Coenzyme F420

Structure of Coenzyme F420

Coenzyme F420 is a family of coenzymes involved in redox reactions in a number of bacteria and archaea. It is derived from coenzyme FO (7,8-didemethyl-8-hydroxy-5-deazariboflavin) and differs by having a oligoglutamyl tail attached via a 2-phospho-L-lactate bridge. F420 is so named because it is a flavin derivative with an absorption maximum at 420 nm.

F420 was originally discovered in methanogenic archaea[1] and in Actinomycetota (especially in Mycobacterium).[2] It is now known to be used also by Cyanobacteria and by soil Proteobacteria, Chloroflexi and Firmicutes.[3] Eukaryotes including the fruit fly Drosophila melanogaster and the algae Ostreococcus tauri also use Coenzyme FO.[4]

F420 is structurally similar to FMN, but catalytically it is similar to NAD and NADP: it has low redox potential and always transfer a hydride. As a result, it is not only a versatile cofactor in biochemical reactions, but also being eyed for potential as an industrial catalyst. Similar to FMN, it has two states: one reduced state, notated as F420-H2, and one oxidized state, written as just F420.[5] FO has largely similar redox properties, but cannot carry an electric charge and as a result probably slowly leaks out of the cellular membrane.[3]

A number of F420 molecules, differing by the length of the oligoglutamyl tail, are possible; F420-2, for example, refers to the version with two glutamyl units attached. Lengths from 4 to 9 are typical.[3]

  1. ^ Deppenmeier U (September 2002). "Redox-driven proton translocation in methanogenic Archaea". Cellular and Molecular Life Sciences. 59 (9): 1513–33. doi:10.1007/s00018-002-8526-3. PMC 11337502. PMID 12440773. S2CID 23199201.
  2. ^ Selengut JD, Haft DH (November 2010). "Unexpected abundance of coenzyme F(420)-dependent enzymes in Mycobacterium tuberculosis and other actinobacteria". Journal of Bacteriology. 192 (21): 5788–98. doi:10.1128/JB.00425-10. PMC 2953692. PMID 20675471.
  3. ^ a b c Ney, B; Ahmed, FH; Carere, CR; Biswas, A; Warden, AC; Morales, SE; Pandey, G; Watt, SJ; Oakeshott, JG; Taylor, MC; Stott, MB; Jackson, CJ; Greening, C (January 2017). "The methanogenic redox cofactor F(420) is widely synthesized by aerobic soil bacteria". The ISME Journal. 11 (1): 125–137. Bibcode:2017ISMEJ..11..125N. doi:10.1038/ismej.2016.100. PMC 5315465. PMID 27505347.
  4. ^ Glas AF, Maul MJ, Cryle M, Barends TR, Schneider S, Kaya E, Schlichting I, Carell T (July 2009). "The archaeal cofactor F0 is a light-harvesting antenna chromophore in eukaryotes". Proceedings of the National Academy of Sciences of the United States of America. 106 (28): 11540–5. Bibcode:2009PNAS..10611540G. doi:10.1073/pnas.0812665106. PMC 2704855. PMID 19570997.
  5. ^ Grinter, Rhys; Greening, Chris (8 September 2021). "Cofactor F420: an expanded view of its distribution, biosynthesis and roles in bacteria and archaea". FEMS Microbiology Reviews. 45 (5). doi:10.1093/femsre/fuab021. PMC 8498797. PMID 33851978.

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