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RESEARCH PRODUCT

Spatial distribution of N-cycling microbial communities showed complex patterns in constructed wetland sediments.

Diana E. MarcoDiana E. MarcoLaurent PhilippotGermán TortosaDavid Correa-galeoteDavid BruEulogio J. Bedmar

subject

Biogeochemical cycleGeologic SedimentsDenitrificationconstructed wetlandsNitrogen[SDV]Life Sciences [q-bio]Nitrous OxideSoil scienceWetland010501 environmental sciencesBiologySpatial distribution01 natural sciencesApplied Microbiology and BiotechnologyMicrobiology03 medical and health sciencesDenitrifying bacteriaAmmoniaspatial patterns030304 developmental biology0105 earth and related environmental sciences2. Zero hunger0303 health sciencesgeographygeography.geographical_feature_categoryNitratesEcologyBacteriaCrenarchaeotaAgriculture15. Life on landNitrification6. Clean waterWetlands[SDE]Environmental SciencesConstructed wetlandSpatial ecologyDenitrificationN-cycling microbesNitrificationEnvironmental Pollutants

description

International audience; Constructed wetlands are used for biological treatment of wastewater from agricultural lands carrying pollutants such as nitrates. Nitrogen removal in wetlands occurs from direct assimilation by plants and through microbial nitrification and denitrification. We investigated the spatial distribution of N-cycling microbial communities and genes involved in nitrification and denitrification in constructed wetland sediments receiving irrigation water. We used quantitative real-time PCR (qPCR) to characterize microbial communities. Geostatistical variance analysis was used to relate them with vegetation cover and biogeochemical sediment properties. The spatial distribution of the N-cycling microbial communities of sediments was heterogeneous and complex. Total communities of bacteria and crenarchaea showed different spatial distributions. Analysis of autocorrelation patterns through semivariance indicated a tendency towards a patchy distribution over scales around 10 m for genes involved in the nitrification and denitrification processes. In contrast, biogeochemical sediment properties showed diverse spatial distributions. While almost no patchiness was found for pH and moisture, patchiness at scales between 8 and 10 m was detected for carbon, nitrate and ammonia. Denitrification variables showed spatial autocorrelation at scales comparable to genes. However, denitrifying enzyme activity and potential N2O production showed a common spatial pattern, different from that of the N2O/(N2O + N2).

10.1111/j.1574-6941.2012.01479.xhttps://pubmed.ncbi.nlm.nih.gov/22928965