Ferrihydrite mineral
Ferrihydrite is an approved mineral species in the September 2026 IMA list, with formula Fe(III)5O7(OH) and approval number 1971-015. The name also occurs in experimental descriptions of poorly crystalline synthetic two-line iron oxyhydroxides; that assay designation does not independently establish ideal IMA formula, natural origin or purity. This record concerns a characterized synthetic nanophase substrate, not iron metal, an ore grade or every Fe(III) oxide. The Ax17 assay is also represented under iron and the paired ferrihydrite/magnetite record; these are substrate/product perspectives on one experiment, not independent replication. No iron criticality designation is inherited.
Microbial & Biochemical Mechanisms (1)
Reduction of synthetic two-line ferrihydrite with secondary mineral formation
Associated Organisms:
Desulfovulcanus ferrireducens (NCBITaxon:2831190)
Growing Desulfovulcanus ferrireducens Ax17 (DSM 111878) reduced synthetic two-line nanophase ferrihydrite and produced a black magnetic solid interpreted from complementary analyses as primarily cation-deficient magnetite. This is microbial Fe redox transformation with secondary mineral formation, not elemental iron production or a purified recovery product. The taxon identifier is species-level; the paper and DSMZ identify the experimental strain.
Laboratory triplicates used 50 mL modified DSM 981 medium in 160 mL serum bottles, reported 100 mmol/L ferrihydrite, initial pH 6.80 +/- 0.05, 0.5 mM cysteine-HCl, and 1.3 mM FeCl2 supplementation. The headspace was H2:CO2 (80:20) at 200 kPa; cultures received a 1% logarithmic-phase inoculum previously transferred at least three times on the acceptor, and grew at 55 degrees C for about five days. Identically composed uninoculated controls were incubated at 55 degrees C or room temperature. Ferrozine after oxalate dissolution gave reported Fe(II) of 24 mM in the biotic medium versus 2-3 mM in controls; this extraction-based measurement is not a dissolved-iron concentration or a recovery percentage. No pilot, industrial, or natural-ore extraction operation was tested. The source reports 84% retention of biogenic iron product in a separate pre-oxalate filtration comparison; this is an operational particulate fraction, not a magnetite phase percentage. No ideal starting ferrihydrite stoichiometry is inferred from the reported 100 mmol/L mineral addition.
sklute2023
sklute2023
Sources & References
-
ima_2026_09: IMA-CNMNC. The New IMA List of Minerals, September 2026. PDF page 69, Ferrihydrite row; page 1 column definitions and page 2 distribution terms.
https://cnmnc.units.it/files/editor/IMA_Master_List_(2026-09).pdf (accessed 2026-10-11) -
sklute2023: Sklute et al. (2023). Fe(III) (oxyhydr)oxide reduction by the thermophilic iron-reducing bacterium Desulfovulcanus ferrireducens. Frontiers in Microbiology 14:1272245. Methods, ferrihydrite Results, Figures 1-4, and Supplementary Figures S2-S5.
https://doi.org/10.3389/fmicb.2023.1272245 (accessed 2026-10-11) -
ncbi_ferrireducens: NCBI Taxonomy 2831190 - Desulfovulcanus ferrireducens; species rank
https://www.ncbi.nlm.nih.gov/Taxonomy/Browser/wwwtax.cgi?id=2831190 (accessed 2026-10-11)
Curation History
| Timestamp | Curator | Action | Summary |
|---|---|---|---|
2026-10-11T09:27:01.990810+00:00 |
codex (GPT-6; codex) | CREATE | Created ferrihydrite species identity with synthetic two-line substrate reduction and mixed-product limits. |
Record source: data/records/ferrihydrite.yaml