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Douglas C.
Currie1, Donna Giberson2,
and Brian V. Brown3
1Centre for Biodiversity and Conservation Biology,
Royal Ontario Museum,
100 Queens Park, Toronto, ON, M5S 2C6
2Department of Biology, University of Prince Edward Island,
550 University Ave., Charlottetown, PEI C1A 4P3
3Entomology Section, Natural History Museum of Los Angeles County,
900 Exposition Boulevard, Los Angeles, CA, 90007, U.S.A.
Introduction
The Canadian north remains among the most inadequately surveyed areas in North America in
terms of its insect fauna. During the late 1940s and early 1950s the
Departments of Agriculture and National Defence collaborated on a project called The
Northern Insect Survey. Although the resulting collections provided valuable insights
about insect diversity in the far north, relatively few sites were sampled and material
collected is unsuitable for modern analysis (e.g., cytology, DNA sequence data). Problems
associated with lack of access and infrastructure continue to hinder efforts to document
insect diversity in much of northern Canada.
With completion of the Insects of the Yukon book, it seems appropriate to
direct attention towards the inadequately surveyed territory between the Mackenzie River
and Hudson Bay. This area, which constitutes mainland Northwest Territories and Nunavut,
corresponds with the Districts of Mackenzie and Keewatin. Scientific Committee members
Doug Currie (Royal Ontario Museum and University of Toronto) and Donna Giberson
(University of Prince Edward Island) are leading a multiyear initiative to survey
representative areas throughout the region. Given the short collecting season and
logistical constraints, the focus of the survey reflects the interests of participating
scientists. However, mass collecting techniques (e.g., Malaise traps, sweep netting,
aquatic kick sampling) provide representatives of many non-target organisms.
The survey is expected to generate valuable new insights about the diversity and
biogeography of northern insects, as well as to provide information about energetics and
food web dynamics.
The Horton River
The Horton River was selected as the venue for the first year of the project because of
its close proximity to the eastern boundary of Beringia. It is situated mainly within the
Northern Interior Plain region of the Mackenzie Lowlands and is characterized by hilly
topography marked with numerous lakes and small streams. Originating north of Great Bear
Lake, the river flows in a northwesterly direction for approximately 700 km before
emptying into Franklin Bay on the Beaufort Sea. There are no settlements along the Horton
River and even the Inuit of Paulatuk (situated some 100 km east on the arctic coast)
rarely travel that far. The water is clear in the upper reaches and flows over
limestone-dominated sedimentary rock through a series of cobble riffles and long deep
pools. The water here is characterised by generally high pH (8.0-8.5) and low conductivity
(160-200 Fs/cm). The surrounding vegetation consists of sedge- and shrub tundra with
scattered black spruce. Spruce, willow and alder are confined mainly to the valley and
south-facing slopes. Approximately 180 km downstream of Horton Lake the river enters an
area with sheer limestone cliffs; and over the next 150 km it flows through a series of
three canyons, each characterised by deep bedrock pools and whitewater rapids. Following
the canyon section the geology changes and the surrounding landscape is characterised by
eroding hillsides and muddy tributaries, which significantly increase the turbidity of the
river. The final 100 km of the Horton River passes through sparsely vegetated badlands
dominated by vast deposits of lignite and sulphur. Lignite spontaneously combusts when
exposed to oxygen and the area is aptly named the Smoking Hills. Tributaries in the
Smoking Hills are muddy and typically highly acidic, reducing the pH of the Horton River
to 6.5-7.5.
The 2000 Horton River Expedition
The process of obtaining a Scientific Research Licence proved to be exceedingly cumbersome
and time consuming. Because our proposal involved two different first nations settlement
regions, approval was needed from both Sahtu and Inuvialuit authorities (i.e., various
Hunters and Trappers Associations and Renewable Resources Councils within the two
regions). The NWT Environmental Impact Screening Committee then reviewed our proposal,
taking into consideration the views and comments of various stakeholders. Finally, a Land
Use Permit from the Inuvialuit Land Administration was needed before a licence could be
issued. It arrived in the mail less than a week before departure.
Our team of 5 entomologists convened in Norman Wells on July 17. Doug
Currie and Donna Giberson were joined by Peter Adler (Clemson University), Brian Brown
(Natural History Museum of Los Angeles), and Malcolm Butler (North Dakota State
University). The five of us, along with our guide Tim Gfeller (Wilderness Adventure
Company), boarded a chartered Twin Otter for the hour and a half flight to Horton Lake. We
carried all our gear and enough food to support our expedition for one month. Given the
absence of roads and the high cost of air transportation, our plan was to travel 620 km by
canoe from Horton Lake to the Beaufort Sea. Although strenuous, this approach gave us
access to a wide variety of microhabitats along the way. The route also provided a
south-to-north transect from the High Subarctic Ecoclimatic Region to the Low Arctic
Ecoclimatic Region.
Although insects were the focus of our expedition the Horton River proved
equally favourable for viewing wildlife. Numerous species of birds were observed including
Arctic loon, ptarmigan, peregrine and gyrfalcons, bald and golden eagles, mergansers,
scoters, plovers, and jaegers, to name a few. Hundreds of caribou were also seen
throughout the journey, along with occasional sightings of muskoxen, moose, fox, wolf, and
grizzly bear. Arctic grayling, lake trout and burbot collected from the Horton
River were welcome additions to our larder.
