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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Particle size effect and the mechanism of hematite reduction by the outer membrane cytochrome OmcA of Shewanella oneidensis MR-1
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Particle size effect and the mechanism of hematite reduction by the outer membrane cytochrome OmcA of Shewanella oneidensis MR-1

机译:沙瓦氏假单胞菌MR-1的外膜细胞色素OmcA的粒径效应和赤铁矿还原机理

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摘要

The cycling of iron at the Earth's near surface is profoundly influenced by dissimilatory metal reducing microorganisms, and many studies have focused on unraveling electron transfer mechanisms between these bacteria and Fe(III)-(oxyhydr) oxides. However, these efforts have been complicated by the fact that these minerals often occur in the micro- to nanosize regime, and in relevant natural environments as well as in the laboratory are subject to aggregation. The nature of the physical interface between the cellular envelope, the outer-membrane cytochromes responsible for facilitating the interfacial electron transfer step, and these complex mineral particulates is thus difficult to probe. Previous studies using whole cells have reported reduction rates that do not correlate with particle size. In the present study we isolate the interaction between the decaheme outer-membrane cytochrome OmcA of Shewanella oneidensis and nanoparticulate hematite, examining the reduction rate as a function of particle size and reaction products through detailed characterization of the electron balance and the structure and valence of iron at particle surfaces. By comparison with abiotic reduction via the smaller molecule ascorbic acid, we show that the reduction rate is systematically controlled by the sterically accessible interfacial contact area between OmcA and hematite in particle aggregates; rates increase once pore throat sizes in aggregates become as large as OmcA. Simultaneous measure of OmcA oxidation against Fe(II) release shows a ratio of 1: 10, consistent with a cascade OmcA oxidation mechanism heme by heme. X-ray absorption spectroscopies reveal incipient magnetite on the reacted surfaces of the hematite nanoparticles after reaction. The collective findings establish the importance of accessibility of physical contact between the terminal reductases and iron oxide surfaces, and through apparent consistency of observations help reconcile behavior reported at the larger more complex scale of whole cell studies. (C) 2016 Elsevier Ltd. All rights reserved.
机译:铁在地球近地表的循环受到异化金属还原微生物的深远影响,许多研究集中于揭示这些细菌与Fe(III)-(羟基)氧化物之间的电子转移机理。但是,由于这些矿物质通常以微米级至纳米级的形式存在,并且在相关的自然环境以及实验室中易于聚集,因此使这些努力变得复杂。因此,很难探测到细胞包膜,负责促进界面电子转移步骤的外膜细胞色素与这些复杂矿物质颗粒之间的物理界面的性质。先前使用全细胞的研究报告了还原速率与颗粒大小无关。在本研究中,我们分离了Shewanella oneidensis的十全血红细胞膜细胞色素OmcA与纳米颗粒赤铁矿之间的相互作用,通过详细描述电子平衡以及铁的结构和化合价来研究还原速率与粒径和反应产物的关系。在粒子表面。通过与通过较小分子抗坏血酸进行非生物还原的比较,我们表明还原速率受颗粒聚集体中OmcA和赤铁矿之间空间可及的界面接触面积的系统控制;一旦聚集体中的孔喉尺寸变得与OmcA一样大,渗透率就会增加。 OmcA氧化对Fe(II)释放的同时测量显示比率为1:10,与血红素级联的OmcA氧化机制血红素一致。 X射线吸收光谱法显示反应后赤铁矿纳米颗粒的反应表面上有初生磁铁矿。集体的发现确立了末端还原酶与氧化铁表面之间物理接触的可及性的重要性,并且通过观察结果的明显一致性,有助于调和更大规模的全细胞研究中报道的行为。 (C)2016 Elsevier Ltd.保留所有权利。

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