Fróðskaparrit - 01.01.1992, Side 58

Fróðskaparrit - 01.01.1992, Side 58
62 THE LICHENS OF THE FAROES area is 1399 km2. The islands are formed of lavas about 50-60 mill. years old. The relief is steep, the highest peaks reaching about 800 m a.s.l. The climate is cold oceanic with month- ly mean temperatures of 11 °C in August and 4°C in February, and with a record maximum of almost 25°C. The precipita- tion amounts to 1200-2700 mm annually, or even more in the mountains, mostly as rain. Snow storms occur during winter, but a snow cover of a longer duration is found only in the mountains. Fog is very com- mon, especially in summer. The islands were perhaps totally covered by ice during the last glaciation. Nunataks may have been present on the highest parts of the northem islands, but this has not been proved. All life forms, or at least the majority of species, must therefore have invaded the area in postglacial time. The recent introduction of some epiphytic lichens and of Xanthoria elegans to the islands was discussed by Alstrup & Alstmp (10). Some genera are well represented and therefore supposed to spread easily. In con- trast Acarospora, Umbilicaria and Cetr- aria e. g. are represented by only four, two and one species respectively. Common and widely distributed northern species as Brodoa intestiniformis, Lecidoma demis- sum, Orphniospora moriopsis, Diplo- schistes scruposus and Icmadophila erice- torum have not been found in the area. The vegetation is superficially tundra- like, but according to Tuhkanen (57) it is a highly oceanic sector of the hemiboreal subzone with the alpine areas above 150 m belonging to the orohemiarctic zone. The Faroes have been inhabited for almost 1.500 years, the present population amounts to c. 50.000 inhabitants. The econ- omy is almost totally dependant on fishery and whaling; sheep-breeding is also impor- tant. (The indeginous name of the country “Føroyar” means Sheep Islands). In prehis- toric time the islands probably had a low forest or scrub of birch and willow, with juniper in some places. Due to the sheep- breeding the scmb vegetation has almost disappeared, and the present vegetation is dominated by grasses and herbs, except for a few plantations of recent age. Rocks are totally covered in lichens and mosses. Lichens are also found on soil, moss, turf, building materials, bones etc. The macrolichens of the Faroes are presently not well-developed in most places due to sheep-browsing. Sheep eat lichens rather indiscriminately, and they are good climbers. Good stands of macro- lichens are therefor found only on steep cliffs and huge blocks where sheep cannot go. These places are also rather inaccessi- ble to lichenologists. Collections of some species of Lobaria, Sticta, Bryoria, Parmelia s.l. and Platismatia are therefore rare in the herbaria, but the species proba- bly still exist in such protected places. Soil- inhabiting lichens also suffer from tram- pling of the sheep (with the exception of Gyalecta foveolaris) and from a dense grasscover, but the epilithic microlichens are well-developed. During the last century small plantations have been established in many places. The plantations are fenced to keep the animals out, and macrolichens thrive well (10).
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