Paleomagnetism and Geochronology Laboratory, Key Laboratory of the Earth's Deep Interior, Institute of Geology and Geophysics, Chinese Academy of Sciences, 100029, Beijing, People's Republic of China.
Biometals. 2012 Feb;25(1):193-202. doi: 10.1007/s10534-011-9497-3. Epub 2011 Oct 22.
Ferritin is not only important for iron storage and detoxification in living organisms, but a multifunctional size-constrained nanoplatform for biomimetic nanoparticles. In order to tailor the biomimetic nanoparticles for future applications, it is essential to investigate the effects of external factors such as temperature on the particle size and structure of reconstituted cores in ferritin. In this study, we systematically investigated the mineral composition, crystallinity, and particle size of human H-ferritin (HuHF) reconstituted at four different temperatures (25, 30, 37, and 42°C) by integrated magnetic and transmission electron microscopy analyses. Our results showed that the particle size of reconstituted ferrihydrite cores (~5 nm) in HuHF was temperature-independent. However, the significant changes of the induced magnetization at 5 T field (M(5T)) and remanent magnetization (M(r)) at 5 K clearly showed that the crystallinity of reconstituted cores increased with increasing temperature, indicating that the reaction temperature deeply affects the structural order of reconstituted ferrihydrite cores rather than the particle size, and the reconstituted cores become more ordered at higher reaction temperatures. Our findings provide useful insights into biomineralization of ferritin under in vivo fever condition as well as in biomimetic synthesis of nanomaterials using ferritin. Furthermore, the rock magnetic methods should be very useful approaches for characterizing finite ferritin nanoparticles.
铁蛋白不仅对生物体内的铁储存和解毒很重要,而且还是仿生纳米颗粒的多功能尺寸受限纳米平台。为了定制适合未来应用的仿生纳米颗粒,研究外部因素(如温度)对铁蛋白中再构成核心的粒径和结构的影响至关重要。在这项研究中,我们通过综合磁性和透射电子显微镜分析,系统地研究了在四个不同温度(25、30、37 和 42°C)下重新构成的人 H 铁蛋白(HuHF)的矿物组成、结晶度和粒径。我们的结果表明,再构成的水铁矿核心(~5nm)的粒径与温度无关。然而,在 5T 磁场下诱导磁化强度(M(5T))和在 5K 时的剩余磁化强度(M(r))的显著变化清楚地表明,再构成核心的结晶度随温度升高而增加,这表明反应温度对再构成水铁矿核心的结构有序性有很大影响,而不是粒径,并且在较高的反应温度下,再构成的核心变得更加有序。我们的发现为体内发热条件下的铁蛋白生物矿化以及使用铁蛋白仿生合成纳米材料提供了有用的见解。此外,岩石磁学方法应该是表征有限铁蛋白纳米颗粒的非常有用的方法。