Münck E, Rhodes H, Orme-Johnson W H, Davis L C, Brill W J, Shah V K
Biochim Biophys Acta. 1975 Jul 21;400(1):32-53. doi: 10.1016/0005-2795(75)90124-5.
We have studied the molybdenum-iron protein (MoFe protein, also known as component I) from Azobacter vinelandi using Mössbauer spectroscopy and electron paramagnetic resonance on samples enriched with 57Fe. These spectra can be interpreted in terms of two EPR active centers, each of which is reducible by one electron. A total of four different chemical environments of Fe can be discerned. One of them is a cluster of Fe atoms with a net electronic spin of 3/2, one of them is high-spin ferrous iron and the remaining two are iron in a reduced state (probably in clusters). The results are as follows: Chemical analysis yields 11.5 Fe atoms and 12.5 labile sulfur atoms per molybdenum atom; the molecule contains two Mo atoms per 300 000 daltons. The EPR spectrum of the MoFe protein exhibits g values at 4.32, 3.65 and 2.01, associated with the ground state doublet of a S = 3/2 spin system. The spin Hamiltonian H = D(S2/z minus 5/4 + lambda(S2/x minus S2/y)) + gbeta/o S-H fits the experimental data for go = 2.00 and lambda = 0.055. Quantitative analysis of the temperature dependence of the EPR spectrum yields D/k = 7.5 degrees K and 0.91 spins/molybdenum atom, which suggests that the MoFe protein has two EPR active centers. Quantitative evaluation of Mössbauer spectra shows that approximately 8 iron atoms give rise to one quadrupole doublet; at lower temperatures magnetic spectra, associated with the groud electronic doublet, are observed; at least two magnetically inequivalent sites can be distinguished. Taken together the data suggest that each EPR center contains 4 iron atoms. The EPR and Mössbauer data can only be reconciled if these iron atoms reside in a spin-coupled (S = 3/2) cluster. Under nitrogen fixing conditions the magnetic Mössbauer spectra disappeared concurrently with the EPR signal and quadrupole doublets are obserced at all temperatures. The data suggest that each EPR active center is reduced by one electron. The Mössbauer investigation reveals three other spectral components characteristic of iron nuclei in an environment of integer or zero electronic spin, i.e. they reside in complexes which are "EPR-silent". One of the components (3-4 iron atoms) has Mössbauer parameters characteristic of the high-spin ferrous iron as in reduced ruberdoxin. However, measurements in strong fields indicate a diamagnetic environment. Another component, representing 9-11 iron atoms, seems to be diamagnetic also. It is suggested that these atoms are incorporated in spin-coupled clusters.
我们使用穆斯堡尔谱和电子顺磁共振技术,对富含(^{57}Fe)的维涅兰德固氮菌钼铁蛋白(MoFe蛋白,也称为组分I)进行了研究。这些谱图可以用两个EPR活性中心来解释,每个中心都可以被一个电子还原。总共可以分辨出四种不同的铁化学环境。其中一种是净电子自旋为(3/2)的铁原子簇,一种是高自旋亚铁,其余两种是还原态的铁(可能在簇中)。结果如下:化学分析表明,每摩尔钼原子含有(11.5)个铁原子和(12.5)个不稳定硫原子;该分子每(300000)道尔顿含有两个钼原子。MoFe蛋白的EPR谱在(4.32)、(3.65)和(2.01)处出现(g)值,与(S = 3/2)自旋系统的基态双重态相关。自旋哈密顿量(H = D(S^2/z - 5/4 + \lambda(S^2/x - S^2/y)) + g\beta/o S - H)在(g_0 = 2.00)和(\lambda = 0.055)时符合实验数据。对EPR谱温度依赖性的定量分析得出(D/k = 7.5)开尔文和(0.91)自旋/钼原子,这表明MoFe蛋白有两个EPR活性中心。穆斯堡尔谱的定量评估表明,大约8个铁原子产生一个四极双重态;在较低温度下观察到与基态电子双重态相关的磁谱;至少可以区分出两个磁不等价的位点。综合这些数据表明,每个EPR中心含有4个铁原子。只有当这些铁原子存在于自旋耦合((S = 3/2))簇中时,EPR和穆斯堡尔数据才能相互协调。在固氮条件下,磁性穆斯堡尔谱与EPR信号同时消失,并且在所有温度下都观察到四极双重态。数据表明,每个EPR活性中心被一个电子还原。穆斯堡尔研究揭示了另外三个光谱成分,它们是整数或零电子自旋环境中铁核的特征,即它们存在于“EPR沉默”的配合物中。其中一个成分(3 - 4个铁原子)具有与还原型红氧还蛋白中高自旋亚铁相同的穆斯堡尔参数。然而,在强场中的测量表明是抗磁环境。另一个成分代表9 - 11个铁原子,似乎也是抗磁的。有人认为这些原子被纳入自旋耦合簇中。