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The methanogenic redox cofactor F₄₂₀ is widely synthesized by aerobic soil bacteria.

ABSTRACT: F₄₂₀ is a low-potential redox cofactor that mediates the transformations of a wide range of complex organic compounds. Considered one of the rarest cofactors in biology, F₄₂₀ is best known for its role in methanogenesis and has only been chemically identified in two phyla to date, the Euryarchaeota and Actinobacteria. In this work, we show that this cofactor is more widely distributed than previously reported. We detected the genes encoding all five known F₄₂₀ biosynthesis enzymes (cofC, cofD, cofE, cofG and cofH) in at least 653 bacterial and 173 archaeal species, including members of the dominant soil phyla Proteobacteria, Chloroflexi and Firmicutes. Metagenome datamining validated that these genes were disproportionately abundant in aerated soils compared with other ecosystems. We confirmed through high-performance liquid chromatography analysis that aerobically grown stationary-phase cultures of three bacterial species, Paracoccus denitrificans, Oligotropha carboxidovorans and Thermomicrobium roseum, synthesized F₄₂₀, with oligoglutamate sidechains of different lengths. To understand the evolution of F₄₂₀ biosynthesis, we also analyzed the distribution, phylogeny and genetic organization of the cof genes. Our data suggest that although the F_o precursor to F₄₂₀ originated in methanogens, F₄₂₀ itself was first synthesized in an ancestral actinobacterium. F₄₂₀ biosynthesis genes were then disseminated horizontally to archaea and other bacteria. Together, our findings suggest that the cofactor is more significant in aerobic bacterial metabolism and soil ecosystem composition than previously thought. The cofactor may confer several competitive advantages for aerobic soil bacteria by mediating their central metabolic processes and broadening the range of organic compounds they can synthesize, detoxify and mineralize.

SUBMITTER: Ney B

PROVIDER: S-EPMC5315465 | biostudies-literature | 2017 Jan

REPOSITORIES: biostudies-literature

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The methanogenic redox cofactor F420 is widely synthesized by aerobic soil bacteria.

Ney Blair B Ahmed F Hafna FH Carere Carlo R CR Biswas Ambarish A Warden Andrew C AC Morales Sergio E SE Pandey Gunjan G Watt Stephen J SJ Oakeshott John G JG Taylor Matthew C MC Stott Matthew B MB Jackson Colin J CJ Greening Chris C

The ISME journal 20160809 1

F420 is a low-potential redox cofactor that mediates the transformations of a wide range of complex organic compounds. Considered one of the rarest cofactors in biology, F420 is best known for its role in methanogenesis and has only been chemically identified in two phyla to date, the Euryarchaeota and Actinobacteria. In this work, we show that this cofactor is more widely distributed than previously reported. We detected the genes encoding all five known F420 bi ...[more]

PMID: 27505347

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Project description:Coenzyme F420 is a redox cofactor involved in hydride transfer reactions in archaea and bacteria. Since F420-dependent enzymes are attracting increasing interest as tools in biocatalysis, F420 biosynthesis is being revisited. While it was commonly accepted for a long time that the 2-phospho-l-lactate (2-PL) moiety of F420 is formed from free 2-PL, it was recently shown that phosphoenolpyruvate is incorporated in Actinobacteria and that the C-terminal domain of the FbiB protein, a member of the nitroreductase (NTR) superfamily, converts dehydro-F420 into saturated F420 Outside the Actinobacteria, however, the situation is still unclear because FbiB is missing in these organisms and enzymes of the NTR family are highly diversified. Here, we show by heterologous expression and in vitro assays that stand-alone NTR enzymes from Thermomicrobia exhibit dehydro-F420 reductase activity. Metabolome analysis and proteomics studies confirmed the proposed biosynthetic pathway in Thermomicrobium roseum These results clarify the biosynthetic route of coenzyme F420 in a class of Gram-negative bacteria, redefine functional subgroups of the NTR superfamily, and offer an alternative for large-scale production of F420 in Escherichia coli in the future.IMPORTANCE Coenzyme F420 is a redox cofactor of Archaea and Actinobacteria, as well as some Gram-negative bacteria. Its involvement in processes such as the biosynthesis of antibiotics, the degradation of xenobiotics, and asymmetric enzymatic reductions renders F420 of great relevance for biotechnology. Recently, a new biosynthetic step during the formation of F420 in Actinobacteria was discovered, involving an enzyme domain belonging to the versatile nitroreductase (NTR) superfamily, while this process remained blurred in Gram-negative bacteria. Here, we show that a similar biosynthetic route exists in Thermomicrobia, although key biosynthetic enzymes show different domain architectures and are only distantly related. Our results shed light on the biosynthesis of F420 in Gram-negative bacteria and refine the knowledge about sequence-function relationships within the NTR superfamily of enzymes. Appreciably, these results offer an alternative route to produce F420 in Gram-negative model organisms and unveil yet another biochemical facet of this pathway to be explored by synthetic microbiologists.

Project description:Coenzyme F420 is a microbial redox cofactor that mediates diverse physiological functions and is increasingly used for biocatalytic applications. Recently, diversified biosynthetic routes to F420 and the discovery of a derivative, 3PG-F420, were reported. 3PG-F420 is formed via activation of 3-phospho-d-glycerate (3-PG) by CofC, but the structural basis of substrate binding, its evolution, as well as the role of CofD in substrate selection remained elusive. Here, we present a crystal structure of the 3-PG-activating CofC from Mycetohabitans sp. B3 and define amino acids governing substrate specificity. Site-directed mutagenesis enabled bidirectional switching of specificity and thereby revealed the short evolutionary trajectory to 3PG-F420 formation. Furthermore, CofC stabilized its product, thus confirming the structure of the unstable molecule and revealing its binding mode. The CofD enzyme was shown to significantly contribute to the selection of related intermediates to control the specificity of the combined biosynthetic CofC/D step. These results imply the need to change the design of combined CofC/D activity assays. Taken together, this work presents novel mechanistic and structural insights into 3PG-F420 biosynthesis and evolution and opens perspectives for the discovery and enhanced biotechnological production of coenzyme F420 derivatives in the future. IMPORTANCE The microbial cofactor F420 is crucial for processes like methanogenesis, antibiotics biosynthesis, drug resistance, and biocatalysis. Recently, a novel derivative of F420 (3PG-F420) was discovered, enabling the production and use of F420 in heterologous hosts. By analyzing the crystal structure of a CofC homolog whose substrate choice leads to formation of 3PG-F420, we defined amino acid residues governing the special substrate selectivity. A diagnostic residue enabled reprogramming of the substrate specificity, thus mimicking the evolution of the novel cofactor derivative. Furthermore, a labile reaction product of CofC was revealed that has not been directly detected so far. CofD was shown to provide another layer of specificity of the combined CofC/D reaction, thus controlling the initial substrate choice of CofC. The latter finding resolves a current debate in the literature about the starting point of F420 biosynthesis in various organisms.

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The methanogenic redox cofactor F₄₂₀ is widely synthesized by aerobic soil bacteria.

Publications

The methanogenic redox cofactor F<sub>420</sub> is widely synthesized by aerobic soil bacteria.

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