Zimmermann R, Münck E, Brill W J, Shah V K, Henzl M T, Rawlings J, Orme-Johnson W H
Biochim Biophys Acta. 1978 Dec 20;537(2):185-207. doi: 10.1016/0005-2795(78)90504-4.
Under anaerobic conditions the molybdenum-iron protein (MoFe protein) from Azotobacter vinelandii can be reversibly oxidized with thionine. Electron paramagnetic resonance studies reveal that the oxidation proceeds in two distinct phases: the MoFe protein can be oxidized by four electrons without loss of the EPR signal from the S = 3/2 cofactor centers. A second oxidation step, involving two electrons, leads to the disappearance of the cofactor EPR signal. In order to correlate the events during the thionine titration with redox reactions involving individual iron centers we have studied the MoFe proteins from A vinelandii and Clostridium pasteurianum with Mössbauer spectroscopy. Spectra were taken in the temperature range from 1.5 K to 200 K in applied magnetic fields of up to 54 kG. Analysis of the Mössbauer data allows us to draw three major conclusions: (1) the holoprotein contains 30 +/- 2 iron atoms. (2) Most probably, 12 iron atoms belong to two, apparently identical, iron clusters (labeled M) which we have shown previously to be structural components of the iron and molybdenum containing cofactor of nitrogenase. The M-centers can be stabilized in three distinct oxidation states, MOXe- in equilibrium MNe- in equilibrium MR. The diamagnetic (S = 0) state MOX is attained by oxidation of the native state MN with either thionine or oxygen. MR is observed under nitrogen fixing conditions. (3) The data strongly suggest that 16 iron atoms are associated with four iron centers which we propose to call P-clusters. Each P-cluster contains four spin-coupled iron atoms. In the native protein the P-clusters are in the diamagnetic state PN, yielding the Mössbauer signature which we have labeled previously 'components D and Fe2+'. Three irons of the D-type and one iron of the Fe2+-type appear to comprise a P-cluster. A one-electron oxidation yields the paramagnetic state POX. Although the state POX is characterized by half-integral electronic spin a peculiar combination of zero-field splitting parameters and spin relaxation renders this state EPR-silent. Spectroscopically, the P-clusters are novel structures; there is, however, evidence that they are closely related to familiar 4Fe-4S centers.
在厌氧条件下,来自棕色固氮菌的钼铁蛋白(MoFe蛋白)可被亚甲蓝可逆氧化。电子顺磁共振研究表明,氧化过程分两个不同阶段进行:MoFe蛋白可被四个电子氧化,而不会损失来自S = 3/2辅因子中心的电子顺磁共振信号。第二步氧化涉及两个电子,导致辅因子电子顺磁共振信号消失。为了将亚甲蓝滴定过程中的事件与涉及单个铁中心的氧化还原反应联系起来,我们用穆斯堡尔谱研究了来自棕色固氮菌和巴氏梭菌的MoFe蛋白。在高达54 kG的外加磁场中,在1.5 K至200 K的温度范围内采集光谱。对穆斯堡尔数据的分析使我们能够得出三个主要结论:(1)全蛋白含有30±2个铁原子。(2)很可能,12个铁原子属于两个明显相同的铁簇(标记为M),我们之前已证明它们是固氮酶含铁和钼辅因子的结构成分。M中心可以稳定在三种不同的氧化态,MOXe-处于平衡态MNe-处于平衡态MR。通过用亚甲蓝或氧气氧化天然态MN可得到抗磁性(S = 0)态MOX。在固氮条件下观察到MR。(3)数据强烈表明,16个铁原子与四个铁中心相关联,我们提议将其称为P簇。每个P簇包含四个自旋耦合的铁原子。在天然蛋白中,P簇处于抗磁性态PN,产生我们之前标记为“组分D和Fe2+”的穆斯堡尔特征。D型的三个铁原子和Fe2+型的一个铁原子似乎构成一个P簇。单电子氧化产生顺磁性态POX。尽管态POX的特征是半整数电子自旋,但零场分裂参数和自旋弛豫的特殊组合使该态在电子顺磁共振中无信号。从光谱学角度看,P簇是新颖的结构;然而,有证据表明它们与常见的4Fe-4S中心密切相关。