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hal.structure.identifierSchool of Natural Resources and the Environment
hal.structure.identifierDepartment of Earth System Science
dc.contributor.authorMEREDITH, Laura K.
hal.structure.identifierDepartment of Earth System Science
hal.structure.identifierSLAC National Accelerator Laboratory [SLAC]
dc.contributor.authorBOYE, Kristin
hal.structure.identifierSchool of Natural Resources and the Environment
dc.contributor.authorYOUNGERMAN, Connor
hal.structure.identifierDepartment of Plant Biology [Carnegie] [DPB]
dc.contributor.authorWHELAN, Mary
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorOGÉE, Jérôme
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorSAUZE, Joana
hal.structure.identifierInteractions Sol Plante Atmosphère [UMR ISPA]
dc.contributor.authorWINGATE, Lisa
dc.date.accessioned2024-04-08T12:06:17Z
dc.date.available2024-04-08T12:06:17Z
dc.date.issued2018
dc.identifier.issn2571-8789
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/196394
dc.description.abstractEnUnderstanding soil production of the trace gas carbonyl sulfide (OCS) is key to its use as a tracer of ecosystem function. Underlying its application is the observation that vascular plants consume atmospheric OCS via their stomatal pores in proportion with CO2 photosynthesis and that soil fluxes of OCS are negligible in comparison. Recent soil-centered studies demonstrate that soils can produce OCS and contribute as much as a quarter of the atmospheric terrestrial flux. Despite the potential widespread importance of soil OCS emissions, insufficient data exist to predict variations in OCS production across ecosystems, and the chemical and biological drivers of OCS production are virtually unknown. In this study, we address this knowledge gap by investigating variables controlling OCS soil production including soil physical and chemical properties, microbial community composition, and sulfur speciation in two independent surveys. We found that soil OCS production was nearly ubiquitous across the 58 sites, increased exponentially with temperature, and was insensitive to visible light conditioning. Soil pH, N, and C/N were predictors of OCS soil production rates in both soil surveys. Patterns in soil S speciation and predicted microbial S-cycling pathways both pointed to S-containing amino acids such as cysteine and methionine and their derivatives as potential precursors for OCS production. Elevated sulfate levels were associated with OCS production in some soils. This study provides new mechanistic insight into OCS production in soils and presents strategies to represent soil OCS fluxes that facilitate the use of OCS as a tracer for leaf-level processes related to carbon and water cycling.
dc.language.isoen
dc.publisherMDPI
dc.rights.urihttp://creativecommons.org/licenses/by/
dc.subjectOCS
dc.subjectCOS
dc.subjectsoil
dc.subject.encarbonyl sulfide
dc.subject.ensulfur cycle
dc.subject.encarbon cycle
dc.title.enCoupled biological and abiotic mechanisms driving carbonyl sulfide production in soils
dc.typeArticle de revue
dc.identifier.doi10.3390/soilsystems2030037
dc.subject.halSciences du Vivant [q-bio]
dc.subject.halSciences de l'environnement
dc.description.sponsorshipEuropeCarbonic anhydrase: where the CO2, COS and H2O cycles meet
bordeaux.journalSoil Systems
bordeaux.page1-27
bordeaux.volume2
bordeaux.hal.laboratoriesInteractions Soil Plant Atmosphere (ISPA) - UMR 1391*
bordeaux.issue3
bordeaux.institutionBordeaux Sciences Agro
bordeaux.institutionINRAE
bordeaux.peerReviewedoui
hal.identifierhal-02620680
hal.version1
hal.popularnon
hal.audienceInternationale
hal.origin.linkhttps://hal.archives-ouvertes.fr//hal-02620680v1
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Soil%20Systems&rft.date=2018&rft.volume=2&rft.issue=3&rft.spage=1-27&rft.epage=1-27&rft.eissn=2571-8789&rft.issn=2571-8789&rft.au=MEREDITH,%20Laura%20K.&BOYE,%20Kristin&YOUNGERMAN,%20Connor&WHELAN,%20Mary&OG%C3%89E,%20J%C3%A9r%C3%B4me&rft.genre=article


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