Particularly protected components. Particularly protected components of nature

Specially protected natural areas (SPNA) are natural areas that are completely or partially removed from economic use for the purpose of conservation, maintenance, restoration (recreation) and study of biodiversity. They have different security regimes and are designed to solve different problems.
The main purpose of specially protected natural areas is to preserve the gene pool of nature. IN common system environmental activities carried out by humans, they are assigned the role of scientific testing grounds.

Depending on the functional purpose and protection regime, four groups of specially protected territories and objects are distinguished: reserve-standard (reserves and reserves with a reserved regime of environmental management); resource-protecting (reserves, soil-protecting and water-protecting forests); object protection (protective strips along highways and railways); environmental protection (green zones around populated areas, resort areas, natural and national parks, etc.); recreational (areas of land or water surface intended for recreation of the population, restoration of health, areas of tourist routes).

The reserve is natural area(or water area) completely excluded from economic use for the protection and study of the natural complex as a whole. One of the main tasks of nature reserves is to preserve standard natural landscapes, typical or unique for a given territory.
Biosphere reserves differ from other reserves in that their territory is subject to constant monitoring and control of anthropogenic changes in the natural environment.

A national park is a territory or water area with intact natural complexes and unique natural objects. National parks combine the tasks of nature conservation and strictly controlled recreational use, i.e. they are open for educational tourism and short-term recreation for citizens.

Natural monuments are unique or typical, valuable in scientific, cultural and health terms natural objects: lakes, waterfalls, river floodplains, caves, groves of rare trees, areas of virgin steppes, unique trees, mineral springs, meteorite craters, rare geological deposits, reference areas of mineral deposits, etc.

Wildlife sanctuaries. Natural reserves differ from previous categories in that their lands may or may not be alienated from owners and users; they can be of both federal and local subordination. Among the reserves federal significance Zoological forms play the largest role, other forms - landscape, botanical, forest, hydrological, geological - are less common. The main function of hunting and complex reserves of federal significance is the protection of game fauna. Hunting is always prohibited, but very significant restrictions are often introduced on forest exploitation, construction and some other types of economic activity.

Reserves. They are created in many countries. In terms of their regime and purpose, they are close to nature reserves and are divided into many categories, but in most cases they are created for an indefinitely long period. For example, in France, the Camargue ornithological reserve in the Rhone delta is designed to protect wintering and nesting waterfowl. The gigantic Central Kalahari Reserve in Africa is intended only for the protection of game animals.

There are many hunting and ornithological reserves in India, Burma, forest and biological reserves in the USA, landscape reserves in the UK, Germany, the Netherlands, Sweden and other European countries. In many natural reserves in Africa, free grazing and residence of the local population who own these lands are allowed, for example in Ambaseli (Kenya) and the famous Ngorongoro Crater (Tanzania). However, some restrictions make it possible to preserve the very rich fauna of large animals here. They are planning the creation of a huge Indian Ocean reserve for the protection of whales.

Territories with ecological and sanitary purposes are divided into objects and environmental protection territories. Of greatest interest are national parks, where picturesque and unique landscapes, little changed by human economic activity, are used for mass recreation and tourism.

Human influence on animal world Deserts are multifaceted and take different paths. One of these ways is an indirect impact through changes in the desert landscape and natural vegetation, including the reduction of trees and shrubs (saxaul and kandym) for fuel. Grazing by livestock leads to a change in vegetation cover in both sandy and clayey deserts as a result of grass consumption and livestock slaughter.

Along with the appearance of a large number of domestic animals and their influence on vegetation, the living conditions of many wild desert animals also change: the soil becomes compacted, the composition and reserves of food, initially of plant and then animal origin, change, since the change in vegetation immediately affects the composition of species and numbers insects Some desert species disappear, while at the same time new ones appear, characteristic of the cultural landscape, or from a few become widespread (for example, flies, blood-sucking dipterans, etc.).

Changes in vegetation and insect populations are reflected in the composition, abundance and distribution of birds. For example, in grazing areas, the numbers of crested larks, hoopoes, nightjars and sometimes desert owls increase.

At the same time, areas where vegetation has been knocked down by livestock become unsuitable for grazing wild ungulates, and thus the area of ​​natural pastures for goitered gazelles, saigas and kulans is reduced. Changes in vegetation and a reduction in the phytomass of food affect the composition of the rodent population, the distribution and number of granivorous birds.

Protected rare species desert animals. Interesting and valuable desert animals also include some rare mammals, for example: wild cats (cheetah, caracal, sand cat), sheep (arkala). Rare is a species that lives in small numbers over a large area.
The reptiles and birds of the desert are protected.



Here we have to talk about specially protected areas of three landscape zones at once. And not because they are so poorly represented in the republic (steppes and forest-steppes exist in both the European and Asian parts of the RSFSR), but because there are too few state reserves in them.

When the first version of the manuscript of this book was completed, in the mentioned landscape-geographical zones of Russia there was only one desert reserve - the well-known Astrakhan. But it can be classified as “desert” based on purely formal criteria, since it is located within a single section of the desert zone Russian Federation: in fact, the nature of the reserve has an intrazonal character.

Then the first semi-desert reserve appeared in the European part of the RSFSR - Dagestan, and a little later - the first steppe reserve in the Asian part - Daursky. This is a gratifying fact, but both of them were born in a stripped down, frankly speaking, mutilated (as opposed to what was intended) form.

The establishment of a semi-desert reserve “Black Lands” in Kalmykia is likely. Its design has been completed, the project is at the approval stage. The work done is both pleasing and saddening - the ecosystems of Kalmykia on the site of the future reserve have been very much destroyed by overgrazing.

Three or four reserves covering a vast territory of three landscape-geographical zones, the ecosystems of which are on the verge of destruction. A little…

Dagestan State Reserve- an example of extremely unsuccessful implementation of environmental projects. According to scientifically based assumptions of scientists and prospectors, it should have included five areas with a total area of ​​about 40 thousand hectares, including such unique ones as the Samur forest and the Guton steppes. Ultimately, the government of the autonomous republic agreed on the conservation of only two sites. In 1986, the reserve was organized on 19.1 thousand hectares, taking under protection the Kizlyar Bay and the Sarykum Dune - completely different landscape formations that do not fully reflect the specific nature of Dagestan.

