1973
DOI: 10.1021/bi00732a008
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Initial reactions in the oxidation of ethylbenzene by Pseudomonas putida

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Cited by 133 publications
(63 citation statements)
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“…With an initial rate of product formation of 0.22 mmol of 3-hydroxy-4-picoline/h/g of dried cells, TDO is ϳ4.5% as active on the heterocyclic substrate as it is towards toluene (5.1 mmol of toluene cis-dihydrodiol/h/g of dried cells). The polar nitrogen-containing heterocycle is not transformed as efficiently as are other nonnatural TDO substrates, such as aromatics with bulky substituents and aliphatic olefins (12,22,33) Directed evolution of TDO. Oxygenase activity is often determined by monitoring consumption of exogenously added NADH (16).…”
Section: Resultsmentioning
confidence: 99%
“…With an initial rate of product formation of 0.22 mmol of 3-hydroxy-4-picoline/h/g of dried cells, TDO is ϳ4.5% as active on the heterocyclic substrate as it is towards toluene (5.1 mmol of toluene cis-dihydrodiol/h/g of dried cells). The polar nitrogen-containing heterocycle is not transformed as efficiently as are other nonnatural TDO substrates, such as aromatics with bulky substituents and aliphatic olefins (12,22,33) Directed evolution of TDO. Oxygenase activity is often determined by monitoring consumption of exogenously added NADH (16).…”
Section: Resultsmentioning
confidence: 99%
“…The organism was grown in mineral salts medium (34) or on mineral salts medium agar (2.0%) plates. Toluene was supplied in the vapor phase as previously described (10). Large quantities of cells used in enzyme purification studies were grown with forced aeration at 25°C in 12-liter cultures in a New Brunswick Microferm fermentor.…”
mentioning
confidence: 99%
“…The common soil microorganism Pseudomonas putida is able to utilize ethylbenzene as a sole source of carbon and energy (Fukuda et al 1989;Gibson et al 1973). In some instances, co-oxidation or cometabolism was observed (i.e., ethylbenzene was degraded by Nocardia sp.…”
Section: Sediment and Soilmentioning
confidence: 99%
“…Biotic transformations by aerobic soil microbes involve oxidation of the ethyl side chain to form phenylacetic acid (Van der Linden and Thijsse 1965) and 1-phenylethanol (Bestetti and Galli 1984); ring hydroxylation to form 2,3-dihydroxy-1-ethylbenzene (Gibson et al 1973), 2-hydroxyphenlacetic acid, 4-hydroxyphenylacetic acid, and 2,5-and 3,4-dihydroxyphenylacetic acid (Van der Linden and Thijsse 1965); and ultimate ring cleavage to form straight chain carboxylic acids such as fumaric and acetoacetic acids (Van der Linden and Thijsse 1965). The major degradation pathways for ethylbenzene are summarized in Figure 6-3.…”
Section: Sediment and Soilmentioning
confidence: 99%