An anoxic, methanogenic enrichment culture defining "lithosyntrophy," an obligate syntrophic interaction in which the electrons driving hydrogenotrophic methanogenesis originate from an inorganic compound. Candidatus Phosphitivorax anaerolimi Phox-21 oxidizes phosphite (oxidation state +3) to phosphate coupled to hydrogenogenesis, in an obligate energetic dependency on a hydrogenotrophic methanogen, Methanoculleus sp. Electrons derived from phosphite drive H2 production via an electron-confurcating hydrogenase; the methanogen consumes the H2 to keep the reaction thermodynamically favorable, establishing interspecies electron transfer that links the phosphorus and carbon redox cycles in anoxic ecosystems.
Taxonomy
| Taxon | Ontology ID | Functional Roles | Abundance |
|---|---|---|---|
| Candidatus Phosphitivorax anaerolimi Phox-21 | NCBITaxon:1918507 |
SYNTROPHIC_PARTNER
ELECTRON_DONOR
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N/A |
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| Methanoculleus sp. | NCBITaxon:45989 |
SYNTROPHIC_PARTNER
ELECTRON_ACCEPTOR
|
N/A |
|
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Ecological Interactions
Lithosyntrophic interspecies H2 transfer
SYNTROPHYSource Taxon: Candidatus Phosphitivorax anaerolimi Phox-21
Target Taxon: Methanoculleus sp.
Metabolites: hydrogen (H2) (CHEBI:18276)
Evidence
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PMID:41811448 - SUPPORT (IN_VITRO)"we describe "lithosyntrophy," a mode of syntrophic interaction in which electrons that drive hydrogenotrophic methanogenesis originate from an inorganic compound rather than from the canonical organic substrates."
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PMID:41811448 - SUPPORT (IN_VITRO)"In this pathway, electrons derived from phosphite drive H2 production via an electron-confurcating hydrogenase."