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Variations in the structure of airborne bacterial communities in Tsogt-Ovoo of Gobi desert area during dust events

机译:沙尘暴期间戈壁沙漠地区Tsogt-Ovoo空中细菌群落结构的变化

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摘要

Asian dust events transport the airborne bacteria in Chinese desert regions as well as mineral particles and influence downwind area varying biological ecosystems and climate changes. However, the airborne bacterial dynamics were rarely investigated in the Gobi desert area, where dust events are highly frequent. In this study, air samplings were sequentially performed at a 2-m high above the ground at the sampling site located in desert area (Tsogt-Ovoo of Gobi desert; Mongolia 44.2304°N, 105.1700°E). During the dust event days, the bacterial cells and mineral particles increased to more than tenfold of concentrations. MiSeq sequencing targeting 16S ribosomal DNA revealed that the airborne bacteria in desert area mainly belonged to the classes Acidobacteria, Actinobacteria, Bacteroidetes, Chloroflexi, Bacilli, Alpha-proteobacteria, Beta-proteobacteria, and Gamma-proteobacteria. The bacterial community structures were different between dust events and non-dust events. The air samples collected at the dust events indicated high abundance rates of Alpha-proteobacteria, which were reported to dominate on the leaf surfaces of plants or in the saline lake environments. After the dust events, the members of Firmicutes (Bacilli) and Bacteroidetes, which are known to form endospore and attach with coarse particles, respectively, increased their relative abundances in the air samples. Presumably, the bacterial compositions and diversities in atmosphere significantly vary during dust events, which carry some particles from grassland (phyllo-sphere), dry lake, and sand surfaces, as well as some bacterial populations such as Firmicutes and Bacteroidetes maintain in the atmosphere for longer time.Electronic supplementary materialThe online version of this article (doi:10.1007/s11869-016-0430-3) contains supplementary material, which is available to authorized users.
机译:亚洲的尘埃事件将中国沙漠地区的空气传播的细菌以及矿物质颗粒转移到了顺风地区,影响着生物生态系统和气候变化。但是,在戈壁沙漠地区粉尘事件频繁发生的地方,很少研究空气传播的细菌动力学。在这项研究中,在位于沙漠地区(戈壁沙漠的Tsogt-Ovoo;蒙古44.2304°N,105.1700°E)的采样点,在海拔2米高的地面上依次进行了空气采样。在沙尘暴期间,细菌细胞和矿物质颗粒的浓度增加到十倍以上。针对16S核糖体DNA的MiSeq测序显示,沙漠地区的空气传播细菌主要属于酸性细菌,放线菌,拟杆菌,绿弯曲菌,芽孢杆菌,α-蛋白细菌,β-蛋白细菌和γ-蛋白细菌。灰尘事件和非灰尘事件之间的细菌群落结构不同。在尘埃事件中收集到的空气样本显示出高含量的丙酸杆菌,据报道在植物的叶片表面或盐湖环境中占主导地位。尘埃事件发生后,已知会形成内生孢子并附着有粗颗粒的Firmicutes(Bacilli)和Bacteroidetes的成员会增加空气样品中的相对丰度。据推测,在尘埃事件期间,大气中的细菌组成和多样性会发生显着变化,这些尘埃携带着一些来自草地(叶层),干燥的湖泊和沙子表面的颗粒,以及一些细菌种群(如Fimicutes和Bacteroidetes)在大气中保持电子补充材料本文的在线版本(doi:10.1007 / s11869-016-0430-3)包含补充材料,授权用户可以使用。

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