Articles | Volume 23, issue 14
https://doi.org/10.5194/bg-23-5239-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-23-5239-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Bacterial community composition changes independently of soil edaphic parameters following localized permafrost disturbance
Patrick Neuberger
Department of Biological Sciences, University of Alberta, Edmonton, T6G 2E9, Canada
Alireza Saidi-Mehrabad
Department of Biological Sciences, University of Alberta, Edmonton, T6G 2E9, Canada
Duane Froese
Department of Earth and Atmospheric Sciences, Edmonton, T6G 2E3, Canada
Department of Biological Sciences, University of Alberta, Edmonton, T6G 2E9, Canada
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Gabrielle K. F. Hatten, Steven V. Kokelj, Sophie Opfergelt, Duane G. Froese, Alejandro Alvarez, Joseph M. Young, and Suzanne E. Tank
EGUsphere, https://doi.org/10.5194/egusphere-2026-1844, https://doi.org/10.5194/egusphere-2026-1844, 2026
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Sorption of organic matter (OM) to recently thawed permafrost sediments can critically alter OM fate. Using 32 sediment samples from a suite of diverse permafrost landscapes, we show that organo-mineral interactions “sort” dissolved OM, enriching the aquatic matrix in labile compounds and increasing biodegradation via shifts in OM composition and nutrient release. Sorption potential varied across and within regions and was tied to sediment characteristics, dictated by landscape history.
Olivia Meier-Legault, Nicholas Brown, Larry Adjun, Michel Allard, Alejandro Alvarez, Maude Auclair, Alex Bevington, Samuel Bilodeau, William Cable, Olivia Carpino, Ariane Castagner, Lin Chen, Alexandre Chiasson, Ryan Connon, Stephanie Coulombe, Jeffrey Crompton, Derek Cronmiller, Gautier Davesne, Mason Dominico, Marc-André Ducharme, Timothy Ensom, Louise Farquharson, Vanessa Foord, Daniel Fortier, Philippe Fortier, Duane Froese, Samuel Gagnon, Francis Gauthier, Marten Geertsema, Etienne Godin, Galina Jonat, Steven V. Kokelj, Michelle Landry, Antoni Lewkowicz, Panya Lipovsky, Emmanual L’Hérault, Hannah Macdonell, Lancelot Massé, Dmitry Nicolsky, Moya Painter, Leesee Papatsie, Victor Pozsgay, William Quinton, Vladimir Romanovsky, Ashley C.A. Rudy, Denis Sarrazin, Emilie Stewart-Jones, Donald Walker, Thomas Wright, Joseph Young, and Stephan Gruber
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2026-96, https://doi.org/10.5194/essd-2026-96, 2026
Revised manuscript under review for ESSD
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Ground temperature data is vital for permafrost and climate research yet data is often fragmented. We created a standardized collection of ground temperatures from over 900 sites across Canada. From 42 published and unpublished sources, we manually verified, cleaned and standardized data with a new software tool. This dataset supports permafrost research on a nationwide scale and can help improve models by acting as a reliable benchmark.
Mahya Roustaei, Joel Pumple, Jordan Harvey, and Duane Froese
The Cryosphere, 19, 4259–4275, https://doi.org/10.5194/tc-19-4259-2025, https://doi.org/10.5194/tc-19-4259-2025, 2025
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This study investigated the application of CT (computed tomography) scanning to tackle the limitations of traditional destructive methods in characterizing permafrost cores. Five different permafrost cores were scanned at resolutions of 65 and 25 μm with new calibration method. The identification of different materials from CT images showed air (gas), ice (excess and pore), and sediments using an Otsu segmentation method. The results were validated by a destructive (cuboid) and a non-destructive method.
Benjamin J. Stoker, Helen E. Dulfer, Chris R. Stokes, Victoria H. Brown, Christopher D. Clark, Colm Ó Cofaigh, David J. A. Evans, Duane Froese, Sophie L. Norris, and Martin Margold
The Cryosphere, 19, 869–910, https://doi.org/10.5194/tc-19-869-2025, https://doi.org/10.5194/tc-19-869-2025, 2025
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The retreat of the northwestern Laurentide Ice Sheet allows us to investigate how the ice drainage network evolves over millennial timescales and understand the influence of climate forcing, glacial lakes and the underlying geology on the rate of deglaciation. We reconstruct the changes in ice flow at 500-year intervals and identify rapid reorganisations of the drainage network, including variations in ice streaming that we link to climatically driven changes in the ice sheet surface slope.
Sophie L. Norris, Martin Margold, David J. A. Evans, Nigel Atkinson, and Duane G. Froese
The Cryosphere, 18, 1533–1559, https://doi.org/10.5194/tc-18-1533-2024, https://doi.org/10.5194/tc-18-1533-2024, 2024
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Associated with climate change between the Last Glacial Maximum and the current interglacial period, we reconstruct the behaviour of the southwestern Laurentide Ice Sheet, which covered the Canadian Prairies, using detailed landform mapping. Our reconstruction depicts three shifts in the ice sheet’s dynamics. We suggest these changes resulted from ice sheet thinning triggered by abrupt climatic change. However, we show that regional lithology and topography also play an important role.
Joel Pumple, Alistair Monteath, Jordan Harvey, Mahya Roustaei, Alejandro Alvarez, Casey Buchanan, and Duane Froese
The Cryosphere, 18, 489–503, https://doi.org/10.5194/tc-18-489-2024, https://doi.org/10.5194/tc-18-489-2024, 2024
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Ice content is a critical variable in the context of thawing permafrost, and permafrost cores provide a means to measure the characteristics of frozen ground; however, these measurements are typically destructive and time intensive. Multi-sensor core logging (MSCL) provides a fast, non-destructive method to image permafrost cores, measure bulk density, and estimate ice content. The use of MSCL will improve existing digital permafrost archives by adding high-quality and reproducible data.
Benjamin J. Stoker, Martin Margold, John C. Gosse, Alan J. Hidy, Alistair J. Monteath, Joseph M. Young, Niall Gandy, Lauren J. Gregoire, Sophie L. Norris, and Duane Froese
The Cryosphere, 16, 4865–4886, https://doi.org/10.5194/tc-16-4865-2022, https://doi.org/10.5194/tc-16-4865-2022, 2022
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The Laurentide Ice Sheet was the largest ice sheet to grow and disappear in the Northern Hemisphere during the last glaciation. In northwestern Canada, it covered the Mackenzie Valley, blocking the migration of fauna and early humans between North America and Beringia and altering the drainage systems. We reconstruct the timing of ice sheet retreat in this region and the implications for the migration of early humans into North America, the drainage of glacial lakes, and past sea level rise.
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Short summary
Permafrost is at increased risk of thaw due to climate change and anthropogenic disturbances. As permafrost thaws, the microbiomes within these systems may become more active and change in composition, releasing greenhouse gases such as CO2 and CH4. In this study, we determined that permafrost thaw caused by road construction caused permafrost microbiomes to become more similar to surface soils, which has implications for greenhouse gas modelling.
Permafrost is at increased risk of thaw due to climate change and anthropogenic disturbances. As...
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