In the decade since the first pan-European testate amoeba-based transfer function for
peatland palaeohydrological reconstruction was published, a vast amount of additional data …

Quantitative reconstructions of the depth to water table (DWT) of ombrotrophic (rain-fed)
peatlands are important for understanding the palaeohydrological responses of peatlands to …

Climate warming and human impacts are thought to be causing peatlands to dry, potentially
converting them from sinks to sources of carbon. However, it is unclear whether the …

Permafrost peatlands contain globally important amounts of soil organic carbon, owing to
cold conditions which suppress anaerobic decomposition. However, climate warming and …

Northern boreal peatlands are important ecosystems in modulating global biogeochemical
cycles, yet their biological communities and related carbon dynamics are highly sensitive to …

Permafrost peatlands are found in high-latitude regions and store globally-important
amounts of soil organic carbon. These regions are warming at over twice the global average …

Climate warming has inevitable impacts on the vegetation and hydrological dynamics of
high-latitude permafrost peatlands. These impacts in turn determine the role of these …

Fossil testate amoeba assemblages have been used to reconstruct peatland
palaeohydrology for more than two decades. While transfer function training sets are …

Testate amoebae (TA) are a common and diverse group of protists and are especially
abundant in peatlands. The structure of peatland TA communities is well correlated to …

We used variation partitioning to assess the relative importance of drainage, climate and
local vegetation composition for the development of a raised bog. As a case study we …