Institute of Multidisciplinary Research for Advanced Materials, Tohoku University, Katahira, Aoba, Sendai 980-8577, Japan.
Inorg Chem. 2010 Apr 19;49(8):3602-9. doi: 10.1021/ic901869t.
Heme oxygenase (HO) catalyzes the regiospecific conversion of heme to biliverdin, CO, and free iron through three successive oxygenation reactions. HO catalysis is unique in that all three O(2) activations are performed by the substrate itself. This Forum Article overviews our current understanding on the structural and biochemical properties of HO catalysis, especially its first and third oxygenation steps. The HO first step, regiospecific hydroxylation of the porphyrin alpha-meso-carbon atom, is of particular interest because of its sharp contrast to O(2) activation by cytochrome P450. HO was proposed to utilize the FeOOH species but not conventional ferryl hemes as a reactive intermediate for self-hydroxylation. We have succeeded in preparing and characterizing the FeOOH species of HO at low temperature, and our analyses of its reaction, together with mutational and crystallographic studies, reveal that protonation of FeOOH by a distal water molecule is critical in promoting the unique self-hydroxylation. The second oxygenation is a rapid, spontaneous autooxidation of the reactive alpha-meso-hydroxyheme in which the HO enzyme does not play a critical role. Further O(2) activation by verdoheme cleaves its porphyrin macrocycle to form biliverdin and free ferrous iron. This third step has been considered to be a major rate-determining step of HO catalysis to regulate the enzyme activity. Our reaction analysis strongly supports the FeOOH verdoheme as the key intermediate of the ring-opening reaction. This mechanism is very similar to that of the first meso-hydroxylation, and the distal water is suggested to enhance the third step as expected from the similarity. The HO mechanistic studies highlight the catalytic importance of the distal hydrogen-bonding network, and this manuscript also involves our attempts to develop HO inhibitors targeting the unique distal structure.
血红素加氧酶 (HO) 通过三个连续的氧合反应催化血红素向胆绿素、CO 和游离铁的区域特异性转化。HO 催化的独特之处在于,所有三个 O(2) 的激活都是由底物本身完成的。本文概述了我们目前对 HO 催化的结构和生化特性的理解,特别是其第一步和第三步氧合反应。HO 的第一步,卟啉 α-中位碳原子的区域特异性羟化,由于其与细胞色素 P450 的 O(2) 激活形成鲜明对比而特别有趣。HO 被提议利用 FeOOH 物种而不是常规的高亚铁血红素作为自身羟化的反应中间体。我们已经成功地在低温下制备和表征了 HO 的 FeOOH 物种,并且我们对其反应的分析,以及突变和晶体学研究,揭示了远端水分子对 FeOOH 的质子化对于促进独特的自身羟化反应至关重要。第二步氧合是活性 α-中位羟血红素的快速自发自氧化,HO 酶在此过程中不起关键作用。进一步的 O(2) 激活通过 verdoheme 裂解其卟啉大环形成胆绿素和游离亚铁。第三步被认为是 HO 催化的主要限速步骤,以调节酶活性。我们的反应分析强烈支持 FeOOH verdoheme 作为环开裂反应的关键中间体。该机制与第一步的中位羟化非常相似,并且从相似性来看,远端水被认为可以增强第三步。HO 机制研究强调了远端氢键网络的催化重要性,本文还涉及我们开发针对独特远端结构的 HO 抑制剂的尝试。