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针铁矿通过阻断S12外膜上的末端还原位点来阻碍偶氮染料的生物还原。

Goethite Hinders Azo Dye Bioreduction by Blocking Terminal Reductive Sites on the Outer Membrane of S12.

作者信息

Zhao Gang, Li Enze, Li Jianjun, Liu Feifei, Liu Fei, Xu Meiying

机构信息

Guangdong Provincial Key Laboratory of Microbial Culture Collection and Application, Guangdong Institute of Microbiology, Guangdong Academy of Sciences, Guangzhou, China.

State Key Laboratory of Applied Microbiology Southern China, Guangzhou, China.

出版信息

Front Microbiol. 2019 Jun 25;10:1452. doi: 10.3389/fmicb.2019.01452. eCollection 2019.

Abstract

Iron (hydr)oxides are the most ubiquitous Fe(III)-containing minerals in the near-surface environments and can regulate organic pollutant biotransformation by participating in bacterial extracellular electron transfer under anaerobic conditions. Mechanisms described so far are based on their redox properties in bacterial extracellular respiration. Here, we find that goethite, a typical iron (hydr)oxide, inhibits the bioreduction of different polar azo dyes by S12 not through electron competition, but by the contact of its surface Fe(III) with the bacterial outer surface. Through the combined results of attenuated total reflectance (ATR) Fourier transform infrared spectroscopy, two-dimensional correlation spectroscopy, and confocal laser scanning microscope, we found that the outer membrane proteins MtrC and OmcA of strain S12 are key binding sites for goethite surface. Meanwhile, they were identified as the important reductive terminals for azo dyes. These results suggest that goethite may block the terminal reductive sites of azo dyes on the bacterial outer membrane to inhibit their bioreduction. This discovered role of goethite in bioreduction provides new insight into the microbial transformation processes of organic pollutants in iron (hydr)oxide-containing environments.

摘要

铁(氢)氧化物是近地表环境中最普遍存在的含铁(III)矿物,在厌氧条件下可通过参与细菌胞外电子转移来调节有机污染物的生物转化。目前所描述的机制是基于它们在细菌胞外呼吸中的氧化还原特性。在此,我们发现针铁矿这种典型的铁(氢)氧化物,抑制S12对不同极性偶氮染料的生物还原作用,并非通过电子竞争,而是通过其表面的Fe(III)与细菌外表面接触来实现。通过衰减全反射(ATR)傅里叶变换红外光谱、二维相关光谱和共聚焦激光扫描显微镜的综合结果,我们发现菌株S12的外膜蛋白MtrC和OmcA是针铁矿表面的关键结合位点。同时,它们被确定为偶氮染料的重要还原末端。这些结果表明,针铁矿可能会阻断细菌外膜上偶氮染料的末端还原位点,从而抑制其生物还原。针铁矿在生物还原中这一被发现的作用,为含铁血(氢)氧化物环境中有机污染物的微生物转化过程提供了新的见解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1ad1/6604703/d000ca36a321/fmicb-10-01452-g001.jpg

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