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taiga

 
Dictionary: tai·ga   (') pronunciation
n.
A subarctic, evergreen coniferous forest of northern Eurasia located just south of the tundra and dominated by firs and spruces.

[Russian taĭga, of Altaic origin.]


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Open coniferous forest (see conifer) growing on swampy ground that is commonly covered with lichens. It is the characteristic vegetation of the subpolar region of northern Eurasia (principally Russia, including Siberia, and Scandinavia) and northern North America, bounded by the colder tundra to the north and the warmer temperate zone to the south. Spruces and pines are the dominant trees. Soil organisms are protozoans, nematodes, and rotifers; larger invertebrates (e.g., insects) that decompose plant litter are lacking, so humus accumulates very slowly. The taiga is rich in fur-bearing animals (e.g., sable, fox, and ermine) and is home to elks, bears, and wolves. Siberian taiga alone accounts for 19% of the world's forested area and possibly 25% of total forest volume. Despite the remoteness of the taiga, it is a major source of lumber for construction, and huge expanses have been clear-cut.

For more information on taiga, visit Britannica.com.

A zone of forest vegetation encircling the Northern Hemisphere between the arctic-subarctic tundras in the north and the steppes, hardwood forests, and prairies in the south. The chief characteristic of the taiga is the prevalence of forests dominated by conifers. The dominant trees are particular species of spruce, pine, fir, and larch. Other conifers, such as hemlock, white cedar, and juniper, occur locally, and the broad-leaved deciduous trees, birch and poplar, are common associates in the southern taiga regions. Taiga is a Siberian word, equivalent to “boreal forest.” See also Tundra.

The northern and southern boundaries of the taiga are determined by climatic factors, of which temperature is most important. However, aridity controls the forest-steppe boundary in central Canada and western Siberia. In the taiga the average temperature in the warmest month, July, is greater than 50°F (10°C), distinguishing it from the forest-tundra and tundra to the north; however, less than four of the summer months have averages above 50°F (10°C), in contrast to the summers of the deciduous forest further south, which are longer and warmer. Taiga winters are long, snowy, and cold—the coldest month has an average temperature below 32°F (0°C). Permafrost occurs in the northern taiga. It is important to note that climate is as significant as vegetation in defining taiga. Thus, many of the world's conifer forests, such as those of the American Pacific Northwest, are excluded from the taiga by their high precipitation and mild winters.


The predominantly coniferous forest located south of the tundra in northern continents. See boreal forest.


[Ge]

Ecological zone that is slightly more temperate than tundra, with a vegetation cover composed of stunted forest, mainly coniferous, on frozen subsoil. Probably much more extensive than tundra in periglacial Europe. Also known as boreal forest.

 
taiga ('), northern coniferous-forest belt of Eurasia, bordered on the north by the treeless tundra and on the south by the steppe. This vast belt, comprising about one third of the forest land of the world, extends south from the tundra to about lat. 62°N in Norway, Sweden, and Finland, but dips still farther south to about lat. 53°N in the Urals. It extends through northern European Russia across the Ural Mountains and over most of Siberia. It has a continental climate, with long, severe winters of 6 or 7 months. Thawing occurs during late April or early May, and the growing season is short. The mean average summer temperatures are fairly high, but there are night frosts. Podzols are the soils of this zone. Only the hardier cereals and roots, such as barley, oats, and potatoes, can be cultivated. The principal species of trees are cedar, pine, spruce, larch, birch, and aspen. The taiga has many swampy areas formed during the spring.


Wikipedia: Taiga
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The taiga is found throughout the high northern latitudes, between the tundra, and the temperate forest, near 50° around the Arctic Circle.
Biomes
Terrestrial biomes
Tundra
Taiga/boreal forests
Montane grasslands and shrublands
Temperate coniferous forests
Tropical and subtropical coniferous forests
Temperate broadleaf and mixed forests
Mediterranean forests, woodlands, and scrub
Tropical and subtropical moist broadleaf forests
Tropical and subtropical dry broadleaf forests
Temperate grasslands, savannas, and shrublands
Tropical and subtropical grasslands, savannas, and shrublands
Deserts and xeric shrublands
Flooded grasslands and savannas
Riparian
Wetland
Aquatic biomes
Pond
Littoral/intertidal zone
Mangrove forests
Kelp forest
Coral reef
Neritic zone
Continental shelf
Pelagic zone
Benthic zone
Hydrothermal vents
Cold seeps
Pack ice
Other biomes
Endolithic zone

