4.7 Review

Cofactor F420: an expanded view of its distribution, biosynthesis and roles in bacteria and archaea

Journal

FEMS MICROBIOLOGY REVIEWS
Volume 45, Issue 5, Pages -

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/femsre/fuab021

Keywords

cofactor 420; redox chemistry; enzymology; cofactor biosynthesis; redox cofactor; cofactor distribution

Categories

Funding

  1. NHMRC [APP1178715, APP5191146, APP1139832, APP1197376]

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F-420 is a redox cofactor produced by many bacteria and archaea, structurally similar to FAD and FMN but catalytically similar to NAD and NADP. Understanding of its distribution, biosynthesis, role, and applications has progressed significantly in the past 5 years. New evidence suggests F-420 is synthesized across bacterial and archaeal domains through horizontal and vertical gene transfer, with new biosynthetic pathways and processes being discovered.
Many bacteria and archaea produce the redox cofactor F-420. F-420 is structurally similar to the cofactors FAD and FMN but is catalytically more similar to NAD and NADP. These properties allow F-420 to catalyze challenging redox reactions, including key steps in methanogenesis, antibiotic biosynthesis and xenobiotic biodegradation. In the last 5 years, there has been much progress in understanding its distribution, biosynthesis, role and applications. Whereas F-420 was previously thought to be confined to Actinobacteria and Euryarchaeota, new evidence indicates it is synthesized across the bacterial and archaeal domains, as a result of extensive horizontal and vertical biosynthetic gene transfer. F-420 was thought to be synthesized through one biosynthetic pathway; however, recent advances have revealed variants of this pathway and have resolved their key biosynthetic steps. In parallel, new F-420-dependent biosynthetic and metabolic processes have been discovered. These advances have enabled the heterologous production of F-420 and identified enantioselective F420H2-dependent reductases for biocatalysis. New research has also helped resolve how microorganisms use F-420 to influence human and environmental health, providing opportunities for tuberculosis treatment and methane mitigation. A total of 50 years since its discovery, multiple paradigms associated with F-420 have shifted, and new F-420-dependent organisms and processes continue to be discovered.

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