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Depth-Resolved Quantification of Anaerobic Toluene Degraders and Aquifer Microbial Community Patterns in Distinct Redox Zones of a Tar Oil Contaminant Plume

机译:焦油油烟羽不同氧化还原区中厌氧甲苯降解物和含水层微生物群落模式的深度解析量化

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Microbial degradation is the only sustainable component of natural attenuation in contaminated groundwater environments, yet its controls, especially in anaerobic aquifers, are still poorly understood. Hence, putative spatial correlations between specific populations of key microbial players and the occurrence of respective degradation processes remain to be unraveled. We therefore characterized microbial community distribution across a high-resolution depth profile of a tar oil-impacted aquifer where benzene, toluene, ethylbenzene, and xylene (BTEX) degradation depends mainly on sulfate reduction. We conducted depth-resolved terminal restriction fragment length polymorphism fingerprinting and quantitative PCR of bacterial 16S rRNA and benzylsuccinate synthase genes (bssA) to quantify the distribution of total microbiota and specific anaerobic toluene degraders. We show that a highly specialized degrader community of microbes related to known deltaproteobacterial iron and sulfate reducers (Geobacter and Desulfocapsa spp.), as well as clostridial fermenters (Sedimentibacter spp.), resides within the biogeochemical gradient zone underneath the highly contaminated plume core. This zone, where BTEX compounds and sulfate—an important electron acceptor—meet, also harbors a surprisingly high abundance of the yet-unidentified anaerobic toluene degraders carrying the previously detected F1-cluster bssA genes (C. Winderl, S. Schaefer, and T. Lueders, Environ. Microbiol. 9:1035-1046, 2007). Our data suggest that this biogeochemical gradient zone is a hot spot of anaerobic toluene degradation. These findings show that the distribution of specific aquifer microbiota and degradation processes in contaminated aquifers are tightly coupled, which may be of value for the assessment and prediction of natural attenuation based on intrinsic aquifer microbiota.
机译:在受污染的地下水环境中,微生物降解是自然衰减的唯一可持续的组成部分,但对其控制,尤其是在厌氧含水层中的控制,仍知之甚少。因此,关键微生物参与者的特定种群与各个降解过程的发生之间的假定空间相关性尚待阐明。因此,我们表征了焦油影响的含水层的高分辨率深度剖面中的微生物群落分布,其中苯,甲苯,乙苯和二甲苯(BTEX)的降解主要取决于硫酸盐的还原。我们进行了深度解析的末端限制性片段长度多态性指纹图谱和细菌16S rRNA和丁二酸苄酯合酶基因(bssA)的定量PCR,以量化总菌群和特定厌氧甲苯降解物的分布。我们显示,与已知的三角藻蛋白铁和硫酸盐还原剂(Geobacter和Desulfocapsa spp。)以及梭菌发酵罐(Sedimentibacter spp。)有关的高度专业化的微生物降解菌群落,位于高度污染的羽状核下方的生物地球化学梯度区内。该区域与BTEX化合物和硫酸盐(一个重要的电子受体)相遇,还携带着令人惊讶的高含量的尚未确定的厌氧甲苯降解物,这些降解物携带着先前检测到的F1簇bssA基因(C. Winderl,S。Schaefer和T Lueders,Environ Microbiol。9:1035-1046,2007)。我们的数据表明,该生物地球化学梯度带是厌氧甲苯降解的热点。这些发现表明,受污染含水层中特定含水层微生物群的分布与降解过程紧密相关,这对于基于固有含水层微生物群的自然衰减的评估和预测可能具有价值。

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