On the Kizlyar site, out of 18,485 hectares under the waters of the bay of the same name, there are 9.3 thousand, the rest is Morskoy Biryuchen Island with floodplains (about 6.4 thousand hectares) and coastal ecosystems. The security zone adjacent to the site from the west is 21,065 hectares.

The flora and fauna of the Kizlyar site are typical for this landscape-geographical zone. In the plant world, all transitions are expressed - from coastal floodplains, meadow-swamp and meadow-salt marshes to semi-desert and desert formations.

The bird fauna is represented mainly by aquatic and semi-aquatic species. Most mass appearance- coot. In addition to Anseriformes, nesting sites include little white and gray herons, little egrets, spoonbills, great cormorants (these five species are in colonies), yellow, great and red herons, night herons, great bitterns, gull-billed terns and others. An important migration route passes through the bay; many thousands of mute swan, mallard, pintail, teal (gad and whistling), and various species of waders stop here to rest and feed. For open spaces Characteristic features include the hoopoe, roller, bee-eater, steppe and skylarks, black-headed and meadow mints, etc.

The most common types of mammals: jungle cat, raccoon dog, wolf, fox, corsac fox, steppe polecat, wild boar. Sometimes a saiga comes in.

The Sarykum Dune site lies about 30 kilometers from Makhachkala, in a well-developed and densely populated area. A daily stream of cars moves past it along the main highway that runs two or three kilometers to the east.

The area of ​​the site is 576 hectares, of which the dune itself accounts for 376 hectares. The height of Sarykum is 262 meters, it is considered the highest stationary dune in Eurasia and deserves protection primarily as a unique geomorphological formation. The flora and fauna have a certain value. Suffice it to mention that here, in the thickets of grasses and bushes at the foot of the dune, viper vipers are not at all uncommon. The flora of Sarykum includes 279 species.

In number rare plants, included in the Red Book of the USSR and protected in the Kizlyar area, include common sword grass, Hyrcanian water chestnut, common bladderwort, and floating salvinia. In the Sarykum area there is leafless juzgun, sharp-lobed iris; there are many relics of desert Central Asian flora.

Among the birds migrating through the Kizlyar Bay are such rare protected species as flamingos, Dalmatian and pink pelicans, Sultan's hen, red-breasted goose, golden eagle, peregrine falcon, white-tailed eagle, little bustard and bustard.

We should also not forget that the Kizlyar Bay is a spawning ground for some species of fish, and the fish resources of the Caspian Sea depend to a certain extent on the condition of these spawning grounds.

The conservation of two areas of natural landscapes in the Dagestan Autonomous Soviet Socialist Republic should be considered only the beginning of a large and complex work on organizing the reserve.

Astrakhan State Order of the Red Banner of Labor biosphere reserve named after V.I. Lenin was organized in 1919. It is located on the territory of the Astrakhan region, in the northern Caspian region. Area 63,400 hectares. During the summer low-water period, the water area occupies 57,570 hectares; during the water rises, it, of course, increases. The reserve has three sections belonging to the Volga delta - Damchinsky, Trekhizbinsky and Obzhorovsky.

The natural features of the Astrakhan Nature Reserve are determined by a very complex and dynamic mosaic of land and water areas, consisting of countless channels, large, small and dying, ilmens (overgrown lakes) inside the islands, vast shallow bays - kultuks and others. Associated with this mosaic is a variety of rich riparian and aquatic vegetation with high biological productivity. In the avandelta (“front delta”), underwater meadows of Vallisneria with inclusions of pierced pondweed and seaweed are well developed; the shallows are occupied by dense clumps of cattails. Floating plants are generously represented in the kultuks - chilim, nymphea, water lily, yellow egg capsule, salvinia, water buttercup, brilliant pondweed; in shallow waters - marsh chastuha and arrowhead. In the low-flowing peaks of the kultuks, along with watercolor, duckweed and hornwort, you can find massifs of the famous Caspian lotus. The banks of the channels are bordered by stripes of angustifolia cattail and reed; on land, reeds form huge dense fields, sometimes stretching for many kilometers. The riverbed banks of the channels and some oxbow lakes are covered with an almost continuous ribbon of white willow, forming the so-called “gallery forests”.

The flora of the reserve includes over 190 species, less than in other specially protected areas. However, the relative poverty of species is more than compensated by the abundance of plants, density of overgrowth, and high biomass.

Naturally, the conditions of the reserve are favorable for the life of organisms associated with aquatic habitats and hydrobionts. About 500 forms of freshwater invertebrates were found here: protozoa, rotifers, various crustaceans, larvae, etc. Insects are represented by 1250 species. IN summer time involuntarily attracts attention to an unimaginable number of blood-sucking insects - mosquitoes, horseflies, midges. They haunt neither people nor animals. Mayflies, dragonflies, orthoptera, bugs, clubbills and butterflies are abundant.

The Volga Delta has long been famous for its fish. Here it has excellent spawning grounds and extensive feeding grounds. The ichthyofauna of the reserve includes almost 50 species, including sturgeon, beluga, stellate sturgeon, roach, rudd, bream, silver bream, carp and many others.

One of the tasks that was set when organizing the Astrakhan Nature Reserve (in addition to preserving spawning grounds) was the protection of nesting sites, molting water birds and their stopping places during seasonal migrations. He coped with this role and does not give up his position these days. The Caspian Ornithological Station operates in the reserve, coordinating research on the biology, abundance and migrations of birds throughout the Caspian region. In the lower reaches of the Volga delta there are about 250 species of birds, of which over 100 breed their offspring here. The predominant species, of course, are waterbirds: mute swan, greylag goose, numerous species of ducks, coot, moorhen, grebes, great cormorant, several species of heron, night heron, spoonbill, ibis, terns and some others. There are colonies of pink and Dalmatian pelicans - rare and protected species. Predators nest - white-tailed eagle, osprey, black kite, marsh harrier, long-eared owl. “Other small things” are also abundant - thrush warbler, great tit, starling, tree sparrow, etc. In salt marsh meadows with sparse reed thickets you can find the North Caucasian pheasant.

