Giulivi C, Davies K J
Institute for Toxicology, University of Southern California, Los Angeles 90033.
J Biol Chem. 1990 Nov 15;265(32):19453-60.
Ferrylhemoglobin (X-FeIV-OH, where X denotes an amino acid residue in the globin moiety) has long been suspected as a cytotoxic agent produced by the interaction of oxyhemoglobin (X-FeIIO2) or methemoglobin (X-FeIII) with H2O2 in red blood cells. To date, however, technical difficulties have prevented the identification and quantification of X-FeIV-OH. Oxyhemoglobin exposed to a continuous flux of H2O2 (generated at a rate of 120 microM/min during the glucose oxidase-catalyzed oxidation of glucose) was oxidized to (a) X-FeIV-OH when [X-FeIIO2] less than 75 microM and (b) X-FeIII when [X-FeIIO2] greater than 75 microM (the production of X-FeIII proceeded with intermediate formation of X-FeIV-OH). The reduction of the X-FeIV-OH to X-FeIII could be explained by either of two alternative mechanisms: a O2(-)-mediated X-FeIV-OH---X-FeIII transition or a comproportionation of X-FeIV-OH and X-FeIIO2 to yield X-FeIII (a process mediated by a tyrosine moiety in the hemoprotein). The low rate of X-FeIIO2 autoxidation plus the negligible decrease in the rate of X-FeIII formation in the presence of either native or heat-denatured superoxide dismutase or apoenzyme (1 microM) suggested that O2- does not contribute to the reduction of X-FeIV-OH. Moreover, the dependence of X-FeIII formation on X-FeIIO2 concentration, together with the results of O2 uptake and H2O2 consumption measurements, provide experimental evidence to support the comproportionation reaction. Comproportionation is apparently catalyzed by intermolecular electron transfer between tyrosine residues, since the reaction did not occur when tyrosine residues were blocked by acetylation. Intact red blood cells exposed to the same flow rate of H2O2 presented a spectral profile which could be explained as a transition from X-FeIIO2 to X-FeIII. The intermediate production of X-FeIV-OH was detected by adding Na2S (2 mM), which revealed a spectral profile identical with that obtained with purified X-FeIV-OH. Measurements of concentrations and relative rate constants for the reaction of various intracellular reductants (glutathione, NAD(P)H, uric acid, ascorbic acid) with X-FeIV-OH revealed that comproportionation of X-FeIV-OH with X-FeIIO2 is the favored reaction. Our results provide (to our knowledge) the first definitive evidence for X-FeIV-OH in intact red blood cells. The rapid comproportionation reaction between X-FeIV-OH and X-FeIIO2 (to produce X-FeIII) explains why X-FeIV-OH has been elusive to date.(ABSTRACT TRUNCATED AT 400 WORDS)
高铁血红蛋白(X-FeIV-OH,其中X表示球蛋白部分的一个氨基酸残基)长期以来一直被怀疑是红细胞中氧合血红蛋白(X-FeIIO2)或高铁血红蛋白(X-FeIII)与H2O2相互作用产生的一种细胞毒性剂。然而,迄今为止,技术难题阻碍了X-FeIV-OH的鉴定和定量。暴露于连续的H2O2流(在葡萄糖氧化酶催化葡萄糖氧化过程中以120微摩尔/分钟的速率产生)的氧合血红蛋白,当[X-FeIIO2]小于75微摩尔时被氧化为(a)X-FeIV-OH,当[X-FeIIO2]大于75微摩尔时被氧化为(b)X-FeIII(X-FeIII的产生伴随着X-FeIV-OH的中间形成)。X-FeIV-OH还原为X-FeIII可以用两种替代机制中的任何一种来解释:一种是O2(-)介导的X-FeIV-OH---X-FeIII转变,另一种是X-FeIV-OH与X-FeIIO2发生歧化反应生成X-FeIII(这一过程由血红蛋白中的酪氨酸部分介导)。在存在天然或热变性的超氧化物歧化酶或脱辅基酶(1微摩尔)的情况下,X-FeIIO2的自氧化速率较低,且X-FeIII形成速率的降低可忽略不计,这表明O2-对X-FeIV-OH的还原没有贡献。此外,X-FeIII形成对X-FeIIO2浓度的依赖性,以及O2摄取和H2O2消耗测量的结果,为支持歧化反应提供了实验证据。歧化反应显然是由酪氨酸残基之间的分子间电子转移催化的,因为当酪氨酸残基被乙酰化阻断时,反应不会发生。暴露于相同流速H2O2的完整红细胞呈现出一种光谱特征,这可以解释为从X-FeIIO2到X-FeIII的转变。通过添加Na2S(2毫摩尔)检测到了X-FeIV-OH的中间产生,其显示出与纯化的X-FeIV-OH获得的光谱特征相同。对各种细胞内还原剂(谷胱甘肽、NAD(P)H、尿酸、抗坏血酸)与X-FeIV-OH反应的浓度和相对速率常数的测量表明,X-FeIV-OH与X-FeIIO2的歧化反应是有利的反应。我们的结果(据我们所知)为完整红细胞中的X-FeIV-OH提供了首个确凿证据。X-FeIV-OH与X-FeIIO2之间的快速歧化反应(产生X-FeIII)解释了为什么迄今为止X-FeIV-OH难以捉摸。(摘要截短至400字)