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Nanoscale study of As biomineralization in an acid mine drainage system

机译:酸性矿山排水系统中砷生物矿化的纳米研究

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Spatial and seasonal variations of the oxidation of Fe(II) and As(III) have been previously documented in the Carnoules (Gard, France) Acid Mine Drainage (AMD) by bulk analyses. These variations may be correlated with the variations in the activity of indigenous As(III)- and Fe(II)-oxidizing bacteria living in the As-rich Carnoules water. The activity of these bacteria indeed plays an important role in the nature and composition of the solid phases that sequester arsenic at this site. In order to better understand the interactions of microbes with Fe and As in the Carnoules AMD, we combined Transmission Electron Microscopy (TEM) and Scanning Transmission X-ray Microscopy (STXM) to collect near-edge X-ray absorption fine structure (NEXAFS) spectra at high spatial and energy resolution and to perform high spatial resolution imaging at the 30-50 nm scale. Spectromicroscopy was performed at the C K-edge, Fe L-2,L-3-edge, and As L-2,L-3-edge, which allowed us to locate living and/or mineralized bacterial cells and to characterize Fe and As oxidation states in the vicinity of those cells. TEM was used to image the same areas, providing higher resolution images and complementary crystallographic and compositional information through electron diffraction and EDXS analysis. This approach provides unique information on heterogeneous geochemical processes that occur in a complex microbial community in an AMD environment at the micrometer and submicrometer-scale. Bacterial cells in the Carnoules AMD were frequently associated with mineral precipitates, and a variety of biomineralization patterns were observed. While many mineral precipitates were not associated with bacterial cells, they were associated with pervasive organic carbon. Finally, abundant biomineralized organic vesicles were observed in the Carnoules AMD. Such vesicles may have been overlooked in highly mineralized extreme environments in the past and may represent an important component in a common biomineralization process in such environments. (C) 2008 Elsevier Ltd. All rights reserved.
机译:Fe(II)和As(III)氧化的空间和季节变化先前已通过本体分析在Carnoules(法国加德)酸性矿山排水(AMD)中得到记录。这些变化可能与生活在富含As的小瓶水中的本地As(III)和Fe(II)氧化细菌的活性变化相关。这些细菌的活性确实在将砷螯合在该部位的固相的性质和组成中起着重要作用。为了更好地了解在Carnoules AMD中微生物与Fe和As的相互作用,我们结合了透射电子显微镜(TEM)和扫描透射X射线显微镜(STXM)来收集近边缘X射线吸收精细结构(NEXAFS)光谱在高空间和能量分辨率,并执行30-50 nm规模的高空间分辨率成像。在C K边缘,Fe L-2,L-3-边缘和As L-2,L-3-边缘进行了光谱显微镜检查,这使我们能够定位活的和/或矿化的细菌细胞并鉴定Fe和在那些细胞附近处于氧化态。 TEM用于对相同区域成像,通过电子衍射和EDXS分析提供更高分辨率的图像以及互补的晶体学和组成信息。这种方法可提供有关微米级和亚微米级的AMD环境中复杂微生物群落中发生的异质地球化学过程的独特信息。 Carnoules AMD中的细菌细胞经常与矿物质沉淀有关,并且观察到各种生物矿化模式。尽管许多矿物沉淀物与细菌细胞无关,但它们与普遍的有机碳有关。最后,在Carnoules AMD中观察到大量生物矿化的有机囊泡。过去在高度矿化的极端环境中可能忽略了这种囊泡,并且这些囊泡在此类环境中代表了常见生物矿化过程中的重要组成部分。 (C)2008 Elsevier Ltd.保留所有权利。

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