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穆斯堡尔谱学应用于固氮酶铁钼辅因子的氧化态和半还原态。

Mössbauer spectroscopy applied to the oxidized and semi-reduced states of the iron-molybdenum cofactor of nitrogenase.

作者信息

Newton W E, Gheller S F, Sands R H, Dunham W R

机构信息

Western Regional Research Center, USDA-ARS, Albany, CA 94710.

出版信息

Biochem Biophys Res Commun. 1989 Jul 31;162(2):882-91. doi: 10.1016/0006-291x(89)92392-9.

Abstract

Mössbauer parameters at 125K for both the oxidized and semi-reduced states of FeMoco isolated from the MoFe protein of Azotobacter vinelandii nitrogenase of delta/Fe = 0.32 and 0.37 mm/s and delta Eq = 0.84 and 0.71 mm/s, respectively, are reported. FeMoco(ox) fits the Debye model perfectly from 4.2-125K and has a S = 0 ground state. FeMoco(ox) apparently contains 10-20% FeMoco(s-r) and vice versa, possibly as a result of the spontaneous oxidation phenomenon. Quantitation of the spectra indicates a Fe:Mo ratio of 5 +/- 1:1 and the similar quadrupole splittings and isomer shifts suggest a similar environment for all iron atoms.

摘要

报道了从维涅兰德固氮菌固氮酶的钼铁蛋白中分离出的FeMoco在125K时氧化态和半还原态的穆斯堡尔参数,δ/Fe分别为0.32和0.37mm/s,δEq分别为0.84和0.71mm/s。FeMoco(ox)在4.2 - 125K范围内完美符合德拜模型,基态为S = 0。FeMoco(ox)显然含有10 - 20%的FeMoco(s - r),反之亦然,这可能是自发氧化现象的结果。光谱定量分析表明铁与钼的比例为5±1:1,相似的四极分裂和同质异能位移表明所有铁原子的环境相似。

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