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使用核磁共振弛豫测量法在脑铁蛋白中寻找生物源磁铁矿。

Looking for biogenic magnetite in brain ferritin using NMR relaxometry.

作者信息

Gossuin Yves, Hautot Dimitri, Muller Robert N, Pankhurst Quentin, Dobson Jon, Morris Chris, Gillis Pierre, Collingwood Joanna

机构信息

Biological Physics Department, University of Mons-Hainaut, Mons, Belgium.

出版信息

NMR Biomed. 2005 Nov;18(7):469-72. doi: 10.1002/nbm.983.

Abstract

Mammalian cellular iron is stored inside the multisubunit protein ferritin, normally taking the structure of a ferrihydrite-like mineral core. It has been suggested that biogenic magnetite, which has been detected in the brain and may be related to neurodegenerative diseases such as Alzheimer's and Parkinson's diseases, could initially form in ferritin. Indeed, as ferritin is present in the brain, the ferrihydrite core could be a precursor for biogenic magnetite formation--particularly in cases where the normal functioning of the ferritin protein is disrupted. In this work, NMR relaxometry was used to detect magnetite inside samples of ferritin extracted from normal and Alzheimer-diseased brains. The method was first calibrated with different fractions of horse spleen ferritin and synthetic magnetite particles. The relaxometry results suggest that the proportion of iron contained in brain ferritin in the form of well-crystallized magnetite instead of ferrihydrite must be <1%, which is much less than that reported for 'magnetite-like' phase in recent transmission electron microscopy studies of similar samples. Consequently, the magnetization of this 'magnetite-like' phase must be very low compared with that of magnetite.

摘要

哺乳动物细胞内的铁储存在多亚基蛋白铁蛋白中,通常呈类水铁矿矿物核心的结构。有人提出,在大脑中检测到的、可能与阿尔茨海默病和帕金森病等神经退行性疾病有关的生物源磁铁矿,最初可能在铁蛋白中形成。事实上,由于铁蛋白存在于大脑中,水铁矿核心可能是生物源磁铁矿形成的前体——特别是在铁蛋白正常功能受到破坏的情况下。在这项研究中,核磁共振弛豫测量法被用于检测从正常大脑和患阿尔茨海默病的大脑中提取的铁蛋白样品中的磁铁矿。该方法首先用不同比例的马脾铁蛋白和合成磁铁矿颗粒进行校准。弛豫测量结果表明,大脑铁蛋白中以结晶良好的磁铁矿而非水铁矿形式存在的铁的比例必须小于1%,这比最近对类似样品进行的透射电子显微镜研究中报道的“类磁铁矿”相的比例要低得多。因此,与磁铁矿相比,这种“类磁铁矿”相的磁化强度必然非常低。

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