omcZ (GSU2076, UniProt Q74BG5) — Geobacter sulfurreducens PCA

Starting point

Residue numbering — read before quoting a residue

The structure papers (Gu et al. 2023 PMID:36732469; Wissink et al. 2026) number
residues on the mature protein, i.e. UniProt position minus 24 (the SignalP
signal peptide). Checked against the Q74BG5 sequence:

paper (mature) UniProt Q74BG5 residue
H40-H41 (heme II/III HH motif) H64-H65 His-His
C53 ... C68-H69 (CX14CH, heme II) C77 ... C92-H93 the non-canonical motif
R85 R109 Arg
H96-H97 (heme I/IV HH motif) H120-H121 His-His
H182-H183 (heme VI/VII HH motif) H206-H207 His-His
N258 (OzpA cleavage region) N282 Asn

The 258-residue nanowire-forming OmcZ30 (Gu 2023, Wissink 2026) corresponds to
UniProt 25-282, matching the PDB 7LQ5 chain range. The review YAML avoids stating
residue numbers for this reason.

Biology, with provenance

Identity, hemes and processing

Structure of the filament

Function: long-range electron transfer to electrodes

Conductivity claims and the controversy

Wissink et al. 2026 (supplied paper) — what it adds for G. sulfurreducens OmcZ

The paper is mainly about the archaeal homologue OmcZ2 of "Ca. Methanoperedens
vercellensis", solved at 3.3 Å from electrode-grown, near-axenic cultures at pH 7.25.
For the Geobacter protein (called OmcZGs in the paper) it adds:
- A structural alignment with an archaeal OmcZ that shares only about 30% sequence
identity. The fold and heme architecture are conserved across domains, with a
"core quadrangle" of four conserved short sequence regions around hemes V and VIII,
and three conserved His-His motifs that link heme pairs.
- Bacterial OmcZ forms its own phylogenetic group, Group VI; Groups I-V are archaeal
(ANME and Borg elements). Archaeal clusters co-occur with serine peptidases,
consistent with an OzpA-type maturation step.
- OmcZGs has only three N-glycosylation motifs and no detectable glycan density,
whereas the archaeal protein is extensively modified.
- In OmcZGs hemes I, III and VI are largely solvent exposed and the nanowires aggregate
into dense networks, while the archaeal filaments are straighter and their hemes more
buried.
- Archaea assemble OmcZ nanowires without a prolyl isomerase in the cluster. This makes
it questionable whether the Geobacter isomerase GSU2074 is needed for OmcZ folding,
as Gu 2023 proposed; it may instead be a lineage-specific requirement.
- The OmcZ phenotype in G. sulfurreducens is not re-tested here; the paper relies on the
earlier literature (its refs 27, 30, 33 = PMID:36732469, PMID:32807967, PMID:33837010).

Annotation decisions (summary)

All rows are NEW, because GOA has nothing for this protein.
- MF GO:0009055 electron transfer activity — IDA (PMID:20400562) — core.
- MF GO:0020037 heme binding — IDA (cryo-EM, PMID:36732469; heme counting, PMID:20400562).
- CC GO:0097311 bacterial biofilm matrix — IDA (immunogold, PMID:23761253) — core location.
- BP GO:0019645 anaerobic electron transport chain — IMP (PMID:19461962). OmcZ is
itself an electron carrier at the end of the chain, so it does part of the work; this
matches the term used for OmcA (SHEON), ImcH and CbcL (GEOSL) in this repository.
- BP GO:0051258 protein polymerization — IDA (in vitro self-assembly after OzpA
cleavage, PMID:36732469).
- Not added:
- GO:0016722 oxidoreductase activity, acting on metal ions — single-turnover in vitro
metal reduction with no growth phenotype on Fe(III) citrate.
- GO:0042710 biofilm formation — the defect is conditional on current-harvesting mode
and absent on fumarate, so it is probably secondary to failed respiration.
- GO:0009986 cell surface — the filaments are extracellular and matrix-embedded; there
is no evidence of an anchoring mechanism.
- Ontology gap: GO has no cellular-component term for an extracellular cytochrome
filament ("nanowire"), so one is proposed (see proposed_new_terms).