知之甚少。为了确定土壤地球化学与硝化微生物群落生态学之间的关系,我们进行了一项基于实验室的操纵实验,以测试关键地球化学变量对南极麦克默多干谷土壤中氨氧化群落的活性和丰度的选择性影响。我们假设,适应干谷内不同环境条件的硝化群落,在受到类似地球化学干扰时会有不同的反应。为了验证这一假设,来自两个地理上遥远且地球化学特征不同的地点——米尔斯谷和比肯谷的土壤,在电导率、氨浓度、铜浓度和有机质含量增加的条件下培养了两个月。对16S rRNA基因和转录本进行扩增子测序,以便比较氨氧化古菌(AOA)和氨氧化细菌(AOB)对每种处理随时间的反应。这种方法与使用氮同位素添加测量NH氧化速率相结合。我们的结果表明,米尔斯谷的硝化潜力更高,其环境条件相对于比肯谷更为温和。与AOB相比,AOA对地球化学变化表现出更好的适应性,特别是对铜和电导率的增加。AOA也是在比肯谷土壤中发现的唯一硝化菌群。这项实验室操纵实验提供了关于硝化菌群如何响应南极沙漠土壤关键地球化学变量变化的新知识,我们相信这些结果为这些生态系统中氮循环的动态提供了新的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/be05/7143839/4e9168688684/microorganisms-08-00404-g001.jpg

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