For the first time, researchers have successfully dated the carbon dioxide (CO2) and methane (CH4) emitted by ponds and lakes on Bylot Island, Nunavut.
The research team observed significant variability in age and emission rates of greenhouse gases (GHG) from aquatic systems located in a continuous permafrost zone. The study, whose lead author is Frédéric Bouchard affiliated to the INRS Eau Terre Environnement Research Centre and the Geography Department of Université de Montréal, appeared in the international journal Biogeosciences.
Ils ont observé des différences significatives quant à l’âge et au taux d’émission de ces gaz à effet de serre (GES) provenant de ces écosystèmes aquatiques situés en zone de pergélisol. Ces résultats sont publiés dans un article de la revue internationale Biogeosciences, dont le premier auteur est le chercheur postdoctoral Frédéric Bouchard du Centre Eau Terre Environnement de l’INRS et du Département de géographie de l’Université de Montréal.
Gas samples taken over the summer showed strikingly different ages and emission rates depending on the size and depth of the water bodies. Carbon-14 dating revealed that gas emitted by shallow ponds was a few centuries old, making it relatively “young”. Certain ponds, covered by cyanobacterial mats, were identified as CO2 sinks and sources of CH4; others, with eroded banks, were significant emitters of both GHG. Compared to ponds, arctic lakes were found to release much older GHG—up to 3,500 years old in the case of CH4—but at a much slower rate, at least in summer.
“This study demonstrates the significant impact of the combined geomorphological, limnological, and hydrological properties of aquatic systems on CO2 and CH4 emissions caused by thawing permafrost.”Isabelle Laurion
The research team approach enabled an estimation of GHG emissions caused by two distinct processes: diffusion and ebullition. Researchers found that diffusion can be a significant mode of emission, especially from ponds. Until now, ebullition had been considered the predominant mode of CH4 emissions in lake systems. “This study on the age of GHG emitted in the Canadian Arctic is one of very few using data from lakes outside of Siberia or Alaska. It sheds light on the specific role played by aquatic systems on carbon dynamics associated with thawing permafrost, and their potential impact on future climate change,” stated researcher Frédéric Bouchard.
This work sets the scene for further research that must not only measure gas exchange rates, but also account for the age of carbon emitted, since this will impact the systems’ potential positive feedback effect on climate.
This research was conducted by Frédéric Bouchard, Isabelle Laurion, and Vilmantas Prėskienis, of the INRS Eau Terre Environnement Research Centre, along with Daniel Fortier of Université de Montréal, Xiaomei Xu of University of California, and Michael J. Whiticar of University of Victoria. The resulting article, “Modern to millennium‐old greenhouse gases emitted from ponds and lakes of the Eastern Canadian Arctic (Bylot Island, Nunavut),” was recently published in the international journal Biogeosciences (DOI: 10.5194/bg-12-7279-2015). Financial support for the research team was provided by ArcticNet, the Natural Sciences and Engineering Research Council of Canada (NSERC), Natural Resources Canada’s Polar Continental Shelf Program, NSERC’s Discovery Frontiers and EnviroNorth programs, and the W. Garfield Weston Foundation.
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