Treeline Emerald (Somatochlora sahlbergi) male on willow at pond along airstrip, Old Crow, Yukon, 67.573° N 139.825° W, 7 July 1983. Photo: Rob Cannings.
March Species of the Month:
Treeline Emerald (Somatochlora sahlbergi )
DSA’s March “Species of the Month” is the Treeline Emerald (Somatochlora sahlbergi) in the family Corduliidae, the Emerald dragonflies. The Treeline Emerald is 48–50 mm in length (approximately 2 inches) and ranges across northern Eurasia, eastwards into Alaska, the Yukon, and a bit of the Northwest Territories. Find out how this species became a favorite subject for Syd and Rob Cannings in the third DSA blog post for 2025.
A Denizen of the Northern Taiga
Back in 1979, I (Syd) was a dragonfly newbie—I’d learned on the fly, as it were, helping my older brother Rob gather information for his Dragonflies of British Columbia handbook (1977). And I had just landed a fantastic job, spending a summer in the Yukon surveying insects as part of the Biological Survey of Canada’s Yukon project.
Before I headed north from Vancouver, odonata expert Dennis Paulson told me to watch out for Somatochlora sahlbergi—an almost mythical dragonfly (it seemed to me) at the time. This dragonfly of the far North was named after the Finnish entomologist, Johan Reinhold Sahlberg (1845–1920). I looked up the species in the third volume of Walker and Corbet’s The Odonata of Canada and Alaska, which had just appeared four years earlier, and they listed only three records for North America: “Kuskokwim River” and Sagwon in Alaska, and Reindeer Depot (now called Reindeer Station) near the mouth of the Mackenzie River in Canada’s Northwest Territories.
Treeline Emerald male (Somatochlora sahlbergi) perched on low vegetation, sheltering from the wind near Nuorgam, Utsjoki municipality, Finland, 24 July 2009. Photo: Sami Karjalainen. From A. Schröter, T. Schneider, E. Schneider, S. Karjalainen, and M. Hämäläinen. 2012. Observations on adult Somatochlora sahlbergi – a species at risk due to regional climate change? (Odonata: Corduliidae). Libellula 31: 41–60. Used with permission.
But although I looked for the species in 1979, I never saw any flying, even though I had briefly driven the just-opened Dempster Highway north past the Arctic Circle and back again. I blamed the foggy weather! I did, however, see an amazing landscape that drew me back again for the next two decades until I finally moved to the Yukon in 2003.
My twin brother Richard (Dick) was tasked with the Yukon insect surveys in 1980, and he focused on the Dempster Highway. Where the highway follows the Ogilvie River, about 65.4° N latitude, he discovered that Treeline Emeralds were common in the valley’s fen ponds and oxbows. We were starting to get to know this mystery beast! I found my first Treeline Emerald the next summer, this time along the Porcupine River in the far north of the Yukon.
Syd Cannings waiting for patrolling Treeline Emeralds (Somatochlora sahlbergi) along the Ogilvie River at km 207, Dempster Highway, Yukon, 65.427° N 138.227° W, 21 July 2009. Photo: Rob Cannings.
The Treeline Emerald is a denizen of the northern taiga—the immense boreal forests stretching across Eurasia and North America. In fact, its southern distributional limit lies farther north than that of any other odonate. In Europe it doesn’t stray south of the Arctic Circle and in northwestern North America most of its populations are north of about 64º N, generally not far from the latitudinal treeline—giving the species its common name. Only in the mountains of eastern and southern Siberia, where it probably lives in isolated populations, does it range south to 51º N. Because the Treeline Emerald lives in remote places, mostly far from roads, dragonfly enthusiasts must undertake a real expedition to find it. Its distribution also seems to be patchy—over its vast range it still is known from fewer than 80 localities.
The range of the Treeline Emerald closely matches the distribution of widespread permafrost—permanently frozen ground. In the northern Yukon and central Alaska, it inhabits peatland ponds underlain by permafrost and topped with floating fen mosses. As you wade out from the pond edge to get close to the patrolling males or ovipositing females, your boots slide on solid ice beneath the peaty muck. In many ponds the slippery ice slopes down to the deep center. You don’t want to fall in! In northern Scandinavia the hummocky tundra habitat of the dragonfly is called “palsa mires”.
Treeline Emerald (Somatochlora sahlbergi) habitat: fen in permafrost along the Blackstone River, Yukon, 65.064º N 138.128º W, 29 June 2019. Photo: Cameron Eckert. Used with permission.
