Iceland boreal birch forests and alpine tundra

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Iceland boreal birch forests and alpine tundra
Tingvallir-2-10 - Flickr - Ragnhild & Neil Crawford.jpg
In Þingvellir National Park, Iceland
Ecoregion PA0602.png
Ecoregion territory (in purple)
Ecology
Realm Palearctic
Biome Boreal forest/taiga
Geography
Area91,681 km2 (35,398 sq mi)
Country Iceland
Coordinates 65°45′N16°15′W / 65.75°N 16.25°W / 65.75; -16.25

The Iceland boreal birch forests and alpine tundra ecoregion (WWF ID: PA0602) covers the island of Iceland in the North Atlantic. The island is volcanic in origin with basaltic soils, and the cold northerly climate prevents any significant crop agriculture. Because the island is young and isolated from larger land masses, species biodiversity is relatively low. Forest cover has been reduced to about 1% of the original birch forest by a long history of timber extraction and soil erosion caused by sheep grazing. Blanket bogs (areas of high rainfall and peat accumulation) are common. [1] [2] [3] [4]

Contents

Location and description

Iceland is a volcanic plateau rising out of the Atlantic 290 km east of Greenland. Three quarters of the island is above 200 metres (660 ft) in elevation, with steep fjords and cliffs along much of its coast. Approximately 20% of the island is bare rock or glacier, with the highest elevation being 2,119 metres (6,952 ft). [5] [3]

Climate

Because the Gulf Stream has a moderating effect, portions of Iceland have an Oceanic climate (subpolar variety) (Koppen Cfc). But most of the ecoregion is Tundra climate (Köppen climate classification ET), a local climate in which at least one month has an average temperature high enough to melt snow (0 °C (32 °F)), but no month with an average temperature in excess of 10 °C (50 °F). [6] [7] Precipitation is lowest in the north, as little as 500 mm/year, and highest in the south with up to 3,500 mm/year in places. [5]

Flora and fauna

Continuous vegetation covers approximately 25% of the island, 16,000 km2 of which is dryland vegetation and 10,000 km2 of wetlands. About 1,360 km2 is employed in crop agriculture, and about 1,250 km2 of the original white birch ( Betula pubescens ) forest remains. Another 60,000 km2 is sparsely or very sparsely covered in vegetation. [5] Most of the birch is shrub-like and under 2 meters tall. About 2% of the forest features trees 8-12 meters tall, mostly in valleys in the north, east and south. Besides birch, there are some stands of rowan ( Sorbus aucuparia ) and tea-leaved willow ( Salix phylicifolia ).

Lake Skorradalsvatn, in western Iceland Skorradalsvatn 2004.jpg
Lake Skorradalsvatn, in western Iceland

There are 483 species of vascular plants recorded in Iceland. The largest families are the sedges (Cyperaceae), with 53 species, and grasses (Poaceae), with 47 species. There are 560 species of bryophytes (liverworts, hornworts, and mosses). [5] The most common mosses are Racomitrium lanuginosum and Racomitrium canescens . There are more than 550 species of lichens, and over 1200 species of fungi. [5] There are no reptiles or amphibians in Iceland.

Only one species of mammal is indigenous to Iceland, the Arctic fox ( Alopex lagopus ). Polar bears ( Ursus maritimus ) visit occasionally on drifting sea ice, and there are introduced species such as the American mink ( Neogale vison ), which was brought in for fur farming but have escaped and formed a significant population. Another introduced species is the wood mouse ( Apodemus sylvaticus ) which is now widespread in wooded areas.

