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六配位过氧亚硝酸根低自旋铁(III)卟啉配合物——一氧化氮(·NO)与铁-超氧物种反应的产物。

A Six-Coordinate Peroxynitrite Low-Spin Iron(III) Porphyrinate Complex-The Product of the Reaction of Nitrogen Monoxide (·NO) with a Ferric-Superoxide Species.

机构信息

Department of Chemistry, Johns Hopkins University , Baltimore, Maryland 21218, United States.

Department of Chemistry, Stanford University , Stanford, California 94305, United States.

出版信息

J Am Chem Soc. 2017 Dec 6;139(48):17421-17430. doi: 10.1021/jacs.7b08468. Epub 2017 Nov 21.

Abstract

Peroxynitrite (OON═O, PN) is a reactive nitrogen species (RNS) which can effect deleterious nitrative or oxidative (bio)chemistry. It may derive from reaction of superoxide anion (O) with nitric oxide (·NO) and has been suggested to form an as-yet unobserved bound heme-iron-PN intermediate in the catalytic cycle of nitric oxide dioxygenase (NOD) enzymes, which facilitate a ·NO homeostatic process, i.e., its oxidation to the nitrate anion. Here, a discrete six-coordinate low-spin porphyrinate-Fe complex [(P)Fe(OON═O)] (3) (P; a porphyrin moiety with a covalently tethered imidazole axial "base" donor ligand) has been identified and characterized by various spectroscopies (UV-vis, NMR, EPR, XAS, resonance Raman) and DFT calculations, following its formation at -80 °C by addition of ·NO to the heme-superoxo species, [(P)Fe(O)] (2). DFT calculations confirm that 3 is a six-coordinate low-spin species with the PN ligand coordinated to iron via its terminal peroxidic anionic O atom with the overall geometry being in a cis-configuration. Complex 3 thermally transforms to its isomeric low-spin nitrato form [(P)Fe(NO)] (4a). While previous (bio)chemical studies show that phenolic substrates undergo nitration in the presence of PN or PN-metal complexes, in the present system, addition of 2,4-di-tert-butylphenol (DTBP) to complex 3 does not lead to nitrated phenol; the nitrate complex 4a still forms. DFT calculations reveal that the phenolic H atom approaches the terminal PN O atom (farthest from the metal center and ring core), effecting O-O cleavage, giving nitrogen dioxide (·NO) plus a ferryl compound [(P)Fe═O] (7); this rebounds to give [(P)Fe(NO)] (4a).The generation and characterization of the long sought after ferriheme peroxynitrite complex has been accomplished.

摘要

过氧亚硝酸盐 (OON═O, PN) 是一种活性氮物种 (RNS),可影响有害的硝化或氧化 (生物) 化学。它可能来自超氧阴离子 (O) 与一氧化氮 (·NO) 的反应,并被认为在一氧化氮双加氧酶 (NOD) 酶的催化循环中形成了一个尚未观察到的结合血红素-铁-PN 中间体,该中间体促进了·NO 的动态平衡过程,即氧化为硝酸盐阴离子。在这里,通过向血红素-过氧物种 [(P)Fe(O)] (2) 中添加·NO,在 -80°C 下形成了离散的六配位低自旋卟啉铁配合物 [(P)Fe(OON═O)] (3)(P;一个共价连接的咪唑轴向“碱基”供体配体的卟啉部分),并通过各种光谱学(UV-vis、NMR、EPR、XAS、共振拉曼)和 DFT 计算进行了表征。DFT 计算证实,3 是一个六配位低自旋物种,PN 配体通过其末端过氧阴离子 O 原子与铁配位,整体几何形状呈顺式构型。配合物 3 受热转化为其异构的低自旋硝化物形式 [(P)Fe(NO)] (4a)。虽然之前的 (生物) 化学研究表明,在 PN 或 PN-金属配合物存在下,酚类底物会发生硝化,但在本系统中,向配合物 3 中添加 2,4-二叔丁基苯酚 (DTBP) 不会导致硝化苯酚;仍形成硝酸盐配合物 4a。DFT 计算表明,酚类 H 原子接近末端 PN O 原子(离金属中心和环核最远),导致 O-O 断裂,生成二氧化氮 (·NO) 和一个铁氧化合物 [(P)Fe═O] (7);这会反弹生成 [(P)Fe(NO)] (4a)。长期以来一直寻求的铁血红素过氧亚硝酸盐配合物的生成和表征已经完成。

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