Taiga (pronounced /ˈtaɪɡə/, from Turkic[1] or Mongolian) is a biome characterized by coniferous forests. Covering most of the inlands Alaska, Canada, Sweden, Finland, inland Norway, the Scottish Highlands and Russia (especially Siberia), as well as parts of the extreme northern continental United States (Northern Minnesota, Michigan's Upper Peninsula, Upstate New York, Vermont, New Hampshire, and Maine), northern Kazakhstan and Japan (Hokkaidō), the taiga is the world's largest terrestrial biome.

Although this biome is correctly named Taiga, the term Boreal forest is usually used to refer to the more southerly part of the biome, while the term Taiga is more often used to describe only the more barren northern areas of the Arctic tree line.

Since North America and Asia were formerly connected by the Bering land bridge, a number of animal and plant species (more animals than plants) were able to colonize both continents and are distributed throughout the taiga biome (see Circumboreal Region). Others differ regionally, typically with each genus having several distinct species, each occupying different regions of the taiga. Taigas also have some small-leaved deciduous trees like birch, alder, willow, and aspen; mostly in areas escaping the most extreme winter cold. However, the deciduous larch tolerates the coldest winters on the northern hemisphere in eastern Siberia. The very southernmost parts of the taiga may also have trees like oak, maple, elm and tilia scattered among the conifers.

Contents

Climate and geography

White Spruce taiga, Denali Highway, Alaska Range, Alaska

Taiga, the world's largest land biome, has a harsh continental climate with a very large temperature range between summer and winter, classified as "Dfc" or "Dfb" in the Köppen climate classification scheme. Aside from the tundra and permanent ice caps, it is the coldest biome on Earth. High latitudes mean that for much of the year the sun does not rise far above the horizon. Winters last at least 5–6 months, with average temperatures below freezing. Temperatures vary from −54°C to 27°C (-65°F to 80°F) throughout the whole year, with eight or more months of temperatures averaging below 10 °C (50°F). The summers, while short, are generally warm and humid. In general, taiga grows to the south of the 10 °C July isotherm, but occasionally as far north as the 9 °C July isotherm.[2] The southern limit is more variable, depending on rainfall; taiga may be replaced by open steppe woodland south of the 15 °C July isotherm where rainfall is very low, but more typically extends south to the 18 °C July isotherm, and locally where rainfall is higher (notably in eastern Siberia and adjacent northern Manchuria) south to the 20 °C July isotherm. In these warmer areas, the taiga has higher species diversity with more warmth-loving species such as Korean Pine, Jezo Spruce and Manchurian Fir, and merges gradually into mixed temperate forest, or more locally (on the Pacific Ocean coasts of North America and Asia) into coniferous temperate rainforests.

The taiga experiences relatively low precipitation throughout the year (200–750 mm annually), primarily as rain during the summer months, but also as fog and snow; as evaporation is also low for most of the year, precipitation exceeds evaporation and is sufficient for the dense vegetation growth. Snow may remain on the ground for as long as nine months in the northernmost extensions of the taiga ecozone.[3]

Much of the area currently classified as taiga was recently glaciated. As the glaciers receded, they left depressions in the topography that have since filled with water, creating lakes and bogs (especially muskeg soil), found throughout the Taiga.

Soils

Taiga soil tends to be young and nutrient-poor; it lacks the deep, organically-enriched profile present in temperate deciduous forests.[4] The thinness of the soil is due largely to the cold, which hinders the development of soil and the ease with which plants can use its nutrients.[4] Fallen leaves and moss can remain on the forest floor for a long time in the cool, moist climate, which limits their organic contribution to the soil; acids from evergreen needles further leach the soil, creating spodosol.[5] Since the soil is acidic due to the falling pine needles, the forest floor has only lichens and some mosses growing on it.

