0000000000245754

AUTHOR

Anthony Gauthier

showing 6 related works from this author

13C differentiation of dissolved organic carbon pool during carbon mineralization in soil from a native deciduous forest and a coniferous plantation

2007

International audience

[SDV] Life Sciences [q-bio][SDE] Environmental Sciencesnative deciduous forestconiferous plantationorganic carboncarbon mineralization[SDV]Life Sciences [q-bio][SDE]Environmental Sciences13CComputingMilieux_MISCELLANEOUSsoil
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13C Differentiation between Dissolved and Solid Organic Carbon in Soils as Induced by Substitution of a Native Deciduous Forest by a Coniferous Forest

2006

International audience

[SDV] Life Sciences [q-bio][SDE] Environmental Sciencesnative deciduous forest13C dissolved[SDV]Life Sciences [q-bio][SDE]Environmental Sciencessolid organic carbonconiferous forestComputingMilieux_MISCELLANEOUSsoil
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Différenciation isotopique (13C) du carbone organique dissous (COD) au cours de la dégradation des matières organiques dans les sols forestiers : inf…

2008

National audience

[SDV] Life Sciences [q-bio][SDE] Environmental Sciencesmatière organique[SDV]Life Sciences [q-bio]différenciation isotopiquecarbone organique dissous[SDE]Environmental SciencesdégradationCOD13Csol forestiervégétationComputingMilieux_MISCELLANEOUS
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13C differentiation of the dissolved organic carbon pool during carbon mineralization in soil from a native deciduous forest and a coniferous plantat…

2007

International audience

[SDV] Life Sciences [q-bio][SDV]Life Sciences [q-bio]ComputingMilieux_MISCELLANEOUS
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Isotopic Differentiation (13C) of Dissolved Organic Carbon and CO2 During Organic Matter Degradation in Forest Soils: Influence of Vegetation

2008

International audience

[SDV] Life Sciences [q-bio][SDE] Environmental Sciencesisotopic differentiation[SDV]Life Sciences [q-bio][SDE]Environmental SciencesCO213Cforest soildissolved organic carbonComputingMilieux_MISCELLANEOUSorganic matter degradation
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Effect of temperature on soil microbial structure and fractionation during C mineralisation

2008

International audience; Microbial carbon mineralization in soils leads to the production of different gaseous or dissolved components that have environmental impacts. Our study deals with the influence of soil temperature on the production of gaseous and dissolved carbon components during carbon mineralization in forest soils in France. After an incubation of soil samples for 42 days at 4 different temperatures, we determined both size and 13C isotopic signature of dissolved organic carbon and CO2 pools. We also characterised the soil microbial community structure (PLFA profiles). While temperature clearly increases the CO2 production, a low decrease of the dissolved organic carbon pool was…

[SDV] Life Sciences [q-bio][SDE] Environmental SciencesC mineralisationeffect of temperature[SDV]Life Sciences [q-bio][SDE]Environmental Sciencesfractionationsoil microbial structurecomplex mixtures
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