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Reconstructing the Genetic Potential of the Microbially-Mediated Nitrogen Cycle in a Salt Marsh Ecosystem

机译:重建盐沼生态系统中微生物介导的氮循环的遗传潜能

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Coastal ecosystems are considered buffer zones for the discharge of land-derived nutrients without accounting for potential negative side effects. Hence, there is an urgent need to better understand the ecological assembly and dynamics of the microorganisms that are involved in nitrogen (N) cycling in such systems. Here, we employed two complementary methodological approaches (i.e., shotgun metagenomics and quantitative PCR) to examine the distribution and abundance of selected microbial genes involved in N transformations. We used soil samples collected along a well-established pristine salt marsh soil chronosequence that spans over a century of ecosystem development at the island of Schiermonnikoog, The Netherlands. Across the examined soil successional stages, the structure of the populations of genes involved in N cycling processes was strongly related to (shifts in the) soil nitrogen levels (i.e., NO 3 ? , NH 4 + ), salinity and pH (explaining 73.8% of the total variation, R ~(2)= 0.71). Quantification of the genes used as proxies for N fixation, nitrification and denitrification revealed clear successional signatures that corroborated the taxonomic assignments obtained by metagenomics. Notably, we found strong evidence for niche partitioning, as revealed by the abundance and distribution of marker genes for nitrification (ammonia-oxidizing bacteria and archaea) and denitrification (nitrite reductase nirK, nirS and nitrous oxide reductase nosZ clades I and II). This was supported by a distinct correlation between these genes and soil physico-chemical properties, such as soil physical structure, pH, salinity, organic matter, total N, NO 3 ? , NH 4 + and SO 4 2 ? , across four seasonal samplings. Overall, this study sheds light on the successional trajectories of microbial N cycle genes along a naturally developing salt marsh ecosystem. The data obtained serve as a foundation to guide the formulation of ecological models that aim to effectively monitor and manage pristine and impacted salt marsh areas. Such models should account for the ecology as well as the historical contingency of N cycling communities.
机译:沿海生态系统被认为是释放土地养分的缓冲区,却没有考虑到潜在的负面影响。因此,迫切需要更好地了解此类系统中参与氮(N)循环的微生物的生态组装和动力学。在这里,我们采用了两种互补的方法学方法(即shot弹枪宏基因组学和定量PCR)来检查参与N转化的所选微生物基因的分布和丰度。我们使用了沿荷兰Schiermonnikoog岛上建立完整的原始盐沼土壤时间序列的土壤样本,该序列跨越了一个多世纪的生态系统发展。在研究的土壤演替阶段中,参与N循环过程的基因种群结构与土壤氮水平(即NO 3?,NH 4 +),盐度和pH(解释为73.8%)密切相关。总变异数的R((2)= 0.71)。量化用作N固定,硝化和反硝化代理的基因,揭示了清晰的连续签名,证实了宏基因组学所获得的分类学分配。值得注意的是,我们发现了利基分配的有力证据,如硝化作用(氨氧化细菌和古细菌)和反硝化作用(亚硝酸还原酶nirK,nirS和一氧化二氮还原酶nosZ进化枝I和II)的标记基因的丰富和分布所揭示。这些基因与土壤理化特性之间存在明显的相关性,例如土壤物理结构,pH,盐度,有机质,总N,NO 3 ,NH 4 +和SO 4 2? ,在四个季节采样中进行。总体而言,这项研究揭示了沿自然发展的盐沼生态系统的微生物N循环基因的演替轨迹。所获得的数据为指导生态模型的制定奠定了基础,这些模型旨在有效地监测和管理原始和受影响的盐沼地区。这样的模型应该考虑到N个自行车社区的生态以及历史偶然性。

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