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Metagenomic reconstruction of nitrogen cycling pathways in a CO2- enriched grassland ecosystem

机译:二氧化碳草原生态系统中氮循环途径的偏血态重建

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The nitrogen (N) cycle is a collection of important biogeochemical pathways mediated by microbial communities and is an important constraint in response to elevated CO2 in many terrestrial ecosystems. Previous studies attempting to relate soil N cycling to microbial genetic data mainly focused on a few gene families by PCR, protein assays and functional gene arrays, leaving the taxonomic and functional composition of soil microorganisms involved in the whole N cycle less understbod. In this study, 24 soil samples were collected from the long-term experimental site, BioCON, in 2009. A shotgun metagenome sequencing approach was employed to survey the microbial gene families involved in soil N cycle in the grassland that had been exposed to elevated CO2 (eCO(2)) for >12 years. In addition to evaluating the responses of major N cycling gene families to long-term eCO(2), we also aimed to characterize the taxonomic and functional composition of these gene families involved in soil N transformations. At the taxonomic level, organic N metabolism and nitrate reduction had the most diverse microbial species involved. The distinct taxonomic composition of different N cycling processes suggested that the complex N cycle in natural ecosystems was a result of multiple processes by many different microorganisms. Belowground microbial communities that mediate N cycling responded to eCO(2) in several different ways, including through stimulated abundances of the gene families related with organic decomposition, dissimilatory nitrate reduction, and N-2 fixation, and suppressed abundances of the gene families in glutamine synthesis and anammox. This study provides a genetic basis of the microorganisms involved in key processes in the N cycle in complex ecosystems, and shows that long-term eCO(2) selectively affects N cycling pathways instead of tuning up every process. (C) 2016 Elsevier Ltd. All rights reserved.
机译:氮(N)循环是由微生物群群介导的重要生物地球化学途径的集合,并且是在许多陆地生态系统中恢复升高的二氧化碳的重要约束。以前的研究试图将土壤N循环到微生物遗传数据的循环主要专注于少数基因家族,蛋白质测定和功能基因阵列,留下整个N个循环中涉及的土壤微生物的分类和功能组成较少。在这项研究中,从2009年从长期实验部位收集了24种土壤样品。使用霰弹枪偏心组测序方法来调查涉及过升高二氧化碳的草原的土壤N循环的微生物基因家族(ECO(2))> 12年。除了评估主要N循环基因家族对长期生态(2)的反应外,我们还旨在表征参与土壤N转化的这些基因家族的分类和功能组成。在分类水平,有机性N代谢和硝酸盐还原具有涉及的多种微生物物种。不同N循环过程的不同分类组成表明,天然生态系统中的复杂N循环是许多不同微生物的多种过程的结果。地下微生物群落中介导N循环以几种不同的方式响应ECO(2),包括通过与有机分解,含有硝酸盐的硝酸盐还原和N-2固定相关的基因家族的受刺激的大量,以及谷氨酰胺基因家族的受抑制性的丰度合成和厌氧毒素。本研究提供了在复杂生态系统中N个循环中的关键过程中涉及的微生物的遗传基础,并且表明长期Eco(2)选择性地影响N循环途径而不是调整每个过程。 (c)2016 Elsevier Ltd.保留所有权利。

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