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Chemical Forms of Selenium in the Metal-Resistant Bacterium Ralstonia metallidurans CH34 Exposed to Selenite and Selenate

机译:暴露于亚硒酸盐和硒酸盐的抗金属细菌Ralstonia metallidurans CH34中硒的化学形式

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摘要

Ralstonia metallidurans CH34, a soil bacterium resistant to a variety of metals, is known to reduce selenite to intracellular granules of elemental selenium (Se0). We have studied the kinetics of selenite (SeIV) and selenate (SeVI) accumulation and used X-ray absorption spectroscopy to identify the accumulated form of selenate, as well as possible chemical intermediates during the transformation of these two oxyanions. When introduced during the lag phase, the presence of selenite increased the duration of this phase, as previously observed. Selenite introduction was followed by a period of slow uptake, during which the bacteria contained Se0 and alkyl selenide in equivalent proportions. This suggests that two reactions with similar kinetics take place: an assimilatory pathway leading to alkyl selenide and a slow detoxification pathway leading to Se0. Subsequently, selenite uptake strongly increased (up to 340 mg Se per g of proteins) and Se0 was the predominant transformation product, suggesting an activation of selenite transport and reduction systems after several hours of contact. Exposure to selenate did not induce an increase in the lag phase duration, and the bacteria accumulated approximately 25-fold less Se than when exposed to selenite. SeIV was detected as a transient species in the first 12 h after selenate introduction, Se0 also occurred as a minor species, and the major accumulated form was alkyl selenide. Thus, in the present experimental conditions, selenate mostly follows an assimilatory pathway and the reduction pathway is not activated upon selenate exposure. These results show that R. metallidurans CH34 may be suitable for the remediation of selenite-, but not selenate-, contaminated environments.
机译:Ralstonia metallidurans CH34是一种对多种金属具有抗性的土壤细菌,已知可将亚硒酸盐还原为元素硒(Se 0 )的细胞内颗粒。我们研究了亚硒酸盐(Se IV )和硒酸盐(Se VI )累积的动力学,并使用X射线吸收光谱法确定了硒酸盐的累积形式,以及这两个含氧阴离子转化过程中可能的化学中间体。如前所述,在滞后阶段引入亚硒酸盐会延长该阶段的持续时间。引入亚硒酸盐之后是一段缓慢吸收的过程,在此期间细菌中Se 0 和亚硒酸烷基酯的含量相同。这表明发生了两个动力学相似的反应:同化途径导致亚硒酸烷基酯和缓慢解毒途径导致Se 0 。随后,亚硒酸盐的摄取急剧增加(每克蛋白质高达340 mg Se),Se 0 是主要的转化产物,表明接触数小时后亚硒酸盐转运和还原系统被激活。暴露于硒酸盐中不会导致滞后阶段持续时间的增加,并且细菌积累的硒比暴露于亚硒酸盐时少约25倍。硒酸盐引入后的前12 h中检测到Se IV 为瞬时物质,Se 0 也为次要物质,主要积累形式为烷基硒化物。因此,在目前的实验条件下,硒酸盐主要遵循同化途径,并且在硒酸盐暴露后还原途径不被激活。这些结果表明,金属利德里亚霉菌CH34可能适合修复亚硒酸盐污染的环境,但不适用于硒酸盐污染的环境。

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