Donal Mullan

TL;DR: In this article, the authors investigated the potential for increased soil erosion under future climate change, and illuminated the need to address key limitations in previous studies with respect to the treatment of future projections, and crucially, the factoring in of future land use and management.

TL;DR: In this article, the authors analyse testate amoeba-derived hydrological reconstructions from 31 peatlands across Britain, Ireland, Scandinavia and Continental Europe to examine changes in peatland surface wetness during the last 2,000 years.

TL;DR: In this paper, the impact of climate change and its impacts on soil erosion was investigated using the Water Erosion Prediction Project (WEPP) model, where the direct and indirect impacts of changing land use and management were modelled using statistical downscaling methods and a simple sensitivity analysis.

TL;DR: A high-resolution palaeoecological approach is used to understand the longer-term response of peatlands in contrasting states of permafrost degradation to recent rapid warming and suggests a shared ecohydrological trajectory towards a common end point: inundated Arctic fen.

TL;DR: Canonical correspondence analysis and non-metric multidimensional scaling illustrate that water table depth is a significant control on the distribution of testate amoebae, similar to the results from mid- and high-latitude peatlands.