Sun Weimin, Xiao Tangfu, Sun Min, Dong Yiran, Ning Zengping, Xiao Enzong, Tang Song, Li Jiwei
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China Department of Biochemistry and Microbiology, Rutgers University, New Brunswick, New Jersey, USA.
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang, China
Appl Environ Microbiol. 2015 Aug;81(15):4874-84. doi: 10.1128/AEM.00935-15. Epub 2015 May 15.
Located in southwest China, the Aha watershed is continually contaminated by acid mine drainage (AMD) produced from upstream abandoned coal mines. The watershed is fed by creeks with elevated concentrations of aqueous Fe (total Fe > 1 g/liter) and SO4 (2-) (>6 g/liter). AMD contamination gradually decreases throughout downstream rivers and reservoirs, creating an AMD pollution gradient which has led to a suite of biogeochemical processes along the watershed. In this study, sediment samples were collected along the AMD pollution sites for geochemical and microbial community analyses. High-throughput sequencing found various bacteria associated with microbial Fe and S cycling within the watershed and AMD-impacted creek. A large proportion of Fe- and S-metabolizing bacteria were detected in this watershed. The dominant Fe- and S-metabolizing bacteria were identified as microorganisms belonging to the genera Metallibacterium, Aciditerrimonas, Halomonas, Shewanella, Ferrovum, Alicyclobacillus, and Syntrophobacter. Among them, Halomonas, Aciditerrimonas, Metallibacterium, and Shewanella have previously only rarely been detected in AMD-contaminated environments. In addition, the microbial community structures changed along the watershed with different magnitudes of AMD pollution. Moreover, the canonical correspondence analysis suggested that temperature, pH, total Fe, sulfate, and redox potentials (Eh) were significant factors that structured the microbial community compositions along the Aha watershed.
阿哈流域位于中国西南部,持续受到上游废弃煤矿产生的酸性矿山排水(AMD)污染。该流域由小溪供水,这些小溪中水溶性铁(总铁>1克/升)和硫酸根离子(>6克/升)的浓度较高。AMD污染在下游河流和水库中逐渐减少,形成了一个AMD污染梯度,导致了整个流域一系列的生物地球化学过程。在本研究中,沿着AMD污染位点采集沉积物样本进行地球化学和微生物群落分析。高通量测序发现了该流域以及受AMD影响的小溪中与微生物铁和硫循环相关的各种细菌。在这个流域中检测到了很大比例的铁和硫代谢细菌。主要的铁和硫代谢细菌被鉴定为属于金属杆菌属、嗜酸铁单胞菌属、嗜盐单胞菌属、希瓦氏菌属、铁杆菌属、 Alicyclobacillus属和互营杆菌属的微生物。其中,嗜盐单胞菌属、嗜酸铁单胞菌属、金属杆菌属和希瓦氏菌属此前在受AMD污染的环境中很少被检测到。此外,微生物群落结构随着流域内不同程度的AMD污染而变化。而且,典范对应分析表明,温度、pH值、总铁、硫酸盐和氧化还原电位(Eh)是构建阿哈流域微生物群落组成的重要因素。