FORESTS

The nature reserve is situated on the north of the taiga zone, at its very border with forest-tundra. According to different classifications, the territory belongs to different districts and areas:

  • According to geobotanical zoning of the Non-Chernozem region (1989), it forms part of the Lotto-Tuloma area of northern taiga forests in the Kola-Karelian taiga sub-province.

  • As per the floristic zoning of the region, it belongs to the Imandra floristic district, which is a subregion of the Lotto-Tuloma lowland.

  • As to the classification of Scandinavian scientists, the nature reserve belongs to the Lapponia petsamoënsis (Lps) biogeographic province of Pechenga Lapland.
Forest area: 7 626 hectares, which is approximately 51.92% of the territory.

Forest age: old, the maximum age is 470 years. Pine forests over 140 years old account for 59% of the forests.

Forest value: these are the northernmost forests in the European part of Russia and the most valuable ones in the Murmansk region.
Forest resources
Pine forests
  • Pine forests are sparse and are located at the edge of their habitat in Europe.
  • Area coverage is 6 876 hectares, which is approximately 46.81% of the reserve's total area and 90.16% of the area of its forest lands.
  • Forests are composed of the northern form of the common pine Pinus sylvestris (P. sylvestris L. var. lapponica Fr. ex Hartm., P. frieseana Wichura, P. lapponica (Hartm.) Mayr).
  • Total stock: 411.6 cubic meters.
  • Current state: natural or after felling and fires.

There are signs of old selective cuttings of low intensity across most of the territory of the nature reserve. A very small part of green moss and lichen pine forests was clearcut on the cusp of the XIX — the XX centuries. Currently, there are middle-aged and maturing forest stands. In the central part of the nature reserve, around the Kalkuplya mountain, there are primary pine forests that are more than 200 years old, that have never been logged.
    Birch forests
    • There are 5 species of birches growing in the nature reserve, 4 of them are tree species and one is a shrub.
    • Area coverage: 725 hectares, which is approximately 4,93% of the total area of the nature reserve and 9,5% of its forest lands.
    • Primary birch forests are located along the stream and river banks, while secondary stands can be found in the former agricultural lands and felling sites.
    • Average age: 70 years.
    • Total stock: 28 cubic meters.
    • Forest stands are often formed by birches and pine trees.
    • Current state: natural and after felling. The Pasvik river floods the coastal areas of the forests during the high water periods.
    Aspen forests

    Aspens are widely distributed on the territory of the Pasvik nature reserve. Occasionally aspen forms small secondary forests on former agricultural lands and logging areas. It can also grow on more fertile soils in pine and birch forests. This species tends to appear in non-swampy forests including birch elfinwood. It is hardly possible to come across aspens in the alpine tundra belt.

    • Stand composition: Aspen — Populus tremula L.
    • Area coverage is 4,5 hectares in total, which is less than 1% of the forest area in the nature reserve.
    • Total stock: 0,4 cubic meters.
    • Forest age: on average aspen forests are 45 years old, with the oldest communities being around 80 years old.
    • These are the densest (0,69) and the most productive forests (the IV yield class) in the nature reserve.
    • The undergrowth is developed to a greater or lesser extent in the green moss aspen forests.
    • Ground cover is dominated by low shrubs and in some cases by grasses.
    • Grassy aspen forests are mostly located along the banks of the Pasvik river and in confluence areas. They can be found on former agricultural lands, as indicated by the presence of several preserved meadow plant species.
    • The undergrowth and moss layers are usually poorly developed.
    Spruce forests
    • In the Pasvik river valley, spruce forests are extremely rare.
    • There are a few small groups of spruces (Picea obovata Ledeb. (P. abies (L.) H. Karst. subsp. obovate (Ledeb.) Domin) in the central part of the nature reserve, at the foot of the Kalkuplya mountain.
    • Spruce grows along the streams and swampy lake shores as well as in the inter-ridge depressions.
    • In small groups of spruces, the trees are suppressed. There are signs of selective cutting, however, the renewal of spruces hasn’t been registered. Nevertheless, spruces show the IV yield class, which is a very good mark for the communities located in the Extreme North. The diameter growth in the last 10 years equals 1 centimeter, which tells us that the spruces are continuously growing.
    • To the south of the Pasvik reserve, there are some large and sparse rupicolous low shrub spruce forests. These forests extend to the east as far as the eye can reach.
    • The maximum determined spruce age is 190 years. The diameter of the spruce trunks reaches up to 30−45 cm.
    Composition of forest-forming tree species
    Composition of forest-forming tree species
    Pine

    young: 312 hа
    middle-aged: 2378 hа
    maturing: 728 hа
    mature: 2231 hа
    overmature: 1227 hа
    Birch

    middle-aged: 405 hа
    maturing: 174 hа
    mature: 146 hа
    Aspen

    young: 1 hа
    middle-aged: 3 hа
    Zonation
    There is a vertical or altitudinal zonation on Kalkupya mountain. This is the only mountain in the Pasvik reserve and it is 357 m above sea level.

