在一个无氧甲性转化协会中对氧化还原活性细胞外聚合物质的表征
Xueqin Zhang1, Jing Zhao2, Dirk V Erler3
1Australian Centre for Water and Environmental Biotechnology, The University of Queensland, Brisbane, Queensland, Australia.
Journal of environmental management
|June 20, 2024
概括
甲 (AOM) 的无氧氧氧化使古生物产生富含蛋白质的细胞外聚合物质 (EPS). 这些EPS含有c型细胞染色体,使电子转移和减轻银毒性.
科学领域:
- 微生物学 微生物学
- 生物地质化学生物地质化学
- 环境科学 环境科学
背景情况:
- 甲无氧氧化 (AOM) 是全球碳循环中的一个关键的微生物过程.
- 厌氧甲类古生物 (ANME) 调解AOM,但它们的生理学仍然不太清楚.
- 细胞外聚合物 (EPS) 是微生物群落的关键组成部分,但它们在ANME中的作用在很大程度上是未知的.
研究的目的:
- 研究来自ANME丰富培养的EPS的生化和氧化还原活性特性.
- 阐明EPS在AOM过程中的生理作用.
- 描述ANME衍生的EPS的组成和功能组.
主要方法:
- 使用了一个由"Candidatus Methanoperedens nitroreducens"主导的财团.
- 使用福里埃变换红外光谱 (FTIR) 和X射线光电子光谱 (XPS) 进行了EPS的特征化.
- 通过血红反应性染色和光谱分析证实了EPS中c型细胞染色体的存在和功能,并使用Ag+减小试验测试了细胞外电子转移 (EET) 能力.
主要成果:
- 在ANME EPS矩阵中,蛋白质与多糖的比例很高 (~8),并且由蛋白质相关的功能组占主导地位.
- 在蛋白质丰富的EPS中确定了C型细胞染色体,赋予了电活性特性.
- 通过EPS介导的细胞外电子转移将Ag+降低到金属Ag,EPS矩阵中的纳米粒子形成减少了细胞内银的毒性.
结论:
- 这项研究提供了对无氧甲类联盟的EPS的第一个生化见解.
- 这些发现揭示了EPS在ANME中的新生理作用,特别是在细胞外电子转移和金属排毒中.
- 蛋白质主导的电活性EPS矩阵对于ANME在潜在的金属暴露环境中的生存和功能至关重要.
更多相关视频
07:31Author Spotlight: Designing Simple and Inexpensive Techniques to Grow Methane-Oxidizing Bacteria in the Laboratory
Published on: September 6, 2024
929
10:23Characterizing Mediated Extracellular Electron Transfer in Lactic Acid Bacteria with a Three-Electrode, Two-Chamber Bioelectrochemical System
Published on: August 23, 2024
749
相关概念视频
Microbial Nutrition
2.0K
Organisms exhibit remarkable metabolic diversity, categorized based on how they acquire energy and carbon. These strategies enable survival in various ecological niches and are essential for maintaining energy flow and nutrient cycling within ecosystems.Energy and Carbon SourcesOrganisms are classified as phototrophs or chemotrophs based on energy acquisition. Phototrophs use light as their energy source, while chemotrophs rely on oxidizing chemical compounds. Further differentiation arises...
2.0K
Metabolism of Chemolithotrophs
1.3K
Chemolithotrophs are microorganisms that obtain energy by oxidizing inorganic molecules such as hydrogen gas (H₂), ammonia (NH₃), reduced sulfur compounds (H₂S, S²⁻), and ferrous iron (Fe²⁺). Unlike heterotrophic organisms that rely on organic carbon, chemolithotrophs transfer electrons from these inorganic donors to the electron transport chain (ETC), generating a proton motive force (PMF) that drives ATP synthesis through oxidative phosphorylation.
1.3K
Microbial Mats
75
Microbial communities forming biofilms and mats represent complex, spatially structured ecosystems where metabolic processes are stratified according to light, oxygen, and nutrient gradients. Biofilms are initial colonization stages, only a few millimeters thick, while mature microbial mats can reach centimeter-scale thickness and display intricate vertical organization. Their structural and functional heterogeneity allows microorganisms to occupy distinct ecological niches within a few...
75
Microbes and Methanogenesis
108
Methanogenesis is a critical microbial process in anaerobic ecosystems responsible for the biological production of methane, a potent greenhouse gas and valuable biofuel. This metabolic pathway is primarily facilitated by methanogenic archaea, which thrive in anoxic environments such as wetlands, sediments, and animal gastrointestinal tracts. The absence of oxygen in these habitats prevents aerobic respiration, thereby favoring alternative biochemical pathways for organic matter degradation.In...
108
Microbes and Other Elemental Cycles
95
Microbial activity plays a pivotal role in the biogeochemical cycling of iron and manganese, especially at the redox gradients characteristic of stratified aquatic environments. These cycles are driven by microbial transformations between oxidized and reduced forms of the metals, allowing organisms to exploit them for metabolic energy and structural purposes.Iron Cycling Across Redox GradientsIn neutral, oxygen-rich surface waters, iron is predominantly found in its oxidized, insoluble ferric...
95
Deep Sea Microbial Ecology
55
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches...
55
