从电缆细菌富集物中分离出的新型革兰氏阳性微生物 Microbacterium deferre sp.

Jamie J.M. Lustermans, Naja Basu, Kartik Aiyer
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摘要

微细菌科(Microbacteriaceae)是一类新陈代谢多变的革兰氏阳性细菌,存在于多种环境中。在布满丝状缆索细菌的沉积物中,微生物与缆索细菌之间存在着种间相互作用。从电缆菌丝附近分离出了一种新型革兰氏阳性细菌--Microbacterium deferre 菌株 A1-JK,它能够将细胞外电子转移(EET)到铁(III)氧化物和电极上。用三电极细胞中的 M.deferre A1-JK 纯培养物进行的电化学实验显示,细胞壁中存在可溶性扩散介质,通过 HPLC 分析确定其为黄素。基因组分析进一步发现了完整的核黄素合成途径,在氧气受限的条件下观察到黄素产量增加,从而促进了 EET 的产生。M. deferre A1-JK 编码外质细胞色素 FccA,负责在黄素载体上传递电子。除了在碱性(pH 8-10)和盐水(4% NaCl)条件下表现出微弱的电活性外,M. deferre A1-JK 还表现出从有氧代谢到以 EET 为基础的代谢的快速转换。这些结果凸显了它的适应能力,即利用 EET 作为一种有效的生存策略来应对快速波动的沉积物环境。这些结果为阐明缺氧-缺氧界面的代谢动态以及进一步了解沉积物中的生物地球化学循环带来了希望。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A flavin-based extracellular electron transfer strategy in a novel gram-positive microbe Microbacterium deferre sp. nov. strain A1-JK, isolated from cable bacteria enrichments
Microbacteriaceae are a class of metabolically versatile gram-positive bacteria found in diverse environments. In sediments populated with filamentous cable bacteria, electric interspecies interactions between microbes and cable bacteria have been suggested. A novel, gram-positive bacterium, Microbacterium deferre strain A1-JK was isolated from the vicinity of a cable bacterium filament, capable of extracellular electron transfer (EET) to Fe(III) oxides and electrodes. Electrochemical experiments with pure cultures of M.deferre A1-JK in three-electrode cells revealed the presence of soluble mediators diffusing through the cell wall, identified through HPLC analysis as flavins. Genomic analyses further uncovered the complete riboflavin synthesis pathway, with heightened flavin production observed under oxygen-limited conditions to facilitate EET. M. deferre A1-JK encodes the periplasmic cytochrome FccA, responsible for transferring electrons on flavin carriers. M. deferre A1-JK exhibited a fast switch from aerobic metabolism to EET-based metabolism, aside from demonstrating weak electroactivity in alkaline (pH 8-10) and saline (4% NaCl) conditions. These results underscore its adaptability to use EET as an efficient survival strategy to deal with rapidly fluctuating sediment environments. These results hold promise for elucidating metabolic dynamics at oxic-anoxic interfaces along with further understanding of biogeochemical cycling in sediments.
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