Makino R, Uno T, Nishimura Y, Iizuka T, Tsuboi M, Ishimura Y
J Biol Chem. 1986 Jun 25;261(18):8376-82.
Resonance Raman investigations on compound II of native, diacetyldeuteroheme-, and manganese-substituted horseradish peroxidase (isozyme C) revealed that the metal-oxygen linkage in the compound differed from one another in its bond strength and/or structure. Fe(IV) = O stretching frequency for compound II of native enzyme was pH sensitive, giving the Raman line at 772 and 789 cm-1 at pH 7 and 10, respectively. The results confirmed the presence of a hydrogen bond between the oxo-ligand and a nearby amino acid residue (Sitter, A. J., Reczek, C. M., and Terner, J. (1985) J. Biol. Chem. 260, 7515-7522). The Fe(IV) = O stretch for compound II of diacetylheme-enzyme was located at 781 cm-1 at pH 7 which was 9 cm-1 higher than that of native enzyme compound II. At pH 10, however, the Fe(IV) = O stretch was found at 790 cm-1, essentially the same frequency as that of native enzyme compound II. The pK value for the pH transition, 8.5, was also the same as that of native compound II. Unlike in native enzyme, D2O-H2O exchange did not cause a shift of the Fe(IV) = O frequency of diacetylheme-enzyme. Thus, the metal-oxygen bond at pH 7 was stronger in diacetylheme-enzyme due to a weaker hydrogen bonding to the oxo-ligand, while the Fe(IV) = O bond strength became essentially the same between both enzymes at alkaline pH upon disruption of the hydrogen bond. A much lower reactivity of the diacetylheme-enzyme compound II was accounted to be due to the weaker hydrogen bond. Compound II of manganese-substituted enzyme exhibited Mn(IV)-oxygen stretch about 630 cm-1, which was pH insensitive but down-shifted by 18 cm-1 upon the D2O-H2O exchange. The finding indicates that its structure is in Mn(IV)-OH, where the proton is exchangeable with a water proton. These results establish that the structure of native enzyme compound II is Fe(IV) = O but not Fe(IV)-OH.
对天然辣根过氧化物酶(同工酶C)、二乙酰氘代血红素辣根过氧化物酶和锰取代辣根过氧化物酶的化合物II进行共振拉曼研究,结果表明,化合物中的金属 - 氧键在键强度和/或结构上彼此不同。天然酶化合物II的Fe(IV)=O伸缩频率对pH敏感,在pH 7和10时,拉曼谱线分别位于772和789 cm-1处。结果证实了氧配体与附近氨基酸残基之间存在氢键(西特,A.J.,雷切克,C.M.,和特纳,J.(1985年)《生物化学杂志》260,7515 - 7522)。二乙酰血红素酶化合物II的Fe(IV)=O伸缩在pH 7时位于781 cm-1处,比天然酶化合物II高9 cm-1。然而,在pH 10时,Fe(IV)=O伸缩出现在790 cm-1处,与天然酶化合物II的频率基本相同。pH转变的pK值为8.5,也与天然化合物II相同。与天然酶不同,D2O - H2O交换不会导致二乙酰血红素酶的Fe(IV)=O频率发生位移。因此,由于与氧配体的氢键较弱,二乙酰血红素酶在pH 7时的金属 - 氧键更强,而在碱性pH下氢键断裂后,两种酶的Fe(IV)=O键强度基本相同。二乙酰血红素酶化合物II活性较低被认为是由于氢键较弱。锰取代酶的化合物II表现出约630 cm-1的Mn(IV)-氧伸缩,它对pH不敏感,但在D2O - H2O交换后下移了18 cm-1。这一发现表明其结构为Mn(IV)-OH,其中质子可与水质子交换。这些结果证实天然酶化合物II的结构是Fe(IV)=O而非Fe(IV)-OH。