Desert

No precise definition of a desert exists. From an ecological viewpoint the scarcity of rainfall is all important, as it directly affects plant productivity which in turn affects the abundance, diversity, and activity of animals. It has become customary to describe deserts as extremely arid where the mean precipitation is less than 2.5–4 in. (60–100 mm), arid where it is 2.5–4 to 6–10 in. (60–100 to 150–250 mm), and semiarid where it is 6–10 to 10–20 in. (150–250 to 250–500 mm). However, mean figures tend to distort the true state of affairs because precipitation in deserts is unreliable and variable. In some areas, such as the Atacama in Chile and the Arabian Desert, there may be no rainfall for several years. It is the biological effectiveness of rainfall that matters and this may vary with wind and temperature, which affect evaporation rates. The vegetation cover also alters the evaporation rate and increases the effectiveness of rainfall. Rainfall, then, is the chief limiting factor to biological processes but intense solar radiation, high temperatures, and a paucity of nutrients (especially of nitrogen) may also limit plant productivity, and hence animal abundance. See also: Precipitation (meteorology)

The deserts of the world; those within the tropics are hot as well as arid.

 

 

 

بزرگنمایی تصویر

 

 

 

The main desert regions of the world are shown in the illustration. Most lie within the tropics and hence are hot as well as arid. The Namib and Atacama coastal deserts are kept cool by the Benguela and Humboldt ocean currents, and many desert areas of central Asia are cool because of high latitude and altitude.

 

Plant production

 

As a consequence of unreliable rainfall, plant productivity is much more variable than in most ecosystems. It may vary from none to 880 dry lb/acre · yr (1000 dry kg/ha · yr) although in most places there is usually some productivity even when there is no rainfall. The average biomass is generally low at 0.004–0.144 dry lb/ft2 (0.02–0.7 dry kg/m2) compared to 9.25 dry lb/ft2 (45 dry kg/m2) in tropical forest and 6.17 dry lb/ft2 (30 dry kg/m2) in temperate forest. Another feature of desert vegetation is the low percentage of green, photosynthetic plant biomass. There is also about three times as much dead as living plant material, a high figure compared to most other ecosystems. See also: Biological productivity; Biomass

Between 10 and 20% of the living plant material is eaten by consumers, a figure typical of terrestrial ecosystems, where the level of consumption may be as low as 5% (compared to over 90% in ocean ecosystems). Much desert vegetation tends to be hard and prickly and hence unpalatable to many consumers. Dead plant material does not accumulate and is utilized by the decomposers, particularly wood-eating termites. Seeds are abundant and can survive a long time without germinating. Many animals, including rodents, ants, and birds, depend heavily upon them for food. There is evidence of both intra- and interspecific competition for seeds, the production of which varies markedly with variations in rainfall.

A common viewpoint is that desert plants and animals live in a harsh environment and as a consequence have evolved many morphological and behavioral adaptations that enable them to “escape” the rigors of their surroundings. Certainly extreme aridity coupled with extreme heat seems a stressful environment, but whether desert organisms really possess more escape adaptations than, say, rainforest organisms is a matter for conjecture. Nevertheless, specific adaptations to drought and heat can be readily identified.

 

Adaptations in plants

 

In many deserts, annual rather than perennial plants form the bulk of the climax vegetation, quite unlike the situation in most terrestrial ecosystems where perennial plants dominate. Deserts, especially those within the tropics, periodically “bloom” with flowering annuals soon after a significant rainfall. In general, the more unreliable the rainfall in a desert, the greater the abundance and diversity of annual plants. Estimates vary, but these annuals account for up to half the primary production in a year, although for a given site they may fail altogether if there is no rain. Many annuals last for only a very short time. They tend to have the C4 photosynthetic pathway, which means they grow quickly and opportunistically. It is these plants in particular that produce the vast quantities of seed which under extreme aridity can last for years, providing a “seed bank” until conditions are right for germination. Most ephemeral annuals do not have special drought-resistant or drought-tolerant adaptations: they are simply opportunists, much like the annuals of wetter communities which, however, tend to be successional rather than climax species. See also: Photosynthesis

