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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...
Large Stocks of Peatland Carbon and Nitrogen are Vulnerable to Permafrost Thaw
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Northern peatlands have accumulated large stocks of organic carbon (C) and nitrogen (N), but their spatial distribution and vulnerability to climate warming remain uncertain. Here, we used machine...
Recent Climate Change has Driven Divergent Hydrological Shifts in High-latitude Peatlands
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High-latitude peatlands are changing rapidly in response to climate change, including permafrost thaw. Here, we reconstruct hydrological conditions since the seventeenth century using testate amoeba...
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...
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...
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...
Warming Response of Peatland CO2 Sink is Sensitive to Seasonality in Warming Trends
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This resource is available on an external database and may require a paid subscription to access it. It is included on the CCLM to support our goal of capturing and sharing the breadth of all...