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Conservation Close to Home - Story Map
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Conservation Assessment for Southern Canada The Nature Conservancy of Canada (NCC) has completed a comprehensive assessment of the conservation needs and opportunities in southern Canada. The first of...
Conservation through Co-occurrence: Woodland Caribou as a Focal Species for Boreal Biodiversity
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Assessment of the focal/umbrella value of boreal caribou for conservation of mammalian and avian richness, based on evaluation of co-occurrence and conducting systematic conservation planning.
Controls on Plot-Scale Growing Season CO2 and CH4 Fluxes in Restored Peatlands: Do They Differ From Unrestored and Natural Sites?
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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...
Digging Into Canadian Soils - An Introduction to Soil Science
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Written entirely by members of the Canadian Society of Soil Science, "Digging into Canadian Soils: An Introduction to Soil Science" provides an introduction to the core disciplines of soil science...
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...
Graminoids Vary in Functional Traits, Carbon Dioxide and Methane Fluxes in a Restored Peatland: Implications for Modeling Carbon Storage
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One metric of peatland restoration success is the re-establishment of a carbon sink, yet considerable uncertainty remains around the timescale of carbon sink trajectories. Conditions post-restoration...
Impact of Heat Advection on the Thermal Regime of Roads Built on Permafrost
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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...
Increasing Contributions of Peatlands to Boreal Evapotranspiration in a Warming Climate
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The response of evapotranspiration (ET) to warming is of critical importance to the water and carbon cycle of the boreal biome, a mosaic of land cover types dominated by forests and peatlands. The...
Interweaving Local, Expert, and Indigenous Knowledge into Quantitative Wildlife Analyses: A Systematic Review
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Inclusion of local, expert, or Indigenous knowledge about wildlife populations and their habitats can inform wildlife research, while also increasing knowledge holder engagement and support for...
Lichens: A Limit to Peat Growth?
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The fruticose lichens Cladina stellaris and Cladina rangiferina, form thick mats that can cover large areas of northern peatlands (above c. 50° latitude), including the extensive peatlands of the...
Litter Decomposition and Nutrient Dynamics of Four Macrophytes in Intact, Restored, and Constructed Freshwater Marshes of Canada
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The restoration and construction of wetlands offer opportunities to rewet soils, inhibit decomposition, and enhance nutrient retention in decomposing litters. Here, we report the decomposition rates...
Natural Climate Solutions for Canada
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Alongside the steep reductions needed in fossil fuel emissions, natural climate solutions (NCS) represent readily deployable options that can contribute to Canada’s goals for emission reductions. We...
Potential Impact of Restricted Caribou (Rangifer tarandus) Consumption on Anemia Prevalence Among Inuit Adults in Northern Canada
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Abstract Background Caribou ( Rangifer tarandus) is the top dietary source of iron and several micronutrients necessary for red blood cell production (erythropoiesis) in the contemporary diet of Inuit...
The Biophysical Climate Mitigation Potential of Boreal Peatlands During the Growing Season
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Peatlands and forests cover large areas of the boreal biome and are critical for global climate regulation. They also regulate regional climate through heat and water vapour exchange with the...
The Essential Carbon Service Provided by Northern Peatlands
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Northern peatlands have cooled the global climate by accumulating large quantities of soil carbon (C) over thousands of years. Maintaining the C sink function of these peatlands and their immense long...