Flora

Boreal Forest near Lake Baikal in Russia

There are two major types of taiga, closed forest, consisting of many closely-spaced trees with mossy ground cover, and lichen woodland, with trees that are farther-spaced and lichen ground cover; the latter is more common in the northernmost taiga.[6] In the northernmost taiga the forest cover is not only more sparse, but often stunted in growth form; moreover, ice pruned asymmetric Black Spruce are often seen, with diminished foliage on the windward side.[7]

The forests of the taiga are largely coniferous, dominated by larch, spruce, fir, and pine. Evergreen species in the taiga (spruce, fir, and pine) have a number of adaptations specifically for survival in harsh taiga winters, although larch, the most cold-tolerant of all trees,[citation needed] is deciduous. Taiga trees tend to have shallow roots to take advantage of the thin soils, while many of them seasonally alter their biochemistry to make them more resistant to freezing, called "hardening".[8] The narrow conical shape of northern conifers, and their downward-drooping limbs, also help them shed snow.[8]

Because the sun is low in the horizon for most of the year, it is difficult for plants to generate energy from photosynthesis. Pine and spruce do not lose their leaves seasonally and are able to photosynthesize with their older leaves in late winter and spring when light is good but temperatures are still too low for new growth to commence. The adaptation of evergreen needles limits the water lost due to transpiration and their dark green color increases their absorption of sunlight. Although precipitation is not a limiting factor, the ground freezes during the winter months and plant roots are unable to absorb water, so desiccation can be a severe problem in late winter for evergreens.

Moss (Ptilium crista-castrensis) cover on the floor of taiga

Although the taiga is dominated by coniferous forests, some broadleaf trees also occur, notably birch, aspen, willow, and rowan. Many smaller herbaceous plants grow closer to the ground. Periodic stand-replacing wildfires (with return times of between 20-200 years) clear out the tree canopies, allowing sunlight to invigorate new growth on the forest floor. For some species, wildfires are a necessary part of the life cycle in the taiga; some, e.g. Jack Pine have cones which only open to release their seed after a fire, dispersing their seeds onto the newly cleared ground. Grasses grow wherever they can find a patch of sun, and mosses and lichens thrive on the damp ground and on the sides of tree trunks. In comparison with other biomes, however, the taiga has a low biological diversity.

Coniferous trees are the dominant plants of the taiga biome. A very few species in four main genera are found: the evergreen spruce, fir, and pine, and the deciduous larch or tamarack. In North America, one or two species of fir and one or two species of spruce are dominant. Across Scandinavia and western Russia the Scots pine is a common component of the taiga.

Fauna

The taiga is home to a number of large herbivorous mammals and smaller rodents. These animals have also adapted to survive the harsh climate. Some of the larger mammals, such as bears, eat during the summer in order to gain weight and then go into hibernation during the winter. Other animals have adapted layers of fur or feathers to insulate them from the cold.

A number of wildlife species threatened or endangered with extinction can be found in the Canadian Boreal forest including woodland caribou, American black bear, grizzly bear and wolverine. Habitat loss due to destructive development, mostly in the form of logging, is the main cause of decline for these species.

Due to the climate, carnivorous diets are an inefficient means of obtaining energy; energy is limited, and most energy is lost between trophic levels. However, predatory birds (owls and eagles) and other smaller carnivores, including foxes and weasels, feed on the rodents. Larger carnivores, such as lynx and wolves, prey on the larger animals. Omnivores, such as bears and raccoons are fairly common, sometimes picking through human garbage.

A considerable number of birds such as Siberian Thrush, White-throated Sparrow and Black-throated Green Warbler, migrate to this habitat to take advantage of the long summer days and abundance of insects found around the numerous bogs and lakes. Of the perhaps 300 species of birds that summer in the taiga, only 30 stay for the winter.[9] These are either carrion-feeding or large raptors that can take live mammal prey, including Golden Eagle, Rough-legged Buzzard, and Raven, or else seed-eating birds, including several species of grouse and crossbills.

