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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...
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...
Watching, Listening, and Learning to Understand Change: Developing a Community-Based Monitoring (CBM) Initiative in Ontario’s Far North
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Ontario’s Far North is one of the world’s largest and most intact expanses of boreal forest and wetlands. The region has almost no industrial development today, but that could change with plans for...
Webinar - Wetland Delineation Methods
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This presentation provides an overview of methods for delineating wetland boundaries using a three-factor approach, which involves indicators of hydrophytic vegetation, hydric soil, and wetland...