Ginorite mineral
Ginorite is the grandfathered calcium borate species listed as Ca2B14O20(OH)6(H2O)3·2H2O in the September 2026 IMA-CNMNC list. Its 1934 entry is a description year, not an approval identifier. The older Ca2[B14O20(OH)6]·5H2O formula has the same elemental stoichiometry. A natural Sasso Pisano crystal studied by Perchiazzi et al. has a monoclinic P21/a structure with borate sheets, calcium sites and hydrogen bonding; three water molecules per formula unit coordinate calcium and two do not. Hydrogen positions were refined with O-H distance restraints. The study's tabulated chemical analyses came from earlier publications, while its own preliminary SEM/EDAX screen found strontium below detection. This species is distinct from strontioginorite, elemental boron and the borates commodity. Neither a criticality designation nor microbial extraction or commercial recovery is inferred from its boron content.
Microbial & Biochemical Mechanisms (1)
Laboratory endothermic response on heating
Natural ginorite from Twenty Mule Team Canyon, Death Valley, showed an initial endothermic response at 70-80 degrees C and reported troughs at 100, 150, 310, 360 and 470 degrees C during differential thermal analysis. These are instrumental thermal features of that specimen, not identified product phases, an equilibrium decomposition sequence or a boron recovery yield.
Allen's 1957 procedure started with a cold furnace and used a nominal heating rate of 30 degrees C per minute through 500 degrees C. Samples were sieved to the reported -50+200 mesh range and lightly tamped in crucibles; ginorite was run at medium sensitivity. Temperature readings were taken at 10-degree intervals. Each mineral was analyzed at least three times, but individual ginorite replicate curves and statistical uncertainties were not reported. The mineral was checked microscopically, chemically and by X-ray diffraction before the thermal experiment. Sample mass, controlled atmosphere, evolved-gas analysis and post-run ginorite phase identification were not reported.
allen_dta1957
allen_kramer1957
Sources & References
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ima_2026_09: IMA-CNMNC, The New IMA List of Minerals, September 2026: PDF page 83, Ginorite row; page 1, status/year definitions. Fresh official list and current landing page checked on 16 October 2026. The coordinated-water notation preserves the total of five water molecules per formula unit.
https://cnmnc.units.it/files/editor/IMA_Master_List_(2026-09).pdf (accessed 2026-10-16) -
perchiazzi2016: Perchiazzi, Armienti, Iaccarino and Lezzerini (2016), A contribution to the mineralogy of the Larderello geothermal field. X-ray crystallographic studies on borate minerals bechilite and lagonite and crystal structure determination of ginorite, Atti della Societa Toscana di Scienze Naturali, Memorie Serie A 123, 79-87, DOI 10.2424/ASTSN.M.2016.23. Complete publisher article in institutional PDF, printed pp. 79-87 (PDF pp. 5-13): historical chemistry Table 2, diffraction Tables 3-6, methods p. 84 and Figures 3-4 p. 85. The natural crystal came from museum specimen 7678; this is not a synthetic or microbially formed specimen.
https://iris.unito.it/retrieve/e27ce42c-6e27-2581-e053-d805fe0acbaa/009_PERCHIAZZI.pdf (accessed 2026-10-16) -
allen_kramer1957: Allen and Kramer (1957), Ginorite and sassolite from Death Valley, California, American Mineralogist 42, 56-61. Complete six-page original: locality pp. 56-57; warm-water removal of sassolite and 105-degree drying pp. 57-58; chemical analysis Table 1 p. 58; powder patterns Table 4 p. 60. Original and residue-corrected compositions are separate columns. This is a different specimen/locality from the later Italian and Kazakhstan structural studies.
https://msaweb.org/AmMin/AM42/AM42_56.pdf (accessed 2026-10-16) -
allen_dta1957: Allen (1957), Differential thermal analysis of selected borate minerals, USGS Bulletin 1036-K, 193-208, DOI 10.3133/b1036K. Complete official report: apparatus/methods pp. 193-195; repeat runs and temperature summary p. 196; ginorite curve Figure 20 p. 198.
https://pubs.usgs.gov/bul/1036k/report.pdf (accessed 2026-10-16) -
pankova2018: Pankova, Gorelova, Krivovichev and Pekov (2018), The crystal structure of ginorite, Ca2[B14O20(OH)6]·5H2O, and the analysis of dimensional reduction and structural complexity in the CaO-B2O3-H2O system, European Journal of Mineralogy 30, 277-287, DOI 10.1127/ejm/2018/0030-2695. Complete publisher PDF from the RRUFF repository: Chelkar sample and qualitative microprobe screening p. 279; structure Figures 1-2 p. 282. Abstract and Table 2 data row use 296(2) K, whereas methods and several table labels use 293 K; the second dataset is 150(2) K. Supplementary Tables S1-S3 were not acquired. Detailed thermal-expansion or hydrogen-bond measurements are therefore not imported. Its P21/c description and the earlier P21/a description are not treated as evidence of a phase transition; neither paper is a processing experiment.
https://www.rruff.net/odr/view/downloadfile/83281 (accessed 2026-10-16)
Curation History
| Timestamp | Curator | Action | Summary |
|---|---|---|---|
2026-10-16T04:26:58.244082Z |
codex (GPT-6; codex) | CREATE | Created a distinct ginorite species record with verified natural structure and bounded laboratory thermal response; retained specimen and source inconsistencies. |
Record source: data/records/ginorite.yaml