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Balancing Between Predation Risk and Food by Boreal Breeding Ducks
Resource
Wetlands belong to the globally most threatened habitats, and organisms depending on them are of conservation concern. Wetland destruction and quality loss may affect negatively also boreal breeding...
Controls on Plot-Scale Growing Season CO2 and CH4 Fluxes in Restored Peatlands: Do They Differ From Unrestored and Natural Sites?
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...
Decreased Carbon Accumulation Feedback Driven by Climate‐Induced Drying of Two Southern Boreal Bogs over Recent Centuries
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...
Digging Into Canadian Soils - An Introduction to Soil Science
Resource
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...
Effects of Ungulate Density and Sociality on Landscape Heterogeneity: A Mechanistic Modeling Approach
Resource
Animals can be important vectors of nutrient transfer within and across landscapes, with important implications for ecosystem productivity and composition. While it is presumed large ungulates are...
Environmental Spaces for Palsas and Peat Plateaus are Disappearing at a Circumpolar Scale
Resource
The anthropogenic climate change threatens northern permafrost environments. This compromises the existence of permafrost landforms, such as palsas and peat plateaus, which have been assessed to be...
Graminoids Vary in Functional Traits, Carbon Dioxide and Methane Fluxes in a Restored Peatland: Implications for Modeling Carbon Storage
Resource
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
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...
Increasing Contributions of Peatlands to Boreal Evapotranspiration in a Warming Climate
Resource
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...
Integrating Coastal Vulnerability and Community-Based Subsistence Resource Mapping in Northwest Alaska
Project
Organization:
This project integrates physical, anthropological, and survey data to assess coastal vulnerability and to identify areas of concern for local and regional planning and environmental protection. This...
Integrating Coastal Vulnerability and Community-Based Subsistence Resource Mapping in Northwest Alaska
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...
Interweaving Local, Expert, and Indigenous Knowledge into Quantitative Wildlife Analyses: A Systematic Review
Resource
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...
Intra- and Interspecific Variation in Spectral Properties of Dominant Sphagnum Moss Species in Boreal Peatlands
Resource
Boreal peatlands store ~25 % of global soil organic carbon and host many endangered species; however, they face degradation due to climate change and anthropogenic drainage. In boreal peatlands...
Lichens: A Limit to Peat Growth?
Resource
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...