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Dual C–Cl isotope fractionation offers potential to assess biodegradation of 1,2-dichloropropane and 1,2,3-trichloropropane by Dehalogenimonas cultures

dc.contributor.authorTrueba-Santiso, Alba
dc.contributor.authorTorrentó, Clara
dc.contributor.authorSoder-Walz, Jesica M.
dc.contributor.authorFernández-Verdejo, David
dc.contributor.authorRosell, Mònica
dc.contributor.authorMarco-Urrea, Ernest
dc.date.accessioned2024-10-14T09:06:26Z
dc.date.available2024-10-14T09:06:26Z
dc.date.issued2024-06-01
dc.date.updated2024-10-14T09:06:26Z
dc.description.abstract1,2-dichloropropane (1,2-DCP) and 1,2,3-trichloropropane (1,2,3-TCP) are hazardous chemicals frequently detected in groundwater near agricultural zones due to their historical use in chlorinated fumigant formulations. In this study, we show that the organohalide-respiring bacterium <em style="color:black">Dehalogenimonas alkenigignens</em><span style="color:black"> strain BRE15M can grow during the dihaloelimination of </span>1,2-DCP and 1,2,3-TCP to propene and allyl chloride, respectively. Our work also provides the first application of dual isotope approach to investigate the anaerobic reductive dechlorination of 1,2-DCP and 1,2,3-TCP. Stable carbon and chlorine isotope fractionation values for 1,2-DCP (Ɛ<sub>C </sub>= -13.6 ± 1.4 ‰ and Ɛ<sub>Cl</sub>= -27.4 ± 5.2 ‰) and 1,2,3-TCP (Ɛ<sub>C </sub>= -3.8 ± 0.6 ‰ and Ɛ<sub>Cl</sub>= -0.8 ± 0.5 ‰) were obtained resulting in distinct dual isotope slopes (Λ<sub>12DCP</sub>= 0.5 ± 0.1, Λ<sub>123TCP</sub>= 4 ± 2). However direct comparison of Λ<sub>C-Cl</sub> among different substrates is not possible and investigation of the C and Cl apparent kinetic isotope effects lead to the hypothesis that <em>concerted </em>dichloroelimination mechanism is more likely for both compounds. In fact, whole cell activity assays using cells suspensions of the <em>Dehalogenimonas</em>-containing culture grown with 1,2-DCP and methyl viologen as electron donor suggest that the same set of reductive dehalogenases was involved in the transformation of 1,2-DCP and 1,2,3-TCP. This study opens the door to the application of isotope techniques for evaluating biodegradation of 1,2-DCP and 1,2,3-TCP, which often co-occur in groundwaters near agricultural fields.
dc.format.extent11 p.
dc.format.mimetypeapplication/pdf
dc.identifier.idgrec748322
dc.identifier.issn0045-6535
dc.identifier.urihttps://hdl.handle.net/2445/215727
dc.language.isoeng
dc.publisherElsevier Ltd
dc.relation.isformatofReproducció del document publicat a: https://doi.org/10.1016/j.chemosphere.2024.142170
dc.relation.ispartofChemosphere, 2024, vol. 358
dc.relation.urihttps://doi.org/10.1016/j.chemosphere.2024.142170
dc.rightscc-by-nc-nd (c) The Author(s), 2024
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.sourceArticles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)
dc.subject.classificationHidrologia d'aigües subterrànies
dc.subject.classificationContaminació de l'aigua
dc.subject.classificationIsòtops
dc.subject.otherGroundwater hydrology
dc.subject.otherWater pollution
dc.subject.otherIsotopes
dc.titleDual C–Cl isotope fractionation offers potential to assess biodegradation of 1,2-dichloropropane and 1,2,3-trichloropropane by Dehalogenimonas cultures
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/acceptedVersion

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