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Low-Abundance Members of the Firmicutes Facilitate Bioremediation of Soil Impacted by Highly Acidic Mine Drainage From the Malanjkhand Copper Project India

机译:来自印度Malanjkhand铜矿项目的低丰度成员可促进受到高酸性矿山排水影响的土壤的生物修复

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摘要

Sulfate- and iron-reducing heterotrophic bacteria represented minor proportion of the indigenous microbial community of highly acidic, oligotrophic acid mine drainage (AMD), but they can be successfully stimulated for in situ bioremediation of an AMD impacted soil (AIS). These anaerobic microorganisms although played central role in sulfate- and metal-removal, they remained inactive in the AIS due to the paucity of organic carbon and extreme acidity of the local environment. The present study investigated the scope for increasing the abundance and activity of inhabitant sulfate- and iron-reducing bacterial populations of an AIS from Malanjkhand Copper Project. An AIS of pH 3.5, high soluble SO42− (7838 mg/l) and Fe (179 mg/l) content was amended with nutrients (cysteine and lactate). Thorough geochemical analysis, 16S rRNA gene amplicon sequencing and qPCR highlighted the intrinsic metabolic abilities of native bacteria in AMD bioremediation. Following 180 days incubation, the nutrient amended AIS showed marked increase in pH (to 6.6) and reduction in soluble -SO42− (95%), -Fe (50%) and other heavy metals. Concomitant to physicochemical changes a vivid shift in microbial community composition was observed. Members of the Firmicutes present as a minor group (1.5% of total community) in AIS emerged as the single most abundant taxon (∼56%) following nutrient amendments. Organisms affiliated to Clostridiaceae, Peptococcaceae, Veillonellaceae, Christensenellaceae, Lachnospiraceae, Bacillaceae, etc. known for their fermentative, iron and sulfate reducing abilities were prevailed in the amended samples. qPCR data corroborated with this change and further revealed an increase in abundance of dissimilatory sulfite reductase gene (dsrB) and specific bacterial taxa. Involvement of these enhanced populations in reductive processes was validated by further enrichments and growth in sulfate- and iron-reducing media. Amplicon sequencing of these enrichments confirmed growth of Firmicutes members and proved their sulfate- and iron-reduction abilities. This study provided a better insight on ecological perspective of Firmicutes members within the AMD impacted sites, particularly their involvement in sulfate- and iron-reduction processes, in situ pH management and bioremediation.
机译:还原硫酸盐和铁的异养细菌在高酸性低营养矿山排水系统(AMD)的本地微生物群落中所占比例很小,但是可以成功地刺激它们,以便对受AMD污染的土壤(AIS)进行原位生物修复。这些厌氧微生物虽然在硫酸盐和金属的去除中起着重要作用,但由于有机碳的缺乏和当地环境的极端酸性,它们在AIS中仍然没有活性。本研究调查了增加Malanjkhand铜矿项目的AIS居民硫酸盐和铁还原细菌种群的丰度和活性的范围。用营养物质(半胱氨酸和乳酸)修正pH值为3.5的AIS,高溶解度的SO4 2-(7838 mg / l)和Fe(179 mg / l)。全面的地球化学分析,16S rRNA基因扩增子测序和qPCR强调了AMD生物修复中天然细菌的内在代谢能力。孵育180天后,经过修正的营养物AIS显示pH值显着增加(至6.6),可溶性-SO4 2-(95%),-Fe(50%)和其他重金属的含量降低。伴随着理化变化,微生物群落组成发生了明显变化。在营养改良后,AIS的Firmicutes成员(占社区总数的1.5%)成为单一的最丰富的分类单元(约56%)。在修正的样品中,以梭菌科,肽球菌科,Veillonellaceae,Christensenellaceae,Lachnospiraceae,Bacillaceae等附属的生物以其发酵,铁和硫酸盐还原能力闻名。 qPCR数据证实了这一变化,并进一步揭示了异化亚硫酸盐还原酶基因(dsrB)和特定细菌类群的丰度增加。这些增加的种群参与还原过程已通过硫酸盐和铁还原介质的进一步富集和生长得到证实。这些富集的扩增子测序证实了Firmicutes成员的生长,并证明了其硫酸盐和铁的还原能力。这项研究为AMD受灾地区的Firmicutes成员的生态学观点提供了更好的见解,尤其是他们参与硫酸盐和铁的还原过程,原位pH管理和生物修复。

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