    In the lower parts of the mountain slopes, there are pine and birch green moss and lichen forests, which are similar to plain forests in their composition.

    Starting from 200 meters above sea level, forest communities become more sparse, gradually transitioning into birch elfinwood. The most widespread are the low shrub-lichen and lichen birch forests growing on shallow soils. The lichen cover in these forests can reach up to 20−30%.

    Alpine tundra lays at an altitude of more than 300 m, covering the top of the mountain. The total area of alpine tundra is 347 hectares, which is approximately 2.5% of Pasvik reserve territory. This zone is dominated by rupicolous-shrub, low shrub-lichen, and lichen communities, where shrubs, low shrubs, lichens, mosses, and liverworts prevail in various combinations and proportions.
    Cherepanov birch (Betula czerepanovii N.I. Orlova — B. pubescens subsp. czerepanovii (N.I. Orlova) Hämet-Ahti, B. tortuosa auct.) is an alpine form of the downy birch. It grows in small groups or individually as a shrub in alpine tundra. Lichen cover in some tundra communities can reach up to 70−80%. There are frequent spots of frost heaving and frost boils that are devoid of vegetation except for liverworts. This is what creates a mosaic of small patches and results in the spotted appearance of alpine tundra.
    Cherepanov birch (Betula czerepanovii N.I. Orlova — B. pubescens subsp. czerepanovii (N.I. Orlova) Hämet-Ahti, B. tortuosa auct.) is an alpine form of the downy birch. It grows in small groups or individually as a shrub in alpine tundra. Lichen cover in some tundra communities can reach up to 70−80%. There are frequent spots of frost heaving and frost boils that are devoid of vegetation except for liverworts. This is what creates a mosaic of small patches and results in the spotted appearance of alpine tundra.
    BOGS

    The territory of the Pasvik nature reserve is significantly swamped. There are bogs of various types. This is due, among other things, to the position of the reserve, which is located in the transition zone between the palsa and aapa mires.

    • Area coverage: 3 741 ha, which is around 25,48% of the total area of the nature reserve.

    • The largest swamp areas are located to the south of Kalkupya mountain, to the east of lake Langvatnet, and in the northeastern part of Menikk Island. Typically the swamps are located in areas of marine deposits.

    • Swamp age: the deposition of peat and the development of bogs began about 9 thousand years ago.

    • Composition: mosses of the genus Sphagnum, red-stemmed feathermoss Pleurozeum schreberi, sedge Carex, cotton grass Eriophorum, wild rosemary Ledum palustre, bog rosemary Andromeda polifolia, species of the genus Vaccinium and dwarf birch Betula nana.

    • Types of bogs: heterotrophic, eutrophic, mesotrophic, and oligotrophic.

    • Current state: natural, most of the swamps are located along the banks of the Pasvik river, around the lakes and streams.
    Types of bogs
    • These swamps are widely spread all over the Pasvik nature reserve.
    • They tend to appear on the fluvioglacial landforms.
    • There is a well-developed nanorelief of low shrub-cloudberry-lichen-sphagnum ridges and tussocks as well as cotton grass-sphagnum carpets and pools.
    • Lichen cover reaches up to 30−40% on ridges and tussocks.
    Main characteristics of bog types
    Детальные исследования болотных экосистем заповедника выполнены лабораторией болотных экосистем Института биологии КарНЦ РАН (г. Петрозаводск) в 2011–2015 годах.
    Main characteristics of bog types
    Detailed studies of the Pasvik Nature Reserve bog ecosystems were carried out by the Bog ecosystems laboratory of the Institute of Biology, KarRC RAS (Petrozavodsk) in 2011−2015.
    Ombrotrophic type and vegetation class
    Detailed studies of the Pasvik Nature Reserve bog ecosystems were carried out by the Bog ecosystems laboratory of the Institute of Biology, KarRC RAS (Petrozavodsk) in 2011−2015.
    Oligotrophic class
    Communities in this class are composed of mesooligotrophic species for which low groundwater salinity is sufficient. The class consists of 11 associations sorted into three groups.
    Mesotrophic class
    This class is represented by four associations sorted into two groups. Dividing communities into mesotrophic and eutrophic is always controversial and rather tentative since most of the species composing such communities have a wide ecology. There are a few typical eutrophic calciophilic species in the northern bogs. Nevertheless, they indicate the richest keystone biotopes with eutrophic vegetation.
    Eutrophic class
    Eutrophic communities are widespread and highly diverse within the wetlands of the reserve. They are represented by 17 syntaxa belonging to 4 groups of associations.

