| Ain Allegua Tunisie | −12.21 ‰ | | 1 | cerussite crust on galena | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Angleur Belgique | −15.1 ‰ | | 1 | supergene cerussite | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
| Bou Grine Tunisie | −0.54 ± 1.76 ‰ | −2.13 / 1.92 ‰ | 4 | smithsonite (host-rock replacement and crusts) | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Bou Grine Tunisie | −5.13 ± 0.19 ‰ | −5.27 / −5 ‰ | 2 | supergene calcite after smithsonite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Bou Grine Tunisie | 3.15 ± 0.91 ‰ | 2.5 / 3.79 ‰ | 2 | Bahloul Formation host limestone (Cenomanian-Turonian) | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Bou Jaber Tunisie | 2.05 ± 1.88 ‰ | −2 / 3.9 ‰ | 13 | Late Aptian host limestone (barren and mineralised) | Bouhlel et al. (2016), A salt diapir-related Mississippi Valley-type deposit: the Bou Jab… |
| Bou Jaber Tunisie | 2.88 ± 0.44 ‰ | 2.4 / 3.6 ‰ | 6 | ankerite 1 and 2 (before and after barite) | Bouhlel et al. (2016), A salt diapir-related Mississippi Valley-type deposit: the Bou Jab… |
| Bou Jaber Tunisie | 0.47 ± 0.96 ‰ | −0.4 / 1.5 ‰ | 3 | ankerite 3 (geodes after fluorite) | Bouhlel et al. (2016), A salt diapir-related Mississippi Valley-type deposit: the Bou Jab… |
| Bou Jaber Tunisie | 2.56 ± 1.18 ‰ | 1.3 / 3.8 ‰ | 5 | calcite 1 (post-ore) | Bouhlel et al. (2016), A salt diapir-related Mississippi Valley-type deposit: the Bou Jab… |
| Bou Jaber Tunisie | 3.6 ± 0.95 ‰ | 2.6 / 6.2 ‰ | 11 | calcite 2 (post-ore) | Bouhlel et al. (2016), A salt diapir-related Mississippi Valley-type deposit: the Bou Jab… |
| Bou Jaber Tunisie | −2.87 ‰ | | 1 | concretionary smithsonite from the oxidised zone | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Bou Jaber Tunisie | −5.62 ‰ | | 1 | cerussite crystals on a galena vein | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Campo Pisano Italy | −6.16 ‰ | | 1 | supergene smithsonite pseudomorphous after calcite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Mendip Hills orefield (Priddy, Whatley, Merehead) United Kingdom | −4.6 ± 3.3 ‰ | −7.8 / −1.3 ‰ | 3 | supergene smithsonite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Mendip Hills orefield (Priddy, Whatley, Merehead) United Kingdom | −6.9 ± 0.3 ‰ | −7.1 / −6.6 ‰ | 3 | supergene cerussite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| South Pennine orefield (Derbyshire) United Kingdom | −6.4 ± 4.2 ‰ | −9.9 / 0.2 ‰ | 5 | supergene smithsonite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| South Pennine orefield (Derbyshire) United Kingdom | −17.6 ± 3.9 ‰ | −20.4 / −14.9 ‰ | 2 | supergene cerussite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Cloghatrida (Rathkeale) Irlande | −7.1 ‰ | | 1 | supergene smithsonite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| La Calamine and Moresnet district (Vieille-Montagne) Belgique | −8.78 ± 2.7 ‰ | −11.6 / −1.5 ‰ | 14 | supergene smithsonite (Moresnet, La Calamine, Fossey) | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
| La Calamine and Moresnet district (Vieille-Montagne) Belgique | −7.6 ‰ | | 1 | Fe-rich smithsonite (monheimite) from Fossey | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
| La Calamine and Moresnet district (Vieille-Montagne) Belgique | −7.38 ± 1.75 ‰ | −10.4 / −6.1 ‰ | 5 | oxidation-zone calcite associated with smithsonite | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
