Yang C Y, Bryan A M, Theil E C, Sayers D E, Bowen L H
J Inorg Biochem. 1986 Dec;28(4):393-405. doi: 10.1016/0162-0134(86)80025-3.
Variations in the turnover of storage iron have been attributed to differences in apoferritin and in the cytoplasm but rarely to differences in the structure of the iron core (except size). To explore the idea that the iron environment in soluble iron complexes could vary, we compared horse spleen ferritin to pharmaceutically important model complexes of hydrous ferric oxide formed from FeCl3 and dextran (Imferon) or chondroitin sulfate (Blutal), using x-ray absorption (EXAFS) and Mössbauer spectroscopy. The results show that the iron in the chondroitin sulfate complex was more ordered than in either horse spleen ferritin or the dextran complex (EXAFS), with two magnetic environments (Mössbauer), one (80%-85%) like Fe2O3 X nH2O (ferritinlike) and one (15%-20%) like Fe2O3 (hematite); since sulfate promotes the formation of inorganic hematite, the sulfate in the chondroitin sulfate most likely nucleated Fe2O3 and hydroxyl/carboxyls, which are ligands common to chondroitin sulfate, ferritin and dextran most likely nucleated Fe2O3 X nH2O. Differences in the structure of the iron complexed with chondroitin sulfate or dextran coincide with altered rates of iron release in vivo and in vitro and provide the first example relating function to local iron structure. Differences might also occur among ferritins in vivo, depending on the apoferritin (variations in anion-binding sites) or the cytoplasm (anion concentration).
储存铁周转率的变化归因于脱铁铁蛋白和细胞质的差异,但很少归因于铁芯结构的差异(除了大小)。为了探究可溶性铁络合物中铁环境可能存在差异的观点,我们使用X射线吸收(EXAFS)和穆斯堡尔光谱,将马脾铁蛋白与由FeCl3和右旋糖酐(Imferon)或硫酸软骨素(Blutal)形成的具有药学重要性的水合氧化铁模型络合物进行了比较。结果表明,硫酸软骨素络合物中的铁比马脾铁蛋白或右旋糖酐络合物中的铁更有序(EXAFS),具有两种磁性环境(穆斯堡尔),一种(80%-85%)类似于Fe2O3·nH2O(铁蛋白样),一种(15%-20%)类似于Fe2O3(赤铁矿);由于硫酸促进无机赤铁矿的形成,硫酸软骨素中的硫酸很可能使Fe2O3成核,而羟基/羧基是硫酸软骨素、铁蛋白和右旋糖酐共有的配体,很可能使Fe2O3·nH2O成核。与硫酸软骨素或右旋糖酐络合的铁的结构差异与体内外铁释放速率的改变相一致,并提供了第一个将功能与局部铁结构联系起来的例子。体内铁蛋白之间也可能存在差异,这取决于脱铁铁蛋白(阴离子结合位点的变化)或细胞质(阴离子浓度)。