Table 2 Thermodynamic parameters and Gibbs free energies for anaerobic benzoate and hexadecane degradation scenarios

From: Metabolic potential of uncultured bacteria and archaea associated with petroleum seepage in deep-sea sediments

Substrates

Reaction types

Reactions

ΔGo (kJ)

ΔHo (kJ)

ΔG (kJ)a

Hexadecane

1. Hydrogenogenic oxidation

C16H34 + 16H2O → 8CH3COO + 17H2 + 8 H+

1089.1

1069.8

753.3

2. Acetogenic oxidation

C16H34 + 8.5HCO3 → 12.25CH3COO + 3.75 H+ + H2O

176.3

98.4

133.9

3. Complete oxidation

C16H34 + 12.25SO42− → 16HCO3 + 12.25HS + H2O + 3.75 H+

−407.3

24.9

−653.3

Benzoate

4. Hydrogenogenic oxidation

C7H5O2 + 7H2O → 3CH3COO + HCO3 + 3 H2 + 3H+

120.9

117.4

12.8

5. Acetogenic oxidation

C7H5O2 + 0.5HCO3 → 3.75CH3COO + 2.25 H+

−846.3

−1091.3

−950.3

6. Complete oxidation

C7H5O2 + 3.75SO42− + 4H2O → 7HCO3 + 3.755HS + 2.25 H+

−76.2

29.4

−230.7

  1. aThe Gibbs free energies were calculated for deep-sea conditions of 4 °C, 300 atm, pH 8 and 2 mM bicarbonate concentrations31