Skógræktarritið - 15.05.2001, Qupperneq 140

Skógræktarritið - 15.05.2001, Qupperneq 140
podzol horizon contains 4.1% (Ushakova, 1997). Climate. In general, the climate of the cen- tral part of the province is more continental than the climate of the eastern and coastal parts (Anon. 1965, 1968). The western part has a higher precipitation, than the central and coastal area of the White Sea. The average annual temperature is below 0° C in the whole area, but inland and at the White Sea it is clearly cold- er than in the western region. The western and coastal parts of the region show evidence of maritime climate by their reduced summer rainfall (less than 35 % of the annual distribution for June, luly, and August) Data collection. Field work was carried out in 1990-1999 in the Khibiny, Keyvy, Chuna-Tundra, Monche-tundra and Salnye Tundry Mts. and along the shore of the White Sea. A total of 82 sample plots (10 x 10 m) were made in birch stands considered uniform in floristic composition and struc- ture. Percentage cover of each taxon was estimated using the following variant of the Braun- Blanquet scale: « 1% cover, < 1%, 1-5%, 6-25%, 26-50%, 51-75%, and 76-100%. Altitude, aspect and slope were estimated with the help of a map and compass. Height and diame- ter of trees were measured and the density of canopy and cover of understory species were est- mated. The botanical nomencla- ture follows Lid and Lid (1994) for vascular plants, Ignatov and Afonina (1992) and Konstantinova et al. (1992) for mosses and Santesson (1993) for lichens. In addition, birch forest vegeta- tion samples taken by Avrorin et al. (1935), Nekrasova (1938) and Neshatayev & Neshatayeva (1993) were included. These sam- ples were comparable to Braun- Blanquet releves. Data analyses The numerical technique TWINSPAN, which gives both a grouping of species and classifi- cation of sample plots (Hill, 1979), was used to analyse the more than 110 releves (stands). Three levels of division were taken into account in order to produce the final community units. The TWINSPAN sequence of species was rearranged in order to characterize the groups of communities obtained in terms of their floristic composi- tion and to reveal clearly at a glance the similarity and dissimi- larity of samples. Results The two large groups delineated by the first TWINSPAN division corespond to heath and meadow birch forests (Fig.l). Within these, the following birch forest community types were defined. I. The Arctostaphylos uva-ursi type of heath birch forest is widely distributed at low elevations, mainly on southerly plains. The tree layer is open, with policormic birches growing far apart, and the field-layer consists mainly of Arctostapfiylos uva-ursi and Empetrum hermaphroditum. Lichens of the genera Cladina and Cladonia form the ground layer. II. The Empetrum - Flavocetraria type comprises the driest and the most infertile birch stands. They are common in the moun- tains of the eastern part of the province. The birches here grow in bush islands, standing far apart. Dwarf shrubs and chiono- phobous lichens of the genera Cladina, Cladonia and Flavocetraria form scattered cover. III and IV. The third group of birch forests is where mosses make up an essential part of the ground-layer. Here birches are often in the form of individual trees, the stands occupying more sheltered positions. There is a dense ground layer with a large proportion of mosses and liver- worts, some vascular plants and the constant presence of mesophilous foliose lichens. This group is divided into sub-units, which differ in accordance with the abundance of lichen and moss in the ground layer; the Empetrum - Cladina and Empetrum - Hylocomium types. V. The Empetrum - Cornus type contains the transitional charac- teristics of the heath to meadow birch forest. These stands occupy rather steep warm slopes with good water supplies served by numerous brooks. Polycormic oblique birches form a dense tree layer and the field layer con- sisis mainly of herbs, although dwarf shrubs are a significant component too. The ground layer is weakly developed (almost absent). Owing to their particular position and ecological condi- tions these stands provide shel- ter to some interesting rare Red Book species such as Epipactis atrorubens, Veronica fruticans and Castillea lapponica. VI and VII. The two last types rep- resent meadow birch forests, which are mainly situated close to springs and rivers as well as in mountains in the submaritime zone, where meadow forests are most prevalent. The birches here are tall, straight or oblique. Mountain ash and alder are com- mon in the tree-layer. Luxuriant tall herbs, grasses and ferns form 138 SKÓGRÆKTARRITIÐ 2001 l.tbl.
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