Transformation of the composition and horizontal structure of steppe communities in East Mongolia under anthropogenic influence and its reflection on large-scale maps

1995 ◽  
pp. 22-41
Author(s):  
V. N. Khramtsov ◽  
P. P. Dmitriev

In 1989–1990 participants of the joint Soviet-Mongolian Complex Biological Expedition conducted the works on the estimation of the present-day state of nature ecosystems in Mongolia. The anthropogenic dynamics (transformation) of steppe ecosystems was studied in the East Steppe Stationary in the territory of state-farm Tumen-Tsogt in the Sukhebator District. During these works the series of maps was compiled for the territory of state-farm and for separate key plots (S. 1 : 1 000 000; 1 : 200 000; 1 : 100 000) showing the anthropogenic change of vegetation of animal populations, of soils and of ecosystems as a whole. The article represents some results of the investigations on transformation of vegetation cover under grazing the leading anthropogenic factor in Mongolia. The basic map is the vegetation map in scale of 1 : 100 000 (fig. 1, fragment). The legend of this map reflects the relations between vegetation and relief and soils. The highest divisions of the legend represent the vegetation of major forms of relief: «Vegetation of low mountains», «Vegetation of flat alluvial-deluvial plains», etc. These divisions subordinate the subzonal and altitudinal-subbelt types: «Rich in forbs grass meadow steppes on the mountain chernoziom soils», «Forb and forb-bunch grass steppes on the dark-chestnut soils», etc. The communities and their combinations, belonging to the definite edaphic variants of zonal vegetation, are taken as mapping units. 7 edaphic variants are distinguished in the whole. In the legend the concrete series of transformation of vegetation cover are given. Numbers 1–17 represent the undisturbed communities. The figure indices at the numbers (for instance: 10'–104) differentiate communities of the same digression serie - fr om less to most degradated ones. In the case of fallow lands such indices indicate the stage of reconstruction – from less to the most reconstructed vegetation (18–185). It has been paid attention to the heterogeneity of vegetation that is reflected in the map legend in characterizing the map divisions. The attention has been attracted also to the pattern of the horizontal structure of these complexes. The classic complexes of plant communities are not characteristic of the steppe zone of Mongolia, especially of its central and eastern regions as they are characteristic, for instance of the Kazakhstan steppes wh ere their distribution and development are caused by the processes of salt accumulation and salt removing from soils. In Mongolia the heterogeneity of vegetation and soil cover is conditioned by the burrow activity of rodents. The patterns of horizontal structure of phytocoenotic complexes appeared to be diverse and peculiar of definite landscapes depending on animal population and environmental conditions. It was ascertained that at grazing not only the phytocoenotic parameters (species composition, coverage, abundance, etc.) are transformed but also community dimensions, their proportion in complexes and the pattern itself of these complexes. It was interesting to reveal the transformation series of these patterns in complex biogeocoenoses. Fig. 2 shows the fragment of map representing the horizontal structure of biogeocoenoses, s. 1 : 1 000 000. The legend of the map is given in the table form (see table). The map shows both the reconstructed and the actual structure of vegetation cover. The undisturbed and slightly disturbed structural types are given by the main numbers (1–12) with figure index 1 (V–12'). The structures disturbed in various extents are shown by figure indices at the main number (for instance, 22–24). The indices correspond the degree of disturbance: 2 – middle disturbed, 3 – strongly disturbed, 4 – the most disturbed. The schematic drawings of horizontal structure of the natural and transformed complexes of plant communities are given in figure 3. Figure 4 proposes the fragment of analytic map of horizontal structure of biogeocoenoses. This map shows the actual pattern of plant community complexes. The last map (fig. 5) represents the percentage contribution of zoophytochoras in background undisturbed vegetation in various landscape elements.

