Biofunctional Catalyst Research Team, RIKEN Center for Sustainable Resource Science, 2-1 Hirosawa, Wako, Saitama 351-0198, Japan.
Chem Commun (Camb). 2021 Apr 4;57(26):3267-3270. doi: 10.1039/d0cc07318k. Epub 2021 Mar 2.
The CO-to-CO reduction by carbon monoxide dehydrogenase (CODH) with a [NiFeS] cluster is considered to be the oldest pathway of biological carbon fixation and therefore may have been involved in the origin of life. Although previous studies have investigated CO reduction by Fe and Ni sulfides to identify the prebiotic origin of the [NiFeS] cluster, the reaction mechanism remains largely elusive. Herein, we applied in situ electrochemical ATR-FTIR spectroscopy to probe the reaction intermediates of greigite (FeS) and violarite (FeNiS). Intermediate species assignable to surface-bound CO and formyl groups were found to be stabilized in the presence of Ni, lending insight into its role in enhancing the multistep CO reduction process.
一氧化碳脱氢酶(CODH)利用 [NiFeS] 簇将 CO 还原为 CO2 被认为是生物固碳的最古老途径,因此可能参与了生命的起源。尽管先前的研究已经研究了 Fe 和 Ni 硫化物对 CO 的还原作用,以确定 [NiFeS] 簇的前生物起源,但反应机制在很大程度上仍难以捉摸。在此,我们应用原位电化学 ATR-FTIR 光谱法来探测磁黄铁矿(FeS)和镍黄铁矿(FeNiS)的反应中间体。在 Ni 的存在下,发现可归属为表面结合的 CO 和甲酰基的中间物种得到稳定,这深入了解了 Ni 在增强多步 CO 还原过程中的作用。