Akob Denise M, Lee Sang Hyon, Sheth Mili, Küsel Kirsten, Watson David B, Palumbo Anthony V, Kostka Joel E, Chin Kuk-Jeong
Florida State University Tallahassee, FL, USA.
Front Microbiol. 2012 Aug 9;3:280. doi: 10.3389/fmicb.2012.00280. eCollection 2012.
Though iron- and sulfate-reducing bacteria are well known for mediating uranium(VI) reduction in contaminated subsurface environments, quantifying the in situ activity of the microbial groups responsible remains a challenge. The objective of this study was to demonstrate the use of quantitative molecular tools that target mRNA transcripts of key genes related to Fe(III) and sulfate reduction pathways in order to monitor these processes during in situ U(VI) remediation in the subsurface. Expression of the Geobacteraceae-specific citrate synthase gene (gltA) and the dissimilatory (bi)sulfite reductase gene (dsrA), were correlated with the activity of iron- or sulfate-reducing microorganisms, respectively, under stimulated bioremediation conditions in microcosms of sediments sampled from the U.S. Department of Energy's Oak Ridge Integrated Field Research Challenge (OR-IFRC) site at Oak Ridge, TN, USA. In addition, Geobacteraceae-specific gltA and dsrA transcript levels were determined in parallel with the predominant electron acceptors present in moderately and highly contaminated subsurface sediments from the OR-IFRC. Phylogenetic analysis of the cDNA generated from dsrA mRNA, sulfate-reducing bacteria-specific 16S rRNA, and gltA mRNA identified activity of specific microbial groups. Active sulfate reducers were members of the Desulfovibrio, Desulfobacterium, and Desulfotomaculum genera. Members of the subsurface Geobacter clade, closely related to uranium-reducing Geobacter uraniireducens and Geobacter daltonii, were the metabolically active iron-reducers in biostimulated microcosms and in situ core samples. Direct correlation of transcripts and process rates demonstrated evidence of competition between the functional guilds in subsurface sediments. We further showed that active populations of Fe(III)-reducing bacteria and sulfate-reducing bacteria are present in OR-IFRC sediments and are good potential targets for in situ bioremediation.
尽管铁还原菌和硫酸盐还原菌在受污染的地下环境中介导铀(VI)还原方面广为人知,但对负责该过程的微生物群体的原位活性进行量化仍然是一项挑战。本研究的目的是展示使用定量分子工具,这些工具靶向与铁(III)和硫酸盐还原途径相关的关键基因的mRNA转录本,以便在地下原位铀(VI)修复过程中监测这些过程。在美国田纳西州橡树岭美国能源部橡树岭综合现场研究挑战(OR - IFRC)场地采集的沉积物微观世界中,在刺激生物修复条件下,地杆菌科特异性柠檬酸合酶基因(gltA)和异化(双)亚硫酸盐还原酶基因(dsrA)的表达分别与铁还原或硫酸盐还原微生物的活性相关。此外,还并行测定了OR - IFRC中度和高度污染的地下沉积物中主要电子受体存在情况下的地杆菌科特异性gltA和dsrA转录水平。对由dsrA mRNA、硫酸盐还原菌特异性16S rRNA和gltA mRNA产生的cDNA进行系统发育分析,确定了特定微生物群体的活性。活跃的硫酸盐还原菌是脱硫弧菌属、脱硫杆菌属和脱硫肠状菌属的成员。与铀还原菌地杆菌和道尔顿地杆菌密切相关的地下地杆菌分支成员,是生物刺激微观世界和原位岩心样本中具有代谢活性的铁还原菌。转录本与过程速率的直接相关性证明了地下沉积物中功能群落之间存在竞争的证据。我们进一步表明,OR - IFRC沉积物中存在具有活性的铁(III)还原菌和硫酸盐还原菌群体,它们是原位生物修复的良好潜在目标。