Nagai M, Kaminaka S, Ohba Y, Nagai Y, Mizutani Y, Kitagawa T
Biological Laboratory, Kanazawa University School of Allied Medical Professions, Japan.
J Biol Chem. 1995 Jan 27;270(4):1636-42. doi: 10.1074/jbc.270.4.1636.
Environmental changes of tyrosine and tryptophan residues of hemoglobin (Hb) upon its T to R transition of quaternary structure were investigated with ultraviolet resonance Raman (UVRR) spectroscopy excited at 235 nm. DeoxyHb A (T-form) showed a UVRR spectrum distinctly different from those of the ligated Hbs (R-form) including oxyHb, COHb, and metHb A, whereas the ligated Hbs exhibited similar UVRR spectra irrespective of the ligand species and the oxidation state of the heme. To characterize the spectral change of Trp-beta 37 at the alpha 1 beta 2 interface due to the quaternary structure transition, the UVRR spectra of Hb A were compared with the corresponding spectra of Hb Hirose (Trp-beta 37-->Ser). A difference spectrum between deoxyHb A and deoxyHb Hirose showed only Trp resonance Raman (RR) bands, which were reasonably ascribed to Trp-beta 37 in deoxyHb A. RR bands at 873 cm-1 (W17) and at 1360 and 1343 cm-1 (W7, Fermi doublet) indicated that the indole ring of Trp-beta 37 in deoxyHb A formed a strong hydrogen bond at the N1H site in hydrophobic environments. Tyr residues in deoxyHb Hirose seemed to be in the same environments as those of deoxyHb A. In contrast, the difference spectrum between Hb A and Hb Hirose in the ligated state displayed peaks for RR bands of both Trp and Tyr. The difference spectra were unaltered by the addition of 5 mM inositol hexaphosphate. This means that the differences were not caused by the tetramer to dimer dissociation but by a conformation change within a tetramer. Comparison of the Hb A-Hb Hirose difference spectra in the oxy and deoxy states revealed that the oxygenation-induced changes of Trp RR bands arose mostly from Trp-beta 37 with the small portion of remaining changes coming from Trp-beta 15, demonstrating that Trp-beta 37 plays a pivotal role in the quaternary structural change in Hb A.
利用在235nm激发的紫外共振拉曼(UVRR)光谱研究了血红蛋白(Hb)从四级结构的T态向R态转变时酪氨酸和色氨酸残基的环境变化。脱氧Hb A(T态)的UVRR光谱与包括氧合Hb、一氧化碳Hb和高铁Hb A在内的结合态Hb(R态)的光谱明显不同,而结合态Hb无论配体种类和血红素的氧化态如何,都表现出相似的UVRR光谱。为了表征由于四级结构转变导致的α1β2界面处Trp-β37的光谱变化,将Hb A的UVRR光谱与Hb Hirose(Trp-β37→Ser)的相应光谱进行了比较。脱氧Hb A和脱氧Hb Hirose之间的差谱仅显示色氨酸共振拉曼(RR)带,这些带合理地归因于脱氧Hb A中的Trp-β37。873cm-1(W17)以及1360和1343cm-1(W7,费米双峰)处的RR带表明,脱氧Hb A中Trp-β37的吲哚环在疏水环境中的N1H位点形成了强氢键。脱氧Hb Hirose中的酪氨酸残基似乎与脱氧Hb A处于相同的环境中。相反,结合态下Hb A和Hb Hirose之间的差谱显示出色氨酸和酪氨酸的RR带的峰。加入5mM肌醇六磷酸后,差谱没有改变。这意味着差异不是由四聚体向二聚体的解离引起的,而是由四聚体内的构象变化引起的。氧合和脱氧状态下Hb A-Hb Hirose差谱的比较表明,氧合诱导的色氨酸RR带变化主要来自Trp-β37,其余小部分变化来自Trp-β15,这表明Trp-β37在Hb A的四级结构变化中起关键作用。