Outputs (2)

Towards a Holarctic synthesis of peatland testate amoeba ecology: Development of a new continental-scale palaeohydrological transfer function for North America and comparison to European data (2018)
Journal Article
Amesbury, M. J., Booth, R. K., Roland, T. P., Bunbury, J., Clifford, M. J., Charman, D. J., …Warner, B. G. (2018). Towards a Holarctic synthesis of peatland testate amoeba ecology: Development of a new continental-scale palaeohydrological transfer function for North America and comparison to European data. Quaternary Science Reviews, 201, 483-500. https://doi.org/10.1016/j.quascirev.2018.10.034

Fossil testate amoeba assemblages have been used to reconstruct peatland palaeohydrology for more than two decades. While transfer function training sets are typically of local-to regional-scale in extent, combining those data to cover broad ecohydro... Read More about Towards a Holarctic synthesis of peatland testate amoeba ecology: Development of a new continental-scale palaeohydrological transfer function for North America and comparison to European data.

Latitudinal limits to the predicted increase of the peatland carbon sink with warming (2018)
Journal Article
Gallego-Sala, A. V., Charman, D. J., Brewer, S., Page, S. E., Prentice, I. C., Friedlingstein, P., …Zhao, Y. (2018). Latitudinal limits to the predicted increase of the peatland carbon sink with warming. Nature Climate Change, 8(10), 907–913. https://doi.org/10.1038/s41558-018-0271-1

The carbon sink potential of peatlands depends on the balance of carbon uptake by plants and microbial decomposition. The rates of both these processes will increase with warming but it remains unclear which will dominate the global peatland response... Read More about Latitudinal limits to the predicted increase of the peatland carbon sink with warming.