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Diversity Abundance and Activity of Archaeal Populations in Oil-Contaminated Groundwater Accumulated at the Bottom of an Underground Crude Oil Storage Cavity

机译:地下原油储藏腔底部积累的石油污染的地下水中古细菌种群的多样性丰度和活动

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摘要

Fluorescence in situ hybridization has shown that cells labeled with an Archaea-specific probe (ARCH915) accounted for approximately 10% of the total cell count in oil-contaminated groundwater accumulated at the bottom of an underground crude oil storage cavity. Although chemical analyses have revealed vigorous consumption of nitrate in cavity groundwater, the present study found that the methane production rate was higher than the nitrate consumption rate. To characterize the likely archaeal populations responsible for methane production in this system, fragments of 16S ribosomal DNA (rDNA) were amplified by PCR using eight different combinations of universal and Archaea-specific primers. Sequence analysis of 324 clones produced 23 different archaeal sequence types, all of which were affiliated with the kingdom Euryarchaeota. Among them, five sequence types (KuA1, KuA6, KuA12, KuA16, and KuA22) were obtained in abundance. KuA1 and KuA6 were closely related to the known methanogens Methanosaeta concilii (99% identical) and Methanomethylovorans hollandica (98%), respectively. Although no closely related organism was found for KuA12, it could be affiliated with the family Methanomicrobiaceae. KuA16 and KuA22 showed substantial homology only to some environmental clones. Both of these branched deeply in the Euryarchaeota, and may represent novel orders. Quantitative competitive PCR showed that KuA12 was the most abundant, accounting for ∼50% of the total archaeal rDNA copies detected. KuA1 and KuA16 also constituted significant proportions of the total archaeal rDNA copies (7 and 17%, respectively). These results suggest that limited species of novel archaea were enriched in the oil storage cavity. An estimate of specific methane production rates suggests that they were active methanogens.
机译:荧光原位杂交表明,用古细菌特异性探针(ARCH915)标记的细胞约占地下原油储存腔底部积累的被油污染的地下水总数的10%。尽管化学分析显示腔室地下水中硝酸盐的消耗量很大,但本研究发现甲烷的产生速率高于硝酸盐的消耗速率。为了表征该系统中可能产生甲烷的古细菌种群,使用八种通用和古细菌特异性引物组合通过PCR扩增了16S核糖体DNA(rDNA)片段。 324个克隆的序列分析产生了23种不同的古细菌序列类型,所有这些类型都与Euryarchaeota王国相关。其中,获得了五种序列类型(KuA1,KuA6,KuA12,KuA16和KuA22)。 KuA1和KuA6分别与已知的产甲烷甲烷菌Methanosaeta conilili(99%相同)和Methanomethylovorans hollandica(98%)密切相关。尽管没有发现与KuA12密切相关的生物,但它可能与Methanomicrobiaceae科有关。 KuA16和KuA22仅对某些环境克隆显示出实质同源性。这两个分支在Euryarchaeota中都有很深的分支,可能代表着新颖的秩序。定量竞争PCR显示,KuA12含量最高,占检测到的古细菌rDNA拷贝总数的50%。 KuA1和KuA16也占总古细菌rDNA拷贝的很大比例(分别为7%和17%)。这些结果表明,在贮油腔中富集了数量有限的新型古细菌。对特定甲烷产量的估计表明它们是活性产甲烷菌。

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