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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:外膜细胞瘤OMCA的粒度效应和赤膜细胞学MR-1的机制

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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:地球附近表面的铁的循环受到不明化金属还原微生物的深受影响,许多研究集中于在这些细菌和Fe(IIII) - (氧水)氧化物之间的解开电子转移机制。然而,这些努力使这些矿物经常发生在微量到纳米化制度中,以及在相关的自然环境中以及实验室中受到聚集的影响。因此,难以探测蜂窝封套,负责促进界面电子转移步骤的外膜细胞变性的物理界面的性质,因此难以探测这些复杂的矿物质。使用全细胞的先前研究报告了与粒径不相关的减少率。在本研究中,我们将癸奈末端和纳米颗粒赤铁矿之间的癸米外膜细胞色素OMCA之间的相互作用隔离,通过电子平衡的详细表征和铁的结构和价值来检查作为粒度和反应产物的函数的减少率在颗粒表面。通过通过较小的分子抗坏血酸对非生物减少进行比较,我们表明,通过在颗粒聚集体中的OMCA和赤铁矿之间的间可接近的界面接触面积系统地控制还原率;一旦聚集体中的孔喉部尺寸随着OMCA大大增加,速率增加。对Fe(II)释放的OMCA氧化的同时测量显示为1:10的比例,与血红素的级联OMCA氧化机制血红素一致。 X射线吸收光谱揭示反应后赤铁矿纳米粒子的反应表面上的初生磁铁矿。集体调查结果确定了终端还原酶和氧化铁表面之间的物理接触可达性的重要性,并且通过观察的表观一致性有助于协调行为以较大的全细胞研究规模较大。 (c)2016 Elsevier Ltd.保留所有权利。

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