脱硫弧菌铁氧还蛋白中的三铁簇低温磁圆二色性研究

Andrew J. Thomson , A.Edward Robinson , Michael K. Johnson , Jose J.G. Moura , Isobel Moura , Antonio V. Xavier , Jean Legall
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引用次数: 58

摘要

来自gigas Desulphovibrio Ferredoxin II是一种含有由三个铁原子组成的新型铁硫簇的四聚体蛋白。在大约波长范围内测量了氧化和二硫代还原形式的铁氧还蛋白II的低温磁圆二色性(MCD)光谱。300 - 800 nm。两个氧化水平的团簇显示为顺磁性,尽管只有氧化形式给出EPR信号。在温度范围内建立了MCD磁化曲线。1.5 - 150k,在0 - 5.1特斯拉之间。氧化蛋白的曲线可以拟合到自旋S = 12的基态,各向同性g因子为2.01。有证据表明,在50 K以上的低洼电子态存在热居族。还原蛋白给出了一组独特的磁化曲线,暂定为S = 2的基态,主要是轴向零场畸变,使双重态Ms =±2的能量最低。零场分量的最大能量分布约为。15厘米−1。这使得轴向零场参数d的上限为4 cm−1。团簇的氧化和还原形式的MCD光谱彼此非常不同。氧化态的光谱也不同于来自Chromatium的氧化高电位铁蛋白的光谱,应该为区分最高氧化水平的四铁簇和三铁簇提供有用的标准。
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The three-iron cluster in a ferredoxin from Desulphovibrio gigas A low-temperature magnetic circular dichroism study

Ferredoxin II from Desulphovibrio gigas is a tetrameric protein containing a novel iron-sulphur cluster consisting of three iron atoms. The low-temperature magnetic circular dichroism (MCD) spectra of the oxidized and dithionite-reduced forms of ferredoxin II have been measured over the wavelength range approx. 300–800 nm. Both oxidation levels of the cluster are shown to be paramagnetic, although only the oxidized form gives an EPR signal. MCD magnetization curves have been constructed over the temperature range approx. 1.5–150 K and at fields between 0 and 5.1 Tesla. The curve for the oxidized protein can be fitted to a ground state of spin S = 12 with an isotropic g factor of 2.01. There is evidence for the thermal population of a low-lying electronic state above 50 K. The reduced protein gives a distinctive set of magnetization curves that are tentatively assigned to a ground state of S = 2, with a predominantly axial zero-field distortion that leaves the doublet Ms = ±2 lowest in energy. The zero-field components have a maximum energy spread of approx. 15 cm−1. which places an upper limit of 4 cm−1 on the axial zero-field parameter D. The MCD spectra of the oxidized and reduced forms of the cluster are quite distinctive from one another. The spectra of the oxidized state are also different from those of oxidized high-potential iron protein from Chromatium and should provide a useful criterion for distinguishing between four- and three-iron clusters in their highest oxidation levels.

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