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Increased Denitrification Rates Associated with Shifts in Prokaryotic Community Composition Caused by Varying Hydrologic Connectivity

机译:与因水文连通性变化而引起的原核生物群落转变相关的反硝化率增加

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摘要

While modern developments in agriculture have allowed for increases in crop yields and rapid human population growth, they have also drastically altered biogeochemical cycles, including the biotransformation of nitrogen. Denitrification is a critical process performed by bacteria and fungi that removes nitrate in surface waters, thereby serving as a potential natural remediation strategy. We previously reported that constant inundation resulted in a coupling of denitrification gene abundances with denitrification rates in sediments, but these relationships were not maintained in periodically-inundated or non-inundated environments. In this study, we utilized Illumina next-generation sequencing to further evaluate how the microbial community responds to these hydrologic regimes and how this community is related to denitrification rates at three sites along a creek in an agricultural watershed over 2 years. The hydrologic connectivity of the sampling location had a significantly greater influence on the denitrification rate (P = 0.010), denitrification gene abundances (P < 0.001), and the prokaryotic community (P < 0.001), than did other spatiotemporal factors (e.g., creek sample site or sample month) within the same year. However, annual variability among denitrification rates was also observed (P < 0.001). Furthermore, the denitrification rate was significantly positively correlated with water nitrate concentration (Spearman's ρ = 0.56, P < 0.0001), denitrification gene abundances (ρ = 0.23–0.47, P ≤ 0.006), and the abundances of members of the families Burkholderiaceae, Anaerolinaceae, Microbacteriaceae, Acidimicrobineae incertae sedis, Cytophagaceae, and Hyphomicrobiaceae (ρ = 0.17–0.25, P ≤ 0.041). Prokaryotic community composition accounted for the least amount of variation in denitrification rates (22%), while the collective influence of spatiotemporal factors and gene abundances accounted for 37%, with 40% of the variation related to interactions among all parameters. Results of this study suggest that the hydrologic connectivity at each location had a greater effect on the prokaryotic community than did spatiotemporal differences, where inundation is associated with shifts favoring increased denitrification potential. We further establish that while complex interactions among the prokaryotic community influence denitrification, the link between hydrologic connectivity, microbial community composition, and genetic potential for biogeochemical cycling is a promising avenue to explore hydrologic remediation strategies such as periodic flooding.
机译:现代农业发展已使作物产量增加和人口迅速增长,但它们也大大改变了生物地球化学循环,包括氮的生物转化。反硝化是细菌和真菌执行的关键过程,可去除地表水中的硝酸盐,从而成为潜在的自然修复策略。我们以前曾报道说,持续的淹没导致沉积物中反硝化基因丰度与反硝化率的耦合,但是在定期淹没或未淹没的环境中这些关系没有得到维持。在这项研究中,我们利用了Illumina的新一代测序技术,进一步评估了微生物群落如何响应这些水文状况,以及该群落如何与2年多来农业流域中一条小河沿岸三个地点的反硝化率相关。与其他时空因素(如小溪)相比,采样地点的水文连通性对反硝化率(P = 0.010),反硝化基因丰度(P <0.001)和原核生物群落(P <0.001)的影响更大。样本网站或样本月份)。但是,也观察到反硝化率之间的年度差异(P <0.001)。此外,反硝化率与硝酸盐水浓度(Spearmanρ= 0.56,P <0.0001),反硝化基因丰度(ρ= 0.23-0.47,P≤0.006)以及伯克霍尔德氏菌科,Anaerolinaceae科成员的丰度显着正相关。 ,微细菌科,不动酸杆菌,胞吞噬菌体和低微生物菌科(ρ= 0.17–0.25,P≤0.041)。原核生物群落组成的反硝化率变化最少(22%),而时空因素和基因丰度的集体影响占37%,其中40%的变化与所有参数之间的相互作用有关。这项研究的结果表明,与时空差异相比,每个位置的水文连通性对原核生物群落的影响更大,在时空差异中,淹没与有利于反硝化潜力增加的变化有关。我们进一步确定,虽然原核生物群落之间复杂的相互作用会影响反硝化作用,但水文连通性,微生物群落组成和生物地球化学循环的遗传潜力之间的联系是探索水文修复策略(如定期洪水)的有前途的途径。

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