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An 11,000 Year Record Of Plant Community Stability And Paludification In A Patterned Rich Fen In Northeastern Alberta, Canada
Resource
This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Current Symptoms of Climate Change in Boreal Forest Trees and Wildlife
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This is a chapter from the book, Boreal Forests in the Face of Climate Change: Sustainable Management . Measuring climate change impacts on forest ecosystems can be challenging, as many of these...
Developing a Reclamation Costing Framework for the Athabasca Oil Sands
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The Athabasca oil sands are a significant component of the economy in Alberta. However, they also represent a large environmental risk. At the end of mining operations, companies are expected to begin...
Environmental and Management Drivers of Carbon Dioxide and Methane Emissions From Actively-Extracted Peatlands in Alberta, Canada
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The installation of drainage ditches and removal of vegetation in preparation for vacuum harvesting alters the carbon dynamics of peatlands. However, we lack the measurements to understand the spatial...
Inuit Qaujimajatuqangit about Population Changes and Ecology of Peary Caribou and Muskoxen on the High Arctic Islands of Nunavut
Project
Organization:
This master's project collected and documented Inuit observations to describe the population distribution of caribou and muskoxen in Nunavut.
Inuit Qaujimajatuqangit about Population Changes and Ecology of Peary Caribou and Muskoxen on the High Arctic Islands of Nunavut
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Abstract Over the past 40 years, severe population fluctuations in Peary caribou ( Rangifer tarandus pearyi) and muskoxen ( Ovibos moschatus) living in the High Arctic of Nunavut has caused widespread...
Moss Cellulose 18O Applied to Reconstruct Past Changes in Water Balance of a Boreal Wetland Complex, Northeastern Alberta
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Overall, the study established existence of long-term groundwater source areas around the margins of the peatland, as well as contemporary permafrost thaw zones within the McClelland Wetland itself.
Peatland Pools are Tightly Coupled to the Contemporary Carbon Cycle
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Peatlands are globally important stores of soil carbon (C) formed over millennial timescales but are at risk of destabilization by human and climate disturbance. Pools are ubiquitous features of many...
Remediation of Hydrocarbon Contaminated Soils in the Canadian Arctic by Landfarming
Resource
This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Seismic Line Impacts on Proximal Boreal Forest and Wetland Environments in Alberta
Resource
This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...
Swamplands: Tundra Beavers, Quaking Bogs, and the Improbable World of Peat
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In a world filled with breathtaking beauty, we have often overlooked the elusive charm and magic of certain landscapes. A cloudy river flows into a verdant Arctic wetland where sandhill cranes and...
The Impacts of Climate and Social Changes on Cloudberry (Bakeapple) Picking: A Case Study from Southeastern Labrador
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Abstract The traditional subsistence activities of Indigenous communities in Canada's subarctic are being affected by the impacts of climate change, compounding the effects of social, economic and...
The Role of Microhabitat for Bryophyte Establishment in Reclamation of Boreal Wetlands
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Minerogenous peatlands that accumulate deep deposits of organic matter (fens) were an important part of the pre-disturbance landscape across Alberta’s oil sands mining area. Bryophytes occupy 80–100%...
Theses - Queen's University
Project
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This community is a joint endeavour of the School of Graduate Studies and Research and the Library to make available Queen's University graduate theses and projects in electronic form via the...