Whaley-Martin Kelly, Jessen Gerdhard L, Nelson Tara Colenbrander, Mori Jiro F, Apte Simon, Jarolimek Chad, Warren Lesley A
Civil and Mineral Engineering Department, University of Toronto, Toronto, ON, Canada.
Commonwealth Scientific Industry and Research Organization, Clayton, VIC, Australia.
Front Microbiol. 2019 Mar 8;10:297. doi: 10.3389/fmicb.2019.00297. eCollection 2019.
The biogeochemistry of acid mine drainage (AMD) derived from waste rock associated sulfide mineral oxidation is relatively well-characterized and linked to spp.. However, little is understood about the microbial communities and sulfur cycling before AMD develops, a key component of its prevention. This study aimed to examine circum-neutral mining impacted water (MIW) communities and its laboratory enrichments for sulfur oxidizing bacteria (SoxBac). MIW microbial communities differed in diversity, structure and relative abundance consistent with site specific variations in total aqueous sulfur concentrations (TotS; 2-17 mM), pH (3.67-7.34), and oxygen (22-93% saturation). However, the sulfur oxidizer, spp. dominated seven of the nine total SoxBac enrichment communities (76-100% relative abundance), spanning three of the four mines. The presence and relative abundance of the identified sixteen known and five unclassified spp. here, were the important clustering determinants across parent MIW and enrichment communities. Further, the presence of spp. was associated with driving the pH <4 in enrichment experiments, and the combination of specific spp. in the enrichments affected the observed acid to sulfate ratios indicating differential sulfur cycling. spp. also dominated the parent communities of the two acidic MIWs providing corroborating evidence for its active role in net acid generation within these waters. These results identify a putative indicator organism specific to mine tailings reservoirs and highlight the need for further study of tailings associated sulfur cycling for better mine management and environmental stewardship.
源自与硫化物矿物氧化相关的废石的酸性矿山排水(AMD)的生物地球化学特征相对明确,且与某些物种有关。然而,在AMD形成之前,其预防的关键组成部分——微生物群落和硫循环却鲜为人知。本研究旨在研究接近中性的采矿影响水(MIW)群落及其对硫氧化细菌(SoxBac)的实验室富集情况。MIW微生物群落在多样性、结构和相对丰度方面存在差异,这与总水溶硫浓度(TotS;约2 - 17 mM)、pH值(3.67 - 7.34)和氧气(22 - 93%饱和度)的特定场地变化一致。然而,硫氧化菌在九个总SoxBac富集群落中的七个中占主导地位(相对丰度约为76 - 100%),涵盖了四个矿山中的三个。这里鉴定出的16种已知和5种未分类的某些物种的存在和相对丰度,是母体MIW和富集群落的重要聚类决定因素。此外,在富集实验中,某些物种的存在与将pH值驱动至<4有关,并且富集中特定某些物种的组合影响了观察到的酸与硫酸盐的比例,表明硫循环存在差异。某些物种在两个酸性MIW的母体群落中也占主导地位,为其在这些水体中净酸生成中的积极作用提供了确凿证据。这些结果确定了一种特定于尾矿库的推定指示生物,并强调需要进一步研究与尾矿相关的硫循环,以实现更好的矿山管理和环境 stewardship(此处stewardship未明确对应中文,可保留英文)。