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Metagenomics Reveals Pervasive Bacterial Populations and Reduced Community Diversity across the Alaska Tundra EcosystemThawing permafrost increases old soil and autotrophic respiration in tundra: partitioning ecosystem respiration using δ(13) C and ∆(14) C.Circumpolar assessment of permafrost C quality and its vulnerability over time using long-term incubation data.Permafrost degradation stimulates carbon loss from experimentally warmed tundra.Decadal warming causes a consistent and persistent shift from heterotrophic to autotrophic respiration in contrasting permafrost ecosystems.Nitrogen availability increases in a tundra ecosystem during five years of experimental permafrost thaw.Climate change. Permafrost and the global carbon budget.A climate-driven switch in plant nitrogen acquisition within tropical forest communities.Plants, microorganisms, and soil temperatures contribute to a decrease in methane fluxes on a drained Arctic floodplain.Greater temperature sensitivity of plant phenology at colder sites: implications for convergence across northern latitudes.The effect of permafrost thaw on old carbon release and net carbon exchange from tundra.The effect of nutrient deposition on bacterial communities in Arctic tundra soil.Climate change: High risk of permafrost thaw.Carbon loss from an unprecedented Arctic tundra wildfire.A pan-Arctic synthesis of CH4 and CO2 production from anoxic soil incubations.Elucidating the nutritional dynamics of fungi using stable isotopes.NifH-Harboring Bacterial Community Composition across an Alaskan Permafrost Thaw Gradient.Relationships among precipitation regime, nutrient availability, and carbon turnover in tropical rain forests.Quantifying fire severity, carbon, and nitrogen emissions in Alaska's boreal forest.Global patterns of foliar nitrogen isotopes and their relationships with climate, mycorrhizal fungi, foliar nutrient concentrations, and nitrogen availability.Fuel-reduction management alters plant composition, carbon and nitrogen pools, and soil thaw in Alaskan boreal forest.Microbial functional diversity covaries with permafrost thaw-induced environmental heterogeneity in tundra soil.Comparative analysis of cellulose preparation techniques for use with 13C, 14C, AND 18O isotopic measurements.Shifts of tundra bacterial and archaeal communities along a permafrost thaw gradient in Alaska.Ecosystem carbon storage in arctic tundra reduced by long-term nutrient fertilization.Predicting soil carbon loss with warming.Ecology: Nitrogen from the deep.Cross-scale controls on carbon emissions from boreal forest mega-fires.Losing Legacies, Ecological Release, and Transient Responses: Key Challenges for the Future of Northern Ecosystem ScienceRecovery of Aboveground Plant Biomass and Productivity After Fire in Mesic and Dry Black Spruce Forests of Interior AlaskaEvidence and implications of recent and projected climate change in Alaska's forest ecosystemsVulnerability of Permafrost Carbon to Climate Change: Implications for the Global Carbon CycleLegacy of Fire Slows Carbon Accumulation in Amazonian Forest RegrowthBiomass offsets little or none of permafrost carbon release from soils, streams, and wildfire: an expert assessmentLong-term drainage reduces CO<sub>2</sub> uptake and increases CO<sub>2</sub> emission on a Siberian floodplain due to shifts in vegetation community and soil thermal characteristicsStable nitrogen isotope patterns of trees and soils altered by long-term nitrogen and phosphorus addition to a lowland tropical rainforestLong-term CO2 production following permafrost thawNitrogen Isotope Patterns in Alaskan Black Spruce Reflect Organic Nitrogen Sources and the Activity of Ectomycorrhizal FungiPotential carbon emissions dominated by carbon dioxide from thawed permafrost soilsThe Disappearing Cryosphere: Impacts and Ecosystem Responses to Rapid Cryosphere Loss
P50
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P50
name
Edward A G Schuur
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Edward A G Schuur
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Edward A G Schuur
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type
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Edward A G Schuur
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Edward A G Schuur
@en
Edward A G Schuur
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Edward A G Schuur
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Edward A G Schuur
@en
Edward A G Schuur
@nl