Succulent plants occur in all deserts but nowhere as conspicuously as in the Sonoran Desert of North America. These fleshy plants store water in their tissues, and tend to be especially prickly, a defense against browsers which need water as well as food. In American deserts the obvious succulents are Cactaceae; in Africa where cactus is almost absent, many species of Euphorbiaceae have the same types of growth form and occupy essentially the same ecological niches. See also: Cactus; Caryophyllales

Other perennial plants include trees and shrubs with long tap roots that can reach underground water, making them independent of scarce and unreliable rainfall. Some perennials burst into leaf only after rain, and are hence leafless most of the time. Yet others retain leaves throughout dry periods; the leaves tend to be small and narrow and require relatively little water to photosynthesize. These plants, mostly small shrubs and grasses, invariably have an extensive root system which enables them to maximize their acquisition of water. See also: Physiological ecology (plant); Plant-water relations; Plants, life forms of

 

Adaptations in animals

 

A majority of terrestrial invertebrates are cryptic in coloration, matching almost exactly components of the background on which they normally live. Many invertebrates and small vertebrates, such as rodents and snakes, spend the day in holes and burrows, and become active at night, when it is cooler. In all environments there are many small animals that escape by hiding, in most places to escape from predators; but in deserts escape from high daytime temperatures and radiation appears to be the chief adaptive response. The burrow constructed by the New World kangaroo rat, Dipodomys, protects the animal from daytime heat and radiation and also from predatory snakes and birds. The entrance of the burrow is sealed with soil which allows a high (30%) relative humidity to develop which helps the animal maintain its water budget. Kangaroo rats do not drink but exist on water derived from seeds they eat; their urine is the most concentrated of all mammals, another antidesiccation adaptation. Desert birds also shelter and avoid the heat of the day. In the Kalahari, the social weaverbird, Philetarius socius, builds a gigantic communal nest in an acacia or other suitable tree. The insulation in the nest protects the birds from the heat of the day and the cold of the night. See also: Excretion; Protective coloration

The largest of all birds, the ostrich, Struthio camelus, is an inhabitant of arid regions of Africa. The birds are too large to retreat into hiding during the day, although they may seek the shade of a big tree. With a high ambient temperature (95°F or 35°C or more) and no wind an ostrich loses heat by panting and by erecting the sparsely distributed feathers on its back. If there is wind, panting ceases and heat is lost by convection across the erect back feathers. At night when it is cool or even cold (below 64°F or 18°C), the back feathers are flattened and an insulating layer of air is trapped which reduces heat loss.

Soon after heavy rainfall, holes and depressions in sand or rock fill with water and within a few hours teem with microscopic life, chiefly algae, bacteria, and protozoa. After a few days countless small crustaceans appear, such as fairy and tadpole shrimps. These grow and reproduce with great rapidity. They can tolerate high water temperatures and also the high salinity which often builds up in temporary desert pools. The pools soon disappear and the land may then remain dry for months, even years, before the next downpour. The shrimps and other organisms diapause in the soil, usually as eggs which are remarkably resistant to high temperatures and extreme desiccation. See also: Physiological ecology (animal)

 

Aestivation

 

The term aestivation is used to describe a lengthy period of dormancy during which metabolism is much reduced. Many desert animals are capable of prolonged aestivation which enables them to survive during periods of food and water scarcity. In insects such as butterflies, which have a complete metamorphosis (clear-cut egg, larval, pupal, and adult stages), aestivation can occur at any stage of the life cycle but is almost invariably confined to a particular stage for a given species. Before entering aestivation, most animals seek out a secluded place that provides the best protection from temperature fluctuations and solar radiation, as well as from predators. Many species, ranging from lungfish to insect larvae, construct some form of protective cocoon in which to aestivate. See also: Hibernation and estivation

 

Migration and movement

 

An alternative to aestivation is migration or other movement away in search of better feeding and breeding conditions. Some of the African antelopes, such as the oryx, Oryx gazella, undertake long-distance movements which are correlated with changes in the quality and quantity of grass upon which they feed. These grass characteristics in turn are determined by rainfall, so there may be regular movements to and from areas where the rainfall is predictable and regular, or much more erratic movements in areas of unpredictable rainfall.

