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Carbon isotope fractionation during aerobic biodegradation of trichloroethene by Burkholderia cepacia G4: A tool to map degradation mechanisms

Barth, Johannes A. C. ; Slater, Greg ; Schüth, Christoph ; Bill, Markus ; Downey, Angela ; Larkin, Mike ; Kalin, Robert M. (2002)
Carbon isotope fractionation during aerobic biodegradation of trichloroethene by Burkholderia cepacia G4: A tool to map degradation mechanisms.
In: Applied and Environmental Microbiology, 68 (4)
doi: 10.1128/AEM.68.4.1728-1734.2002
Artikel, Bibliographie

Kurzbeschreibung (Abstract)

The strain Burkholderia cepacia G4 aerobically mineralized trichloroethene (TCE) to CO(2) over a time period of approximately 20 h. Three biodegradation experiments were conducted with different bacterial optical densities at 540 nm (OD(540)s) in order to test whether isotope fractionation was consistent. The resulting TCE degradation was 93, 83.8, and 57.2% (i.e., 7.0, 16.2, and 42.8% TCE remaining) at OD(540)s of 2.0, 1.1, and 0.6, respectively. ODs also correlated linearly with zero-order degradation rates (1.99, 1.11, and 0.64 micromol h(-1)). While initial nonequilibrium mass losses of TCE produced only minor carbon isotope shifts (expressed in per mille delta(13)C(VPDB)), they were 57.2, 39.6, and 17.0 per thousand between the initial and final TCE levels for the three experiments, in decreasing order of their OD(540)s. Despite these strong isotope shifts, we found a largely uniform isotope fractionation. The latter is expressed with a Rayleigh enrichment factor, epsilon, and was -18.2 when all experiments were grouped to a common point of 42.8% TCE remaining. Although, decreases of epsilon to -20.7 were observed near complete degradation, our enrichment factors were significantly more negative than those reported for anaerobic dehalogenation of TCE. This indicates typical isotope fractionation for specific enzymatic mechanisms that can help to differentiate between degradation pathways.

Typ des Eintrags: Artikel
Erschienen: 2002
Autor(en): Barth, Johannes A. C. ; Slater, Greg ; Schüth, Christoph ; Bill, Markus ; Downey, Angela ; Larkin, Mike ; Kalin, Robert M.
Art des Eintrags: Bibliographie
Titel: Carbon isotope fractionation during aerobic biodegradation of trichloroethene by Burkholderia cepacia G4: A tool to map degradation mechanisms
Sprache: Englisch
Publikationsjahr: April 2002
Verlag: American Society for Microbiology
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Applied and Environmental Microbiology
Jahrgang/Volume einer Zeitschrift: 68
(Heft-)Nummer: 4
DOI: 10.1128/AEM.68.4.1728-1734.2002
URL / URN: http://www.ncbi.nlm.nih.gov/pubmed/11916690 http://www.pubme...
Kurzbeschreibung (Abstract):

The strain Burkholderia cepacia G4 aerobically mineralized trichloroethene (TCE) to CO(2) over a time period of approximately 20 h. Three biodegradation experiments were conducted with different bacterial optical densities at 540 nm (OD(540)s) in order to test whether isotope fractionation was consistent. The resulting TCE degradation was 93, 83.8, and 57.2% (i.e., 7.0, 16.2, and 42.8% TCE remaining) at OD(540)s of 2.0, 1.1, and 0.6, respectively. ODs also correlated linearly with zero-order degradation rates (1.99, 1.11, and 0.64 micromol h(-1)). While initial nonequilibrium mass losses of TCE produced only minor carbon isotope shifts (expressed in per mille delta(13)C(VPDB)), they were 57.2, 39.6, and 17.0 per thousand between the initial and final TCE levels for the three experiments, in decreasing order of their OD(540)s. Despite these strong isotope shifts, we found a largely uniform isotope fractionation. The latter is expressed with a Rayleigh enrichment factor, epsilon, and was -18.2 when all experiments were grouped to a common point of 42.8% TCE remaining. Although, decreases of epsilon to -20.7 were observed near complete degradation, our enrichment factors were significantly more negative than those reported for anaerobic dehalogenation of TCE. This indicates typical isotope fractionation for specific enzymatic mechanisms that can help to differentiate between degradation pathways.

Fachbereich(e)/-gebiet(e): 11 Fachbereich Material- und Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften
11 Fachbereich Material- und Geowissenschaften > Geowissenschaften > Fachgebiet Hydrogeologie
Hinterlegungsdatum: 17 Apr 2018 12:14
Letzte Änderung: 10 Mär 2022 14:42
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