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cheese# ] (or continental) biomes and
In ], a ''biome'' is a major regional group of distinctive ] and ] ] best adapted to the region's physical ], ], ], and ]. A biome is made up of ] at stable steady state and all associated transitional, disturbed, or degraded, ], ] and ], but can often be identified by the ] type.

A fundamental classification of biomes is into:
# ] (or continental) biomes and
# Aquatic biomes. # Aquatic biomes.


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Revision as of 16:43, 25 September 2006

cheese# Terrestrial (or continental) biomes and

  1. Aquatic biomes.

Biomes are often given local names. For example, a Temperate grassland or shrubland biome is known commonly as steppe in central Asia, savanna or veld in southern Africa, prairie in North America, pampa in South America and outback or scrub in Australia. Sometimes an entire biome may be targeted for protection, especially under an individual nation's Biodiversity Action Plan.

Latitude classification

Latitude is a major climate-influencing factor determining biomes. There is a good correlation between the distribution of climates with latitude, and homogeneous vegetation bands. Another major factor is humidity. This can be illustrated by the fact that biodiversity increases away from the poles towards the equator, and increases with humidity. The most widely used classification of biomes is related to latitude (or temperature zoning) and humidity

Arctic or subarctic area

Subarctic and boreal area

The Boreal Forest is the largest of all biomes. It is located in the northern hemishphere just south of the tundra.

Temperate cold

Tropical

Aquatic

Altitude and latitude classification

Another system of classification takes into account altitude and humidity, ignoring temperature as a factor. This classification is used to define the Global 200 list of ecoregions identified by the World Wildlife Fund (WWF) as priorities for conservation.

This classification gives the following terrestrial biomes :

Other biomes

The Endolithic biome, consisting entirely of microscopic life in rock pores and cracks, kilometers beneath the surface, has only recently been discovered and does not fit well into most classification schemes.

See also

External link

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