Basic Iron-Sulfur Centers.

Claudia Andreini, Simone Ciofi-Baffoni
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引用次数: 2

Abstract

Iron-sulfur clusters are ubiquitous protein cofactors composed of iron and inorganic sulfur. These cofactors are among the most ancient ones and may have contributed to the birth of life on Earth. Therefore, they are found even today in many enzymes central to metabolic processes like nitrogen fixation, respiration, and DNA processing and repair. Due to the toxicity associated with iron and sulfur ions, living organisms evolved dedicated machineries to synthetize and then transfer iron-sulfur clusters into client proteins. The iron-sulfur cluster (ISC) machinery is responsible for iron-sulfur cluster biogenesis in prokaryotes and in the mitochondrion of eukaryotes; the sulfur mobilization (SUF) machinery is present in prokaryotes and in the chloroplasts of plants; finally, the cytosolic iron-sulfur assembly (CIA) machinery is only present in the cytoplasm of eukaryotes. Genome analysis allowed the prediction of the proteins containing iron-sulfur clusters across a broad variety of living organisms, establishing links between the size and composition of iron-sulfur proteomes and the types of organisms that encode them. For example, the iron-sulfur proteomes of aerobes are generally smaller than those of anaerobes with similar genome size; furthermore, aerobes are enriched in [2Fe-2S] proteins compared to anaerobes, which predominantly use [4Fe-4S] proteins. This relates to the lower bioavailability of iron and the higher lability of [4Fe-4S] clusters within aerobic environments. Analogous considerations apply to humans, where the occurrence and functions of iron-sulfur proteins depend on the cellular compartment where they are localized. For example, an emerging primary role for nuclear iron-sulfur proteins is in DNA maintenance. Given their key functions in metabolism, dysfunctions of mutations in iron-sulfur proteins, or in proteins participating in iron-sulfur cluster biogenesis, are associated with serious human diseases.

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碱性铁硫中心。
铁硫簇是普遍存在的由铁和无机硫组成的蛋白质辅因子。这些辅助因素是最古老的因素之一,可能对地球上生命的诞生做出了贡献。因此,即使在今天,它们也存在于许多代谢过程的核心酶中,如固氮、呼吸和DNA加工和修复。由于铁和硫离子的毒性,生物体进化出了专门的机器来合成铁-硫簇,然后将其转移到客户蛋白中。铁硫团簇(ISC)机制在原核生物和真核生物线粒体中负责铁硫团簇的生物形成;硫动员(SUF)机制存在于原核生物和植物叶绿体中;最后,胞质铁硫组装(CIA)机制只存在于真核生物的细胞质中。基因组分析可以预测多种生物体中含有铁硫簇的蛋白质,在铁硫蛋白质组的大小和组成与编码它们的生物体类型之间建立联系。例如,在基因组大小相似的情况下,需氧菌的铁硫蛋白质组通常比厌氧菌的要小;此外,与厌氧菌相比,需氧菌富含[2Fe-2S]蛋白质,厌氧菌主要使用[4Fe-4S]蛋白质。这与铁的低生物利用度和[4Fe-4S]簇在有氧环境中的高不稳定性有关。类似的考虑也适用于人类,其中铁硫蛋白的发生和功能取决于它们所处的细胞区室。例如,核铁硫蛋白的主要作用是维持DNA。鉴于铁硫蛋白在代谢中的关键功能,铁硫蛋白突变或参与铁硫簇生物发生的蛋白质的功能失调与严重的人类疾病有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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Introduction: Transition Metals and Sulfur. Sulfur, the Versatile Non-metal. The Type 1 Blue Copper Site: From Electron Transfer to Biological Function. Purple Mixed-Valent Copper A. The Tetranuclear Copper-Sulfide Center of Nitrous Oxide Reductase.
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