Laboratory of Microbial Biochemistry and Biotechnology, School of Biological Sciences, University of Auckland, Private Bag 92019, Auckland, New Zealand.
Curr Opin Chem Biol. 2024 Jun;80:102468. doi: 10.1016/j.cbpa.2024.102468. Epub 2024 May 21.
Cofactor F has been historically known as the "methanogenic redox cofactor". It is now recognised that F has essential roles in the primary and secondary metabolism of archaea and bacteria. Recent discoveries highlight the role of F as a redox cofactor in the biosynthesis of various natural products, including ribosomally synthesised and post-translationally modified peptides, and a new class of nicotinamide adenine dinucleotide-based secondary metabolites. With the vast availability of (meta)genomic data, the identification of uncharacterised F-dependent enzymes offers the potential for discovering novel secondary metabolites, presenting valuable prospects for clinical and biotechnological applications.
辅因子 F 历史上被称为“产甲烷菌氧化还原辅因子”。现在人们认识到,F 在古菌和细菌的初级和次级代谢中具有重要作用。最近的发现强调了 F 作为各种天然产物生物合成的氧化还原辅因子的作用,包括核糖体合成和翻译后修饰的肽,以及一类新的烟酰胺腺嘌呤二核苷酸为基础的次级代谢物。随着(宏)基因组数据的大量出现,鉴定未表征的依赖 F 的酶为发现新型次级代谢物提供了潜力,为临床和生物技术应用带来了有价值的前景。