Tundra Biome: The Coldest Biome (original) (raw)

Autumn tundra landscape in Norway, Europe. Photo © Paul Oomen / Getty Images.

Updated on March 06, 2017

The tundra is a terrestrial biome that is characterized by extreme cold, low biological diversity, long winters, brief growing seasons, and limited drainage. The harsh climate of the tundra imposes such formidable conditions on life that only the hardiest plants and animals can survive in this environment. The vegetation that grows on the tundra is restricted to a low diversity of small, ground-hugging plants that are well-adapted to survive in nutrient-poor soils. The animals that inhabit the tundra are, in most cases, migratory—they visit the tundra during the growing season to breed but then retreat to warmer, more southern latitudes or lower elevations when temperatures drop.

Tundra habitat occurs in regions of the world that are both very cold and very dry. In the Northern Hemisphere, the Arctic lies between the North Pole and the boreal forest. In the Southern Hemisphere, the Antarctic tundra occurs on the Antarctic peninsula and on the remote islands that lie off the coast of Antarctica (such as the South Shetland Islands and the South Orkney Islands). Outside of the polar regions, there is another type of tundra—alpine tundra—which occurs at at high altitudes on mountains, above the treeline.

The soils that blanket the tundra are mineral-deprived and nutrient-poor. Animal droppings and dead organic matter provide the bulk of what nourishment is present in tundra soil. The growing season is so brief that only the topmost layer of soil thaws during the warm months. Any soils below a few inches deep remain permanently frozen, creating a layer of earth known as permafrost. This permafrost layer forms a water-barrier that prevents drainage of meltwater. During the summer, any water that thaws in the upper layers of the soil is trapped, forming a patchwork of lakes and marshes across the tundra.

Tundra habitats are vulnerable to the effects of climate change and scientists fear that as global temperatures rise, tundra habitats might play a role in accelerating the rise in atmospheric carbon. Tundra habitats are traditionally carbon sinks—places that store more carbon than they release. As global temperatures rise, tundra habitats may shift from storing carbon to releasing it in massive volumes. During the summer growing season, tundra plants grow quickly and, in doing so, they absorb carbon dioxide from the atmosphere. The carbon remains trapped because when the growing season ends, the plant material freezes before it can decay and release the carbon back into the environment. As temperatures rise and areas of permafrost thaw, the tundra releases the carbon it has stored for millennia back into the atmosphere.

Key Characteristics

The following are the key characteristics of tundra habitats:

Classification

The tundra biome is classified within the following habitat hierarchy:

Biomes of the World > Tundra Biome

The tundra biome is divided into the following habitats:

Animals of the Tundra Biome

Some of the animals that inhabit the tundra biome include: