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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 Boreal-Arctic Wetland and Lake Dataset
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Here we present the Boreal–Arctic Wetland and Lake Dataset (BAWLD), a land cover dataset based on an expert assessment, extrapolated using random forest modelling from available spatial datasets of...
Video - Carbon Accumulation and the Return of Microbial Function in Soils
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The resource link will access Part 1 of this presentation. Part 2 can be accessed here. Mark Tibbett's presentation is focused around one question: can we change the amount of carbon in soil through...
Wildfire and Degradation Accelerate Northern Peatland Carbon Release
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The northern peatland carbon sink plays a vital role in climate regulation; however, the future of the carbon sink is uncertain, in part, due to the changing interactions of peatlands and wildfire...