| La Calamine and Moresnet district (Vieille-Montagne) Belgique | 2.8 ‰ | 2.8 / 2.8 ‰ | 2 | black host dolomite (Tournaisian, La Calamine) | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
| Djebba Tunisie | −10.1 ‰ | | 1 | supergene calcite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Fedj el Adoum Tunisie | −1.7 ± 5.38 ‰ | −5.5 / 2.11 ‰ | 2 | smithsonite (sulfide-associated and concretionary with goethite) | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Fedj el Adoum Tunisie | 0.84 ‰ | | 1 | Triassic host dolomite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Galmoy Irlande | −7.5 ± 0.9 ‰ | −8.6 / −5.7 ‰ | 11 | supergene smithsonite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Galmoy Irlande | −4.3 ± 6 ‰ | −8.6 / −0.1 ‰ | 2 | supergene cerussite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Gays River Canada | 1.21 ± 0.62 ‰ | 0.5 / 1.99 ‰ | 5 | recrystallised host dolomite (pre-ore) | Akande et Zentilli (1984), Geologic, fluid inclusion, and stable isotope studies of the G… |
| Gays River Canada | −1.97 ± 0.59 ‰ | −2.96 / −1.34 ‰ | 7 | dedolomitised secondary limestone | Akande et Zentilli (1984), Geologic, fluid inclusion, and stable isotope studies of the G… |
| Gays River Canada | 2.6 ± 0.36 ‰ | 2.22 / 3.12 ‰ | 10 | ore-stage vein calcite | Akande et Zentilli (1984), Geologic, fluid inclusion, and stable isotope studies of the G… |
| Gays River Canada | −1.97 ± 2.77 ‰ | −5.68 / 1.58 ‰ | 6 | late rhombohedral calcite | Akande et Zentilli (1984), Geologic, fluid inclusion, and stable isotope studies of the G… |
| Gays River Canada | −0.49 ± 0.29 ‰ | −0.7 / −0.29 ‰ | 2 | late scalenohedral encrusting calcite | Akande et Zentilli (1984), Geologic, fluid inclusion, and stable isotope studies of the G… |
| Gays River Canada | 4.31 ± 0.33 ‰ | 3.61 / 4.55 ‰ | 7 | brachiopods of the unmineralised Miller limestone (regional reference) | Akande et Zentilli (1984), Geologic, fluid inclusion, and stable isotope studies of the G… |
| Huize China | −2.81 ± 0.41 ‰ | −3.5 / −2.1 ‰ | 21 | ore gangue calcite (massive, disseminated and veined) | Li et al. (2007), Isotope geochemistry of the Huize Zn-Pb ore field, Yunnan Province, Sou… |
| Huize China | −3.2 ± 0.28 ‰ | −3.4 / −3 ‰ | 2 | NE-trending fault calcite, 150 and 540 m from ore | Li et al. (2007), Isotope geochemistry of the Huize Zn-Pb ore field, Yunnan Province, Sou… |
| Huize China | 0.8 ± 0.42 ‰ | 0.5 / 1.1 ‰ | 2 | karst cavity calcite in Permian carbonates, 450 and 500 m from ore | Li et al. (2007), Isotope geochemistry of the Huize Zn-Pb ore field, Yunnan Province, Sou… |
| Huize China | 0.02 ± 0.67 ‰ | −0.8 / 0.7 ‰ | 4 | coarse host dolomite (Baizuo Formation) | Li et al. (2007), Isotope geochemistry of the Huize Zn-Pb ore field, Yunnan Province, Sou… |
| Jebel Azreg Tunisie | −10.76 ‰ | | 1 | concretionary hydrozincite in cavity | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Jebel Azreg Tunisie | 1.62 ± 1.32 ‰ | 0.69 / 2.55 ‰ | 2 | carbonate host rock (calcite and dolomite) | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Jebel Ben Amara Tunisie | −8.16 ± 0.47 ‰ | −8.49 / −7.83 ‰ | 2 | concretionary smithsonite (two generations) | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Jebel Ben Amara Tunisie | −11.24 ‰ | | 1 | supergene calcite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Jebel Hallouf Tunisie | 5.47 ± 0.66 ‰ | 5 / 5.94 ‰ | 2 | hydrothermal