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A Strong Mitigation Scenario Maintains Climate Neutrality of Northern Peatlands
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Northern peatlands store 300–600 Pg C, of which approximately half are underlain by permafrost. Climate warming and, in some regions, soil drying from enhanced evaporation are progressively...
Biogeochemical Response to Vegetation and Hydrologic Change in an Alaskan Boreal Fen Ecosystem
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Boreal peatlands store approximately one third of the earth’s terrestrial carbon, locked away in currently waterlogged and frozen conditions. Peatlands of boreal and arctic ecosystems are affected...
Drought Effects on Wet Soils in Inland Wetlands and Peatlands
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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...
Guidelines for the Reclamation of Land in Alberta
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Regulatory expectations with respect to the detailed content of applications for approvals of surface disturbances and the reclamation of lands.
Measuring Success in Land Reclamation – A Joint Government and Industry Workshop
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The question we are faced with today is: How do we establish a system or systems for measuring success in reclamation?
Minimum Reclamation Requirements for Public and Private Lands in Alberta
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These are the minimum requirements that the Land Conservation and Reclamation Council will apply in assessing whether the reclamation of lands has been satisfactory
Minimum Reclamation Standards for Patented Land
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Minimum reclamation standards that should be followed to ensure proper conservation and reclamation on patented and and land that was the property of the Crown but covered by the Public Lands Act
Peat Loss Collocates with a Threshold in Plant–Mycorrhizal Associations in Drained Peatlands Encroached by Trees
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Drainage-induced encroachment by trees may have major effects on the carbon balance of northern peatlands, and responses of microbial communities are likely to play a central mechanistic role. We...
Recent Climate Change has Driven Divergent Hydrological Shifts in High-latitude Peatlands
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High-latitude peatlands are changing rapidly in response to climate change, including permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century using testate amoeba...
The Third Generation of Pan-Canadian Wetland Map at 10 m Resolution Using Multisource Earth Observation Data on Cloud Computing Platform
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Development of the Canadian Wetland Inventory Map (CWIM) has thus far proceeded over two generations, reporting the extent and location of bog, fen, swamp, marsh, and water wetlands across the country...