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Microbial diversity in the deep-subsurface hydrothermal aquifer feeding the giant gypsum crystal-bearing Naica Mine, Mexico

机译:墨西哥巨大的含石膏晶体奈卡矿的深地下热液含水层中的微生物多样性

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摘要

The Naica Mine in northern Mexico is famous for its giant gypsum crystals, which may reach up to 11 m long and contain fluid inclusions that might have captured microorganisms during their formation. These crystals formed under particularly stable geochemical conditions in cavities filled by low salinity hydrothermal water at 54–58°C. We have explored the microbial diversity associated to these deep, saline hydrothermal waters collected in the deepest (ca. 700–760 m) mineshafts by amplifying, cloning and sequencing small-subunit ribosomal RNA genes using primers specific for archaea, bacteria, and eukaryotes. Eukaryotes were not detectable in the samples and the prokaryotic diversity identified was very low. Two archaeal operational taxonomic units (OTUs) were detected in one sample. They clustered with, respectively, basal Thaumarchaeota lineages and with a large clade of environmental sequences branching at the base of the Thermoplasmatales within the Euryarchaeota. Bacterial sequences belonged to the Candidate Division OP3, Firmicutes and the Alpha- and Beta-proteobacteria. Most of the lineages detected appear autochthonous to the Naica system, since they had as closest representatives environmental sequences retrieved from deep sediments or the deep subsurface. In addition, the high GC content of 16S rRNA gene sequences belonging to the archaea and to some OP3 OTUs suggests that at least these lineages are thermophilic. Attempts to amplify diagnostic functional genes for methanogenesis (mcrA) and sulfate reduction (dsrAB) were unsuccessful, suggesting that those activities, if present, are not important in the aquifer. By contrast, genes encoding archaeal ammonium monooxygenase (AamoA) were amplified, suggesting that Naica Thaumarchaeota are involved in nitrification. These organisms are likely thermophilic chemolithoautotrophs adapted to thrive in an extremely energy-limited environment.
机译:墨西哥北部的奈卡矿因其巨大的石膏晶体而闻名,该石膏晶体可能长达11 m,并包含可能在形成过程中捕获微生物的流体包裹体。这些晶体是在地球化学条件特别稳定的情况下在54-58°C的低盐度热水中填充的空腔中形成的。我们已经通过使用古细菌,细菌和真核生物特异的引物扩增,克隆和测序小亚基核糖体RNA基因,探索了与在最深(约700–760 m)矿井中收集的这些深盐水热水有关的微生物多样性。在样品中不能检测到真核生物,并且鉴定出的原核生物多样性非常低。在一个样本中检测到两个古细菌分类单位(OTU)。它们分别与基底伞菌属和在环孢菌属中的热线虫基部分支的大量环境序列聚类。细菌序列属于候选分部OP3,菌毛和阿尔法和贝塔蛋白菌。所检测到的大多数血统似乎都是Naica系统的自发体,因为它们是从深层沉积物或深层地下获取的最接近的环境序列。另外,属于古细菌和某些OP3 OTU的16S rRNA基因序列的高GC含量表明至少这些谱系是嗜热的。扩增用于甲烷生成(mcrA)和硫酸盐还原(dsrAB)的诊断功能基因的尝试均未成功,表明这些活动(如果存在)在含水层中并不重要。相比之下,编码古细菌铵单加氧酶(AamoA)的基因被扩增,表明Naica Thaumarchaeota参与硝化作用。这些生物很可能是嗜热的化学自养生物,适合在极其有限的能量环境中壮成长。

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