The greatest ecological threat facing the island is soil erosion. While 50-60% of the island was covered in vegetation at the time of human arrival, the decline to the current 25% has been the result of soil loss caused by deforestation for firewood and timber, and overgrazing by sheep. In recent years, however, the nation has pursued afforestation and soil conservation programs that have stopped and reversed the decline. [5]

Protected areas

Over 12% of the ecoregion is officially protected. [3] These protected areas include:

Related Research Articles

<span class="mw-page-title-main">Geography of Iceland</span> Geographical features of Iceland

Iceland is an island country at the confluence of the North Atlantic and Arctic oceans, east of Greenland and immediately south of the Arctic Circle, atop the constructive boundary of the northern Mid-Atlantic Ridge. The island country is the world's 18th largest in area and one of the most sparsely populated. It is the westernmost European country when not including Greenland and has more land covered by glaciers than continental Europe. Its total size is 103,125 km2 (39,817 sq mi) and possesses an exclusive economic zone of 751,345 km2 (290,096 sq mi).

<span class="mw-page-title-main">Scandinavian montane birch forest and grasslands</span> Tundra ecoregion in Scandinavia

The Scandinavian montane birch forests and grasslands is defined by the World Wildlife Fund (WWF) as a terrestrial tundra ecoregion in Norway, Sweden, and Finland.

<span class="mw-page-title-main">Katun Nature Reserve</span> Strict nature reserve in the Altai Republic, Russia

Katun Nature Reserve is a Russian zapovednik located in the highlands of the central Altai Mountains of south Siberia. The Katun River runs down through a valley in the reserve, serving as the primary source of the Ob River. The headwaters of the Katun River originate on Mount Belukha, the highest mountain in Siberia at 4,506 metres (14,783 ft), which is located on the far eastern edge of the preserve. Katun is an internationally important center of biodiversity, forming part of the "Golden Mountains of Altai" UNESCO World Heritage Site. Katun Nature Reserve is situated in the Ust-Koksinsky District of Altai Republic.

<span class="mw-page-title-main">Bashkiriya Nature Reserve</span> Nature reserve in Bashkortostan, Russia

Bashkirsky Nature Reserve (Zapovednik) is located in the central part of the Bashkir (Southern) Urals. It features forested mountain slopes from the western slopes of the southern Ural Mountains to the Kaga River, and a displays the transition from mountain forest to steppe-forest. The reserved is situated in the Burzyansky District of Bashkortostan.

<span class="mw-page-title-main">Vitim Nature Reserve</span> Nature reserve in Irkutsk Oblast, Russia

Vitim Nature Reserve is a Russian 'zapovednik' in the mountains 400 km northeast of Lake Baikal in the Irkutsk region of Siberia. It covers the upper reaches of the Vitim River, a left tributary of the Lena River. The reserve protects a wide variety high-altitude, continental climate flora and fauna complexes: larch taiga, cedar thickets, mountain tundra, and sub-alpine meadows of the Delyun-Uran and Kodar Mountains. The reserve is located in the southeast of the Bodaybinsky District of Irkutsk Oblast, 150 km east of the regional city of Bodaybo. It was formally established in 1982, and covers 585,838 ha (2,261.93 sq mi).

<span class="mw-page-title-main">West Siberian taiga</span> Ecoregion which covers the West Siberian Plain in Russia

The West Siberian taiga ecoregion covers the West Siberian Plain in Russia, from the Ural mountains in the west to the Yenisei River in the east, and roughly from 56° N to 66° N latitude. It is a vast, flat lowland region of boreal forests (taiga), and wetlands, covering an area about 1,800 km west–east, by 1,000 km north–south.

<span class="mw-page-title-main">Northeast Siberian taiga</span> Ecoregion in northeastern Siberia, Russia

The Northeast Siberian taiga ecoregion is an area of "sparse taiga forest" between the Lena River and the Kolyma River in northeastern Siberia, Russia. The ecoregion's internal borders form a patchwork of territory constituting the southern part of the East Siberian Lowland, as well as lowlands around the East Siberian Mountains, including the ridges and peaks of the Verkhoyansk Range and the Chersky Range. On the southern border of the ecoregion is the north coast of the Sea of Okhotsk, giving the region maritime boreal forests as well as the continental forests situated inland. The ecoregion is one of the largest tracts of virgin boreal forest in the world, due to the very sparse population and difficult access. It is mostly in the Sakha Republic.

