The path from root input to mineral-associated soil carbon is dictated by habitat-specific microbial traits and soil moisture
Noah W. Sokol, Megan Foley, Steven J. Blazewicz, Amrita Bhattacharyya, Nicole DiDonato, Katerina Estera‐Molina, Mary K. Firestone, Alex Greenlon, Bruce A. Hungate, Jeffrey A. Kimbrel, José E. Liquet y González, Marissa Lafler, Maxwell A. T. Marple, Peter Nico, Ljiljana Paša‐Tolić, Eric Slessarev, Jennifer Pett‐Ridge
Topics & Concepts
RhizosphereSoil carbonBiogeochemical cycleMicrobial population biologyBiomass (ecology)δ13CIsotopic signatureBulk soilEnvironmental chemistrySoil organic matterCarbon cycleChemistryBiologyEcologySoil waterStable isotope ratioBacteriaEcosystemPhysicsQuantum mechanicsGeneticsSoil Carbon and Nitrogen DynamicsMicrobial Community Ecology and PhysiologyMycorrhizal Fungi and Plant Interactions