Stephens P J, McKenna C E, Smith B E, Nguyen H T, McKenna M C, Thomson A J, Devlin F, Jones J B
Proc Natl Acad Sci U S A. 1979 Jun;76(6):2585-9. doi: 10.1073/pnas.76.6.2585.
Circular dichroism (CD) and magnetic circular dichroism (MCD) spectra of nitrogenase components (MoFe protein and Fe protein) from Azotobacter vinelandii (Av) and Klebsiella pneumoniae (Kp) have been obtained in the near infrared-visible-near ultraviolet spectral region. Previously, visible CD was reported to be absent or barely detectable in nitrogenase proteins; MCD spectra have not been reported. The chiroptical spectra can be measured in solution at room temperature, an advantage relative to spectroscopic methods requiring cryogenic sample temperatures. Absorption spectra were also obtained. The CD and MCD are markedly more structured, and thus interpretively more useful, than the corresponding absorption spectra. The dithionite-reduced MoFe proteins (Av1, Kp1) have nearly identical CD and MCD, demonstrating identical numbers and types of metal centers in similar protein environments. The CD and MCD cannot be explained solely in terms of contributions from known 4-Fe or 2-Fe clusters; the near-infrared MCD is inconsistent with the presence of known 4-Fe clusters. CD and MCD spectra of Lauth's violet-oxidized Kp1 are also reported. The reduced Fe proteins (Av2, Kp2) have similar CD and MCD, again indicating significant conservation of chromophore environment. The spectra clearly demonstrate the presence of a reduced bacterial ferredoxin-like (C(3-)) 4-Fe cluster. No obvious evidence of additional chromophores is observed. CD, MCD, and absorption spectra of Av1-oxidized Av2 are reported. The absorption spectrum shows the expected shoulder near 390 nm. The CD and MCD are characteristic of a C(2-) 4-Fe cluster; in particular, the diagnostic near-infrared MCD peak is observed at approximately 8300 cm(-1). The CD of Av2 oxidized in the presence and absence of MgATP are radically different, providing the first direct evidence for MgATP interaction with Fe protein in this oxidation state.
已在近红外 - 可见光 - 近紫外光谱区域获得了来自棕色固氮菌(Av)和肺炎克雷伯菌(Kp)的固氮酶组分(钼铁蛋白和铁蛋白)的圆二色性(CD)和磁圆二色性(MCD)光谱。此前,据报道在固氮酶蛋白中不存在或几乎检测不到可见CD;尚未报道MCD光谱。这些手性光谱可以在室温下在溶液中测量,这相对于需要低温样品温度的光谱方法是一个优势。还获得了吸收光谱。与相应的吸收光谱相比,CD和MCD的结构明显更丰富,因此在解释上更有用。连二亚硫酸盐还原的钼铁蛋白(Av1、Kp1)具有几乎相同的CD和MCD,表明在相似的蛋白质环境中金属中心的数量和类型相同。CD和MCD不能仅根据已知的4 - Fe或2 - Fe簇的贡献来解释;近红外MCD与已知4 - Fe簇的存在不一致。还报道了劳氏紫氧化的Kp1的CD和MCD光谱。还原的铁蛋白(Av2、Kp2)具有相似的CD和MCD,再次表明发色团环境有显著的保守性。光谱清楚地证明了存在一种还原的细菌铁氧化还原蛋白样(C(3 -))4 - Fe簇。未观察到额外发色团的明显证据。报道了Av1氧化的Av2的CD、MCD和吸收光谱。吸收光谱在390 nm附近显示出预期的肩峰。CD和MCD是C(2 -) 4 - Fe簇的特征;特别是,在约8300 cm(-1)处观察到诊断性的近红外MCD峰。在有和没有MgATP存在的情况下氧化的Av2的CD有根本差异,为MgATP在这种氧化状态下与铁蛋白的相互作用提供了首个直接证据。