Ford G C, Harrison P M, Rice D W, Smith J M, Treffry A, White J L, Yariv J
Philos Trans R Soc Lond B Biol Sci. 1984 Feb 13;304(1121):551-65. doi: 10.1098/rstb.1984.0046.
Although essential for most forms of life, too much iron is harmful. To cope with these antagonistic phenomena an iron-storage molecule, ferritin, has evolved. The structure of horse spleen apoferritin, which has recently been refined, consists of 24 symmetrically related subunits forming a near-spherical hollow shell. In ferritin the central cavity is occupied by an iron core of 'ferrihydrite', a geologically ephemeral mineral found in hot or cold springs and in mine workings, or produced in the laboratory by heating solutions of ferric salts. Ferritin itself forms most readily from apoferritin, in the presence of dioxygen, from FeII, not FeIII. Access to its interior is through small intersubunit channels, and the protein influences both the rate of FeII-oxidation and the form of oxide produced.
尽管铁对大多数生命形式至关重要,但铁过量是有害的。为了应对这些相互矛盾的现象,一种铁储存分子——铁蛋白应运而生。马脾脱铁铁蛋白的结构最近得到了优化,它由24个对称相关的亚基组成,形成一个近球形的中空壳。在铁蛋白中,中央腔被“水铁矿”的铁芯占据,水铁矿是一种在温泉或冷泉、矿井中发现的地质上短暂存在的矿物,或者在实验室中通过加热铁盐溶液产生。铁蛋白本身最容易在有氧的情况下由脱铁铁蛋白从亚铁离子(FeII)而非铁离子(FeIII)形成。进入其内部是通过亚基间的小通道,并且该蛋白质既影响亚铁离子氧化的速率,也影响所产生氧化物的形式。