The semiregular migrations of several species of African weaverbirds (Ploceidae) are strongly associated with the seeding of wild grasses. The birds may form flocks of thousands or even tens of thousands of individuals and descend on and devour ripening seeds before moving on. Some of these birds, including the black-faced dioch, Quelea quelea, have become serious pests of millet and other cereals grown on land irrigated from underground water. See also: Migratory behavior

The blooming of desert annuals and the leafing out of trees and shrubs soon after rainfall often result in a dramatic increase in abundance of leaf-eating insects. Eggs that have remained dormant for months produce larvae which can be so numerous as to defoliate vegetation. In Africa, white butterflies, Belenois, may migrate in vast numbers from areas where the larval food plants have been defoliated to areas where there is fresh growth. Pastoral people and their livestock undertake similar movements in response to changes in the availability of graze and browse for their animals, and to some extent, in response to changes in the risk of diseases such as trypanosomiasis, which affects both humans and domestic animals.

One of the most successful groups of desert animals is the grasshoppers. In many deserts there is a considerable variety of species, some of which are abundant. A few species are able to build up suddenly in numbers, often in response to unseasonal rain which has promoted a rapid growth of vegetation. They then undertake long-distance irruptive movements, followed by further breeding until they reach such numbers that they invade higher-rainfall areas and devastate crops. One of these grasshoppers, the desert locust, Schistocerca gregaria, can invade and seriously affect the vegetation of an area extending through 110° of longitude from West Africa to Assam, north to Turkey and south to southern Tanzania. Plagues of desert locusts may last for years and then suddenly stop, the locust reverting to a normal desert grasshopper.

 

Species diversity

 

The diversity of species of animals in a desert is generally correlated with the diversity of plant species, which to a considerable degree is correlated with the predictability and amount of rainfall. There is a rather weak latitudinal gradient of diversity with relatively more species nearer the Equator than at higher latitudes. This gradient is much more conspicuous in wetter ecosystems, such as forests, and in deserts appears to be overridden by the manifold effects of rainfall. Animals, too, may affect plant diversity: the burrowing activities of rodents create niches for plants which could not otherwise survive, and mound-building termites tend to concentrate decomposition and hence nutrients, which provide opportunities for plants to colonize.

 

Convergent evolution

 

Each desert has its own community of species, and these communities are repeated in different parts of the world. Very often the organisms that occupy similar niches in different deserts belong to unrelated taxa. The overall structural similarity between American cactus species and African euphorbias is an example of convergent evolution, in which separate and unrelated groups have evolved almost identical adaptations under similar environmental conditions in widely separated parts of the world. Convergent structural modification occurs in many organisms in all environments, but is especially noticeable in deserts where possibly the small number of ecological niches has necessitated greater specialization and restriction of way of life. The face and especially the large ears of desert foxes of the Sahara and of North America are remarkably similar, and there is an extraordinary resemblance between North American sidewinding rattlesnakes and Namib sidewinding adders. See also: Euphorbiales; Organic evolution

 

Desert community

 

Ecological change in deserts seems to occur slowly. Plant and animal succession is much less obvious than in other communities, although there is some evidence of cyclical change in which species replace one another. In the Chihuahuan Desert of North America, the shrub Larrea tridentata reduces the wind speed enough to cause accumulation of soil and organic nutrients around the bottom of the trunk. This enables other plants to establish themselves, including the cactus Opuntia leptocaulis, whose seeds are introduced into the accumulated soil via the feces of rodents and birds which eat the fruit. The cactus grows and its roots overrun and outcompete those of the Larrea shrub, which then dies and falls over. Wind and water erosion then dislodge the rather shallow roots of the cactus, which itself dies and topples over. The vacant space is eventually filled by another Larrea, and the cycle starts again. No one has witnessed the complete cycle, which is believed to take many years to complete, but all stages can be identified and the presumed sequence of events drawn together. See also: Ecological communities; Ecological succession; Ecology; Ecosystem

Denis F. Owen

 

Bibliography

 

 

  • G. N. Louw and M. K. Seely, Ecology of Desert Organisms, 1982
  • G. M. O. Maloiy (ed.), Comparative Physiology of Desert Animals, 1972
  • K. Schmidt-Nielsen, Desert Animals: Physiological Problems of Heat and Water, 1964
  • F. H. Wagner, Wildlife of the Deserts, 1980
  • alifazeli=egeology.blogfa.com