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首页> 外文期刊>Frontiers in Microbiology >Aerobic Lineage of the Oxidative Stress Response Protein Rubrerythrin Emerged in an Ancient Microaerobic, (Hyper)Thermophilic Environment
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Aerobic Lineage of the Oxidative Stress Response Protein Rubrerythrin Emerged in an Ancient Microaerobic, (Hyper)Thermophilic Environment

机译:古代微好氧(超)嗜热环境中产生的氧化应激反应蛋白赤藓红的有氧谱系

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Rubrerythrins (RBRs) are non-heme di-iron proteins belonging to the ferritin-like superfamily. They are involved in oxidative stress defense as peroxide scavengers in a wide range of organisms. The vast majority of RBRs, including classical forms of this protein, contain a C-terminal rubredoxin-like domain involved in electron transport that is used during catalysis in anaerobic conditions. Rubredoxin is an ancient and large protein family of short length (<100 residues) that contains a Fe-S center involved in electron transfer. However, functional forms of the enzyme lacking the rubredoxin-like domain have been reported (e.g., sulerythrin and ferriperoxin). In this study, phylogenomic evidence is presented that suggests that a complete lineage of rubrerythrins, lacking the rubredoxin-like domain, arose in an ancient microaerobic and (hyper)thermophilic environments in the ancestors of the Archaea Thermoproteales and Sulfolobales. This lineage (termed the “aerobic-type” lineage) subsequently evolved to become adapted to environments with progressively lower temperatures and higher oxygen concentrations via the acquisition of two co-localized genes, termed DUF3501 and RFO, encoding a conserved protein of unknown function and a predicted Fe-S oxidoreductase, respectively. Proposed Horizontal Gene Transfer events from these archaeal ancestors to Bacteria expanded the opportunities for further evolution of this RBR including adaption to lower temperatures. The second lineage (termed the cyanobacterial lineage) is proposed to have evolved in cyanobacterial ancestors, maybe in direct response to the production of oxygen via oxygenic photosynthesis during the Great Oxygen Event (GOE). It is hypothesized that both lineages of RBR emerged in a largely anaerobic world with “whiffs” of oxygen and that their subsequent independent evolutionary trajectories allowed microorganisms to transition from this anaerobic world to an aerobic one.
机译:赤霉素(RBR)是属于类铁蛋白超家族的非血红素二铁蛋白。它们作为多种生物中的过氧化物清除剂,参与了氧化应激防御。绝大多数RBR,包括该蛋白的经典形式,都包含一个涉及电子传输的C端氧化还原蛋白样结构域,该结构在厌氧条件下的催化过程中使用。 Rubredoxin是一个古老而又庞大的蛋白质家族,具有较短的长度(<100个残基),其中包含一个涉及电子转移的Fe-S中心。然而,已经报道了缺乏红氧还蛋白样结构域的酶的功能形式(例如,磺胺草胺和铁力霉素)。在这项研究中,提供了系统生物学证据,表明在古细菌和古细菌的先祖中,在古老的微需氧和(超)嗜热环境中,出现了缺少类氧化还原酶样结构域的完整的赤藓红素谱系。该谱系(称为“有氧型”谱系)随后演变为通过获取两个共同定位的基因DUF3501和RFO来适应温度逐渐降低和氧气浓度较高的环境,这两个基因编码了功能未知的保守蛋白,并且预测的Fe-S氧化还原酶。拟议的从这些古细菌祖先到细菌的水平基因转移事件扩大了该RBR进一步进化的机会,包括适应较低的温度。有人提出第二种谱系(称为蓝细菌谱系)已经在蓝细菌祖先中进化,可能直接响应了大氧气事件(GOE)期间通过光合作用产生的氧气。据推测,RBR的两个谱系都在一个带有氧气“鞭子”的很大程度上厌氧的世界中出现,并且它们随后独立的进化轨迹使微生物从该厌氧世界过渡到有氧世界。

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