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Influence of hydrological fluxes on the structure of nitrate-reducing bacteria communities in a peatland

机译:水文通量对泥炭地硝酸盐还原菌群落结构的影响

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Factors influencing nitrate dynamics and nitrate-reducing bacteria in peat soil in the field, were investigated in laboratory experiments. A previous study had indicated that the on-site effects of redox conditions and nutrient fluxes on microbial activity were influenced by hydrological conditions. However, the laboratory experiments indicated that peat samples from sites under different hydrological regimes exhibited different microbial activities independently of oxygenation conditions. The effects of redox conditions and nutrient fluxes (i.e. influence of NO3- and O2 concentration) on the nitrate reducer community were therefore assessed. Microbial community structures in peat samples from sites under different hydrologic regimes were compared using Terminal-Restriction Fragment Length Polymorphism diversity signatures of the narG gene. This gene encodes the catalytic subunit of the nitrate reductase. Unexpectedly, the nitrate reducer communities were very similar at the beginning of the experiment whatever the peatland soil analysed. However, a strong structuration and divergence within the nitrate reducer communities, that was site-dependent, was evident after 76 h of incubation. These modifications within the microbial communities seemed to be due to differences in peat saturation at the sampling sites resulting from the different hydrological regimes. Of the forcing variables tested, oxygenation had a slight effect on the composition of the nitrate-reducers' community whereas nitrate addition had no effect. This study shows that a physical constraint such as hydrological regime might be considered important in microbial community composition.
机译:在实验室实验中,研究了田间泥炭土壤中影响硝酸盐动力学和减少硝酸盐细菌的因素。先前的研究表明,氧化还原条件和养分通量对微生物活性的现场影响受水文条件的影响。然而,实验室实验表明,在不同水文条件下,来自地点的泥炭样品表现出不同的微生物活性,而与氧化条件无关。因此,评估了氧化还原条件和养分通量(即NO3-和O2浓度的影响)对硝酸盐还原剂群落的影响。使用narG基因的末端限制片段长度多态性多样性特征,比较了不同水文制度下位点泥炭样品中的微生物群落结构。该基因编码硝酸还原酶的催化亚基。出乎意料的是,无论泥炭土壤如何分析,硝酸盐还原剂群落在实验开始时都非常相似。但是,经过76 h的培养后,硝酸还原剂群落内部存在强烈的结构化和发散性,这是位点依赖性的。微生物群落中的这些变化似乎是由于不同水文状况导致的采样点泥炭饱和度的差异。在测试的强迫变量中,氧合对硝酸盐还原剂群落的组成影响不大,而硝酸盐的添加则没有影响。这项研究表明,诸如水文状况之类的物理约束条件可能被认为对微生物群落组成很重要。

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