Wetlands
The term wetland has changed over time and with various political and regulatory instruments. Wetlands cover wet or very humid vegetated habitats with no or very little open water surface: mires and bogs, as well as habitats with open water: rivers, lakes. Wetlands can be inland, coastal or marine. The marine wetlands are dealt with by the marine chapters on the North Sea and the northeast Atlantic Ocean.
Heathlands formerly covered wide areas of the region as in the Continental region. Present cover is less than 8%. Atlantic heathlands are characterised by dwarf shrubs and occur normally on nutrient poor soils. The following habitats occur in this ecosystem: Northern Atlantic wet heaths with Erica tetralix, European dry heaths, Active raised bogs, Transition mires and quaking bogs, Alkaline fens (European Environment Agency, Europe’s biodiversity, The Atlantic region - ETC/NPB).
More information
- Recovery of fen peatland microbiomes and predicted functional profiles after rewetting
- Converting agricultural lands into heathlands: the relevance of soil processes
- Barriers to restoration: Soil acidity and phosphorus limitation constrain recovery of heathland plant communities after sod cutting
- Effects of heathland management on seedling recruitment of common juniper (Juniperus communis)
- Long-term effects of liming on soil physico-chemical properties and micro-arthropod communities in Scotch pine forest
- Salinization lowers nutrient availability in formerly brackish freshwater wetlands; unexpected results from a long-term field experiment
- Literature study into the effect of exotic crayfish, other grazers and bio-builders on the development of young terrestilization vegetation with a view to potential measures
- Facilitating ecosystem assembly: Plant-soil interactions as a restoration tool
- Heathland restoration by application of slow release minerals
- Pathways for the effects of increased nitrogen deposition on fauna
- Continuous and cumulative acidification and N deposition induce P limitation of the micro-arthropod soil fauna of mineral-poor dry heathlands
- Alternatives for sod-cutting wet heaths Effects in the medium-long term
- Can changes in soil biochemistry and plant stoichiometry explain loss of animal diversity of heathlands?
- Soil iron content as a predictor of carbon and nutrient mobilization in rewetted fens
- Terrestrialisation in peat turf ponds
- Topsoil removal in degraded rich fens: Can we force an ecosystem reset?
- Salinization of coastal freshwater wetlands; effects of constant versus fluctuating salinity on sediment biogeochemistry
- Restoration of lowland streams through the reintroduction of macroinvertebrate species
- Ecological restoration of rich fens in Europe and North America; from trial and error to an evidence-based approach
- How Does Tree Density Affect Water Loss of Peatlands? A Mesocosm Experiment