gangue calcite associated with galena | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Jebel Ressas Tunisie | −5.22 ‰ | | 1 | concretionary calcite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Jebel Ressas Tunisie | 2.12 ± 0.42 ‰ | 1.53 / 2.51 ‰ | 4 | Jurassic carbonate host rock (Oust Formation) | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Jebel Trozza Tunisie | −1.78 ‰ | | 1 | hydrozincite veinlet | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Jebel Trozza Tunisie | −1.3 ‰ | | 1 | host dolomite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Kilbricken Irlande | −6.3 ‰ | | 1 | supergene smithsonite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Masua Italy | −5.8 ± 2.96 ‰ | −7.9 / −2.41 ‰ | 3 | supergene smithsonite (Masua-Lanusei) | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Masua Italy | −3.45 ‰ | | 1 | hydrothermal scalenohedral calcite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Mecella Tunisie | −3.79 ± 3.82 ‰ | −6.49 / −1.09 ‰ | 2 | banded and colloform smithsonite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Mecella Tunisie | −7.34 ‰ | | 1 | supergene banded calcite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Mount Agruxiau Italy | −5.75 ± 1.58 ‰ | −6.9 / −3.95 ‰ | 3 | supergene smithsonite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Monteponi Italy | −3.2 ± 2.62 ‰ | −5.83 / −0.59 ‰ | 3 | supergene smithsonite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Monteponi Italy | −2.42 ‰ | | 1 | supergene hydrozincite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Monteponi Italy | −11.63 ‰ | | 1 | supergene cerussite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Monteponi Italy | −8.2 ± 1.47 ‰ | −9.24 / −7.16 ‰ | 2 | supergene phosgenite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Monteponi Italy | −10.01 ± 0.22 ‰ | −10.17 / −9.76 ‰ | 3 | calcite associated with calamine (Nicolay, Villamarina) | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Nanisivik Canada | 2.63 ± 0.38 ‰ | 1.7 / 3.1 ‰ | 21 | unmineralised host dolostone (Society Cliffs Formation) | Ghazban et al. (1990), Carbon and sulfur isotope evidence for in situ reduction of sulfat… |
| Nanisivik Canada | 2.59 ± 2.52 ‰ | −0.8 / 6.3 ‰ | 11 | recrystallised "salt-and-pepper" dolomite of the replacement front | Ghazban et al. (1990), Carbon and sulfur isotope evidence for in situ reduction of sulfat… |
| Nanisivik Canada | −4.91 ± 3.84 ‰ | −13.3 / 0.3 ‰ | 12 | reaction-rim dolomite | Ghazban et al. (1990), Carbon and sulfur isotope evidence for in situ reduction of sulfat… |
| Nanisivik Canada | −5.12 ± 3.49 ‰ | −12.4 / 2.5 ‰ | 65 | ore-stage white sparry dolomite (zebra) | Ghazban et al. (1990), Carbon and sulfur isotope evidence for in situ reduction of sulfat… |
| Nanisivik Canada | −2.96 ± 2.36 ‰ | −5.7 / 2.9 ‰ | 20 | overgrowth calcite | Ghazban et al. (1990), Carbon and sulfur isotope evidence for in situ reduction of sulfat… |
| Nanisivik Canada | −29.34 ± 1.09 ‰ | −30.5 / −27.6 ‰ | 5 | vug bitumen | Ghazban et al. (1990), Carbon and sulfur isotope evidence for in situ reduction of sulfat… |
| Nebida Italy | −6.93 ± 3.3 ‰ | −10.37 / −1.78 ‰ | 9 | supergene smithsonite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Nebida Italy | −9.21 ‰ | | 1 | calcite associated with calamine (Nebida-Carroccia) | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| San Benedetto Italy | −7.95 ‰ | | 1 | supergene smithsonite concretion (type IV) | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| San Vicente Peru | 1.7 ‰ | 0.9 / 2.5 ‰ | 11 | dark replacement dolomite (I) | Spangenberg et al. (1996), Carbon and oxygen isotope study of hydrothermal carbonates in … |