Plesetsk Cosmodrome is situated in the taiga

Threats

Human activities

Large areas of Siberia’s taiga have been harvested since the collapse of the Soviet Union.[10] In Canada, less than eight percent of the Boreal forest is protected from development and more than 50% has been allocated to logging companies for cutting.[11] The main form of forestry in the Boreal forest in Canada is clearcutting, where most if not all trees are removed from an area of forest. Clearcut upwards of 110 km² have been recorded in the Canadian Boreal forest. Some of the products from logged Boreal forests include toilet paper, copy paper, newsprint and lumber. More than 80% of Boreal forest products from Canada are exported for consumption and processing in the United States.

Most companies that harvest in Canadian forests are certified by an independent third party agency such as the Forest Stewardship Council (FSC), Sustainable Forests Initiative (SFI), or the Canadian Standards Association (CSA). While the certification process differs between these various groups, all of them include forest stewardship, respect for aboriginal peoples, compliance with local, provincial and/or national environmental laws, forest worker safety, education and training, and other environmental, business and social requirements. The prompt renewal of all harvest sites by planting or natural renewal is also required.

Insects

Recent years have seen outbreaks of insect pests in forest-destroying plagues: the spruce-bark beetle (Dendroctonus rufipennis) in the Yukon Territory, Canada, and Alaska;[12] the aspen-leaf miner; the larch sawfly; the spruce budworm (Choristoneura fumiferana);[13] the spruce coneworm.[14]

See also

References

  1. ^ "taiga." Dictionary.com Unabridged (v 1.1). Random House, Inc. 12 Mar. 2008. web link
  2. ^ Arno & Hammerly 1984, Arno et al. 1995
  3. ^ A.P. Sayre, Taiga, (New York: Twenty-First Century Books, 1994) 16.
  4. ^ a b Sayre, 19.
  5. ^ Sayre, 19-20.
  6. ^ Sayre, 12-3.
  7. ^ C. Michael Hogan, Black Spruce: Picea mariana, GlobalTwitcher.com, ed. Nicklas Stromberg, November, 2008
  8. ^ a b Sayre, 23.
  9. ^ Sayre, 28.
  10. ^ Taiga Deforestation
  11. ^ Global Forest Watch Canada 2000. Canada’s Forests At A Crossroads — An Assessment in the Year 2000
  12. ^ http://www.colorado.edu/INSTAAR/AW2004/get_abstr.html?id=88 A New Method to Reconstruct Bark Beetle Outbreaks
  13. ^ Spruce budworm and sustainable management of the boreal forest
  14. ^ http://www.fs.fed.us/pnw/pubs/journals/pnw_2006_chapin001.pdf

Notes

  • Arno, S. F. & Hammerly, R. P. 1984. Timberline. Mountain and Arctic Forest Frontiers. The Mountaineers, Seattle. ISBN 0-89886-085-7
  • Arno, S. F., Worral, J., & Carlson, C. E. (1995). Larix lyallii: Colonist of tree line and talus sites. Pp. 72–78 in Schmidt, W. C. & McDonald, K. J., eds., Ecology and Management of Larix Forests: A Look Ahead. USDA Forest Service General Technical Report GTR-INT-319.
  • Sayre, A. P. (1994). Taiga. New York: Twenty-First Century Books. ISBN 0-8050-2830-7

External links


Translations: Taiga
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Dansk (Danish)
n. - taiga

Nederlands (Dutch)
taiga (streek met naaldhout)

Français (French)
n. - Taïga

Deutsch (German)
n. - Taiga (sibirische Waldsteppe)

Ελληνική (Greek)
n. - (γεωγρ.) τάιγκα, (περιοχή με) δάση κωνοφόρων

Italiano (Italian)
taiga

Português (Portuguese)
n. - taiga (f)

Русский (Russian)
Тайга

Español (Spanish)
n. - taiga

Svenska (Swedish)
n. - tajga

中文(简体)(Chinese (Simplified))
针叶树林地带

中文(繁體)(Chinese (Traditional))
n. - 針葉樹林地帶

한국어 (Korean)
n. - 타이가 (침엽수 지대)

日本語 (Japanese)
n. - タイガ

العربيه (Arabic)
‏(الاسم) ألتيغه - غابه صنوبر سبخه‏

עברית (Hebrew)
n. - ‮טייגה (איזור יערות עצי מחט בסיביר)‬


 
 
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