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Detection Methanogens in Newly Settled Sediments from Xuanwu Lake in Nanjing, China

机译:南京玄武湖新近沉淀沉积物中产甲烷菌的检测

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Sediments from Xuanwu Lake have been dredged in the past 3 years to improve the water quality, but methanogenesis should still exist in the newly settled sediment. Methane production, methanogens, and physiochemical parameters were detected in the surface sediments (0–5 cm) and/or vertical sediments (0–21 cm, segmented at interval of 3 cm). Methane flux at water–air interface varied among five detected sites. Principal component analysis showed that CH4 flux, content of water and the concentration of total nitrogen (TN), CH4 and organic matters (OM) weighed most heavily on the component I in surface sediments while different patterns were observed for vertical sediments. The copy number of the 16S rRNA gene for bacteria was lower in the surface sediment (0–6 cm) than that in deeper sediments (12–21 cm), while 16S rRNA genes of Archaea were almost evenly distributed in the vertical sediments. Representatives belonging to the orders Methanobacteriales, Methanomicrobiales, and Methanosarcinales were detected in all samples of the vertical sediments, except that no members of the Methanococcales were detected in the samples at 0–6 cm. The level of Methanobacteriales reached a highest density at 18.1 × 104 copies g−1 dry weight (dw) at 6–9 cm; for Methanosarcinales (76.89 × 106 copies g−1 dw) and Methanococcales (82.70 × 103 copies g−1 dw) at 12–15 cm, whereas for Methanomicrobiales (43.37 × 106 copies g−1 dw) at 9–12 cm. Methanosarcinaceae and Methanosaetaceae reached to their highest densities at 6–9 and 9–12 cm, respectively. These data provided useful information for better understanding the methanogenesis in the newly settled sediments of a recently dredged lake.
机译:过去三年中,疏wu了玄武湖的沉积物,以改善水质,但新沉降的沉积物中仍应存在产甲烷作用。在表面沉积物(0-5 cm)和/或垂直沉积物(0-21 cm,以3 cm的间隔分段)中检测到甲烷的产生,产甲烷菌和理化参数。水-空气界面处的甲烷通量在五个检测到的位置之间变化。主成分分析表明,CH 4 通量,水含量和总氮(TN),CH 4 和有机物(OM)的浓度占最大地表沉积物中的I,而垂直沉积物观察到不同的模式。细菌的16S rRNA基因的拷贝数在表层沉积物中(0–6 cm)低于在较深的沉积物(12–21 cm)中,而古细菌的16S rRNA基因几乎垂直分布在垂直沉积物中。在垂直沉积物的所有样品中均检出了属于甲烷细菌,甲烷微生物和甲烷菌的细菌的代表,但在0-6 cm的样品中未检出甲烷球菌。甲烷细菌的水平在6–9 cm时达到18.1×10 4 份g -1 干重(dw)的最高密度;甲虫网虫(76.89×10 6 副本g -1 dw)和甲烷菌球菌(82.70×10 3 副本g -1 dw)在12–15 cm处,而Methanomicrobiales(43.37×10 6 副本g -1 dw)在9–12 cm处。甲烷藻科和甲烷藻科分别达到6-9和9-12 cm的最高密度。这些数据提供了有用的信息,可用于更好地了解最近疏lake的湖泊新沉降的沉积物中的甲烷生成。

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