Caddisflies: an agapetus caddisfly
Profile prepared by Celeste Mazzacano, The Xerces Society for Invertebrate Conservation
Agapetus montanus is a saddle case- or tortoise case-making caddisfly endemic to Montana and Idaho; it may also occur in Manitoba. This species is found in moderate gradient, fast flowing, open canopy foothill and mountain streams, where it inhabits the upper surface and sides of cobbles and boulders. Livestock grazing, logging, mining, and extensive recreational use in the national forests where this species occurs may threaten A. montanus habitat. Global climate change could also threaten this species’ habitat in the long-term. Research should focus on understanding the biology of this species and establishing the distribution and population status.
Canada – Species at Risk Act: N/A
Canada – provincial status: Manitoba SNR Not ranked
USA – Endangered Species Act: N/A
USA – state status: Idaho S1 Endangered; Montana S2 Vulnerable
NatureServe: G2 Imperiled
IUCN Red List: N/A
Agapetus montanus has no federal status. It is currently a US Forest Service Species of Concern (SOC) in the Bitterroot, Flathead, and Lolo National Forests in Montana, and is listed as endangered in Idaho and vulnerable to extirpation in Montana.
Agapaetus montanus is a caddisfly in the family Glossosomatidae (saddle case- or tortoise casemakers). Larvae, which reach up to 6 mm (0.24 inches), construct a case from small pebbles and sand grains that resembles a tortoise shell. The case has a domed top and a transverse strap beneath that creates two opening on the ventral surface (underside). The larva clings to the substrate and carries the case with it by extending its thoracic legs through the opening at one end and its anal claws through the opening at the other end. At each successive larval instar, larvae in this family construct a new, larger case; final instar larvae remove the transverse strap, attach the case to the substrate, and pupate within it. Larvae of Agapetus generally construct cases that have larger rocks along the edge. Agapetus larvae can be distinguished from other genera in this family by the presence of 2 small hardened plates (sclerites) on the dorsal surface of the 2nd thoracic segment (mesonotum), instead of 3. Adults are also called “little dark caddisflies”; they are small and moth-like with dark hairy wings held rooflike over their bodies, and long slender antennae.
Agapetus montanus (Denning 1949)
Agapetus montanus larvae occur on the upper surfaces and sides of cobbles and boulders in moderate gradient, fast flowing, foothill to mountain streams. Members of this genus appear to prefer streams that are intermediate between higher elevation, cold mountain streams and large warmer transitional rivers downstream. They are also usually found in stream reaches where the riparian canopy is partially open and less shaded than in forested mountain streams. Agapetus larvae graze beneath the protection of their domed case, scraping algae, diatoms, and fine detritus from the surfaces of rocks (Wiggins 1996). Adults of this species emerge from mid-June to mid-August. Adult caddisflies have reduced mouthparts and lack mandibles, but may ingest liquids.
Agapetus montanus is known from Idaho, Montana, and Manitoba. Agapetus montanus appears to be the only known species in this genus in Montana, where it has been reported from ~30 streams in western and south-central Montana, including Missoula, Mineral, Gallatin, Granite, Powell, Meagher, Flathead, Deer Lodge, Lewis and Clark, Lincoln, Beaverhead, and Sanders Counties. The occurrences in Montana include at least one site in almost every National Forest, including Beaverhead-Deerlodge, Flathead, Gallatin, Helena, Kootenai, Lewis & Clark, and Lolo. In Idaho, A. montanus has been collected from 2 locations at a small mountain stream in the Targhee National Forest around 1800 m (5905 feet) elevation (Beaver Creek, Clarke County). Most of the sites in which this species occurs are managed by the U.S. Forest Service or Bureau of Land Management.
Specific threats to Montana & Idaho populations of A. montanus have not been identified. In Idaho, the Beaverhead Mountain region is a significant portion of this species range, and A. montanus is ranked as a Species of Greatest Conservation Need by the Idaho Department of Fish & Game. The dominant land use in this area is livestock grazing, along with logging, mining, and recreational use such as climbing, biking, hiking, and camping. All of these activities, when unregulated or not subjected to strictly enforced Best Management Practices, can result in impaired water quality due to increased siltation from erosion and runoff, pollutants, increased water temperature, and decreased dissolved oxygen. As a species that requires clean cobble substrate in clear cold streams, A. montanus would be negatively impacted by these types of aquatic habitat degradation.
Global climate change could also pose a long-term threat to the survival of this species. Assessment of climate change trends in North America has already revealed changes in precipitation patterns, stream hydrology, and plant bloom time. Overall, annual mean air temperature increased in North America from 1955-2005, and stream flows in the central Rocky Mountain region have decreased throughout the past century (Rood et al. 2005). The effects of global climate change are projected to include warming in the western mountains, causing snow pack and ice to melt earlier in the season (Field et al. 2007). This could lead to increased flooding early in the spring and drier summer conditions, particularly in arid western areas where snow melt sustains stream flows. Spring and summer snow cover has already been documented as decreasing in the western United States, and drought has become more frequent and intense (Intergovernmental Panel on Climate Change 2007). Floods and droughts are projected to increase in frequency and intensity; erosion is also projected to increase due to decreased soil stability from higher temperatures and reduced soil moisture, and increases in winds and high intensity storms. The projected cumulative effects of continuing global climate change including increased frequency and severity of seasonal flooding and droughts, reduced snow pack to feed stream flow, increased siltation, and increasing air and water temperatures could seriously impair A. montanus habitat.
Field, C.B., Mortsch, L.D., Brklacich, M., Forbes, D.L., Kovacs, P., Patz, J.A., Running, S.W. and Scott, M.J. 2007. Chapter 14: North America. In: Climate Change 2007: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (Parry, M.L., Canziani, O.F., Palutikof, J.P., van der Linden, P.J. and Hanson, C.E., eds.). Cambridge University Press, Cambridge, UK.
Intergovernmental Panel on Climate Change. 2007. Summary for Policymakers. In: Climate Change 2007: Impacts, Adaptation and Vulnerability. Contribution of Working Group II to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (Parry, M.L., Canziani, O.F., Palutikof, J.P., van der Linden, P.J. and Hanson, C.E., eds.). Cambridge University Press, Cambridge, UK.
Newell, R.L. and D.S. Potter. 1973. Distribution of some Montana caddisflies. Proceedings of the Montana Academy of Sciences 33: 12-21.
Newell, R.L. and G.W. Minshall. 1977. An annotated list of the aquatic insects of southeastern Idaho, Part II: Trichoptera. Great Basin Naturalist 37: 253-257.
Rood, S.B., Samuelson, G.M., Weber, J.K., and Wywrot, K.A. 2005. Twentieth-century decline in streamflows from the hydrographic apex of North America. Journal of Hydrology, 306: 215- 233.
Stagliano, David, M., George M. Stephens and William R. Bosworth. 2007. Aquatic Invertebrate Species of Concern on USFS Northern Region Lands. Report to USDA Forest Service, Northern Region. Montana Natural Heritage Program, Helena, Montana and Idaho Conservation Data Center, Boise, Idaho. 95 pp. plus appendices.
Wiggins, G.B. 1996. Larvae of the North American caddisfly genera (Trichoptera). University of Toronto Press, Toronto, Ontario. 2nd Edition. 457 pp.