Hanna P M, Chen Y, Chasteen N D
Department of Chemistry, University of New Hampshire, Durham 03824.
J Biol Chem. 1991 Jan 15;266(2):886-93.
In ferritin, iron is stored by oxidative deposition of the ferrous ion to form a hydrous ferric oxide mineral core. Two intermediates, formed during the initial stages of iron accumulation in apoferritin, have been observed previously in our laboratory and have been identified as a mononuclear Fe3(+)-protein complex and a mixed-valence Fe2(+)-Fe3(+)-protein complex. The physical characteristics of the mixed-valence Fe2(+)-Fe3+ complex and its relationship to the mononuclear Fe3+ complex in horse spleen apoferritin samples to which 0-240 iron atoms were added was examined by EPR spectroscopy. The results indicate that the mononuclear complex is not a precursor to the formation of the mixed-valence complex. Competitive binding studies with Cd2+, Zn2+, Tb3+, and UO2+(2) suggest that the mixed-valence complex is formed on the interior of the protein in the vicinity of the 2-fold axis of the subunit dimer. The mixed-valence complex could be generated by the partial oxidation of Fe2+ in apoferritin containing 120 Fe2+ or by the addition of up to 120 Fe2+ to ferritin already containing 18 Fe3+/protein molecule. The fact that the complex is generated during early Fe2+ oxidation suggests that it may be a key intermediate during the initial oxidative deposition of iron in the protein. The unusual EPR powder lineshape at 9.3 GHz of the mixed-valence complex was simulated with a rhombic g-tensor (gx = 1.95, gy = 1.88, gz = 1.77) and large linewidths and g-strain parameters. The presence of significant g-strain in the complex probably accounts for the failure to observe an EPR signal at 35 GHz and likely reflect considerable flexibility in the structure of the metal site. The temperature dependence of the EPR intensity in the range 8-38 K was modeled successfully by an effective spin Hamiltonian including exchange coupling (-2JS1.S2) and zero-field terms, from which an antiferromagnetic coupling of J = -4.0 +/- 0.5 cm-1 was obtained. This low value for J may reflect the presence of a mu-oxo bridge(s) in the dimer.
在铁蛋白中,铁通过亚铁离子的氧化沉积来储存,形成水合氧化铁矿物核心。在我们实验室之前已经观察到脱铁铁蛋白中铁积累初始阶段形成的两种中间体,并已鉴定为单核Fe3(+)-蛋白复合物和混合价态Fe2(+)-Fe3(+)-蛋白复合物。通过电子顺磁共振光谱法研究了添加0 - 240个铁原子的马脾脱铁铁蛋白样品中混合价态Fe2(+)-Fe3+复合物的物理特性及其与单核Fe3+复合物的关系。结果表明,单核复合物不是混合价态复合物形成的前体。用Cd2+、Zn2+、Tb3+和UO2+(2)进行的竞争性结合研究表明,混合价态复合物在亚基二聚体2重轴附近的蛋白质内部形成。混合价态复合物可以通过含有120个Fe2+的脱铁铁蛋白中Fe2+的部分氧化产生,或者通过向已经含有18个Fe3+/蛋白分子的铁蛋白中添加多达120个Fe2+产生。该复合物在早期Fe2+氧化过程中产生这一事实表明,它可能是铁在蛋白质中初始氧化沉积过程中的关键中间体。用菱形g张量(gx = 1.95,gy = 1.88,gz = 1.77)以及大的线宽和g应变参数模拟了混合价态复合物在9.3 GHz时异常的电子顺磁共振粉末线形。复合物中显著的g应变的存在可能是未能在35 GHz观察到电子顺磁共振信号的原因,并且可能反映了金属位点结构中相当大的灵活性。通过包含交换耦合(-2JS1.S2)和零场项的有效自旋哈密顿量成功模拟了8 - 38 K范围内电子顺磁共振强度的温度依赖性,由此得到反铁磁耦合J = -4.0 +/- 0.5 cm-1。J的这个低值可能反映了二聚体中存在μ-氧桥。