Seasonal patterns in greenhouse gas emissions from lakes and ponds in a High Arctic polygonal landscape

• Published in: Limnology and Oceanography
• Main Authors: Prėskienis, Vilmantas, Laurion, Isabelle, Bouchard, Frédéric, Douglas, Peter M. J., Billett, Michael F., Fortier, Daniel, Xu, Xiaomei
• Other Authors: Natural Environment Research Council, Natural Resources Canada, Natural Sciences and Engineering Research Council of Canada, W. Garfield Weston Foundation
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2021
• Subjects: Arctic; Ice; permafrost; Thermokarst; Tundra; wedge*
• Online Access: http://dx.doi.org/10.1002/lno.11660; https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11660; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.11660; https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.11660

Abstract Lakes and ponds can be hotspots for CO 2 and CH 4 emissions, but Arctic studies remain scarce. Here we present diffusive and ebullition fluxes collected over several years from 30 ponds and 4 lakes formed on an organic‐rich polygonal tundra landscape. Water body morphology strongly affects the mixing regime—and thus the seasonal patterns in gas emissions—with ice‐out and autumnal turnover periods identified as hot moments in most cases. The studied thermokarst lake maintained relatively high ebullition rates of millennia‐old CH 4 (up to 3405 14 C YBP). Larger and deeper kettle lakes maintained low fluxes of both gases (century to millennium‐old), slowly turning into a CO 2 sink over the summer. During winter, lakes accumulated CO 2 , which was emitted during the ice‐out period. Coalescent polygonal ponds, influenced by photosynthesizing benthic mats, were continuous CO 2 sinks, yet important CH 4 emitters (modern carbon). The highest fluxes were recorded from ice‐wedge trough ponds (up to 96 mmol CO 2 equivalent m −2 d −1 ). However, despite clear signs of permafrost carbon inputs via active shore erosion, these sheltered ponds emitted modern to century‐old greenhouse gases. As the ice‐free period lengthens, scenarios of warmer and wetter conditions could favor both the production of CO 2 and CH 4 from thawing permafrost carbon, and CH 4 production from recently fixed carbon through an atmospheric CO 2 ‐to‐CH 4 shunt at sites in which primary production is stimulated. This must be carefully considered at the landscape scale, recognizing that older carbon stocks can be mineralized efficiently in specific locations, such as in thermokarst lakes.