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Permafrost Thaw Causes Large Carbon Loss in Boreal Peatlands While Changes to Peat Quality are Limited
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Rapid, ongoing permafrost thaw of peatlands in the discontinuous permafrost zone is exposing a globally significant store of soil carbon (C) to microbial processes. Mineralization and release of this...
Revealing the Hidden Carbon in Forested Wetland Soils
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Inland wetlands are critical carbon reservoirs storing 30% of global soil organic carbon (SOC) within 6% of the land surface. However, forested regions contain SOC-rich wetlands that are not included...
Reviewing and analyzing shrinkage of Peat and Other Organic Soils in Relation to Selected Soil Properties
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Peat and other organic soils (e.g., organo-mineral soils) show distinctive volume changes through desiccation and wetting. Important processes behind volume changes are shrinkage and swelling. There...
The Importance of Continuous Dialogue in Community-Based Wildlife Monitoring: Case Studies of Dzan and łuk Dagaii in the Gwich’in Settlement Area
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Rapid environmental change in the Arctic elicits numerous concerns for ecosystems, natural resources, and ways of life. Robust monitoring is essential to adaptation and management in light of these...
Using Perceptions as Evidence to Improve Conservation and Environmental Management
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The conservation community is increasingly focusing on the monitoring and evaluation of management, governance, ecological, and social considerations as part of a broader move toward adaptive...