Table S1.
Results of DNA and biomass PO4 oxygen isotope analyses for 14 1-L batch culture experiments and calculation of the metabolic water component of intracellular water
| Microbial strains | T, °C | δ18OH2O, ‰ | δ18OPO4, ‰ | δ18OH2O,* ‰ | 1,000 ln α (PO4−H2O) |
| DNA | |||||
| P. fluorescens | 23 | −5.05 | 17.2 | −4.6 | 21.6 |
| 30 | −5.01 | 16.8 | −4.5 | 21.2 | |
| 37 | −5.02 | 14.0 | −4.6 | 18.5 | |
| Acinetobacter | 23 | −5.56 | 17.9 | −4.9 | 22.7 |
| 30 | −5.32 | 16.1 | −4.8 | 20.7 | |
| 37 | −5.09 | 15.5 | −4.6 | 20.0 | |
| M. aquaeolei | 24 | −5.57 | 17.4 | −4.9 | 22.2 |
| 37 | −5.54 | 13.9 | −4.9 | 18.7 | |
| 30 | 6.30 | 24.5 | 3.3 | 20.9 | |
| 37 | 6.28 | 22.0 | 3.3 | 18.5 | |
| 45 | 6.34 | 22.8 | 3.3 | 19.3 | |
| 30 | 28.75 | 39.5 | 18.8 | 20.2 | |
| 37 | 28.47 | 38.7 | 18.6 | 19.6 | |
| 45 | 28.20 | 39.3 | 18.4 | 20.3 | |
| Biomass | |||||
| P. fluorescens | 23 | −5.05 | 17.2 | −4.4 | 21.4 |
| 30 | −5.01 | 16.5 | −4.4 | 20.7 | |
| 37 | −5.02 | 15.3 | −4.4 | 19.6 | |
| Acinetobacter | 23 | −5.56 | 16.6 | −4.7 | 21.2 |
| 30 | −5.32 | 16.1 | −4.6 | 20.6 | |
| 37 | −5.09 | 15.9 | −4.4 | 20.2 | |
| M. aquaeolei | 24 | −5.57 | 16.8 | −4.7 | 21.4 |
| 37 | −5.54 | 15.2 | −4.7 | 20.3 | |
| 30 | 6.30 | 23.4 | 2.3 | 20.8 | |
| 37 | 6.28 | 22.4 | 2.3 | 19.9 | |
| 45 | 6.34 | 21.1 | 2.3 | 18.6 | |
| 30 | 28.75 | 37.7 | 15.5 | 21.6 | |
| 37 | 28.47 | 35.0 | 15.4 | 19.2 | |
| 45 | 28.20 | 35.3 | 15.2 | 19.6 |
The δ18OH2O value of intracellular water is recalculated based on the assumption that metabolic water with a δ18OH2O value of −3.5‰ accounts for 31% (for DNA) and 41% (for biomass) of intracellular water.