Soil organic matter properties drive microbial enzyme activities and greenhouse gas fluxes along an elevational gradient
dc.contributor.author
dc.date.accessioned
2024-09-25T11:09:00Z
dc.date.available
2024-09-25T11:09:00Z
dc.date.issued
2024-09
dc.identifier.issn
1872-6259
dc.identifier.uri
dc.description.abstract
Mountain ecosystems, contributing substantially to the global carbon (C) and nitrogen (N) biogeochemical cycles, are heavily impacted by global changes. Although soil respiration and microbial activities have been extensively studied at different elevation, little is known on the relationships between environmental drivers, microbial functions, and greenhouse gas fluxes (GHGs; carbon dioxide [CO2], methane [CH4] and nitrous oxide [N2O]) in soils of different elevation. Here, we measured how in situ GHG fluxes were linked to soil properties, soil organic matter (SOM) quantity and composition (the proportion of humic-like vs. protein-like OM), microbial biomass, enzyme activities and functional gene abundances in natural soils spanning an elevational gradient of ∼2400 m in Switzerland. Soil CO2 fluxes did not significantly vary from low (lowland zone) to higher (montane and subalpine zones) elevation forests, but decreased significantly (P<0.001) from the treeline to the mountain summit. Multivariate analyses revealed that CO2 fluxes were controlled by C-acquiring enzymatic activities which were mainly controlled by air mean annual temperature (MAT) and SOM quantity and composition. CH4 fluxes were characterized by uptake of atmospheric CH4, but no trend was observed along the elevation. N2O fluxes were also dominated by uptake of atmospheric N2O. The flux rates remained stable with increasing elevation below the treeline, but decreased significantly (P<0.001) from the treeline to the summit. N2O fluxes were driven by specific nitrifying and denitrifying microbial genes (ammonia-oxidizing amoA and N2O-producing norB), which were again controlled by SOM quantity and composition. Our study indicates the treeline as a demarcation point changing the patterns of CO2 and N2O fluxes along the elevation, highlighting the importance of SOM quantity and composition in controlling microbial enzyme activities and GHG fluxes
dc.description.sponsorship
Aquest estudi ha estat finançat per la Fundació Nacional de Ciència Suïssa (SNF 31BD30_193667), l' Agència Estatal d'Investigació Espanyola (PCI2020-120702-2/AEI/10).13039/501100011033), el Fons d'Innovació Dinamarca (BiodivClim-76 GRADCATCH), i el Departament de Ciència i Innovació de la República de Sud-àfrica (GRADCATCH), a través del
2019-2020 BiodivERsUna convocatòria conjunta de propostes de recerca, dins del programa BiodivClim ERA-Net COFUND
dc.format.mimetype
application/pdf
dc.language.iso
eng
dc.publisher
Elsevier
dc.relation
PCI2020-120702-2
dc.relation.isformatof
Reproducció digital del document publicat a: https://doi.org/10.1016/j.geoderma.2024.116993
dc.relation.ispartof
Geoderma, 2024, vol. 449, art. núm. 116993
dc.relation.ispartofseries
Articles publicats (D-CCAA)
dc.rights
Attribution 4.0 International
dc.rights.uri
dc.subject
dc.title
Soil organic matter properties drive microbial enzyme activities and greenhouse gas fluxes along an elevational gradient
dc.type
info:eu-repo/semantics/article
dc.rights.accessRights
info:eu-repo/semantics/openAccess
dc.relation.projectID
info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PCI2020-120702-2/ES/USING NATURAL ENVIRONMENTAL GRADIENTS TO DECIPHER THE ADAPTATION OF SOIL MICROBIAL COMMUNITIES TO CLIMATE CHANGE/
dc.type.version
info:eu-repo/semantics/publishedVersion
dc.identifier.doi
dc.identifier.idgrec
039107
dc.contributor.funder
dc.type.peerreviewed
peer-reviewed
dc.relation.FundingProgramme
dc.relation.ProjectAcronym
dc.identifier.eissn
0016-7061
dc.description.ods
13. Acció climàtica