Search results for "CO2 EXCHANGE"

showing 2 items of 2 documents

Ecosystem carbon response of an Arctic peatland to simulated permafrost thaw

2019

Permafrost peatlands are biogeochemical hot spots in the Arctic as they store vast amounts of carbon. Permafrost thaw could release part of these long-term immobile carbon stocks as the greenhouse gases (GHGs) carbon dioxide (CO 2 ) and methane (CH 4 ) to the atmosphere, but how much, at which time-span and as which gaseous carbon species is still highly uncertain. Here we assess the effect of permafrost thaw on GHG dynamics under different moisture and vegetation scenarios in a permafrost peatland. A novel experimental approach using intact plant–soil systems (mesocosms) allowed us to simulate permafrost thaw under near-natural conditions. We monitored GHG flux dynamics via high-resolution…

0106 biological scienceshiilidioksidiPeat010504 meteorology & atmospheric sciencesPermafrostikiroutaPermafrostAtmospheric sciences01 natural sciencesMethaneCO2 EXCHANGEclimate warmingPALSA MIREchemistry.chemical_compoundDissolved organic carbonGeneral Environmental SciencekasvihuoneilmiöGlobal and Planetary ChangeCLIMATE-CHANGEEcologyArctic Regionsmethane oxidationhiilen kiertopermafrost-carbon-feedbackPlantsmesocosmCOORGANIC-MATTERkasvihuonekaasutCH4 FLUXESgreenhouse gasNORTHERN PEATLANDSCarbon dioxideCO2MethaneOxidation-ReductionBiogeochemical cycleTUNDRA SOILSClimate Changeta1172ta1171010603 evolutionary biologymetaaniCarbon CycleGreenhouse GasesMETHANE EMISSIONSEnvironmental Chemistry0105 earth and related environmental sciencesAtmosphere15. Life on landCarbon DioxideWATER-TABLEEXTRACTION METHODArcticchemistry13. Climate actionGreenhouse gasEnvironmental science
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Integrating Decomposers, Methane-Cycling Microbes and Ecosystem Carbon Fluxes Along a Peatland Successional Gradient in a Land Uplift Region

2021

AbstractPeatlands are carbon dioxide (CO2) sinks that, in parallel, release methane (CH4). The peatland carbon (C) balance depends on the interplay of decomposer and CH4-cycling microbes, vegetation, and environmental conditions. These interactions are susceptible to the changes that occur along a successional gradient from vascular plant-dominated systems to Sphagnum moss-dominated systems. Changes similar to this succession are predicted to occur from climate change. Here, we investigated how microbial and plant communities are interlinked with each other and with ecosystem C cycling along a successional gradient on a boreal land uplift coast. The gradient ranged from shoreline to meadows…

DYNAMICSPeatecosystem respirationmethane emissionSphagnumCOMMUNITY COMPOSITIONDecomposerCO2 EXCHANGEbakteeritmethanotrophsmethanogensturvemaatBogFUNGALBiomass (ecology)geography.geographical_feature_categoryEcologybiologyEcologyFUNCTIONAL TYPEShiilen kiertofood and beveragesactinobacteriaFEN ECOSYSTEMprimary paludification1181 Ecology evolutionary biologymicrobial communityEcosystem respirationsienetWATER-LEVEL DRAWDOWNTERMmetaaniEnvironmental ChemistryEcosystembiomassa (ekologia)PLANT-COMMUNITIESVEGETATION SUCCESSION1172 Environmental sciencesEcology Evolution Behavior and Systematicsgeographymicrobial biomassbiology.organism_classificationpeatland developmentmaankohoaminenmikrobistoMicrobial population biologyACTINOBACTERIAL COMMUNITIEShiilinielutEnvironmental sciencefungipeatland development.Ecosystems
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