Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
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Plant-derived compounds stimulate the decomposition of organic matter in arctic permafrost soilsMetagenomics Reveals Pervasive Bacterial Populations and Reduced Community Diversity across the Alaska Tundra EcosystemEcosystem responses to warming and watering in typical and desert steppes.Predicted responses of arctic and alpine ecosystems to altered seasonality under climate change.Decadal warming causes a consistent and persistent shift from heterotrophic to autotrophic respiration in contrasting permafrost ecosystems.Permafrost collapse alters soil carbon stocks, respiration, CH4 , and N2O in upland tundra.Nitrogen availability increases in a tundra ecosystem during five years of experimental permafrost thaw.Nonlinear CO2 flux response to 7 years of experimentally induced permafrost thaw.A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.Long-term increase in snow depth leads to compositional changes in arctic ectomycorrhizal fungal communities.Direct and indirect climate change effects on carbon dioxide fluxes in a thawing boreal forest-wetland landscape.Alpine soil carbon is vulnerable to rapid microbial decomposition under climate cooling.Simple additive simulation overestimates real influence: altered nitrogen and rainfall modulate the effect of warming on soil carbon fluxes.Microbial nitrogen dynamics in organic and mineral soil horizons along a latitudinal transect in western Siberia.Shrub encroachment in Arctic tundra: Betula nana effects on above- and belowground litter decomposition.Warming effects on permafrost ecosystem carbon fluxes associated with plant nutrients.Long-term in situ permafrost thaw effects on bacterial communities and potential aerobic respirationPermafrost Degradation and Subsidence Observations during a Controlled Warming ExperimentInitial Stages of Tundra Shrub Litter Decomposition May Be Accelerated by Deeper Winter Snow But Slowed Down by Spring WarmingLong-term experimentally deepened snow decreases growing-season respiration in a low- and high-arctic tundra ecosystemPotential carbon emissions dominated by carbon dioxide from thawed permafrost soilsDetecting the permafrost carbon feedback: talik formation and increased cold-season respiration as precursors to sink-to-source transitionsTransitions in Arctic ecosystems: Ecological implications of a changing hydrological regimeTundra is a consistent source of CO2 at a site with progressive permafrost thaw during 6 years of chamber and eddy covariance measurements
P2860
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P2860
Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
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name
Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
@ast
Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
@en
type
label
Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
@ast
Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
@en
prefLabel
Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
@ast
Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
@en
P2093
P2860
P356
P1433
P1476
Permafrost degradation stimulates carbon loss from experimentally warmed tundra.
@en
P2093
Elizabeth E Webb
Kathryn G Crummer
Susan M Natali
P2860
P304
P356
10.1890/13-0602.1
P407
P577
2014-03-01T00:00:00Z