| San Vicente Peru | 1.1 ‰ | −0.1 / 1.7 ‰ | 115 | white sparry dolomite (II), main stage | Spangenberg et al. (1996), Carbon and oxygen isotope study of hydrothermal carbonates in … |
| San Vicente Peru | −0.8 ‰ | −11.5 / 0.7 ‰ | 25 | late void-filling calcite (IIIc) | Spangenberg et al. (1996), Carbon and oxygen isotope study of hydrothermal carbonates in … |
| San Vicente Peru | −2.6 ‰ | −4.5 / 0.8 ‰ | 11 | calcite replacing evaporitic sulfates (EPc) | Spangenberg et al. (1996), Carbon and oxygen isotope study of hydrothermal carbonates in … |
| San Vicente Peru | | −0.3 / 1.1 ‰ | 10 | late void-filling dolomite (IIId) | Spangenberg et al. (1996), Carbon and oxygen isotope study of hydrothermal carbonates in … |
| San Vicente Peru | | 0.4 / 1 ‰ | 7 | dolomite replacing evaporitic sulfates (EPd) | Spangenberg et al. (1996), Carbon and oxygen isotope study of hydrothermal carbonates in … |
| San Vicente Peru | | −27 / −26.4 ‰ | 3 | host-rock organic matter | Spangenberg et al. (1996), Carbon and oxygen isotope study of hydrothermal carbonates in … |
| San Vicente Peru | | −27 / −23 ‰ | 6 | hydrothermal bitumen | Spangenberg et al. (1996), Carbon and oxygen isotope study of hydrothermal carbonates in … |
| Seddas Moddizzis Italy | −5.46 ± 1.48 ‰ | −6.8 / −3.865 ‰ | 3 | supergene smithsonite | Boni et al. (2003), The calamine of southwest Sardinia: geology, mineralogy, and stable i… |
| Sekarna (Saint-Pierre) Tunisie | −5.25 ± 0.91 ‰ | −6.57 / −4.55 ‰ | 4 | concretionary smithsonite (types 1 and 2) | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Sekarna (Saint-Pierre) Tunisie | 1.75 ± 0.36 ‰ | 1.5 / 2.01 ‰ | 2 | carbonate host rock (Metlaoui Group and Abiod Formation) | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Sheshodonnell Irlande | −0.7 ± 0.7 ‰ | −1.3 / 0.1 ‰ | 3 | supergene smithsonite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Silvermines Irlande | −4.9 ‰ | | 1 | supergene smithsonite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Slata Fer Tunisie | −2.52 ‰ | | 1 | hydrothermal calcite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Slata Fer Tunisie | 2.4 ± 0.18 ‰ | 2.27 / 2.52 ‰ | 2 | Aptian host dolomite | Garnit et al. (2018), C-O stable isotopes geochemistry of Tunisian nonsulfide zinc deposi… |
| Theux Belgique | −1.9 ± 0.42 ‰ | −2.2 / −1.6 ‰ | 2 | supergene smithsonite concretion (type V) | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
| Theux Belgique | −14.83 ± 0.15 ‰ | −15 / −14.7 ‰ | 3 | supergene cerussite | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
| Tynagh Irlande | −7.8 ± 5.1 ‰ | −10.9 / 1.3 ‰ | 5 | supergene smithsonite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Tynagh Irlande | −15.4 ± 1.3 ‰ | −16.4 / −13.9 ‰ | 3 | supergene cerussite | Boni et al. (2019), Stable isotopes of nonsulphide Zn-Pb ores in Britain and Ireland: flu… |
| Welkenraedt Belgique | −7.98 ± 2.61 ‰ | −10.2 / −3.2 ‰ | 6 | supergene smithsonite | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
| Welkenraedt Belgique | −18.4 ‰ | | 1 | supergene cerussite | Coppola et al. (2008), The calamine nonsulfide Zn-Pb deposits of Belgium: petrographical,… |
