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Kinetic Characterization of OmcA and MtrC, Terminal Reductases Involved in Respiratory Electron Transfer for Dissimilatory Iron Reduction in Shewanella oneidensis MR-1▿

机译:运动蛋白OmcA和MtrC的动力学特征,参与呼吸电子转移的异化铁还原希瓦氏菌MR-1▿中的末端还原酶。

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摘要

We have used scaling kinetics and the concept of kinetic competence to elucidate the role of hemeproteins OmcA and MtrC in iron reduction by Shewanella oneidensis MR-1. Second-order rate constants for OmcA and MtrC were determined by single-turnover experiments. For soluble iron species, a stopped-flow apparatus was used, and for the less reactive iron oxide goethite, a conventional spectrophotometer was used to measure rates. Steady-state experiments were performed to obtain molecular rate constants by quantifying the OmcA and MtrC contents of membrane fractions and whole cells by Western blot analysis. For reduction of soluble iron, rates determined from transient-state experiments were able to account for rates obtained from steady-state experiments. However, this was not true with goethite; rate constants determined from transient-state experiments were 100 to 1,000 times slower than those calculated from steady-state experiments with membrane fractions and whole cells. In contrast, addition of flavins to the goethite experiments resulted in rates that were consistent with both transient- and steady-state experiments. Kinetic simulations of steady-state results with kinetic constants obtained from transient-state experiments supported flavin involvement. Therefore, we show for the first time that OmcA and MtrC are kinetically competent to account for catalysis of soluble iron reduction in whole Shewanella cells but are not responsible for electron transfer via direct contact alone with insoluble iron-containing minerals. This work supports the hypothesis that electron shuttles are important participants in the reduction of solid Fe phases by this organism.
机译:我们已经使用定标动力学和动力学能力的概念来阐明血红蛋白OmcA和MtrC在onewanensis Shewanella oneidensis MR-1还原铁中的作用。通过单周转实验确定OmcA和MtrC的二阶速率常数。对于可溶性铁物质,使用了停止流动的设备,对于反应性较低的氧化铁针铁矿,使用了常规的分光光度计来测量速率。通过蛋白质印迹分析定量膜级分和全细胞的OmcA和MtrC含量,进行稳态实验以获得分子速率常数。为了还原可溶性铁,从瞬态实验确定的速率可以考虑从稳态实验获得的速率。但是,针铁矿并非如此。由瞬态实验确定的速率常数比由膜部分和全细胞的稳态实验计算的速率常数慢100到1,000倍。相比之下,在针铁矿实验中加入黄素可产生与瞬态和稳态实验一致的速率。稳态结果的动力学模拟以及从瞬态实验获得的动力学常数支持黄素的参与。因此,我们首次证明OmcA和MtrC在动力学上足以说明整个希瓦氏菌细胞中可溶性铁还原的催化作用,但不负责通过直接与不溶性含铁矿物质直接接触进行电子转移。这项工作支持以下假设:电子梭是该生物体还原固态铁相的重要参与者。

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