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Deep Subsurface Life from North Pond: Enrichment Isolation Characterization and Genomes of Heterotrophic Bacteria

机译:来自北部池塘的深层地下生活:异养细菌的富集分离鉴定和基因组

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摘要

Studies of subsurface microorganisms have yielded few environmentally relevant isolates for laboratory studies. In order to address this lack of cultivated microorganisms, we initiated several enrichments on sediment and underlying basalt samples from North Pond, a sediment basin ringed by basalt outcrops underlying an oligotrophic water-column west of the Mid-Atlantic Ridge at 22°N. In contrast to anoxic enrichments, growth was observed in aerobic, heterotrophic enrichments from sediment of IODP Hole U1382B at 4 and 68 m below seafloor (mbsf). These sediment depths, respectively, correspond to the fringes of oxygen penetration from overlying seawater in the top of the sediment column and upward migration of oxygen from oxic seawater from the basalt aquifer below the sediment. Here we report the enrichment, isolation, initial characterization and genomes of three isolated aerobic heterotrophs from North Pond sediments; an Arthrobacter species from 4 mbsf, and Paracoccus and Pseudomonas species from 68 mbsf. These cultivated bacteria are represented in the amplicon 16S rRNA gene libraries created from whole sediments, albeit at low (up to 2%) relative abundance. We provide genomic evidence from our isolates demonstrating that the Arthrobacter and Pseudomonas isolates have the potential to respire nitrate and oxygen, though dissimilatory nitrate reduction could not be confirmed in laboratory cultures. The cultures from this study represent members of abundant phyla, as determined by amplicon sequencing of environmental DNA extracts, and allow for further studies into geochemical factors impacting life in the deep subsurface.
机译:对地下微生物的研究几乎没有产生与环境有关的分离物用于实验室研究。为了解决这种缺乏的培养微生物的问题,我们对北池塘的沉积物和下伏的玄武岩样品进行了一些富集,该沉积池由玄武岩露头环绕的沉积盆地构成,该盆地位于22°N大西洋中脊以西的贫营养水柱下方。与缺氧富集相反,在海底(mbsf)下方4和68 m处,IODP孔U1382B沉积物中的有氧,异养富集中观察到生长。这些沉积物深度分别对应于沉积物柱顶部上覆海水的氧气渗透条纹和沉积物下方玄武岩含水层中含氧海水中氧气的向上迁移。在这里,我们报告了北塘沉积物中三种分离的好氧异养菌的富集,分离,初始特征和基因组。来自4 mbsf的节杆菌物种,以及来自68 mbsf的副球菌和假单胞菌物种。这些培养细菌在从整个沉积物中创建的扩增子16S rRNA基因文库中都有代表,尽管相对丰度很低(最高2%)。我们从分离株中提供了基因组证据,证明了关节杆菌和假单胞菌分离株具有释放硝酸盐和氧气的潜力,尽管在实验室培养中无法证实异化硝酸盐的还原。通过环境DNA提取物的扩增子测序确定,本研究的培养物代表丰富的门,并允许进一步研究影响深地下生命的地球化学因素。

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