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. 2002 Oct;68(10):5191–5194. doi: 10.1128/AEM.68.10.5191-5194.2002

TABLE 1.

13C/12C and D/H isotope fractionation by different aerobic bacterial strains during growth with aromatic hydrocarbonsa

Strain Enzyme mechanism Carbon source ɛCn ɛDl
P. putida strain mt-2 Methyl monooxygenase Toluene −3.3 ± 0.3 −905 ± 71
Methyl monooxygenase m-Xylene −1.7 ± 0.04 NDb
Methyl monooxygenase p-Xylene −2.3 ± 0.3 ND
R. pickettii strain PKO1 Ring monoooxygenase Toluene −1.1 ± 0.2 −16 ± 5.3
P. putida strain F1 Ring dioxygenase Toluene −0.4 ± 0.3 −28 ± 10
P. putida strain NCIB 9816 Ring dioxygenase Naphthalene −0.1 ± 0.2 −65 ± 13
a

Stable carbon isotope fractionation is given as the enrichment factor, ɛn, and was calculated with equations 1 and 2. Hydrogen isotope fractionation with mixtures (50:50) of per-deuterated and nonlabeled substrate was determined with equation 3. The enrichment factor for labeled substances, ɛ1, was determined by equation 2. Mean values ± standard deviation are given based on three independent growth experiments with fivefold isotope analysis per data point.

b

ND, not determined.