The mammal fauna is relatively poor, represented by only 17 species. Various rodents live, including acclimatizers - muskrat and beaver; Among the predators are fox, badger, ermine, otter. Wolves often visit the protected delta. One of the most common species that has adapted to difficult environmental conditions is the wild boar. He has a lot of food here and excellent shelters. He finds himself in a difficult situation only when the water rises high and floods the delta.

The Astrakhan Nature Reserve has enormous environmental significance as a reserve of valuable commercial fish and wetlands game birds. It preserves typical highly productive delta complexes, which in other places are used thoughtlessly and are destroyed, and the gene pool of plants and animals, including relict and endemic ones, is preserved.

To the reserve’s previous troubles associated with the regulation of the Volga flow and the pollution of its waters, a new, very menacing one has been added: growing pollution atmospheric air Astrakhan gas condensate complex.

In the reserve, the ecosystems of the lower reaches of the Volga delta are studied in conditions of fluctuations in the level of the Caspian Sea, regulation and redistribution of the Volga flow.

Daursky State Reserve organized in 1987. Located in the Ononsky and Borzinsky districts of the Chita region. Area 44.8 thousand hectares. Initially, about 200 thousand hectares were requested for the reserve, but it was not possible to agree on this entire amount with land users. The protected zone covers 72 thousand hectares. Part of the territory planned for the reserve is given to the Tsasucheysko-Toreysky Republican Nature Reserve (57.9 thousand hectares), where the famous Tsasucheysky Forest is protected. It is advisable to consider the reserve, its protective zone and the reserve (174.7 thousand hectares in total) as a single environmental object with different regimes.

The reserve contains 32.3 thousand hectares of water land (Lake Barun-Torey), 7.8 thousand hectares of agricultural land (arable land, hayfields, pastures), 2675 hectares of swamps and bushes. The agricultural land was transferred to the reserve in not excellent condition. According to the designers, almost 30 percent of the pastures were in the last stage of failure; there were no areas of the steppe left that were not fundamentally changed by economic activity, which affected not only rare, but also widespread species of animals.

The Daursky Reserve consists of a main massif, including Lake Barun-Torey and part of its coastal areas, and four small isolated areas, three of which are located on the northern coast of the neighboring Lake Zun-Torey, one to the northwest of Lake Barun-Torey. The territory as a whole belongs to the Prionon-Torey dry steppe district, which is part of the Central Asian physical-geographical region. The Torey Basin is part of the Onon-Argun steppe.

In this basin there are about 100 plant species representing the Dauro-Mongolian, Siberian-Mongolian and Manchurian floras. Steppe vegetation consists mainly of forb-grass and tansy-grass formations and feather grass steppes, occupying intermountain depressions, coastal plains and islands. There are also chalk and fescue steppes. There are areas of meadow and meadow-swamp vegetation, and a few tree and shrub plant species. In the protected Tsasucheysky pine forest, the main forest-forming species is Krylov pine.

The mammal fauna includes 35 species. 15 species of rodents live here, including the Daurian pika, tolai hare, steppe polecat, badger, weasel, fox, and roe deer.

The avifauna of the Torey Basin includes 256 species, including 122 species of nesting birds. There are 14 species of predators, among them the Central Asian buzzard is the most common. On the islands of Lake Barun-Torey there are colonies of the great cormorant, dry-billed goose, blackheaded tern, gull-billed tern, shelduck, white-naped crane, and demoiselle. Waterbirds are highly dependent on the variable hydrological regime of local lakes.

The fauna of amphibians, reptiles and fish is poor. Typical Siberian frog, common muzzle, silverfish and minnow.

The organization of the Daursky Nature Reserve should serve to protect and restore many rare forms of living organisms. Of the animals, these are, first of all, listed in the Red Book of the RSFSR, the Daurian hedgehog (from being common for the region to very rare), the Pallas's cat (on the verge of extinction), the gazelle (in 1985, a herd of four individuals was noted that came from Mongolia), the swan-nose, Behr's pochard, steppe eagle, saker falcon, white-naped crane, black crane, demoiselle, stilt, avocet, Asian snipe, relict gull, bustard (60 individuals were counted in 1985), Mongolian ground sparrow, mandarin duck.

The conservation of a section of the Daurian landscape will contribute to the protection of some other species of animals that are rare in the region, as well as the preservation of the remnants of local steppe phytocenoses that have not been completely degraded under the influence of overgrazing.

Despite all the shortcomings caused by the difficulties in allocating the territory, the Daursky environmental complex has the opportunity to contribute huge contribution to achieve a noble goal - to preserve the nature of a unique region of our country.

Detailed solution to paragraph § 37 on geography for 8th grade students, authors V. P. Dronov, I. I. Barinova, V. Ya. Rom, A. A. Lobzhanidze 2014

questions and assignments

1. Name the main types of specially protected natural areas, indicate how they differ from each other.

Specially protected natural areas and water areas include: reserves, sanctuaries, national and natural parks, natural monuments, forest park protective zone, suburban green zone, etc. They differ from each other in the specific purpose of education, the degree of conservation and permissible economic activity. A reserve is a natural territory (or water area) completely excluded from economic use for the protection and study of the natural complex as a whole. National parks combine the tasks of nature conservation and strictly controlled recreational use, that is, they are open for educational tourism and short-term recreation for citizens.

2. When did the system of nature reserves begin to form in Russia?

The first nature reserves in Russia were formed at the beginning of the 20th century. The first official state reserve in Russia was the Barguzinsky Nature Reserve in northeastern Transbaikalia (1916). Before this, examples of unofficial reserves were known: Suputinsky in the Far East (1911), since 1913 - Ussuriysky, Sayansky (1916), Kedrovaya Pad (1916). The first Soviet nature reserve - Astrakhan - was established on April 11, 1919.

By the beginning of 1998, there were 97 nature reserves in Russia (total area - 30 million hectares).

3. Tell us about how nature reserves are distributed throughout the territory of our country, name and show the largest of them.

Nature reserves are distributed unevenly throughout the country. The largest number of reserves are in forest zone(24). A large number of nature reserves are located in the mountains of Southern Siberia (16) and the Far East (19).

