A biome, or "major life zone," is a large geographic region of the earth's surface with distinctive plant and animal communities. There are both terrestrial biomes, such as grasslands and tropical rain forests, and aquatic biomes, such as estuaries.
A biome may also be defined as an extensive ecosystem (ecological unit of living organisms and their abiotic environment) spread over a wide geographic area, or as a grouping of many ecosystems that share similar environmental features and communities (organisms living together in a certain area). Collectively, biomes comprise the biosphere, which is the thin area of the earth's surface where all organisms live.
Biomes are a dynamic, rather than static, entity, and have changed throughout geological history. More recently, biomes have been impacted by human activity. Some of these impacts, such as deforestation, have caused significant environmental challenges. It is important that people understand their local, regional, and global impacts and act responsibly toward the environment, such that future generations can enjoy the integrity and diversity of nature. In biblical terms, this is referred to as the "third blessing," the role of humans to care for all of creation, both the biotic component and the abiotic physical environment.
Biomes represent a superficial and somewhat arbitrary classification of ecosystems. Biologists are not unanimous in how they classify biomes or in the number of biomes. One biologist may classify one particular area as one biome, while another classifies the same region as an ecotone (the area where one biome overlaps another) or as a different biome. In some cases, the word "biome type" is utilized, whereby several biomes are combined into this biome type. For example, the coniferous forest biome type includes the coniferous forest biomes of Europe, Asia, and North America.
Among commonly recognized land biomes are tundra, taiga, temperate deciduous forest, grasslands, deserts, and tropical rain forests, and two major water biomes are those of marine and fresh water. Others add such biomes as temperate rain forests, chaparral, and coniferous forests, and further delineate aquatic biomes into ocean, estuaries, and so forth.
It has long been noted that regions of the earth with similar climate tend to have plants and animals with similar adaptations. For example, regions with long, dry periods of little rainfall (deserts) contain plants and animals adapted to these dry conditions. Such plants may flower during the rare periods of rainfall, and tend to be tough, woody shrubs or succulents.
Biomes represent a useful, albeit crude way of classifying ecosystems. Classification of biomes varies and no one system dominates biogeographical studies.
A fundamental classification of biomes is into:
Four specific classification methods are discussed below.
Biomes are most strongly defined by global distributions of vegetation types, which are influenced by global climate, soils, and other physical environment factors. In turn, climate and soil depend partly on latitude, altitude, and terrain factors.
With the exception of deserts and the polar biomes, terrestrial biomes are generally named for the dominant type of vegetation (climax vegetation), such as deciduous forests and coniferous forests.
The following is a common classification of biomes that one might find in introductory textbooks on the topic:
Arctic and Antarctic regions
Northern North America, Europe, and Asia
Northern Hemisphere, south of Tundra
About one-fourth of land surface of the earth
Extensive areas found on all continents
The subcategories of the Marine Biome (Ocean, Intertidal Zones, and Estuaries) are also considered biomes.
Biomes are often given local names. For example, a temperate grassland, savanna, and 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 in Australia.
Latitude is a major climate-influencing factor determining biomes. There is a good correlation between the distribution of climates with latitude, and homogenous 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:
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:
Climate, simply defined, is the long-term weather of an area. World terrestrial biomes are controlled by climate, and in particular by air temperature and precipitation. The Koppen Climate Classification System is the most widely employed system for classifying the world's climates. This system recognizes five major climate types, based on the annual and monthly averages of temperature and precipitation. For example, Moist Tropical Climates are known for their high temperatures year round and for the large amount of rain year round. Further subgroups distinguish specific seasonal characteristics of temperature and precipitation. The Koppen symbol is presented by a capital letter and small letter system. Using the Koppen Classification system, terrestrial biomes are listed such as Tropical Rainforest (Af), Tropical Rainforest, evergreen forest (Am), Savannah (Aw), Desert (BW), Polar (E), and so forth.
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