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Didymo Mat Growth due to Climate Change?

Communiqué de presse

24 février 2014

New research stemming from collaborations between scientists at Queen’s University, l’Institut national de la recherche scientifique (INRS), and Brock University demonstrates that the diatom Didymosphenia geminata (commonly known as didymo or “rock snot”) is not an invasive algal species to eastern Canada. These findings debunk commonly held assumptions of many river ecosystem managers and government authorities across North America regarding contemporary didymo blooms.

This nuisance species was first officially reported in the Gaspésie region of Quebec in the summer of 2006. At the time, the Matapédia River was covered with thick, woolly mats of algal growth on its rocky bottom. Many river management authorities believed that human transfer by recreational users was the most plausible explanation for didymo’s occurrence. Didymo has since proliferated across the region with blooms being observed in more than 25 river ecosystems. Blooms have become a cause for concern because of habitat overlap with juvenile Atlantic salmon and potential negative consequences for vulnerable salmonid populations. An examination of dated lake sediments, the fossil algal assemblages preserved within them, and historical reports has revealed that didymo has been present in these river ecosystems long before 2006.

“The concept of an ‘invasive’ microorganism such as a diatom is flawed,” says lead author Michelle Lavery, a former student at Queen’s University and current Master’s student at the Canadian Rivers Institute (University of New Brunswick, Fredericton). “Didymo has been present in the regional algal community for much longer than many people thought. Instead of human introduction, an environmental trigger is a more probable cause for its recent proliferation.”

Algal remains preserved in dated sediment cores from two lakes in Gaspésie were analyzed along with long-term climatic data and historical algae surveys. Reconstructions of the lakes’ past aquatic communities corroborated historical reports of didymo from the early 20th century and revealed an all-too familiar environmental trend – the likely additional impacts of global climate change on regional algal communities. The authors show that increased regional temperatures beginning ~1970 and earlier ice-out dates may have created conditions favorable to didymo’s growth, enabling the species to proliferate in the mass quantities observed.

“The lack of detailed monitoring data, which is common for almost all aquatic ecosystems, often makes it difficult to determine ‘cause and effect’ when dealing with environmental issues”, notes John Smol, a professor in the Department of Biology who also holds the Canada Research Chair in Environmental Change. “Fortunately, lake sediments can act as a ‘time machine’ to reconstruct these missing data sets. Once again, our study suggests that we may have yet another negative impact of climate warming.”

“We now have a clearer picture of what is causing didymo blooms in these iconic salmon rivers,” says Dr. Joshua Kurek, a Postdoctoral Fellow at Queen’s University, Department of Biology. “However, questions remain - namely the relative importance of didymo as a stressor compared to other threats to juvenile salmon populations.”

This study, published in the Canadian Journal of Fisheries and Aquatic Sciences, refutes the “human-transfer hypothesis” for explaining recent didymo blooms and instead suggests that these blooms may be linked to the far-reaching effects of global climate change on aquatic ecosystems.

Funding for the research was provided by the Atlantic Salmon Conservation Foundation (ASCF) and the Natural Sciences and Engineering Research Council of Canada (NSERC).




Carole-Anne Gillis, Biologiste, B.Sc., SE
Étudiante au Doctorat en Sciences de l'eau    »<)))°>
carole-anne.gillis@aquaconfluence.com
Institut national de la recherche scientifique
Centre Eau Terre Environnement
C.P. 306 Matapédia (QC)
CANADA
T 418 750-5314
F 418 654-2600