Giant reserves (area > 1 million hectares): Bolshoi Arctic, Komandorsky, Putoransky, Ust-Lensky, Taimyrsky, Kronotsky.

4. Using materials from the textbook, write a description of one of the reserves in Russia.

Barguzinsky Reserve

Geographical position

Located in Buryatia, on the northeastern coast of Lake Baikal and the western slopes of the Barguzinsky ridge, at an altitude of up to 2840 m.

Date and purpose of foundation

This is one of the oldest nature reserves in Russia; it was founded in 1916 to protect and comprehensively study the nature of the western slope of the Barguzinsky ridge, as well as to preserve the valuable Barguzin sable.

The area of ​​the reserve is over 263 thousand hectares. The reserve is located on the picturesque slopes of the Barguzinsky ridge, descending to Lake Baikal. It includes a strip 45-80 km wide and about 100 km long, as well as a three-kilometer strip of the water area of ​​Lake Baikal.

Flora and fauna

Altitudinal zonation is clearly expressed on the territory of the reserve. Dark coniferous taiga predominates, consisting mainly of fir, cedar with an admixture of larch. The fauna is particularly rich: the Barguzin sable and the endemic Baikal seal, squirrel, brown bear, elk, and reindeer are numerous. There are otter, weasel, wolverine, and ermine; Birds include capercaillie, hazel grouse, white-tailed eagle, buzzard, osprey, etc. The nature of the reserve remains untouched. By the time of its organization, there were only 20-30 sables on the territory of the reserve (Barguzin sable is recognized as the best in the world). Now their number has increased sharply. Moreover, sable leaves the boundaries of the reserve and settles beyond its borders. Thus, the reserve enriches the hunting grounds of Buryatia.

FINAL ASSIGNMENTS ON THE TOPIC

1. Prove that a natural area is a natural complex.

A natural area is a large natural complex with a common temperature conditions and moisture, soils, vegetation and fauna. It is the commonality of natural components that makes a natural area a natural complex. All components natural area are interconnected. Changing one component changes all other components.

2. Which Russian scientist was the founder of the doctrine of natural zones?

The founder of the doctrine of natural zones was V.V. Dokuchaev.

3. Name all the natural zones of Russia. Prove that they are placed regularly.

On the territory of Russia there is a change from north to south of the following natural zones: arctic deserts, tundras, forest-tundras, taiga, mixed and deciduous forests, forest-steppes, steppes, semi-deserts.

4. Name the treeless zones of our country. Where are they located? What are their similarities and what are their differences?

The treeless zones of our country are arctic deserts, tundra and forest-tundra, steppes, semi-deserts and deserts. The Arctic desert zone is located on the islands of the Arctic Ocean and in the far north of the Taimyr Peninsula. The tundra zone is located on the coast of the Arctic Ocean from the western border of the country to the Bering Strait. The forest-tundra zone stretches in a narrow strip along the southern border of the tundra zone. The steppe zone occupies the south of the European part of the country and Western Siberia. Semi-deserts and deserts of Russia are located in the Caspian region and Eastern Ciscaucasia.

The similarity of these natural zones lies in the absence of forests. Herbaceous vegetation predominates here, and in northern regions– mosses and lichens. Natural areas are open spaces.

The difference between treeless zones is temperature conditions, moisture, soils, flora and fauna.

5. What natural zone of our country occupies largest territory? Find areas within its boundaries that have different natural conditions and think about what explains this.

The largest area in Russia is occupied by the natural taiga zone. In different areas of the vast taiga zone, many natural conditions are different - the general severity of the climate, the degree of moisture, mountainous or flat terrain, the number of sunny days, soil diversity. Therefore, the coniferous trees that form the taiga are also different, which, in turn, changes the appearance of the taiga in certain areas. Dark coniferous spruce-fir forests predominate in the European part of the zone and in Western Siberia, where they are joined by pine forests. Most of the Middle and Eastern Siberia covered larch forests. Pine forests grow everywhere on sandy and gravelly soils. The forests of the Far Eastern Primorye have a very special character, where on the Sikhote-Alin ridge the usual conifers - spruce and fir - are joined by such southern species as Amur velvet, cork oak, etc.

6. What natural areas are there in your republic (region, region)? Give an assessment of the agroclimatic resources of your republic (territory, region).

The Moscow region is located in a natural area mixed forests. The Moscow region is located in the central part of the Russian Plain. The relief of the region is heterogeneous. The river network of the region is quite dense. In the Moscow region, soddy-podzolic soils are most common; they occupy most of the territory. In river valleys the soils are alluvial. In the north-east of the region, in the areas of the Upper Volga and Meshcherskaya lowlands, the soils are almost entirely sandy and sandy loam swampy.

The climate of the Moscow region is characterized by warm summer, moderate cold winter with stable snow cover and well-defined transition seasons. The average monthly air temperature warm month- July varies across the territory from 17° in the northwest to 18.5° in the southeast. The air temperature of the coldest month, January, is -10° in the west of the region, and -11° in the east. Annual amplitude average monthly temperature 27 - 28.5°. The first half of winter is noticeably warmer than the second; the coldest time of the year is shifted to the second half of January and early February. The warm period, i.e. the period with a positive average daily temperature, lasts on average 206-216 days. The length of the day in summer is 15–17 hours.

The Moscow region belongs to a zone of sufficient moisture. The average annual precipitation is 550-650 mm, with fluctuations in some years from approximately 270 to 900 mm. Two thirds of the year's precipitation falls in the form of rain, one third in the form of snow. In the warm part of the year, rains of medium intensity predominate, well moistening the soil.

A stable snow cover usually forms at the end of November. The earliest and latest dates for the formation of stable snow cover were noted on October 23 and January 28, respectively. By the end of winter, the height of the snow cover reaches an average of 30-45 cm. The largest reserve of water in the snow is on average 80-105 mm.

In general, the agroclimatic resources of the region contribute to Agriculture.

