Morgan T V, Stephens P J, Devlin F, Stout C D, Melis K A, Burgess B K
Proc Natl Acad Sci U S A. 1984 Apr;81(7):1931-5. doi: 10.1073/pnas.81.7.1931.
The Fe(CN)3-(6) oxidation of the crystallographically characterized [[3Fe-3S], [4Fe-4S]] ferredoxin I of Azotobacter vinelandii has been studied using absorption, circular dichroism, magnetic circular dichroism, and EPR spectroscopies. A paramagnetic intermediate is observed en route to Fe-S cluster-free apoprotein, possessing an anisotropic g approximately equal to 2 EPR signal, surviving to temperatures greater than 77 K. This species is shown to result from 3-electron oxidation of the [4Fe-4S] cluster, without modification of the [3Fe-3S] cluster. However, it does not give rise to observable paramagnetic magnetic circular dichroism in the visible-near UV spectral region and is therefore neither an oxidized HIPIP [4Fe-4S] cluster nor an oxidized [3Fe-3S] cluster. We identify the paramagnetic species as a cysteinyldisulfide radical formed on dissociation of an oxidized cysteinate and an oxidized sulfide ion from the [4Fe-4S] cluster. This conclusion is consistent with the observed reaction stoichiometry, the spectroscopic results obtained, known EPR spectra of disulfide radicals, and the reconstitution of the native [4Fe-4S] cluster by dithiothreitol alone. This reaction, earlier interpreted as a HIPIP-type oxidation, is a previously uncharacterized oxidation reaction of [4Fe-4S] clusters.
利用吸收光谱、圆二色光谱、磁圆二色光谱和电子顺磁共振光谱,对维涅兰德固氮菌晶体学表征的[[3Fe-3S],[4Fe-4S]]铁氧化还原蛋白I的Fe(CN)3-(6)氧化过程进行了研究。在生成无铁硫簇脱辅基蛋白的过程中观察到一种顺磁性中间体,其具有各向异性g约等于2的电子顺磁共振信号,在高于77 K的温度下仍存在。该物种是由[4Fe-4S]簇的3电子氧化产生的,[3Fe-3S]簇未发生改变。然而,它在可见-近紫外光谱区域没有产生可观测的顺磁性磁圆二色性,因此既不是氧化型高电位铁硫蛋白[4Fe-4S]簇,也不是氧化型[3Fe-3S]簇。我们将这种顺磁性物种鉴定为在一个氧化型半胱氨酸盐和一个氧化型硫离子从[4Fe-4S]簇解离时形成的半胱氨酰二硫自由基。这一结论与观察到的反应化学计量、获得的光谱结果、已知的二硫自由基电子顺磁共振光谱以及仅用二硫苏糖醇重建天然[4Fe-4S]簇相一致。该反应早期被解释为高电位铁硫蛋白型氧化,是一种以前未被表征的[4Fe-4S]簇氧化反应。