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Ammonia-oxidizing archaea and bacteria in water columns and sediments of a highly eutrophic plateau freshwater lake

机译:氨氧化古物和细菌在水柱和高富养殖高原淡水湖的沉积物中

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Both ammonia-oxidizing archaea (AOA) and bacteria (AOB) can play important roles in the microbial oxidation of ammonia nitrogen in freshwater lake, but information on spatiotemporal variation in water column and sediment community structure is still limited. Additionally, the drivers of the differences between sediment and water assemblages are still unclear. The present study investigated the variation of AOA and AOB communities in both water columns and sediments of eutrophic freshwater Dianchi Lake. The abundance, diversity, and structure of both planktonic and sediment ammonia-oxidizing microorganisms in Dianchi Lake showed the evident changes with sampling site and time. In both water columns and sediments, AOB amoA gene generally outnumbered AOA, and the AOB/AOA ratio was much higher in summer than in autumn. The total AOA amoA abundance was relatively great in autumn, while sediment AOB was relatively abundant in summer. Sediment AOA amoA abundance was likely correlated with ammonia nitrogen (rs = 0.963). The AOB/AOA ratio in lake sediment was positively correlated with total phosphorus (rs = 0.835), while pH, dissolved organic carbon, and ammonia nitrogen might be the key driving forces for the AOB/AOA ratio in lake water. Sediment AOA and AOB diversity was correlated with nitrate nitrogen (rs = -0.786) and total organic carbon (rs = 0.769), respectively, while planktonic AOB diversity was correlated with ammonia nitrogen (rs = 0.854). Surface water and sediment in the same location had a distinctively different microbial community structure. In addition, sediment AOB community structure was influenced by total phosphorus, while total phosphorus might be a key determinant of planktonic AOB community structure.
机译:氨氧化archaea(AOA)和细菌(AOB)都可以在淡水湖中氨氮的微生物氧化中起重要作用,但有关水柱和沉积物群落结构的时空变化的信息仍然有限。此外,沉积物和水组合之间的差异的驱动器仍然不清楚。本研究研究了富养殖淡水滇池两种水柱中AOA和AOB群落的变化。滇池中浮游和沉积物氨氧化微生物的丰富,多样性和结构表明,采样场所和时间随之而来的变化。在水柱和沉积物中,AOB氨基酰胺基因通常超过AOA,夏季的AOB / AOA比率远高于秋季。秋季的AOA Amoa丰度相对较大,夏季沉积物AOB相对丰富。沉积物AOA Amoa丰度可能与氨氮有关(Rs = 0.963)。湖泊沉积物中的AOB / AOA比与总磷(Rs = 0.835)呈正相关,而pH,溶解的有机碳和氨氮可能是湖水中Aob / Aoa比的关键驱动力。沉积物AOA和AOB分集分别与硝酸氮(Rs = -0.786)和总有机碳(Rs = 0.769)相关,而Plankton AOB分集与氨氮相关(Rs = 0.854)。同一位置的地表水和沉积物具有明显不同的微生物群落结构。此外,沉积物AOB群落结构受到总磷的影响,而总磷可能是浮游毒黑群落结构的关键决定因素。

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