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Differentiation of nitrogen and microbial community in the littoral and limnetic sediments of a large shallow eutrophic lake (Chaohu Lake, China)

机译:大型浅水富营养化湖泊(中国巢湖)的沿海和边缘沉积物中氮和微生物群落的分化

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PurposeNitrogen (N) is one of the major elements causing eutrophication in freshwater lakes, and the N cycle is mainly driven by microorganisms. Lake littoral zones are found to be hotspots for N removal from both the basin and receiving waters. However, the environmental factors that drive the distribution of microorganisms are diverse and unclear. Here, we examined the differentiation of nitrogen and microbial community between the littoral and limnetic sediments to explore their interactions.Materials and methodsSediment samples were collected in the littoral and limnetic zones of Chaohu Lake in winter (ca. 7 degrees C) and autumn (ca. 22 degrees C). Abundances of the bacterial and archaeal genes amoA (ammoxidation), nirS and nirK (denitrification), hzsB (anaerobic ammonium oxidation; anammox), and nrfA (dissimilatory nitrate reduction to ammonium; DNRA) were measured via quantitative real-time polymerase chain reaction (qPCR). Clone libraries were constructed for further phylogenetic analysis to study the community composition.Results and discussionWe observed significant higher concentration values in terms of sedimentary NH4+-N and NO3--N in the limnetic zone than littoral zone (p0.05; n=12). In general, abundance values of the above six genes in the littoral zone were all higher than those in the limnetic zone, while higher in winter (7 degrees C) than in autumn (22 degrees C) (p0.05; n=6). The spatial heterogeneity had the most significant effect on the distribution of ammonia-oxidizing archaea (AOA) and anammox bacteria abundance. Both temporal (temperature) and spatial heterogeneity affected the abundance of ammonia-oxidizing bacteria (AOB). The variation in the abundance of denitrifying bacteria and DNRA bacteria mainly reflected the temporal (temperature) heterogeneity.ConclusionsThe six N-cycle-related microorganisms were affected by different environmental factors and presented different distribution patterns. The lower nitrogen content and the higher microbial abundance and diversity showed that the littoral zone was the hotspot of N-cycling-related microorganisms in a large, eutrophic, and turbid lake. It is suggested that increasing the area and restoring the ecological function of the littoral zone was effective and significant in eutrophic lake management.
机译:目的氮是造成淡水湖富营养化的主要元素之一,氮的循环主要由微生物驱动。发现湖滨带是从流域和接收水中去除氮的热点。但是,驱动微生物分布的环境因素是多种多样的,目前还不清楚。在这里,我们研究了沿岸沉积物和边缘沉积物之间氮和微生物群落的差异,以探讨它们之间的相互作用。材料和方法在冬季(约7摄氏度)和秋季(约7摄氏度)的巢湖沿岸和边缘地带收集沉积物样品。 22摄氏度)。通过定量实时聚合酶链反应(nrA和nirS(厌氧铵氧化;厌氧氨氧化;厌氧氨氧化)和nrfA(硝酸盐还原成铵的异化铵; DNRA))测定了细菌和古细菌基因amoA(氨氧化),nirS和nirK(反硝化),nrfA(异源硝酸还原为铵; DNRA)的丰度。 qPCR)。构建克隆文库以进行进一步的系统发育分析,以研究群落组成。结果与讨论我们观察到,沿河带的沉积NH4 + -N和NO3--N浓度值明显高于沿岸带(p <0.05; n = 12) 。通常,沿岸区上述六个基因的丰度值均高于边缘区,而冬季(7摄氏度)高于秋季(22摄氏度)(p <0.05; n = 6) 。空间异质性对氨氧化古细菌(AOA)和厌氧氨氧化细菌的丰度分布影响最大。时间(温度)和空间异质性都影响氨氧化细菌(AOB)的丰度。反硝化细菌和DNRA细菌的丰度变化主要反映了时间(温度)异质性。结论六种与N循环有关的微生物受到不同环境因素的影响,并呈现出不同的分布方式。较低的氮含量和较高的微生物丰度和多样性表明,在大型,富营养化和浑浊的湖泊中,沿岸带是N循环相关微生物的热点。有人认为,在富营养化湖泊管理中,增加面积并恢复沿海地区的生态功能是有效和重要的。

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