I returned to the Dempster Highway in 1982 and collected several Treeline Emeralds, including many larvae. The larvae clustered into several size-groups, indicating a lifespan of about five, or maybe even six, years—rather long for a modest-sized dragonfly. Larvae were emerging around July 1, and because autumn frosts at that latitude begin in the last two weeks of August, the dragonflies really only can grow during about six weeks each year. Once I knew how to identify the larvae, I discovered that I had found one on my first trip north in 1979! We redescribed the larva based on our collections and documented habitat and other biological information.
Rob Cannings’ illustration of a Treeline Emerald (Somatochlora sahlbergi) larva, from Cannings, S.G. and R.A. Cannings. 1985. The larva of Somatochlora sahlbergi Trybom (Odonata: Corduliidae) with notes on the species in the Yukon Territory, Canada. Odonatologica 14: 3l9–330.
Recent genetic work by Manpreet Kohli and her colleagues shows that the Treeline Emerald has remarkably limited genetic diversity over its immense range on both sides of the Bering Strait. There are several possible explanations for this, but perhaps the most likely one is that colonization of North America occurred relatively recently (less than 10,000 years ago) by a small number of individuals. The relatively long (for a dragonfly) life cycle of the Treeline Emerald would have also limited its post-glacial diversification.
Where its range overlaps with those of the Ringed Emerald (Somatochlora albicincta) and the Hudsonian Emerald (S. hudsonica), considerable hybridization occurs. Hybrids have been found in central Alaska, the Mackenzie River Valley, and the northern Yukon. In these places, obvious hybrids make up about 20 percent of all Emeralds recorded. Hybrids have color patterns and structural characteristics intermediate between those of the parent species.
Rob Cannings hunting Treeline Emeralds (Somatochlora sahlbergi) along the Ogilvie River at km 207, Dempster Highway, Yukon, 65.427º N 138.227º W, 21 July 2009. Photo: Syd Cannings.
Obvious hybrids are not often encountered in dragonfly-watching, and this is the result of “good” female choice. Male dragonflies are not very selective when seeking mates; they will try to mate with any female that is about the right size and shape! It’s the female that decides whether or not to mate. So, apparently, a hybrid results when a female mistakenly accepts a male from a different species. The presence of hybridization in this case tells us that the Treeline Emerald is probably a recent immigrant to North America and is still “learning” to distinguish its new neighbors.
Normally, the three species of emeralds separate themselves by larval habitat: the Treeline Emerald develops in permafrost ponds with floating moss, the Ringed Emerald prefers shallow ponds with little vegetation, and the Hudsonian Emerald lives in ponds with tall sedge edges. But sometimes, wetlands occur that combine two or more of these habitats in close proximity, and in these places the three species may encounter one another.
Treeline Emerald (Somatochlora sahlbergi) habitat; hybrids with Hudsonian Emerald (S. hudsonica) have also been found at this site. Polygon fen in tundra in the Porcupine River drainage, 20 km SW of Old Crow, Yukon, 67.417º N 140.083º W, 5 July1983. Photo: Rob Cannings.
Finally, even though this species can be abundant in its favored habitats, its requirements (permafrost in a dry climate) put the Treeline Emerald at great risk in the face of rapid climate change. The North is warming quickly, much more quickly than temperate areas, and this means that permafrost is disappearing. In parts of the North, the climate is becoming wetter as well, a change which will also reduce the amount of permafrost. I revisited some of my 1982 sites in 2009 and 2019, and evidently the peatlands had dried considerably, presumably because the underlying permafrost had melted. At one site where Treeline Emeralds were once abundant, I could only find the widespread Ringed Emerald.
More thorough monitoring is needed both here and in Eurasia . . . if anyone would like to join in, let us know!
Acknowledgements
We thank Sami Karjalainen and Cameron Eckert for permission to include their photographs.
Our guest bloggers are Syd and Rob Cannings, who grew up beside a grassland in British Columbia’s Okanagan Valley in a family known across Canada for its contributions to natural history and conservation. Both are founding members of the DSA.
Syd has recently retired as a Species at Risk Biologist for the Canadian Wildlife Service in Whitehorse, Yukon. He is an author of several books, including British Columbia: A Natural History and The New B.C. Roadside Naturalist. Email him at syd.cannings@gmail.com.
Rob is an Emeritus Curator at the Royal BC Museum in Victoria, BC, where he was Curator of Entomology from 1980 to 2013. He mainly studies the systematics and faunistics of Odonata and Asilidae (Diptera) but publishes on a variety of insect orders. He is the author of several books, including Introducing the Dragonflies of British Columbia and the Yukon. He can be reached at rcannings@royalbcmuseum.bc.ca.