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High-Resolution Minirhizotrons Advance our Understanding of Root-Fungal Dynamics in an Experimentally Warmed Peatland
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Mycorrhizal fungi enable plants to thrive in the cold, waterlogged, organic soils of boreal peatlands and, with saprotrophic fungi, largely contribute to the sequestration of atmospheric carbon in...
Mapping and Monitoring Peatland Conditions from Global to Field Scale
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Peatlands cover only 3–4% of the Earth’s surface, but they store nearly 30% of global soil carbon stock. This significant carbon store is under threat as peatlands continue to be degraded at alarming...
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...
Warming Response of Peatland CO2 Sink is Sensitive to Seasonality in Warming Trends
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