As ice the melts, the organic carbon found in permafrost is being released once again after ages of confinement in the soil. It is making its way into Arctic and subarctic lakes and ponds, and modifying their composition. The portrait presented by an international team of researchers that includes Professor Isabelle Laurion of INRS shows the influence that thawing permafrost has on surface water biogeochemistry. Published in Limnology and Oceanography Letters, the results demonstrate that organic carbon from permafrost is making its way into the waters of these regions. This type of carbon is particularly good at absorbing sunlight. As a result, these water bodies are getting increasingly darker and stratified, which affects a number of biological processes in these ecosystems.
Frozen tundra soils are one of the largest pools of organic carbon on the planet. With climate warming, permafrost thawing has accelerated, increasing the risk that a large portion of this carbon will be released into the atmosphere as greenhouse gases. However, little study has been done thus far on the effects of permafrost thaw on Arctic and subarctic ponds. Using chemical, biological, optical, and isotopic measurements, researchers from Québec, Denmark, Finland, and Sweden have analyzed hundreds of samples from 14 circumpolar regions spanning from Alaska to Russia (from the subarctic zone to the High Arctic). The samples were taken between 2002 and 2016 from 253 ponds distributed based on their exposure to permafrost thaw.
Read more at Institut National de la Recherche Scientifique - INRS
Photo Credit: Steve Jurvetson via Wikimedia Commons
