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60. Influence of site and soil properties on the DRIFT spectra of northern cold-region soils R. Matamala et al. 10.1016/j.geoderma.2017.05.014
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412. Plant community regulates decomposer response to freezing more strongly than the rate or extent of the freezing regime S. Sistla et al. 10.1002/ecs2.2608
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486. Long‐term Impacts of Permafrost Thaw on Carbon Storage in Peatlands: Deep Losses Offset by Surficial Accumulation L. Heffernan et al. 10.1029/2019JG005501
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488. Quantifying exchangeable base cations in permafrost: a reserve of nutrients about to thaw E. Mauclet et al. 10.5194/essd-15-3891-2023
489. Integrating Arctic Plant Functional Types in a Land Surface Model Using Above‐ and Belowground Field Observations B. Sulman et al. 10.1029/2020MS002396
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492. Transformation of terrestrial organic matter along thermokarst-affected permafrost coasts in the Arctic G. Tanski et al. 10.1016/j.scitotenv.2016.12.152
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496. Boreal forest soil CO2 and CH4 fluxes following fire and their responses to experimental warming and drying X. Song et al. 10.1016/j.scitotenv.2018.07.014
497. Fluvial CO2 and CH4 patterns across wildfire‐disturbed ecozones of subarctic Canada: Current status and implications for future change R. Hutchins et al. 10.1111/gcb.14960
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500. Spatial variation in vegetation productivity trends, fire disturbance, and soil carbon across arctic-boreal permafrost ecosystems M. Loranty et al. 10.1088/1748-9326/11/9/095008
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502. Nitrogen limitation of microbial activity in alpine tundra soils along an environmental gradient: Intra-seasonal variations and effect of rising temperature M. Maslov & O. Maslova 10.1016/j.soilbio.2021.108234
503. High abundance of protein-like fluorescence in the Amerasian Basin of Arctic Ocean: Potential implication of a fall phytoplankton bloom M. Chen et al. 10.1016/j.scitotenv.2017.04.233
504. Thawing Permafrost as a Nitrogen Fertiliser: Implications for Climate Feedbacks E. Burke et al. 10.3390/nitrogen3020023
505. Ice Wedge Degradation and Stabilization Impact Water Budgets and Nutrient Cycling in Arctic Trough Ponds J. Koch et al. 10.1029/2018JG004528
506. High resolution mapping shows differences in soil carbon and nitrogen stocks in areas of varying landscape history in Canadian lowland tundra J. Wagner et al. 10.1016/j.geoderma.2023.116652
507. The evolution of biogeochemistry: revisited T. Bianchi 10.1007/s10533-020-00708-0
508. Vegetation, recent pollen deposition, and distribution of some non-pollen palynomorphs in a degrading ice-wedge polygon mire complex near Pokhodsk (NE Siberia), including size-frequency analyses of pollen attributable to Betula P. de Klerk et al. 10.1016/j.revpalbo.2016.11.015
509. Effect of temperature on carbon accumulation in northern lake systems over the past 21,000 years G. Pfalz et al. 10.3389/feart.2023.1233713
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511. Simulated responses and feedbacks of permafrost carbon under future emissions pathways and idealized solar geoengineering scenarios Y. Chen et al. 10.1088/1748-9326/ad2433
512. A New Process‐Based Soil Methane Scheme: Evaluation Over Arctic Field Sites With the ISBA Land Surface Model X. Morel et al. 10.1029/2018MS001329
513. Modern to millennium-old greenhouse gases emitted from ponds and lakes of the Eastern Canadian Arctic (Bylot Island, Nunavut) F. Bouchard et al. 10.5194/bg-12-7279-2015
514. Drainage enhances modern soil carbon contribution but reduces old soil carbon contribution to ecosystem respiration in tundra ecosystems M. Kwon et al. 10.1111/gcb.14578
515. 14 CO 2 analysis of soil gas: Evaluation of sample size limits and sampling devices A. Wotte et al. 10.1016/j.nimb.2017.10.009
516. Thousands of tons of mercury are trapped in permafrost J. Miller 10.1063/PT.3.3889
517. A revised pan-Arctic permafrost soil Hg pool based on Western Siberian peat Hg and carbon observations A. Lim et al. 10.5194/bg-17-3083-2020
518. Permafrost Causes Unique Fine‐Scale Spatial Variability Across Tundra Soils M. Siewert et al. 10.1029/2020GB006659
519. We Must Stop Fossil Fuel Emissions to Protect Permafrost Ecosystems B. Abbott et al. 10.3389/fenvs.2022.889428
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522. Plants, microorganisms, and soil temperatures contribute to a decrease in methane fluxes on a drained Arctic floodplain M. Kwon et al. 10.1111/gcb.13558
523. Methane Efflux Measured by Eddy Covariance in Alaskan Upland Tundra Undergoing Permafrost Degradation M. Taylor et al. 10.1029/2018JG004444
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525. Towards a more detailed representation of high-latitude vegetation in the global land surface model ORCHIDEE (ORC-HL-VEGv1.0) A. Druel et al. 10.5194/gmd-10-4693-2017
526. Structural Characterization of Dissolved Organic Matter in Permafrost Peatland Lakes D. Folhas et al. 10.3390/w12113059
527. Future projection of greenhouse gas emissions due to permafrost degradation using a simple numerical scheme with a global land surface model T. Yokohata et al. 10.1186/s40645-020-00366-8
528. Warming effects on permafrost ecosystem carbon fluxes associated with plant nutrients F. Li et al. 10.1002/ecy.1975
529. Stable Water Isotope Assessment of Tundra Wetland Hydrology as a Potential Source of Arctic Riverine Dissolved Organic Carbon in the Indigirka River Lowland, Northeastern Siberia S. Takano et al. 10.3389/feart.2021.699365
530. Herbivory changes soil microbial communities and greenhouse gas fluxes in a high-latitude wetland K. Foley et al. 10.1007/s00248-021-01733-8
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