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首页> 外文期刊>Microbial Ecology: An International Journal >Microbial Characterization of Microbial Ecosystems Associated to Evaporites Domes of Gypsum in Salar de Llamara in Atacama Desert
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Microbial Characterization of Microbial Ecosystems Associated to Evaporites Domes of Gypsum in Salar de Llamara in Atacama Desert

机译:阿塔卡马沙漠萨拉拉德拉马拉的与石膏蒸发圆顶相关的微生物生态系统的微生物特征

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The Central Andes in northern Chile contains a large number of closed basins whose central depression is occupied by saline lakes and salt crusts (salars). One of these basins is Salar de Llamara (850 m a.s.l.), where large domed structures of seemingly evaporitic origin forming domes can be found. In this work, we performed a detailed microbial characterization of these domes. Mineralogical studies revealed gypsum (CaSO4) as a major component. Microbial communities associated to these structures were analysed by 454 16S rDNA amplicon sequencing and compared between winter and summer seasons. Bacteroidetes Proteobacteria and Planctomycetes remained as the main phylogenetic groups, an increased diversity was found in winter. Comparison of the upper air-exposed part and the lower water-submerged part of the domes in both seasons showed little variation in the upper zone, showing a predominance of Chromatiales (Gammaproteobacteria), Rhodospirillales (Alphaproteobacteria), and Sphingobacteriales (Bacteroidetes). However, the submerged part showed marked differences between seasons, being dominated by Proteobacteria (Alpha and Gamma) and Verrucomicrobia in summer, but with more diverse phyla found in winter. Even though not abundant by sequence, Cyanobacteria were visually identified by scanning electron microscopy (SEM), which also revealed the presence of diatoms. Photosynthetic pigments were detected by high-performance liquid chromatography, being more diverse on the upper photosynthetic layer. Finally, the system was compared with other endoevaporite, mats microbialite and Stromatolites microbial ecosystems, showing higher similitude with evaporitic ecosystems from Atacama and Guerrero Negro. This environment is of special interest for extremophile studies because microbial life develops associated to minerals in the driest desert all over the world. Nevertheless, it is endangered by mining activity associated to copper and lithium extraction; thus, its environmental protection preservation is strongly encouraged.
机译:智利北部的安第斯山脉中部有许多封闭的盆地,其中央凹陷被盐湖和盐结皮(撒拉)占据。这些盆地之一是Salar de Llamara(850 m.s.l.),在那里可以发现看似蒸发成因的大型圆顶结构,形成圆顶。在这项工作中,我们对这些圆顶进行了详细的微生物表征。矿物学研究表明,石膏(CaSO4)是主要成分。通过454 16S rDNA扩增子测序分析了与这些结构相关的微生物群落,并在冬季和夏季之间进行了比较。拟杆菌属和杆菌属仍是主要的系统发生群体,冬季发现多样性增加。在两个季节中比较穹顶的高空气暴露部分和低水淹没部分时,发现上部区域几乎没有变化,显示出以rom虫(γ变形杆菌),Rhodospirillales(α变形杆菌)和Sphingobacteriales(拟杆菌)为主。但是,淹没的部分显示出季节之间的显着差异,夏季以变形杆菌(Alpha和Gamma)和疣状微生物为主,而冬季则有更多种类的门。尽管序列上并不丰富,但通过扫描电子显微镜(SEM)可以目视鉴定蓝细菌,这也揭示了硅藻的存在。通过高效液相色谱法检测到光合色素,在上层光合层上具有更多的多样性。最后,将该系统与其他内生蒸发物,垫层微辉石和基质生物的微生物生态系统进行了比较,显示出与来自阿塔卡马和格雷罗黑人的蒸发生态系统更高的相似性。对于极端微生物研究而言,这种环境特别受关注,因为微生物生活的发展与世界上最干燥的沙漠中的矿物质有关。然而,它受到与铜和锂提取有关的采矿活动的威胁;因此,强烈鼓励其环境保护。

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