<span class="mw-page-title-main">Okhotsk–Manchurian taiga</span> Ecoregion in the Russian Far East

The Okhotsk-Manchurian taiga ecoregion is an area of coniferous forests in the Russian Far East, covering the Amur River delta, the west coast of the Okhotsk Sea, and the rugged extension of the northern Sikhote-Alin Mountains that run southwest-to-northeast through the Primorsky and Khabarovsk regions. It is the southernmost taiga forest in Eurasia. The ecoregion is distinguished from surrounding ecoregions by the slightly warmer climate due to the maritime influence and the shield of the mountains to the west, and by the mixing of flora and fauna species from Okhotsk-Kamchatka communities to the north and Manchurian species from the south. The forest at lower altitudes is "light taiga", and "dark taiga" at higher altitudes.

<span class="mw-page-title-main">Kamchatka Taiga</span> Ecoregion in the middle of the Kamchatka Peninsula

The Kamchatka Taiga ecoregion is a "conifer island" in the middle of the Kamchatka Peninsula, along the Kamchatka River. It is the easternmost example of Siberian taiga. The region has unusual ecological conditions, a "snow forest" that combines low temperatures, high humidity and boreal forest with heavy snowfall. The local ecology is also affected by volcanic activity. The region is about 300 km long (north–south), and averages about 100 km west–east. It is in the Palearctic realm, and mostly in the Boreal forests/taiga ecoregion with a humid continental climate, cool summer climate. It covers 147,064 km2 (56,782 sq mi).

<span class="mw-page-title-main">Northern Canadian Shield taiga</span> Taiga ecoregion in Canada

Northern Canadian Shield taiga is a taiga ecoregion located in northern Canada, stretching from Great Bear Lake in the Northwest Territories to Hudson Bay in eastern Nunavut. The region supports conifer forests to its northern edge, where the territory grades into tundra. The open forest in this transition zone is characterized by widely scattered, stunted stands of black spruce and tamarack, with some white spruce. The ecoregion lies over the northwestern extent of the Canadian Shield.

<span class="mw-page-title-main">Kamchatka–Kurile meadows and sparse forests</span> Rcoregion that covers parts of the Russian Far East

The Kamchatka-Kurile meadows and sparse forests ecoregion covers the coastal zones of the Kamchatka peninsula, northern section of the Kuril Islands, and the Commander Islands in the Russian Far East. The region noted for its sparse forests of Betula ermanii, and also for extensive tall-herb meadows. It is in the Palearctic realm, and mostly in the boreal forests/taiga biome with a Humid continental climate, cool summer climate. It covers 146,334 km2 (56,500 sq mi).

<span class="mw-page-title-main">Urals montane tundra and taiga</span> Ecoregion which covers the main ridge of the Ural Mountains

The Urals montane tundra and taiga ecoregion covers the main ridge of the Ural Mountains - a 2,000 km (north-south) by 300 km (west-east) region. The region is on the divide between European and Asian ecoregions, and also the meeting point of tundra and taiga. It is in the Palearctic realm, and mostly in the Boreal forests/taiga ecoregion with a Humid continental climate, cool summer climate. It covers 174,565 km2 (67,400 sq mi).

<span class="mw-page-title-main">Katon-Karagay National Park</span>

Katon-Karagay National Park is the largest national park in Kazakhstan, located on the eastern edge of the country, in the Southern Altai Mountains. The park fills the west side of the "X" where the borders of Kazakhstan, Russia, China, and Mongolia meet. The highest peak in Siberia, is on the Russian border in the Katun Range. The park is in Katonkaragay District of East Kazakhstan Region, 1,000 kilometres (620 mi) southeast of the capital city of Astana.

<span class="mw-page-title-main">Altai montane forest and forest steppe</span> Ecoregion in the Altai Mountains

The Altai montane forest and forest steppe ecoregion covers patches of the subalpine forest belt on the Altai Mountains, crossing the border region where Russia, Kazakhstan, Mongolia and China meet. The region has high biodiversity, as it is located in transition zones between different ecoregions, altitudes, and climate zones. It is in the Palearctic realm, with a Cold semi-arid climate. It covers 35,199,998 km2 (13,590,795 sq mi).

