Gálvez Natividad, Fernández Belén, Sánchez Purificación, Cuesta Rafael, Ceolín Marcelo, Clemente-León Miguel, Trasobares Susana, López-Haro Miguel, Calvino Jose J, Stéphan Odile, Domínguez-Vera José M
Departamento de Química Inorgánica, Universidad de Granada, 18071 Granada, Spain.
J Am Chem Soc. 2008 Jun 25;130(25):8062-8. doi: 10.1021/ja800492z. Epub 2008 May 29.
Transmission Electron Microscopy (TEM), X-ray Absorption Near Edge Spectroscopy (XANES), Electron Energy-Loss Spectroscopy (EELS), Small-Angle X-ray Scattering (SAXS), and SQUID magnetic studies were performed in a batch of horse spleen ferritins from which iron had been gradually removed, yielding samples containing 2200, 1200, 500, and 200 iron atoms. Taken together, findings obtained demonstrate that the ferritin iron core consists of a polyphasic structure (ferrihydrite, magnetite, hematite) and that the proportion of phases is modified by iron removal. Thus, the relative amount of magnetite in ferritin containing 2200 to 200 iron atoms rose steadily from approximately 20% to approximately 70% whereas the percentage of ferrihydrite fell from approximately 60% to approximately 20%. These results indicate a ferrihydrite-magnetite core-shell structure. It was also found that the magnetite in the ferritin iron core is not a source of free toxic ferrous iron, as previously believed. Therefore, the presence of magnetite in the ferritin cores of patients with Alzheimer's disease is not a cause of their increased brain iron(II) concentration.
对一批已逐渐去除铁的马脾铁蛋白进行了透射电子显微镜(TEM)、X射线吸收近边光谱(XANES)、电子能量损失光谱(EELS)、小角X射线散射(SAXS)和超导量子干涉仪(SQUID)磁性研究,得到了分别含有2200、1200、500和200个铁原子的样品。综合来看,所获得的研究结果表明,铁蛋白的铁芯由多相结构(水铁矿、磁铁矿、赤铁矿)组成,并且各相的比例会因铁的去除而改变。因此,在含有2200至200个铁原子的铁蛋白中,磁铁矿的相对含量从约20%稳步上升至约70%,而水铁矿的百分比则从约60%降至约20%。这些结果表明存在水铁矿-磁铁矿的核壳结构。还发现,铁蛋白铁芯中的磁铁矿并非如先前认为的那样是游离有毒亚铁的来源。因此,阿尔茨海默病患者铁蛋白铁芯中磁铁矿的存在并非其脑内铁(II)浓度升高的原因。