Fróðskaparrit - 31.12.2000, Side 40

Fróðskaparrit - 31.12.2000, Side 40
44 A REVIEW OF PLANT COMMUNITIES OF THE FAROE ISLANDS Islands. Ostenfeld (1905-1908) made a comprehensive description of the vegeta- tion into associations based on observa- tions. Bocher (1937; 1940) and Hansen (1972) used the method developed by the Danish botanist, Raunkiær, to sample veg- etation. They also registered frequencies of species’ occurrence. Bocher (1937; 1940) also used the Hult-Sernander five-degree scale to measure the cover of vegetation. Both of the scientists used the term socia- tion to describe the plant communities, based on dominant species. The term soci- ation is used mostly in Scandinavia and fits into the Braun-Blanquet system of associa- tion. Dierssen (1982) and Tannhauser (1995) used the Braun-Blanquet system to define the associations. Hobbs and Averis (1991) used the Na- tional Vegetation Classification (Rodwell, 1991 -1995). In their system, a community is roughly equivalent to a Braun-Blanquet association. In this paper the term association is used and a summary is given in Appendix I. Alpine Vegetation Snow cover is very important in alpine ar- eas, protecting the soil surface from frost penetration in winter. Due to mild, sub- zero winter temperatures, plants must be able to withstand a snow-free winter, which is liable to disturb the winter period of in- activity. Only limited information on the duration of the snow cover in the alpine ar- eas is available from the Faroe Islands. Os- tenfeld (1905-1908) made some observa- tions in a two-year period and Bocher (1937) had some information from local people. Meteorological information on the duration of snow cover in Tórshavn in the period 1961-1991 shows that January had the maximum number of days of snow cov- er (10.8 days), while the period from May to October had no snow cover (Cappelen andLaursen, 1998). The most distinctive features in the alpine zone are the flat mountaintops form- ing “fell fields”, described for the first time in Greenland by Warming (1888). These flat pastures are formed as a result of ero- sion and one finds them from an elevation of a few hundred metres up to the highest mountaintop (882 m). Such plateau-like areas are exposed to strong winds, and the substrate freezes and thaws repeatedly. Most of these areas consist of a mosaic of cliff surfaces with moss and lichens, and a few higher plants. The vegetation is very distinctive, though sparse. It is the instabil- ity of the ground and its constant movement that causes the scarcity of flora. The most common plants in the alpine zone are Koenigia islanclica, Silene acciulis, Luzula spicata, Alchemilla alpina, Bistorta vivipara, Juncus trifidus, Deschampsia alpina, Saxifraga rosacea, Loiseleuria procumbens, Sibbaldia procumbens, and Salix herbacea. Ranunculus glacialis, Pa- paver radicatum, and Omalotheca supina occur on the highest mountain peaks only. In the fell fields, a Koenigia - Ranunculus glacialis association has been described at 730 m a.s.l. This association is strongly in- fluenced by species like Salix herbacea, Racomitrium lanuginosum, and R. fascicu- lare (Bocher, 1937). In two places, at alti- tudes of 200 and 350 m.a.s.l., respectively,
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