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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...
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...
Plant mercury Accumulation and Litter Input to a Northern Sedge-dominated Peatland
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Abstract Plant foliage plays an essential role in accumulating mercury (Hg) from the atmosphere and transferring it to soils in terrestrial ecosystems, and many studies have focused on forested...
Warming Response of Peatland CO2 Sink is Sensitive to Seasonality in Warming Trends
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