Articles | Volume 19, issue 17
https://doi.org/10.5194/bg-19-3959-2022
© Author(s) 2022. 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-19-3959-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
31 Aug 2022
Research article |
| 31 Aug 2022
| 31 Aug 2022
The dominant role of sunlight in degrading winter dissolved organic matter from a thermokarst lake in a subarctic peatland
Flora Mazoyer
CORRESPONDING AUTHOR
Laboratoire de limnologie nordique, Centre Eau Terre Environnement, Institut national de la recherche scientifique, Québec, QC, Canada
Centre for Northern Studies, Université Laval, Québec, QC,
Canada
Isabelle Laurion
CORRESPONDING AUTHOR
Laboratoire de limnologie nordique, Centre Eau Terre Environnement, Institut national de la recherche scientifique, Québec, QC, Canada
Centre for Northern Studies, Université Laval, Québec, QC,
Canada
Milla Rautio
Centre for Northern Studies, Université Laval, Québec, QC,
Canada
Laboratoire des sciences aquatiques, Département des sciences fondamentales, Université du Québec à Chicoutimi, Québec, QC, Canada
Related authors
No articles found.
Amélie Pouliot, Isabelle Laurion, Antoine Thiboult, and Daniel F. Nadeau
Biogeosciences, 22, 5413–5433, https://doi.org/10.5194/bg-22-5413-2025, https://doi.org/10.5194/bg-22-5413-2025, 2025
Short summary
Short summary
Small thermokarst lakes release greenhouse gases (GHGs) as permafrost thaws, but most studies focus on diurnal measurements, potentially overlooking significant variations. We measured GHG fluxes from two lakes in Nunavik over two summers – one colder, one warmer – alongside 2 years of continuous water column monitoring. Fluxes were higher in the warmer summer, with strong day–night differences. Our findings show that accurate GHG estimates require full diel measurements and seasonal considerations.
Stéphanie Coulombe, Daniel Fortier, Frédéric Bouchard, Michel Paquette, Simon Charbonneau, Denis Lacelle, Isabelle Laurion, and Reinhard Pienitz
The Cryosphere, 16, 2837–2857, https://doi.org/10.5194/tc-16-2837-2022, https://doi.org/10.5194/tc-16-2837-2022, 2022
Short summary
Short summary
Buried glacier ice is widespread in Arctic regions that were once covered by glaciers and ice sheets. In this study, we investigated the influence of buried glacier ice on the formation of Arctic tundra lakes on Bylot Island, Nunavut. Our results suggest that initiation of deeper lakes was triggered by the melting of buried glacier ice. Given future climate projections, the melting of glacier ice permafrost could create new aquatic ecosystems and strongly modify existing ones.
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Short summary
Dissolved organic matter collected at the end of winter from a peatland thermokarst lake was highly transformed and degraded by sunlight, leading to bacterial stimulation and CO2 production, but a fraction was also potentially lost by photoflocculation. Over 18 days, 18 % of the incubated dissolved organic matter was lost under sunlight, while dark bacterial degradation was negligible. Sunlight could have a marked effect on carbon cycling in organic-rich thermokarst lakes after ice-off.
Dissolved organic matter collected at the end of winter from a peatland thermokarst lake was...
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