<span class="mw-page-title-main">Kamchatka Mountain tundra and forest tundra</span>

The Kamchatka Mountain tundra and forest tundra ecoregion is an ecoregion that covers the central mountain range of the Kamchatka Peninsula in the Russian Far East. The region is one of volcanos, caldera, geysers, and mountain tundra. It is in the Palearctic realm and tundra biome. It has an area of 119,400 square kilometres (46,100 sq mi).

<span class="mw-page-title-main">Faroe Islands boreal grasslands</span> Grasslands ecoregion

The Faroe Islands boreal grasslands ecoregion covers all of the territory of the Faroe Islands, an archipelago of 18 islands in the North Atlantic, roughly equidistant between Scotland, Norway, and Iceland. The ground cover is mostly grassland and dwarf shrub heath, the remainder is bare ground or sparse vegetation. There are no forests on the islands.

<span class="mw-page-title-main">Middle Arctic tundra</span> Tundra ecoregion of Canada

The Canadian Middle Arctic Tundra ecoregion covers a broad stretch of northern Canada - the southern islands of the Arctic Archipelago, plus the northern mainland of Nunavut and, across Hudson Bay to the east, a portion of northern Quebec. This is the coldest and driest ecoregion in Canada, and can be referred to as a 'polar desert'. It is an important region for breeding and migratory birds, and supports 80% of the world's muskox.

<span class="mw-page-title-main">Ogilvie–MacKenzie alpine tundra</span> Tundra ecoregion of Canada and the United States

The Ogilvie–MacKenzie alpine tundra ecoregion covers the mountainous middle of the Yukon Territory in Canada, with extensions into the Northwest Territories. The vegetation is alpine and subalpine open forest of stunted spruce, fir and pine. The area is rugged but sections appear to have been unglaciated in the late Pleistocene and there are therefore relic species in the region. The area is remote and supports large, sustainable predator-prey systems.

<span class="mw-page-title-main">Torngat Mountain tundra</span>

The Torngat Mountain tundra ecoregion covers the Torngat Mountains on the northeastern tip of the Labrador Peninsula where the provinces of Quebec and Newfoundland and Labrador meet. The mountains feature glacially carved U-shaped valleys and deep fjords. The vegetation over most of the territory is that of arctic tundra, herbaceous cover, or bare rock. The region supports seasonal polar bears, black bears, and caribou. The Atlantic coast is on the Atlantic Flyway for migratory birds.

<span class="mw-page-title-main">Zigalga National Park</span>

Zigalga National Park is located on the high Zigalga Ridge of the Southern Ural Mountains in Russia, on the transition between Europe and Siberia. Much of the territory is untouched by human activity and so supports Ice Age relict floral communities through all altitude zones - pine and birch forest, dark coniferous taiga, alpine meadows and mountain tundra. The park was officially created in 2019. The park is located in the Katav-Ivanovsky District of Chelyabinsk Oblast.

References

  1. "Iceland boreal birch forests and alpine tundra". World Wildlife Federation. Retrieved March 21, 2020.
  2. "Map of Ecoregions 2017". Resolve, using WWF data. Retrieved September 14, 2019.
  3. 1 2 3 "Iceland boreal birch forests and alpine tundra". Digital Observatory for Protected Areas. Retrieved August 1, 2020.
  4. "Iceland boreal birch forests and alpine tundra". The Encyclopedia of Earth. Retrieved August 28, 2020.
  5. 1 2 3 4 5 6 "Biodiversity in Iceland. National Report to the Convention on Biodiversity" (PDF). Ministry for the Environment, The Icelandic Institute of Natural History. Retrieved October 13, 2020.
  6. Kottek, M.; Grieser, J.; Beck, C.; Rudolf, B.; Rubel, F. (2006). "World Map of Koppen-Geiger Climate Classification Updated" (PDF). Gebrüder Borntraeger 2006. Retrieved September 14, 2019.
  7. "Dataset - Koppen climate classifications". World Bank. Retrieved September 14, 2019.