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During summer in the Mackenzie Mountains, caribou spend much
of their time sitting on high elevation ice patches seeking
relief from summer insect swarms and warm afternoon temperatures. Recent
research in the Yukon indicates that this relationship has
persisted for millennia and has been recorded in the ice. Ice
patches formed as annual net accumulations of snow were gradually
compressed into permanent ice lenses and, in the process, the
ancient remains of caribou – bone, antler and primarily
dung – were incorporated and preserved within the ice. Humans
have known of this relationship for millennia and have a long
history of hunting caribou on ice patches, sometimes losing
or discarding their hunting implements in the process. Currently,
with changing climate regimes, melting alpine ice patches in
the Yukon are yielding caribou remains and hunting implements,
providing a material record spanning the last 8,000 years. This
record includes unique examples of Aboriginal hunting implements
with preserved organic parts, a remarkable development for
the archaeological record of the Subarctic, where the organic
components of artifacts are quickly degraded by acidic soils
and archaeologists are left to reconstruct past cultures from
stone tools. The bone, antler, wood, sinew, and feather
components of hunting implements are preserved within ice patches,
and these complete artifacts have helped neighbouring Yukon
archaeologists to redefine our understanding of the invention
and use of various hunting technologies, such as the bow and
arrow. Well-preserved biological specimens have also
proven invaluable to Yukon biologists for reconstructing past
environmental conditions and wildlife population dynamics. For
example, pollen trapped in the dung provides a record of past
climate and vegetation, and DNA studies on dung pellets have
assisted in reconstructing the genetic histories of caribou
herds and long-term changes in herd ranges. For Yukon
archaeologists and biologists, this multidisciplinary approach
has resulted in a unique database that informs important questions
of human history and caribou behaviour. Yet, the most
critical lesson from the Yukon experience is that new artifacts
are melting from the ice patches on an annual basis and that
these artifacts, wet, fragile and exposed, require immediate
conservation measures to be preserved.
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Ice
Patch archaeological site showing Glen MacKay examining
caribou dung melting from ice margin.
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Recent work in the Mackenzie Mountains indicates that this
ice patch phenomenon is also present in the Northwest Territories
and in need of immediate attention. We initiated a project
in 2002 to locate and assess ice patches in the Mackenzie Mountains. Working
over three years with satellite imagery and aerial photos – in
partnership with the NWT Centre for Remote Sensing – we
were able to locate areas in the mountains that had visible
summer ice patches. In 2005, working in partnership with
Tulita First Nations Band, we conducted a 5-day helicopter
survey in the middle Mackenzie Mountains, between Norman Wells
and the Yukon border, south to the headwaters of the South
Nahanni River, and as far north as the headwaters of the Arctic
Red River. Two new archaeological sites associated with
ice patches were recorded during this brief survey. One
of the sites produced wooden artifacts – possibly fragments
of a bow made from willow – and the second yielded broken
caribou bone with fracture patterns indicative of human butchering
practices. We also collected caribou dung from the second
site. Analysis is still underway and includes radiocarbon
dating of the cultural remains and bone. NWT biologists
are leading the analysis of biological specimens from the sites,
which include stable isotope analysis, diet composition and
DNA analysis. These analyses will provide information
on environmental changes and a comparison of past and present
ecology of wildlife in the Mackenzie Mountains. This
archaeological and biological work will lead to unique insights
into the human and ecological history of the Mackenzie Mountains
and will also extend the geographical range of the ice patch
work in the Yukon, providing a broader regional scope to these
studies.
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