Table 1 Fe‒S‒C‒O stable isotope composition.

From: Sulphate-reducing bacteria-mediated pyrite formation in the Dachang Tongkeng tin polymetallic deposit, Guangxi, China

Sample

Composition

δ56Fe (‰)

δ34S (‰)

δ13C-PDB

δ18O-PDB

Pyrrhotite

Pyrite

Pyrrhotite

Pyrite

(‰)

(‰)

TK-53-1

Fe-sulphides

0.03

0.11

 − 4.49

 − 4.17

  

TK-53-2

Fe-sulphides

 − 0.43

0.77

 − 4.80

 − 4.30

  

TK-53-3

Fe-sulphides

0.71

0.78

 − 4.91

 − 4.82

  

Mean

 

0.10

0.55

 − 4.73

 − 4.43

  

TK-53-organic 1

Organic carbon

    

 − 35.67

 

TK-53-organic 2

Organic carbon

    

 − 33.63

 

TK-53-organic 3

Organic carbon

    

 − 35.15

 

Mean

     

 − 34.82

 

TK-53-carbon 1

Calcite

    

 − 0.11

 − 15.73

TK-53-carbon 2

Calcite

    

 − 0.60

 − 16.72

TK-53-carbon 3

Calcite

    

 − 0.50

 − 18.92

Mean

     

 − 0.40

 − 17.12