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Living. with Iron (and Oxygen): Questions and Answers about Iron Homeostasis

机译:活的。与铁(和氧气)有关:铁稳态的问答

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Mechanisms to regulate iron homeostasis are very likely billions of years older than those for oxygen homeostasis since contemporary microbes regulate iron in the absence of oxygen and may model ancient organisms that lived before atmospheric oxygen appeared.1 Moreover, proteins that manage iron and oxidants such as the mini-ferritins in contemporary bacteria, also called Dps (DNA protection during stress) proteins, are expressed in anaerobic archea.2 Mini-ferritins are 12 subunit protein cages from archea and bacteria that contrast with maxi-ferritins, the 24 subunit cages from bacteria, animals and plants, which use iron and dioxygen as substrates, by consuming iron and hydrogen peroxide as substrates to make the mineral inside protein nanocages. Such peroxide-consuming ferritins may be progenitors of modern ferritins and may have contributed to the transition from anaerobic to aerobic life with iron and oxygen.
机译:调节铁稳态的机制很可能比氧气稳态机制早数十亿年,因为现代微生物在没有氧气的情况下调节铁,并且可以模拟在大气中氧气出现之前就已经存在的古代生物。1此外,控制铁和氧化剂的蛋白质例如厌氧古细菌中表达了当代细菌中的微型铁蛋白,也称为Dps(应激时的DNA保护)蛋白。2微型铁蛋白是古细菌和细菌中的12个亚基蛋白笼,与maxi-铁蛋白(来自24个亚基笼)形成对比以铁和双氧为底物的细菌,动植物,通过消耗铁和过氧化氢作为底物来制造蛋白质纳米笼中的矿物质。此类消耗过氧化物的铁蛋白可能是现代铁蛋白的祖先,并且可能有助于利用铁和氧从无氧生命过渡到有氧生命。

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