7. Determine what natural zone we are talking about if the following grow in it: a) dwarf birch, dwarf cedar, moss; b) larch, cedar, birch, aspen, alder. Name the soils and typical animals characteristic of both zones.

a) natural tundra zone. The soils of the zone are thin, tundra-gley. They live in the tundra reindeer, arctic foxes, geese, geese.

b) natural zone of mixed forests. In its northern part, mixed coniferous-deciduous forests on soddy-podzolic soils are widespread. In the south there are multi-tiered broad-leaved forests on gray forest soils. The fauna is represented - brown bear, foxes, wolves, hares, black grouse, sables, moose.

8. Which natural zone of Russia has optimal natural conditions for successful farming?

Optimal natural conditions for farming exist in the natural steppe zone.

9. Make a description of any natural area according to plan. Use various sources of geographic information.

Geographical position;

occupies the south of the European part of the country and Western Siberia.

Climate: average temperatures in January and July, total radiation, duration of warm and cold periods, amount of precipitation and its distribution by season, humidification coefficient;

There is little precipitation here - from 300 to 450 mm, approximately the same as in the tundra zone. The humidification coefficient in the steppe zone varies from 0.6-0.8 at the northern border to 0.3 in the south. Summer temperatures in July are high (the average temperature in July is +21...+23°C). average temperature January in the west of the East European Plain -5°C, east of the Volga -15°C, near Krasnoyarsk about -20°C. The sum of active temperatures is 2200-3400°C.

The most typical steppe landscapes are either flat or plains dissected by a network of ravines and gullies.

Annual flow;

Surface runoff in the steppes is insignificant, since there is little precipitation and evaporation is very high, so small rivers steppe zones They have little water; in the second half of summer they become very shallow and sometimes dry out. Large rivers start far outside the zone.

Soils, their basic properties;

In the steppe, chernozems with a very dark color and a granular structure are common. The thickness of the humus horizon in them is 50-80 cm. In the Kuban River basin, this horizon reaches even 1.5 m. Chernozems are the most fertile soils in our country. Tempo-chestnut soils are common in the southern strip of steppes; they are less fertile and often saline.

Flora and fauna, their adaptability to given natural conditions;

Before the beginning of their intensive agricultural development, they were covered with grassy steppe vegetation with a predominance of feather grass. The predominance of herbaceous vegetation is associated with insufficient moisture for the formation of forests. Among the fauna, various small rodents predominate - gophers, marmots, jerboas, hamsters, voles. Small size is an adaptation for life among grasses. The predominance of rodents is explained by the large amount of food for them.

Agriculture;

The steppe is the main grain granary of the country, which is why it is almost completely plowed. Wheat, corn, sunflowers and other important crops are grown here. In the west of the zone, gardening and viticulture are developed.

Particularly protected components of nature.

Little changed natural complexes The forest-steppe and steppe zones are protected and studied in the nature reserves: Kursk, Voronezh, Galichya Gora, Khopersky, Zhigulevsky, Orenburg and Daursky. They all have forested areas and areas of steppes: forests grow in river valleys, ravines, ravines, and steppes are preserved on the slopes of erosional landforms. The largest and most diverse steppes are in the Orenburg Nature Reserve, created in 1989 on the preserved isolated areas of the steppes of the Trans-Volga region, Cis-Urals, Southern Urals and Trans-Urals. Many species of plants and animals of the steppes are included in the Red Books.

The title of this article sounds unusual. Should desert nature be protected? In newspapers and magazines, we are much more accustomed to seeing the titles “Man against the Desert,” “Attack on the Desert,” etc. Nevertheless, protecting the nature of deserts is now a necessary and important national economic task.

Inattention to the conservation of deserts is rooted in a fairly widespread, but erroneous view that deserts represent, as it were, a “mistake of nature” that man is called upon to correct. The natural conclusion from here is the opinion that the more sharply and deeply a person violates the nature of the desert, the sooner he will overcome the desert and force it to retreat. However, these simplified ideas about the relationship between man and the desert not only do not help man actively influence deserts, but also cause great harm to the rational development of deserts.

In order to put deserts at the service of man, one should clearly imagine that they form a vast natural zone, the existence of which is determined by a certain distribution of temperature and moisture on the globe. Therefore, the existence of deserts is as natural and natural a phenomenon as the existence of a tundra zone, a forest zone, etc. Human economic activity in all these zones has specific features; it must have certain characteristics even when developing in deserts. Therefore, we should not talk about the destruction of deserts as such, but about finding a whole set of reasonable measures by which deserts can be used for human needs. This complex will be the rational development of deserts. The forms of such development are very diverse.

Their diversity depends primarily on the significant differences in the deserts themselves. Scientists studying deserts currently count nine different types of deserts: 1 ) sandy, 2) pebble-sand, 3) gravelly, 4) rocky, 5) loamy, 6) loess, 7) clayey (takyr), 8) desert of dissected foothills (the so-called badland), 9) salt marsh.

The development of each of the above-described types of deserts follows its own paths. Some of the deserts may be irrigated to some extent. Others are suitable primarily only as pastures. The uniqueness of the development of each type of desert depends on the specificity of its nature. Each of the listed types of deserts is characterized by its own special, unique, inherent only to this type of connections between the various components of its nature, i.e. between soils, underlying rocks, groundwater, relief, vegetation, wildlife, and to a certain extent, human activity . These connections are so close and deep that by changing any one component of the desert landscape, we cause profound changes in all of it. natural conditions.

