Cheng Y G, Chasteen N D
Department of Chemistry, University of New Hampshire, Durham 03824.
Biochemistry. 1991 Mar 19;30(11):2947-53. doi: 10.1021/bi00225a031.
Ferritins from microorganisms to man are known to contain varying amounts of phosphate which has a pronounced effect on the structural and magnetic properties of their iron mineral cores. The present study was undertaken to gain insight into the role of phosphate in the early stages of iron accumulation by ferritin. The influence of phosphate on the initial deposition of iron in apoferritin (12 Fe/protein) was investigated by EPR, 57Fe Mössbauer spectroscopy, and equilibrium dialysis. The results indicate that phosphate has a significant influence on iron deposition. The presence of 1 mM phosphate during reconstitution of ferritin from apoferritin, Fe(II), and O2 accelerates the rate of oxidation of the iron 2-fold at pH 7.5. In the presence or absence of phosphate, the rate of oxidation at 0 degrees C follows simple first-order kinetics with respect to Fe(II) with half-lives of 1.5 +/- 0.3 or 2.8 +/- 0.2 min, respectively, consistent with a single pathway for iron oxidation when low levels of iron are added to the apoprotein. This pathway may involve a protein ferroxidase site where phosphate may bind iron(II), shifting its redox potential to a more negative value and thus facilitating its oxidation. Following oxidation, an intermediate mononuclear Fe(III)-protein complex is formed which exhibits a transient EPR signal at g' = 4.3. Phosphate accelerates the rate of decay of the signal by a factor of 3-4, producing EPR-silent oligonuclear or polynuclear Fe(III) clusters. In 0.5 mM Pi, the signal decays according to a single phase first-order process with a half-life near 1 min.(ABSTRACT TRUNCATED AT 250 WORDS)
从微生物到人类的铁蛋白都含有不同量的磷酸盐,这些磷酸盐对其铁矿物核心的结构和磁性有着显著影响。本研究旨在深入了解磷酸盐在铁蛋白铁积累早期阶段的作用。通过电子顺磁共振(EPR)、57Fe穆斯堡尔光谱和平衡透析研究了磷酸盐对脱铁铁蛋白(12个铁/蛋白)中铁初始沉积的影响。结果表明磷酸盐对铁沉积有显著影响。在由脱铁铁蛋白、Fe(II)和O2重构铁蛋白的过程中,1 mM磷酸盐的存在使铁在pH 7.5时的氧化速率加快了2倍。无论有无磷酸盐,0℃时的氧化速率相对于Fe(II)都遵循简单的一级动力学,半衰期分别为1.5±0.3分钟或2.8±0.2分钟,这与向脱辅基蛋白中添加低水平铁时铁氧化的单一途径一致。该途径可能涉及一个蛋白质铁氧化酶位点,磷酸盐可能在此结合铁(II),将其氧化还原电位转移到更负的值,从而促进其氧化。氧化后,形成一种中间单核Fe(III)-蛋白质复合物,在g' = 4.3处呈现瞬态EPR信号。磷酸盐使信号衰减速率加快3-4倍,产生EPR沉默的寡核或多核Fe(III)簇。在0.5 mM Pi中,信号根据单相一级过程衰减,半衰期接近1分钟。(摘要截短于250字)