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亚铁氧化硫杆菌中与异化铁还原偶联的厌氧硫代谢。

Anaerobic sulfur metabolism coupled to dissimilatory iron reduction in the extremophile Acidithiobacillus ferrooxidans.

机构信息

Center for Bioinformatics and Genome Biology, Fundacion Ciencia y Vida, Santiago, and Departamento Ciencias Biologicas, Facultad de Ciencias Biologicas, Universidad Andres Bello, Santiago, Chile.

出版信息

Appl Environ Microbiol. 2013 Apr;79(7):2172-81. doi: 10.1128/AEM.03057-12. Epub 2013 Jan 25.

Abstract

Gene transcription (microarrays) and protein levels (proteomics) were compared in cultures of the acidophilic chemolithotroph Acidithiobacillus ferrooxidans grown on elemental sulfur as the electron donor under aerobic and anaerobic conditions, using either molecular oxygen or ferric iron as the electron acceptor, respectively. No evidence supporting the role of either tetrathionate hydrolase or arsenic reductase in mediating the transfer of electrons to ferric iron (as suggested by previous studies) was obtained. In addition, no novel ferric iron reductase was identified. However, data suggested that sulfur was disproportionated under anaerobic conditions, forming hydrogen sulfide via sulfur reductase and sulfate via heterodisulfide reductase and ATP sulfurylase. Supporting physiological evidence for H2S production came from the observation that soluble Cu(2+) included in anaerobically incubated cultures was precipitated (seemingly as CuS). Since H(2)S reduces ferric iron to ferrous in acidic medium, its production under anaerobic conditions indicates that anaerobic iron reduction is mediated, at least in part, by an indirect mechanism. Evidence was obtained for an alternative model implicating the transfer of electrons from S(0) to Fe(3+) via a respiratory chain that includes a bc(1) complex and a cytochrome c. Central carbon pathways were upregulated under aerobic conditions, correlating with higher growth rates, while many Calvin-Benson-Bassham cycle components were upregulated during anaerobic growth, probably as a result of more limited access to carbon dioxide. These results are important for understanding the role of A. ferrooxidans in environmental biogeochemical metal cycling and in industrial bioleaching operations.

摘要

对嗜酸化能自养菌氧化亚铁硫杆菌在有氧和无氧条件下分别以分子氧和高铁作为电子受体、元素硫作为电子供体生长时的基因转录(微阵列)和蛋白水平(蛋白质组学)进行了比较。没有证据支持四硫代硫酸盐水解酶或砷还原酶在介导电子向高铁转移中的作用(如先前的研究所示)。此外,没有发现新的高铁还原酶。然而,数据表明,在厌氧条件下硫发生歧化,通过硫还原酶形成硫化氢,通过异二硫还原酶和 ATP 硫酸化酶形成硫酸盐。H2S 产生的生理证据来自于观察到,在厌氧培养物中包含的可溶性 Cu(2+)被沉淀(似乎是作为 CuS)。由于 H2S 在酸性介质中将高铁还原为亚铁,因此在厌氧条件下的产生表明,厌氧铁还原至少部分通过间接机制介导。获得了证据表明,电子通过包括 bc(1)复合物和细胞色素 c 的呼吸链从 S(0)转移到 Fe(3+),从而提供了一种替代模型。有氧条件下的中心碳途径被上调,与更高的生长速率相关,而厌氧生长期间许多卡尔文-本森-巴斯汉循环组件被上调,可能是由于对二氧化碳的获取更有限。这些结果对于理解氧化亚铁硫杆菌在环境生物地球化学金属循环和工业生物浸出中的作用非常重要。

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