Let's illustrate this with an example. In sandy deserts, the entire development of the landscape greatly depends on the state and degree of fixation of the sand mass. If the sand is loose and not fixed, then both atmospheric precipitation that penetrates deep into it and moisture vapor in the air easily penetrate into it; this leads to the formation of peculiar underground lakes under sandy massifs, the so-called freshwater lenses groundwater. These lenses are usually located under depressions in the sand relief, lying at shallow depths. Due to the presence of fresh water close to the surface, lush moisture-loving vegetation develops in these depressions. Such massifs of scattered sand with thickets of moisture-loving plants (reeds, camel thorns, reeds, willows) in the basins have great importance for water supply sandy deserts. These are the best areas for constructing wells and obtaining shallow fresh water. But their grazing value is small, since cattle find almost no food on the devoid of vegetation, scattered sands, and the thickets of moisture-loving plants in the depressions, although dense, are small in area. Let us now imagine that, in an effort to improve the quality of pastures, we sow the sands with grasses. There will indeed be more feed for livestock here. But the grass will fix the sand, enrich it with organic matter, and worsen the conditions for the penetration of air and water vapor contained in it. Precipitation, which previously, falling * onto the open surface of the sand, were quickly absorbed into it, seeping into the depths, and replenishing the reserves of fresh water in the lens, will now be absorbed by the roots of plants and evaporate again into the atmosphere. The groundwater lens will not be replenished with moisture and will dry up. The wells will dry up. Thus, having created a good pasture, we can destroy the sources of its water supply. In order to prevent this from happening, you need to know well how much moisture enters the lens, how much plants evaporate, how the process of moisture seeping into the sand occurs, how much it will weaken due to the sand being fixed by plants - in a word, you need to know well all the connections between the sand, the covering its vegetation and the underlying waters. Then you can make the appropriate calculation and fix the sands so much that the lens does not dry out, and good pastures will lie around it.

Both in this case and in all others, human intervention in the life of the desert, even small changes in natural conditions, can lead to very far-reaching results. And if human actions are not based on a deep knowledge of the nature of deserts, then these results can be negative, even catastrophic. Instead of human development of deserts, even greater “desertification” and even greater impoverishment of the desert landscape may occur. To avoid this, work on the development of deserts should be carried out on a strictly scientific basis.

Before carrying out any event that reconstructs the desert world and disrupts the system of natural balances that have developed in it, it is necessary to carefully analyze everything possible consequences, using all the experience accumulated by desert science.

The Soviet Union has great achievements in the development of deserts. The main ones were carried out after October revolution, since the tsarist government did not pay serious attention to the development of deserts. Particularly great successes have been achieved in irrigating a number of desert lands. An example of this is primarily the Hungry Steppe in Uzbekistan. Here, on the site of dry plains covered with thickets of camel thorn, a new cotton-growing region with numerous state farms arose. An important stage in the development of desert reclamation was the construction of the Karakum Canal, which crossed a significant part of the southeastern Karakum and the foothill plain lying at the foot of the Kopet-Dag ridge. To ensure irrigation and regulation of rivers, several reservoirs were created - Tyuya-Buguz, Kuyu-Mazar, Chim-Kurgan. A huge Charvak reservoir is being built in the Tashkent region. Much work was carried out to consolidate the sands, especially on the outskirts of cultivated lands, where the sands advanced onto crops and filled up canals. A number of examples of successful desert development can be found abroad.

However, along with the successful and reasonable development of deserts, one can also note cases of ill-conceived human intervention in the life of the desert. Therefore, we will focus on considering some of the most common forms negative impact man into the desert.

Excessive grazing (overgrazing). Deserts have long served as grazing lands for many types of livestock (sheep, camels, and partly horses). In most deserts, livestock graze all year round. Depending on the nature of the vegetation covering the desert pasture, livestock may find greatest number feed in different seasons of the year: on some pastures - in spring, on others - in winter, etc. Therefore, according to the season of use, pastures are usually divided into spring, summer, autumn, winter. If all pasture areas are taken into account, feed reserves for them are calculated and correct pasture rotation is observed (i.e., the sequence of transition of herds from one type of pasture to another), then grazing not only does not lead to damage to pastures, but also improves them. But if pasture rotation is disrupted and some parts of the pastures are overcrowded with a mass of livestock, while others are hardly used, the pastures begin to deteriorate. This is especially noticeable in sandy desert. If the network of wells here is rare and big number The herd must approach the same wells for watering, then the animals quickly destroy everything they can eat, and the vegetation cover around the well almost completely disappears. The sands, previously fixed by vegetation, now become open and defenseless from the action of the wind. The movement of the herds, breaking up the already bare surface of the sand, further helps to disperse it. The sands begin to move, and massifs of dunes form around the wells.

However, excessive grazing is harmful not only for sandy deserts, but also leads to the deterioration of pastures in other types of deserts. In areas overgrown by excessive grazing, a low-growing semi-shrub, known among the Kazakhs as it-tsegek (Anabasis aphylla). It occupies many square kilometers of area around the well. Such areas turn into inconvenience and are unsuitable for pasture.

In foreign deserts, excessive grazing is observed much more often than in the USSR, since in most cases no one tries to establish the correct grazing rotation. Most of The oases of the Sahara, the Libyan Desert, and the deserts of the Arabian Peninsula are surrounded by massifs of shifting sands. Researchers usually explain their occurrence by the accumulation of herds near oases. Afraid to go far from the oasis watering holes (and previously afraid of being raided by neighboring tribes far from their native oasis), the nomads grazed cattle near the border of their tribe’s lands, and the oasis sands were overgrazed.

The best way to combat excessive grazing is strict adherence to the developed pasture rotation. But on the way to its creation there are some difficulties inherent in the natural conditions of the desert. The main one is the sparseness of the well network. When there are few wells, shepherds are forced to drive a large number of herds to the same watering holes. Therefore, the creation of each new well is of great importance for the conservation of desert nature. Particularly great prospects for expanding the well network open up in connection with the use of the previously mentioned fresh water lenses - underground lakes of the desert. Until recently, their existence was almost unknown. Currently, the work of Soviet scientists has explained the mechanism of their occurrence and developed the landscape features by which these lenses can be found. Next in line is the task of plotting all fresh water lenses on a map, determining the water reserves in them and their practical use. This will allow for uniform grazing and protect pastures from degradation.

Unregulated watering and ill-conceived irrigation of deserts. Water in the desert is the greatest treasure. Where there is water, there is life. Since ancient times, water sources in the desert have been the object of rivalry among various tribes; Because of them, armed conflicts, even wars, arose. “The battle for water, for the possession of a well in the desert is the most terrible battle,” writes E. A. Murzaev, a researcher of the deserts of Central Asia. The construction of every well in the desert is a small but significant step in its development. Irrigation of deserts is a great victory of human intelligence and perseverance.

However, not every introduction of masses of water into a desert landscape leads to its improvement. In order for water to be useful in the desert, it must be introduced in forms in which its access could be constantly controlled by man. A person must manage water in the desert, otherwise, instead of benefit, it can cause great harm.

