Search results for "Rhizosphere"

showing 2 items of 112 documents

Microbial succession of nitrate-reducing bacteria in the rhizosphere of Poa alpina across a glacier foreland in the Central Alps

2006

International audience; Changes in community structure and activity of the dissimilatory nitrate-reducing community were investigated across a glacier foreland in the Central Alps to gain insight into the successional pattern of this functional group and the driving environmental factors. Bulk soil and rhizosphere soil of Poa alpina was sampled in five replicates in August during the flowering stage and in September after the first snowfalls along a gradient from 25 to 129 years after deglaciation and at a reference site outside the glacier foreland (> 2000 years deglaciated). In a laboratory-based assay, nitrate reductase activity was determined colorimetrically after 24 h of anaerobic inc…

glacierTime FactorsMolecular Sequence DataBulk soilEcological successionNitrate reductaseNitrate ReductasePlant RootsMicrobiologydiversitysoil03 medical and health scienceschemistry.chemical_compoundNitrateGermanyBotanyIce Coverpâturin des alpesGlacier forelandPoaEcosystemPhylogenySoil MicrobiologyEcology Evolution Behavior and SystematicsPoa alpina030304 developmental biology0303 health sciencesRhizosphereBacteriabiology030306 microbiologyDiscriminant AnalysisGenetic Variation15. Life on landbiology.organism_classificationmolecular anlysispoa alpina[SDV.MP]Life Sciences [q-bio]/Microbiology and Parasitologychemistrycommunity structureMonte Carlo MethodSoil microbiologyPolymorphism Restriction Fragment LengthEnvironmental Microbiology
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Priming effect increases with depth in a boreal forest soil

2016

Abstract Climate warming increases labile carbon (C) inputs to soil through increased photosynthesis and C allocation belowground. This could counterintuitively lead to losses of soil C via priming effects (PE): the stimulation of soil organic matter (SOM) decomposition caused by labile C addition. Systematic quantification of PEs in different ecosystems is needed. We measured PEs of free-living soil microbes in different layers of a boreal forest soil, and found that the relative magnitude of the PE increased with soil depth. The relationship between relative PE and the added glucose amount also depended on the soil layer. Our results indicate that the decomposition of SOM in deeper soil l…

priming effect010504 meteorology & atmospheric sciencesta1172Soil Sciencechemistry.chemical_elementSoil sciencePhotosynthesiscomplex mixtures01 natural sciencesMicrobiologyboreal forest soilOrganic matterEcosystem0105 earth and related environmental scienceschemistry.chemical_classificationRhizosphereChemistrySoil organic matterTaigata118304 agricultural and veterinary sciences15. Life on landNitrogenC & N interactionsclimate change13. Climate action040103 agronomy & agricultureta11810401 agriculture forestry and fisheriesSoil horizonSoil biology & biochemistry
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