Skip to main content
. 2016 May 11;113(21):5862–5867. doi: 10.1073/pnas.1521038113

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.