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Bacterial associations with weathering minerals at the regolith-bedrock interface, Luquillo Experimental Forest, Puerto Rico

机译:波多黎各卢基洛实验森林,风化矿物与风化矿物的细菌联系

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摘要

Microbe-mineral associations in regolith overlying granodiorite bedrock (4.6–4.9 m depth) from the Luquillo Experimental Forest, Puerto Rico, were imaged with confocal scanning laser microscopy at a novel scale of 400X magnification. After adding BacLight™ stain, proportionally more surface area of minerals (quartz, biotite, and mixed opaque kaolinite/goethite) emitted fluorescence from cell-impermeant propidium iodide than from cell-permeant SYTO 9, which suggested greater coverage of minerals by extracellular DNA or DNA in non-intact cells than by intact cells. Microscopic observations of predominantly non-intact cell material in deep saprolite were consistent with the abundance of rRNA sequences related to heterotrophic bacteria in clone libraries prepared from community DNA. A few sequences were affiliated with bacteria recognized to produce siderophores, oxidize Fe(II), or fix N2. Bacterial DNA in deep regolith from two boreholes 1.5 m apart yielded libraries with high diversity and taxa specific for each borehole. Supplemental materials are available for this article. Go to the publisher's online edition of Geomicrobiology Journal to view the free supplemental files.
机译:来自波多黎各卢奎洛实验森林的花岗闪长岩基岩(4.6-4.9 m深度)上的碎屑岩中的微生物-矿物结合,用共聚焦扫描激光显微镜成像,放大倍数为400倍。添加BacLight™染色剂后,成比例的矿物(石英,黑云母和混合的不透明高岭石/针铁矿)的表面积要比不透细胞的碘化丙啶所发射的荧光要多,而透细胞的SYTO 9则要发出荧光,这表明细胞外DNA或矿物对SYTO 9的覆盖率更大。非完整细胞中的DNA比完整细胞中的DNA多。显微镜下观察到深腐泥土中主要是非完整细胞物质,这与从群落DNA制备的克隆文库中与异养细菌有关的rRNA序列丰富有关。一些序列与被认为可产生铁载体,氧化Fe(II)或固定N2的细菌有关。来自两个相距1.5 m的钻孔的深部重块岩中的细菌DNA产生了具有高度多样性和特定于每个钻孔的类群的文库。补充材料可用于本文。转到出版商的《地球微生物学杂志》在线版本,以查看免费的补充文件。

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