The famous Sahara explorer Capo Rey, in his work on the nature and economy of this desert, expressively describes how uncontrolled watering artesian wells turned one of the most important areas of date palm culture (Oued Rir region) into massifs of wet salt marshes. The strongest growth of salt marshes as a result of spills from gushing wells was observed in various parts of the Somali Desert.

Destruction of forest and shrub vegetation. The vegetation cover of deserts was previously much richer in shrubs and even real forests, although peculiar in appearance, than at present. Perhaps no other element of the desert landscape has been so affected by destructive human activity.

both on tree and shrub vegetation. One of the clearest examples of this is the Sahara. In its south and in the adjacent savannas, a monstrous destruction of trees and shrubs is taking place. Researchers have identified the following main reasons for this process: 1) burning of vegetation in order to obtain high yields in the first years after the fire; 2) excessive grazing of livestock: 3) cutting down of bushes by shepherds for the construction of “dzerib”, i.e., pens in which livestock are kept; 4) procuring fuel for domestic needs and for evaporating salt extracts (in the south of the Sahara, a widespread method of extracting salt is based on washing salt-bearing rock with water and evaporating the settled brine in furnaces); 5) destruction tree species With valuable wood for export. The reduction of forested areas opens the way for sand movement. The latter are spreading at an alarming rate. The leader of the international expedition that studied the processes of sand advance in the south of the Sahara, F. Kollmansperger in his book “Drohen– deWΰ ste"(The Threatening Desert) reports that the desert area is growing rapidly. Sands penetrate into the foothills of the Air hill, where they were not previously present. A significant section of the Niger River passes through sands that have moved onto its banks, and every year it is necessary to carry out extensive work to clear the riverbed of sand deposits. Therefore, many researchers of African deserts write about the “advancing Sahara”, about “man-made deserts”, and, unfortunately, we have to admit that these concepts are not without foundation.

The destruction of trees and shrubs is also observed in some parts of the deserts of the USSR. The situation with saxaul is especially alarming.

There are now very few saxaul growers in the northern Aral Sea region. Small massifs have been preserved near the sands of Malye and Bolshie Barsuki. The wider distribution of saxaul in the past can be judged by its individual small groves, preserved in separate small areas inaccessible to humans, mainly on the cliffs of various remnant hills. A lot of saxaul was spent in the past on cattle pens. In the sands there are old sites where the fences are entirely made of it (Fig. 2).

Mechanicaldestruction of desert soils. The various works now being carried out by people in the desert - searching for minerals, building roads, oil pipelines, gas pipelines, various types of engineering and geological surveys - are carried out using new powerful equipment. Heavy trucks, powerful all-terrain vehicles, tractors, and tractors have replaced lines of camels, long chains of donkeys and groups of horsemen forming caravans that were typical of the desert landscape in the old days. The use of new types of transport gives people great benefits and convenience when

his activities in the desert. But all these means have a detrimental effect on thin desert soils. If we are talking about a sandy desert, then machines in it uproot the plants that hold the sand together, break the surface of the sand and easily turn it into a loose mass freely transported by the wind. In a gypsum-rocky desert, soil destroyed by traffic becomes gypsum-bearing powder. Clouds of gypsum dust rise into the air and are carried by its currents, settling in the surrounding areas and increasing their gypsum formation.

Protecting the nature of deserts requires a deep, comprehensive, integrated study of all natural relationships that exist in desert landscapes. We still know little about many of these connections and often do not know how to protect them from destruction and use them for purposes National economy. Relatively recently, the Institute of Deserts was organized in the Turkmen SSR. His employees have accomplished a lot important works. Thus, they developed a method for creating artificial winter pastures in the foothill deserts of Central Asia, and researchers

from the Institute of Botany of the Academy of Sciences of the Uzbek SSR developed methods for improving the etched gypsum-stony desert in the south of Kyzylkum by sowing valuable forage plants, especially ephemerals.

Another important activity in desert conservation is a thorough study of the development of deserts by people in the past. Humanity has accumulated vast experience in “desert farming,” that is, living and working in the desert. We know little about what signs guided craftsmen in the old days when choosing a place to build a well; and at the same time, everyone is involuntarily amazed by the successful placement of wells dug several hundred years ago. After all, the builders of these wells had neither geophysical instruments nor drilling rigs, but how accurately they determined the location of fresh water!

There is experience in modern research to discover reclaimed lands and use the data obtained to determine ways for the development of agriculture in the desert. Aerial photography of deserts can play a major role in this, clearly revealing traces of old settlements, canals, and sites. To successfully resolve these issues, it is necessary to more widely develop cooperation between geographers and archaeologists in the study of deserts. Obviously, it is necessary to take into account, map and study the entire network of abandoned settlements scattered across the deserts. The silent ruins of wintering quarters (Fig. 4), caravanserais, ancient cemeteries (Fig. 5), traces of water-lifting structures, canals, reservoirs should be carefully mapped, compared with the surrounding landscapes, and in this way an answer to the question should be obtained - why people lived here, what they lived with, where they got their water and food from. Ancient caravan routes and historical cattle drive routes must be carefully studied, on which wells that are not marked on any map are still being discovered. Without such comprehensive geographic and historical analysis of desert landscapes, we will continually find ourselves struggling with problems that desert dwellers have already solved in the past.

Finally, it is necessary to provide for restrictive measures that prohibit the destruction of trees and shrubs, unplanned grazing, uncontrolled consumption of groundwater, and the movement of vehicles through desert pastures off roads.

Promoting the ideas of nature conservation, especially among young people, plays a major role in the wise use of desert nature. By instilling in schoolchildren, who tomorrow will become students, and then workers in the national economy and science, ideas about the need to protect nature, including the nature of deserts, a lot can be changed in practice modern activities man in the desert. Paying tribute to man's struggle to improve and enrich desert landscapes, it is necessary to instill in young people the correct view of deserts as complex a natural phenomenon, which cannot simply be destroyed or “cancelled”, but can be mastered on the basis of a deep knowledge of the laws of its development.

- Source-

Pelevin, V.I. Nature conservation / V.I. Pelevin. – M.: Education, 1971.- 120 p.

