Home

FeGP

FeGP is an iron-containing glycoprotein identified in several archaea and some bacteria. It is associated with the biosynthesis of cofactor F430, a nickel-containing tetrapyrrole used by methanogenic archaea to catalyze methane production. FeGP genes are typically located within operons that encode other components of the F430 biosynthetic pathway, suggesting a dedicated role in assembling or modifying the tetrapyrrole scaffold. Biochemical and genetic studies indicate that FeGP binds iron at a central site and contributes to the chemistry required to convert a tetrapyrrole precursor into FeGP or into a downstream intermediate that is further processed to F430. The exact catalytic mechanism is not fully resolved; proposed roles include substrate activation, metal-assisted transformations, or stabilization of reactive intermediates during cofactor assembly. Structural analyses in some members reveal a conserved core fold with residues coordinated to the metal, although the precise active site architecture can vary among organisms.

Distribution and significance: FeGP is predominantly found in methane-producing archaea and, less commonly, in affiliated bacteria

bearing
the
F430
pathway.
Its
presence
correlates
with
organisms
that
synthesize
F430
and
rely
on
nickel-dependent
methane
formation.
Evolutionarily,
FeGP
is
viewed
as
part
of
a
modular
cofactor
biosynthesis
toolkit
that
methanogens
have
refined.
Ongoing
work
aims
to
determine
the
definitive
function,
substrate
scope,
and
mechanistic
details,
as
well
as
the
evolutionary
history
of
the
FeGP
family.