    It is likely that with further research, additional syntaxa will be identified. In particular, it is necessary to describe communities of small areas (1−4 square meters) in "hanging" bogs with spring nutrition. Additional description is needed due to the high mosaicity of the vegetation cover and the small size of biotic communities.

    Moreover, there are some swamp areas covered with birch trees, which also have not been researched yet.
    Minerotrophic vegetation
    Minerotrophic vegetation includes three different classes. The classes are separated according to the degree to which biotic communities are demanding for water-mineral nutrition.
    Composition of bog vegetation
    Further ground studies of the bog flora and vegetation will broaden our knowledge of the flora composition and of the community type range on the territory of the Pasvik nature reserve. They will also serve as a basis for the development of a classification of bog biotopes in the reserve. Additionally, the results of the studies can be used for monitoring of bog ecosystems.
    About 120 species of vascular plants, which is approximately 40% of the flora of the nature reserve
    90 Bryopsida moss species
    Around 15 lichen species
    Several species of liverworts
    High species and cenotic diversity has been proven through the analysis of the composition and structure of bog vegetation.
    MEADOWS

    All meadows in the reserve are secondary. They developed in areas of human settlements and agricultural lands. Forb-grass communities with a rich floristic composition have formed in the meadows. Now the meadows are gradually degrading. They are being overgrown with birch, and to a lesser extent with pine, aspen, willow, and rowan.

    • Composition: gramineous plants and herbs, with smaller amounts of sedges, legumes, and species from other families.

    • Area coverage is less than 0.5% of the total area of the reserve.

    • Meadows are located along the banks of the Pasvik river, in the south and in the north of the reserve. They can also be found around lakes Salmiyarvi, Niliyarvi, Kaitoyarvi, and around the Yaniskoski village.

    • The meadows are characterized by a high level of floristic diversity including adventive species.

    • Current state: recovering from the intense anthropogenic intervention at the beginning of the 20th century.
    Meadows of the Isle of Varlam
    An international botanical expedition of 1995−1996 explored several meadow areas, including the island itself. They managed to compare their results with the Finnish pre-war data.

    The land planning of the area was carried out on the right bank of the Pasvik river in 1928−1929 when the Pechenga region temporarily formed part of Finland. According to the land plan, the total area of the main island was 18.91 hectares (National Survey Board data, Helsinki) and it consisted of three farms with several residential buildings, cowsheds, and barns.

    Now the Isle of Varlam is covered with pine and birch forests, as well as with a few small meadows. Forb-grass meadows with high species diversity prevail among them. These meadows can be divided into several types.

    All these meadows are open, however, there is an overgrowth threat from actively growing downy birch and tea-leaved willow. Also, meadows are being continuously overgrown with fireweed. In some areas tussock-grass forms huge hummocks.
    The meadow flora of the Isle of Varlam
    The meadow flora of the Isle of Varlam is very interesting, especially in its southern part. There are species with so-called eastern connections that are rare in western Fennoscandia. For example, one can find such species as Jacob’s ladder Polemonium acutiflorum, arctic bramble Rubus arcticus, meadow-rue Thalictrum rariflorum Fries, longleaf speedwell Veronica longifolia, and bistort Polygonum viviparum.

    Some species may have been cultivated or introduced by accident during the 20th century. Among such species are wild chamomile Chamomilla suaveolens, white bedstraw Galium album, timothy Phleum pratense, tansy Tanacetum vulgare, red clover Trifolium pratense, germander speedwell Veronica chamaedrys, and others.

    There are also different meadows located to the north along the banks of the Pasvik river. The diversity of species in these areas is much lower than on the Isle of Varlam, however, Jacob’s ladder Polemonium acutiflorum and longleaf speedwell Veronica longifolia are still abundant there.
    PLANT DIVERSITY
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