Post Views: 1,830

Particularly protected components of the tundra nature. Plants and animals of the tundra

The tundra is a unique natural territory, comfortably located north of the taiga zone and south of the Arctic desert. It is a huge area with endless open spaces. permafrost, due to which snow-covered soil rarely thaws completely. As a result, all inhabitants of this zone, including plants, are forced to survive in difficult conditions. climatic conditions. For the same reason, many of them are included in specially protected components of the tundra nature. Let us tell you in more detail what these objects are.

Climate and weather conditions in the tundra: winter

Since we mentioned that the tundra is characterized by a very harsh climate, we will talk about it in a nutshell. So, the winter period on this cold and treeless plain is protracted. Winter lasts approximately 6-8, or even 9 months. Moreover, throughout this entire time, the tundra dwellings will experience frosts, cold winds and even snow storms.

As in any polar zone, there are polar nights in the tundra, which regularly occur in the middle or end of January and last 1-2 months. When the long-awaited polar day arrives, the inhabitants of this area, which are part of the specially protected components of the tundra nature, are hit by streams of strong northern wind and snowstorm. Average air temperature in winter time reaches –30 degrees Celsius.

Autumn, spring and summer

Autumn in the tundra begins in September, spring in May, and summer in July. The shortest time of year in this subarctic climatic zone Summer is considered. Here it flies by quickly and almost unnoticed. The average temperature of July, one of the hottest months by tundra standards (rarely August), is 5-10 degrees Celsius.

During the short term summer period the ground in this permafrost zone does not have time to warm up completely. Thus, during the period when the sun emits heat relatively strongly, the earth manages to warm up only 50 cm deep. Everything that remains below this layer, as practice shows, lies under a layer of dense and frozen soil. For the same reason, water that falls on the ground with precipitation cannot penetrate to a depth of more than half a meter. As a result, numerous lakes and swamps arise in this harsh climatic zone. What are the features of the nature of the tundra, we will tell further.

Flora in the permafrost zone

As you understand, it is very difficult for representatives of the flora to survive in frozen soil. But despite this, in the tundra you can find amazing plants and shrubs. For example, reindeer moss or reindeer lichen looks interesting. Tasty berries such as blueberries, cloudberries and lingonberries also grow here. The tundra is also characterized by a large number of mosses and lichens, which are the favorite food of deer.

The trees of the tundra also deserve special attention, among which there are such opportunistic martyrs as willow and birch. Moreover, both types of trees have small sizes and relate to dwarf species. For the most part, plants in the zone of fleeting summer have low growth and a crown that creeps along the ground, which allows them to endure winter painlessly and enjoy gusts of cool wind in spring and summer.

The world around us: the tundra and its feathered inhabitants

In the tundra you can find a white partridge, which in the summer puts on a brown and motley outfit, and by winter it dresses up in a warm white “fur coat and boots” (this is what the plumage and vegetation completely covering the bird’s legs look like). The white owl does not change its snow-white plumage for a whole year. Thanks to a large number feathers on the body and limbs, this bird can sit in one place for a long time, even in severe frost and strong winds.

Animals living in the tundra

Among the animals of the tundra there are furry lemmings with short legs, a tail and small ears. It is noteworthy that these animals do not fall into hibernation and feel great on and under the snow. Here you can also see beautiful and fast arctic foxes, deer with large and heavy antlers, foxes, wolves, white hares, rodents, bighorn sheep and others. Many of these inhabitants are in danger of extinction and are therefore placed in tundra reserves.

Other inhabitants of the tundra

Due to the large number of swamps and lakes, as well as excessive precipitation (up to 200-300 mm falls here throughout the year), blood-sucking winged insects actively develop in the tundra. In the reservoirs themselves, large fish such as omul, nelma, vendace and broad white swim.

Environmental problems of the tundra

Protecting the nature of the tundra is an important task for ecologists around the world. This conclusion can be made by analyzing information about the construction and other facilities located in this harsh territory that transport and produce oil.

Due to negligence at work and non-compliance with safety regulations, frequent fuel leaks occur. As a result, pollution occurs environment, death of plants and animals.

In addition, industrial road trains move across the tundra, leaving behind garbage that ultimately destroys the vegetation of the soil. Due to the destroyed vegetation, deer and other animals and birds die.

What nature reserves are there in the tundra?

Thanks to the coordinated work of ecologists and other specialists, numerous tundra reserves have been created and are being created. Thus, in this permafrost zone there are several large nature reserves that make it possible to restore the natural balance of the territory and preserve endangered species of tundra inhabitants.

For example, there are the following environmental objects:

• Lapland State Nature Reserve.
• Taimyr Nature Reserve.
• State Nature Reserve "Wrangel Island".
• Altai Nature Reserve.

We will describe below what these specially protected components of tundra nature are.

General information about the Lapland State Nature Reserve

Lapland State Nature Reserve is one of the largest natural objects in Europe. It has huge areas of virgin nature where animals and birds move freely. It is located in a small village Murmansk region and has a total area of ​​278,435 hectares of land. It is home to more than 198 species of birds, about 31 species of animals and 370 varieties of plants.

General information about the Taimyr Nature Reserve

The Taimyr Nature Reserve, created in February 1979, is also included in the specially protected components of the tundra nature. It is located in the Krasnoyarsk Territory near the Taimyr Peninsula. Up to 222 species of mosses and about 265 lichen plants, 116 species of birds, 15 species of fish and approximately 21 species of animals are found here.

General information about the State Reserve "Wrangel Island"

“Wrangel Island” is a large and beautiful reserve with a total area of ​​2,225,650 hectares, including the water area and the security zone. There are many mountains and hills, occupying approximately 2/3 of the entire territory. The reserve protects about 641 species of plants, 169 species of birds and some species of animals. So, arctic foxes and wolverines, bears, stoats, wolves, reindeer and musk oxen feel great here.

General information about the Altai Nature Reserve

Another environmental site is the Altai Nature Reserve, located in the mountains of Southern Siberia. It stretches over 2,000,000 hectares, where all 1,500 plant species grow beautifully, many of which are listed in the Red Book. Approximately 70 species of animals live here, among which 29 are endangered species.