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Table 1 Isotopic compositions of calcites and CO2 content in the Ongeluk basaltic andesites and hydrothermal jaspilites

From: Weak hydrothermal carbonation of the Ongeluk volcanics: evidence for low CO2 concentrations in seawater and atmosphere during the Paleoproterozoic global glaciation

Sample no.

Rock type

Classification of calcite

CO2 (wt%)

δ13C (VPDB, ‰)

δ18O (VPDB, ‰)

Temperature (°C)a

GU033

Basaltic andesite

Disseminated

0

− 14.2

− 15.2

123

GU034

Basaltic andesite

Disseminated

0

− 15.6

− 13.8

109

GU035

Basaltic andesite

Disseminated

0

− 13.2

− 14.6

117

GU036

Basaltic andesite

Disseminated

0.01

− 15.8

− 15.8

130

GU037

Basaltic andesite

Disseminated

0.01

− 16.1

− 14.3

114

GU038

Basaltic andesite

Disseminated

0

− 15.9

− 12.9

100

GU041

Basaltic andesite

Disseminated

0

− 18.9

− 14.1

112

GU045

Basaltic andesite

Disseminated

0

− 18.3

− 13.3

104

GU048

Basaltic andesite

Disseminated

0

− 15.7

− 13.2

103

GU049

Basaltic andesite

Disseminated

0

− 14.9

− 14.6

117

GU054

Basaltic andesite

Disseminated

0

− 23.5

− 14.3

114

GU055

Basaltic andesite

Disseminated

0.01

− 24.9

− 15

121

GU063

Basaltic andesite

Disseminated

0

− 22.3

− 12.3

94

GU110

Pillowed basaltic andesite (core)

Disseminated

0

− 15.6

− 10.2

77

GU172

Basaltic andesite

Disseminated

0

− 18.0

− 10.8

82

GU174

Basaltic andesite with calcite veins

Disseminated/vein

0.060

− 16.1

− 17.1

147

GU144

Interpillow jaspilite

–

0

− 17.0

− 17.6

153

GU149

Interpillow jaspilite

–

0

− 21.3

− 13.4

105

GU151

Interpillow jaspilite

–

0.01

− 31.9

− 17.9

158

GU150

Interpillow jaspilite with calcite/quartz veins

–

0.1

− 15.4

− 17.7

155

GU158

Brecciated interpillow jaspilite

–

0.05

− 12.5

− 17.8

156

  1. aFormation temperature was estimated from the reported oxygen fractionation factor (O’Neil et al. 1969; Friedman and O’Neil 1977; Chacko et al. 2001) assuming a fluid with δ18O = 0‰ (SMOW)