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...
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...
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...