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Last edited February 23, 2026

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Desertic region at the M'Sila Province, Algeria
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Extent of deserts and xeric shrublands

Deserts and xeric shrublands are a biome defined by the World Wide Fund for Nature.[1] Deserts and xeric (Ancient Greek Template:Lang Template:Translit 'dry') shrublands form the largest terrestrial biome, covering 19% of Earth's land surface area.[2] Ecoregions in this habitat type vary greatly in the amount of annual rainfall they receive, usually less than Template:Convert annually except in the margins. Generally evaporation exceeds rainfall in these ecoregions. Temperature variability is also diverse in these lands. Many deserts, such as the Sahara, are hot year-round, but others, such as East Asia's Gobi Desert, become quite cold during the winter.[1]

Temperature extremes are a characteristic of most deserts. High daytime temperatures give way to cold nights because there is no insulation provided by humidity and cloud cover. The diversity of climatic conditions, though quite harsh, supports a rich array of habitats. Many of these habitats are ephemeral in nature, reflecting the paucity and seasonality of available water.[1] Woody-stemmed shrubs and plants characterize vegetation in these regions. Above all, these plants have evolved to minimize water loss. Animal biodiversity is equally well adapted and quite diverse.[1]

Degradation

Desertification

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File:Sengi-landscape Nama Karoo.tif
The Nama Karoo in South Africa is a xeric shrubland that receives between Template:Convert of rain a year.[3]

The conversion of productive drylands to desert conditions, known as desertification, can occur from a variety of causes. One is human intervention, including intensive agricultural tillage or overgrazing[4] in areas that cannot support such exploitation. Climatic shifts such as global warming or the Milankovitch cycle (which drives glacials and interglacials) also affect the pattern of deserts on Earth.

Woody plant encroachment

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Xeric shrublands can experience woody plant encroachment, which is the thickening of bushes and shrubs at the expense of grasses.[5] This process is often caused by unsustainable land management practices, such as overgrazing and fire suppression, but can also be a consequence of climate change. As a result, the shrublands' core ecosystem services are affected, including its biodiversity, productivity, and groundwater recharge.[6] Woody plant encroachment can be an expression of land degradation.[7]

Ecoregions

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The World Wide Fund for Nature highlights a number of desert ecoregions that have a high degree of biodiversity and endemism:[1]

See also

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References

  1. 1.0 1.1 1.2 1.3 1.4 1.5 1.6 Template:CC-notice Deserts and Xeric Shrubland Ecoregions. Retrieved 2019-05-29.
  2. Managing Protected Areas: A Global Guide{{#if:Lockwood|, Lockwood}
  3. Nama Karoo. WWF. Retrieved 2018-12-19.
  4. Template:Cite encyclopedia
  5. Impacts of shrub encroachment on ecosystem structure and functioning: towards a global synthesis: Synthesizing shrub encroachment effects. Ecology Letters({Template:Date).
  6. [{{{url}}} Woody Plant Encroachment: Causes and Consequences]. Springer International Publishing(2017).
  7. Biological Feedbacks in Global Desertification. Science({Template:Date).
  8. Botanical diversity in southern Africa{{#if:|, {{{last}}}}. National Botanical Institute(1994)
  9. Terrestrial ecoregions of North America : a conservation assessment{{#if:|, {{{last}}}}. Island Press(1999). ISBN 1-55963-722-6

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Template:Palearctic desert and xeric shrubland ecoregions Template:Biomes Template:Biodiversity of South Africa