Yang C Y, Meagher A, Huynh B H, Sayers D E, Theil E C
Biochemistry. 1987 Jan 27;26(2):497-503. doi: 10.1021/bi00376a023.
Ferritin is a complex of a hollow, spherical protein and a hydrous, ferric oxide core of less than or equal to 4500 iron atoms inside the apoprotein coat; the apoprotein has multiple (ca. 12) binding sites for monoatomic metal ions, e.g., Fe(II), V(IV), Tb(III), that may be important in the initiation of iron core formation. In an earlier study we observed that the oxidation of Fe(II) vacated some, but not all, of the metal-binding sites, suggesting migration of some Fe during oxidation, possibly to form nucleation clusters; some Fe(III) remained bound to the protein. Preliminary extended X-ray absorbance fine structure (EXAFS) analysis of the same Fe(III)-apoferritin complex showed an environment distinct from ferritin cores, but the data did not allow a test of the Fe cluster hypothesis. In this paper, with improved EXAFS data and with Mössbauer data on the same complex formed with 57Fe, we clearly show that the Fe(III) in the distinctive environment is polynuclear (Fe atoms with Fe-Fe = 3.5 A and TB = 7 K). Moreover, the arrangement of atoms is such that Fe(III) atoms appear to have both carboxylate-like ligands, presumably from apoferritin, and oxo bridges to the other iron atoms. Thus the protein provides sites not only for initiation but also for nucleation of the iron core. Sites commodious enough and with sufficient conserved carboxylate ligands to accommodate such a nucleus occur inside the protein coat at the subunit dimer interfaces. Such Fe(III)-apoferritin nucleation complexes can be used to study the properties of the several members of the apoferritin family.
铁蛋白是一种复合物,由一个中空的球形蛋白质和一个位于脱铁蛋白外壳内、含水的、氧化铁核心组成,该核心包含不超过4500个铁原子;脱铁蛋白具有多个(约12个)单原子金属离子(如Fe(II)、V(IV)、Tb(III))的结合位点,这些位点可能在铁芯形成的起始过程中起重要作用。在早期的一项研究中,我们观察到Fe(II)的氧化使部分但不是全部金属结合位点空出,这表明在氧化过程中一些铁发生了迁移,可能形成了成核簇;一些Fe(III)仍然与蛋白质结合。对同一Fe(III)-脱铁蛋白复合物进行的初步扩展X射线吸收精细结构(EXAFS)分析显示其环境与铁蛋白核心不同,但这些数据无法对铁簇假说进行验证。在本文中,利用改进的EXAFS数据以及关于由57Fe形成的同一复合物的穆斯堡尔数据,我们清楚地表明,处于独特环境中的Fe(III)是多核的(Fe原子之间的Fe-Fe距离为3.5埃,四极分裂为7开尔文)。此外,原子的排列方式使得Fe(III)原子似乎既有可能来自脱铁蛋白的类似羧酸盐的配体,又有与其他铁原子相连的氧桥。因此,蛋白质不仅为铁芯的起始提供了位点,也为其成核提供了位点。在亚基二聚体界面的蛋白质外壳内部存在足够宽敞且具有足够保守羧酸盐配体以容纳这样一个核的位点。这种Fe(III)-脱铁蛋白成核复合物可用于研究脱铁蛋白家族多个成员的特性。