Microb Ecol. 2014 Aug;68(2):339-50. doi: 10.1007/s00248-014-0407-4.
Gradients in abiotic parameters, such as soil moisture,can strongly influence microbial community structure and function. Denitrifying and ammonia-oxidizing microorganisms,in particular, have contrasting physiological responses to abiotic factors such as oxygen concentration and soil moisture. Identifying abiotic factors that govern the composition and activity of denitrifying and ammonia-oxidizing communities is critical for understanding the nitrogen cycle.The objectives of this study were to (i) examine denitrifier andarchaeal ammonia oxidizer community composition and (ii) assess the taxa occurring within each functional group related to soil conditions along an environmental gradient. Soil was sampled across four transects at four locations along a dry to saturated environmental gradient at a restored wetland. Soil pH and soil organic matter content increased from dry to saturated plots. Composition of soil denitrifier and ammonia oxidizer functional groups was assessed by terminal restriction fragment length polymorphism (T-RFLP) community analysis, and local soil factors were also characterized. Microbial community composition of denitrifiers and ammonia oxidizers differed along the moisture gradient (denitrifier:ANOSIM R = 0.739, P < 0.001; ammonia oxidizers: ANOSIMR = 0.760, P < 0.001). Individual denitrifier taxa were observed over a larger range of moisture levels than individual archaeal ammonia oxidizer taxa (Wilcoxon rank sum, W = 2413, P value = 0.0002). Together, our data suggest that variation in environmental tolerance of microbial taxa have potential to influence nitrogen cycling in terrestrial ecosystems.
生物非生物参数(如土壤湿度)的梯度变化会强烈影响微生物群落的结构和功能。特别是反硝化菌和氨氧化微生物,对氧气浓度和土壤湿度等非生物因素具有截然不同的生理响应。确定控制反硝化菌和氨氧化菌群落组成和活性的非生物因素对于了解氮循环至关重要。本研究的目的是:(i)研究反硝化菌和古菌氨氧化菌的群落组成;(ii)评估每个功能组内与土壤条件相关的类群,沿环境梯度进行评估。在一个恢复湿地的四个位置的四个横断面上,沿从干燥到饱和的环境梯度采集土壤样本。土壤 pH 值和土壤有机质含量从干燥到饱和地段逐渐增加。通过末端限制性片段长度多态性(T-RFLP)社区分析评估土壤反硝化菌和氨氧化菌功能组的组成,并对当地土壤因素进行了特征描述。沿湿度梯度,反硝化菌和氨氧化菌的微生物群落组成存在差异(反硝化菌:ANOSIM R = 0.739,P < 0.001;氨氧化菌:ANOSIM R = 0.760,P < 0.001)。与单个古菌氨氧化菌类群相比,单个反硝化菌类群观察到的湿度水平范围更大(Wilcoxon 秩和检验,W = 2413,P 值 = 0.0002)。总的来说,我们的数据表明,微生物类群对环境的耐受度的变化有可能影响陆地生态系统中的氮循环。