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由于磷酸酶活性大幅降低,兼性厌氧菌株芽孢杆菌属JG-TB8在缺氧条件下对U(VI)的固定能力下降。

Decrease of U(VI) immobilization capability of the facultative anaerobic strain Paenibacillus sp. JG-TB8 under anoxic conditions due to strongly reduced phosphatase activity.

作者信息

Reitz Thomas, Rossberg Andre, Barkleit Astrid, Selenska-Pobell Sonja, Merroun Mohamed L

机构信息

Helmholtz-Center Dresden-Rossendorf, Institute of Resource Ecology, Dresden, Germany; Helmholtz-Center for Environmental Research, Department of Soil Ecology, Halle, Germany.

Helmholtz-Center Dresden-Rossendorf, Institute of Resource Ecology, Dresden, Germany.

出版信息

PLoS One. 2014 Aug 26;9(8):e102447. doi: 10.1371/journal.pone.0102447. eCollection 2014.

Abstract

Interactions of a facultative anaerobic bacterial isolate named Paenibacillus sp. JG-TB8 with U(VI) were studied under oxic and anoxic conditions in order to assess the influence of the oxygen-dependent cell metabolism on microbial uranium mobilization and immobilization. We demonstrated that aerobically and anaerobically grown cells of Paenibacillus sp. JG-TB8 accumulate uranium from aqueous solutions under acidic conditions (pH 2 to 6), under oxic and anoxic conditions. A combination of spectroscopic and microscopic methods revealed that the speciation of U(VI) associated with the cells of the strain depend on the pH as well as on the aeration conditions. At pH 2 and pH 3, uranium was exclusively bound by organic phosphate groups provided by cellular components, independently on the aeration conditions. At higher pH values, a part (pH 4.5) or the total amount (pH 6) of the dissolved uranium was precipitated under oxic conditions in a meta-autunite-like uranyl phosphate mineral phase without supplying an additional organic phosphate substrate. In contrast to that, under anoxic conditions no mineral formation was observed at pH 4.5 and pH 6, which was clearly assigned to decreased orthophosphate release by the cells. This in turn was caused by a suppression of the indigenous phosphatase activity of the strain. The results demonstrate that changes in the metabolism of facultative anaerobic microorganisms caused by the presence or absence of oxygen can decisively influence U(VI) biomineralization.

摘要

为了评估依赖氧气的细胞代谢对微生物铀迁移和固定的影响,研究了一种名为芽孢杆菌属JG-TB8的兼性厌氧细菌分离株与U(VI)在有氧和无氧条件下的相互作用。我们证明,在酸性条件(pH 2至6)下,无论是有氧还是无氧培养的芽孢杆菌属JG-TB8细胞,在有氧和无氧条件下都能从水溶液中积累铀。光谱和显微镜方法相结合表明,与该菌株细胞相关的U(VI)的形态取决于pH值以及曝气条件。在pH 2和pH 3时,无论曝气条件如何,铀都仅与细胞成分提供的有机磷酸基团结合。在较高的pH值下,在有氧条件下,一部分溶解的铀(pH 4.5)或全部溶解的铀(pH 6)会在没有额外提供有机磷酸底物的情况下,以类似变水铀矿的磷酸铀酰矿物相沉淀。相比之下,在无氧条件下,在pH 4.5和pH 6时未观察到矿物形成,这显然归因于细胞正磷酸盐释放的减少。这反过来又是由该菌株原生磷酸酶活性的抑制引起的。结果表明,氧气的存在或缺失导致的兼性厌氧微生物代谢变化可以决定性地影响U(VI)的生物矿化。

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