Twenty four days were needed to travel the entire length of the river with
only 2 days of respite from paddling. The weather ranged from stifling heat (30°C+)
during the first part of the trip to uncomfortably cool (4°C) towards the end. On August
9 a chartered Twin Otter retrieved us from a gravel bar near Franklin Bay and flew us to
Inuvik.

Preliminary results
Black Flies (Diptera: Simuliidae)
Doug Currie and Peter Adler made collections at 52 sites along the Horton River and its
tributaries. Immature stages were collected from watercourses that ranged in width from a
few centimetres to more than 100 metres. Larvae were collected mainly into Carnoys
fixative to facilitate cytological study; selected larvae and adults were fixed in 95%
ethanol to facilitate molecular analysis. Adults were collected through a combination of
Malaise trapping, aspirating from team members and the insides of tents, and rearing of
pupae. Identification at the morphospecies level revealed a total of 18 taxa in 3 genera:
Simulium, Metacnephia, and Cnephia. Although the actual number of species
will undoubtedly be higher following cytological screening, it is clear that the simuliid
fauna is depauperate relative to that of similar drainages in Alaska and the Yukon
Territory. This probably reflects, in part, the short period that the Horton River and its
valley has been deglaciated. Interestingly, the Horton drainage includes species that are
sparsely represented or absent from Beringia. The biogeographical implications of this
pattern are a focus of study. Larvae are currently being studied chromosomally by Peter
Adler. Doug Currie is curating the adults and his University of Toronto graduate student,
Miranda Smith, is analysing molecular sequence data from selected species.
Chironomus (Diptera: Chironomidae)
Mac Butler focused on lentic Chironomidae, especially Chironomus. This genus is
well-studied cytogenetically, and karyotypes are necessary to confirm identification of
most species. In collaboration with an international group of colleagues, he has recently
been investigating biogeographic patterns of genetic variation of Chironomus from
Europe, Siberia, and North America. Twenty lentic habitats were sampled along the 620 km
route: ten pools or ponds (<1m depth), and a like number of small lakes. Chironomus
larvae were found in eight of these sites, and pupal exuviae only were collected from an
additional lake. A number of other lentic Chironomidae larvae were collected as well,
primarily Tanypodinae and Tanytarsini. Chironomus was quite rare in shallow
habitats south of the coastal tundra, but larvae were found in all three ponds sampled in
the Smoking Hills. All Chironomus larvae were fixed for karyotype analysis, but
the material has not yet been examined. It is estimated that at least half a dozen species
will be present, perhaps more. In many cases only a few larvae were collected at each
site, and not all specimens are likely to provide good-quality karyotypes. Material
collected at three sites may be sufficient for characterizing populations in terms of
prevailing inversion frequencies, and hopefully to make comparisons with populations from
other parts of the Holarctic Region. Nonetheless, the simple knowledge of what
cytologically-defined species live in this part of the Arctic is a sufficient outcome from
the expedition.
Phorid flies (Diptera: Phoridae)
Phorid flies were collected using mostly Malaise traps. A total of 28 Malaise trap samples
were collected, most of which were overnight samples; a few traps were left up for two
days worth of collecting. The samples vary widely in the number of insects they contain,
due mostly to variation in the weather: warm sunny days produced large diverse catches
whereas cold overcast days led to sparse collections. The higher flies (Brachycera) are
being removed from the Malaise samples by Brian Brown, after which the residues will be
forwarded to Doug Currie to extract lower flies and Donna Giberson will look at the
mayflies, stoneflies and caddisflies. The phorid fauna has not yet been analyzed in
detail, but it is much more diverse than the literature on northern insects indicates. At
least two genera, Megaselia and Triphleba, were collected, with the former predominating
in numbers and species richness. It was interesting to see that phorid flies were abundant
in samples collected on the tundra. Malaise traps were set on tundra sites using canoe
paddles as poles, when the already sparse black spruce stands along the river disappeared.
Energetics and Food Web Ecology of the Horton System
Donna Giberson took samples representing different aquatic insect feeding guilds at
approximately 20-30 km intervals along the river. Stable isotope (carbon and nitrogen)
analysis of the insect samples, along with potential food sources (e.g., detritus, fine
particulate organic matter, biofilms) should provide information about food sources and
feeding patterns of the dominant taxa. Stable isotope analysis is a chemical analysis of
food sources that takes advantage of the fact that different isotopes of common elements
are sequestered by the body in different, but predictable ways, allowing researchers to
trace food sources and trophic levels by analysing the ratios of the isotopes in the body
tissues. Donna also collected water samples along the river to determine basic water
chemistry variables (DO, pH, conductivity) and primary productivity, in collaboration with
Joseph Culp at the National Hydrology Research Institute. Donna will also be identifying
the Ephemeroptera, Plecoptera, and Trichoptera collected during the trip.
Plans for 2001
Discussions concerning 2001 field season are now underway. We plan to undertake a similar
expedition in Nunavut or northern Manitoba, although a specific destination has yet to be
identified. The Thelon, Kazan, and Seal Rivers have been discussed as possible venues, but
further information is needed about logistical problems associated with each river.
Regardless of the destination chosen, the resulting collections will provide a basis for
comparison with collections made along the Horton River in 2000. A number of western
species attain their eastern limit before Hudson Bay; and other species (e.g., Simulium
giganteum) are known in the Nearctic Region only from the vicinity of Hudson Bay. A
west-to-east transect along any of the three rivers should provide more detailed
information about the distribution and composition of northern insects. Such data are
fundamental to developing sound biogeographical hypotheses. Anyone interested in
participating in this project is encouraged to contact us at the addresses given above.

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