Table 1.
Mineral |
Chemical formula |
Reference |
---|---|---|
Carbonates |
|
|
Calcite |
CaCO3 |
[30] |
Dolomite |
CaMg(CO3)2 |
[111, 112] |
Kutnahorite |
CaMn(CO3)2 |
[113] |
Siderite |
FeCO3 |
[114] |
Magnesite |
MgCO3 |
[54, 115] |
Otavite |
CdCO3 |
[116] |
Strontianite |
SrCO3 |
[72] |
Rhodochrosite |
MnCO3 |
[117] |
Cerussite |
PbCO3 |
[118] |
Hydrozincite |
Zn5(CO3)2(OH)6 |
[36, 119] |
Dypingite |
Mg5(CO3)(OH)2·5H2O |
[120] |
Witherite |
BaCO3 |
[121] |
Phosphates |
|
|
Tricalcium phosphate |
Ca3(PO4)2 |
[78] |
Struvite |
NH4MgPO4∙6H2O |
[74, 113] |
Bobierrite |
Mg3(PO4)2·8H2O |
[74, 122] |
Baricite |
(MgFe)3(PO4)2·8H2O |
[74] |
Vivianite |
Fe3(PO4)·2H2O |
[114] |
Autunite |
Ca(UO2)2(PO4)2∙10-12H2O |
[44] |
Uramphite |
NH4UO2PO4 |
[101, 123] |
Apatite |
Ca10(PO4)6(OH)2 |
[124] |
Pb-hydroxyapatite |
Ca2.5Pb7.5(OH)2(PO4)6 |
[125] |
Strengite |
FePO4·2H2O |
[126, 127] |
Variscite |
AlPO4·2H2O |
[97] |
Silicates |
|
|
Gehlenite |
Ca2Al(AlSiO7) |
[128] |
Silica |
SiO2 |
[129] |
Nontronite |
Na0.3Fe3+ 2(Si,Al)4O10(OH)2·nH2O |
[130] |
Chamosite |
(Fe5Al)(Si3Al)10(OH)8 |
[126] |
Kaolinite |
Al4(Si4O10)(OH)4 |
[126] |
Sulphides |
|
|
Mackinawite |
FeS |
[76] |
Greigite |
Fe3S4 |
[76, 131] |
Pyrite |
FeS2 |
[132] |
Covellite |
CuS |
[133, 134] |
Sphalerite |
ZnS |
[135] |
Galena |
PbS |
[134] |
Digenite |
Cu9S5 |
[136] |
Sulphates |
|
|
Gypsum |
CaSO4·2H2O |
[41, 54] |
Celestite |
SrSO4 |
[72] |
Barite |
BaSO4 |
[121, 137] |
Oxides |
|
|
Magnetite |
Fe3O4 |
[114] |
Hematite |
Fe2O3 |
[23, 138] |
Ferrihydrite |
Fe2O3·0.5H2O |
[138] |
Geothite |
α-FeO(OH) |
[138] |
Manganite |
MnOOH |
[139] |
Vernadite |
MnO2 |
|
Hausmannite |
Mn3O4 |
[142] |
Todorokite |
(Ca,Na,K)x(Mn4+,Mn3+)6O10·3.5H2O |
[138] |
Birnessite |
(Na,Ca,K)x(Mn4+,Mn3+)2O4·1.5H2O |
[138] |
Uraninite |
UO2 |
[143–145] |
Calcium Arsenate |
CaHAsO3 |
[146] |
*Note that while these minerals have all been reported to be formed in association with bacterial activity, the mechanisms for their formation are not always known, and some minerals can be formed by multiple different mechanisms. The minerals listed and accompanying sources are non-exhaustive of the examples available in the literature.