2002 ◽  
pp. 44-65 ◽  
Author(s):  
I. N. Safronova

We have performed the phytoecological mapping of the Northern Caspian Region in scale 1 : 2 500 000. The territory includes the Caspian Lowland and the Mangyshlak Peninsula between 45°-53°30 E and 49°-42° N. The earlier published maps of the same scale showed either vegetation of the Caspian Lowland or that of the Mangyshlak Peninsula. We have shown both territories on one map, which has permitted to reflect the peculiar features of the Northern Caspian Region: extensive distribution of the dwarf-semishrub communities not only in desert but also in the steppe zone; differences of desert vegetation cover between areas west and east of the Ural River; the running of zonal steppe/desert boundary along 44° N on the west coast of Caspian Sea whereas on the east coast the middle deserts occur at the same latitude: etc. Our studies were based upon a broad understanding of the desert and steppe types of vegetation. To the desert type of vegetation on the plains of Caspian Region and Turan belong the communities of xerophilous and hyperxerophilous micro- and mesothermic plants of various growth forms, mostly dwarf-semishrubs, semishrubs and shrubs, to the steppe type - plant communities consisting mostly of perennial more or less microthermic xerophilous herbaceous plants, predominantly of bunchgrasses, locally tufted sedges and perennial herbs. One should add that stony-rubble and salted substrates in steppe zone are characterized by distribution of dwarf-semishrub communities. Some researchers, apart from steppe and desert zones distinguish semidesert one in the Caspian Lowland, however it is accepted that there is no semidesert type of vegetation. Therefore it is difficult to agree with the recognition of the semidesert zone. The drawing of zonal boundary between steppe and desert in the Northern Caspian Region involves definite difficulties depending on environmental features of the region and strong anthropogenic press. So, on sand massifs and saline soils vegetation is the same both in desert and steppe zones. Vegetation cover of the Western Caspian Region is transformed considerably under anthropogenic influence. It is known that in steppe region at ploughing up of the worm- wood-bunchgrass steppes one of the stages of restoration of fallow lands is the wormwood one, physiognomically similar to desert. The same appearance is assumed by steppe at the strong grazing when grasses are destroyed and wormwoods is growing up. Such anthropogenic wormwood communities are widely spread at the boundary between zones. This resulted in that on earlier published vegetation maps the desert zone in the interfluve of Volga-Ural was shifted fairly far to the North up to 49°N. At present we believe that it is possible to assign the northern part of Ryn-Sands to steppe zone and to draw the zonal boundary along the latitude of 48°30 N. The boundary is determined by climate, geological history, hydrology, edaphic conditions and. vegetation. Somewhat differently than earlier we draw the zonal boundary in the Caspian Lowland between the Volga River and the Ergeni Height. It goes from Prishib's settlement to south-west to Yashkul's settlement (45°30 E) and further westward of Achinery's settlement to south-east up to the Kuma River. We could specify its position since during the last years the part of fallow lands, occupying large areas to the west and north of this line, restored up to steppes of Stipa sareptana-Artemisia lerchiana and those of Agropyron desertorum-Artemisia lerchiana. In the course of cartographic works we compiled the vegetation map of the Northern Caspian Region. This map became the base for series of maps: phytoecological one. the map of dominating plant formations, the map of edaphic variants of plant communities, the map of transformation of ecosystems of the Lower Volga Region. Phytoecological map (Fig. 1) gives an idea of latitudinal differentiation of vegetation in the Northern Caspian Region which depends on climate, and reflects its interrelation with soil conditions on plains and with lithological composition in low mountains. The map of edaphic variants of plant communities (Fig. 2) well reflects the peculiar features of various parts of the Northern Caspian Region: between the Terek River and the Ural River psammophyte and hemipsammophyte variants there predominate; east of the Ural River halophyte ones prevail: on the Mangyshlak Peninsula all variants are represented. Pelitophyte variants predominate in the west of the Region and along its northern margin within the limits of steppe zone. On the map of dominating formations (Fig. 3) we could show the distribution of 17 formations and 1 group of formations. A part of formations is restricted exclusively to steppe zone or desert zone, another part is spread throughout the both. This map helps to understand such peculiar feature of the region as wide distribution of dwarf-semishrub communities not only in deserts but also in steppes, which is due to presence of large areas of sands and saline soils in region. The Caspian Region was intensively used by man for a long time. By present time vegetation cover is noticeable transformed. We tried to show cartographically the degree of this transformation and differences in economical utilization of the Lower Volga area (Fig. 4). 4 degrees of transformation are distinguished: Tl-weak, T2-moderate, T3-strong, T4-very strong. Each polygon is considered from standpoint of type of anthropogenic influence: such as pastures (index «a»), fallow lands (index «b»). For pastures degree of grazing is recorded - from weak grazing to overgrazing. For fallow lands the stage of restoration is detected: from the tall weed one up to the perennial herb one conventionally restored.


This article is devoted to study the characteristics of ecological-cenotic structure and directions of vegetation cover transformations in riparian and coastal zones of forest swamps within the forest-steppe zone (north-western part of Kharkiv Oblast, Ukraine). The survey has been conducted in 2013–2018 in the territory of the Slobozhansky National Natural Park. Plant communities were surveyed both in phanerophyte and grass biotopes types, having different genesis and degree of disturbance (from terrestrial to aquatic, from native to artificially created forest plantations). A number of regionally rare plant species were identified in their composition (Dryopteris carthusiana (Vill.) H.P.Fuchs, Majanthemum bifolium (L.) F.W.Schmidt, Calluna vulgaris (L.) Hull, Equisetum sylvaticum L., Potentilla erecta (L.) Raeusch., Rubus saxatilis L., Eriophorum angustifolium Honck., E. vaginatum L., Drosera rotundifolia L., Nymphaea candida C.Presl, Utricularia vulgaris L.) and U. minor L. – a species listed in the Red Book of Ukraine. Route and stationary techniques of field surveys were used for clarification the general features of horizontal vegetation structural organization, as well as for studying the effect of environmental factors on state and stability of plant communities. Usage of mobile GIS applications in geodata collection and their further processing in ArcMap project allowed us to develop a large-scale geobotanical map (1:1500) as an area of permanent botanical survey (1.9 ha). According to the results of phytoindication, indicators of 7 environmental edaphotop regimes in 25 plant communities studied (objects of mapping and further monitoring) have been identified. Based on the geobotanical map, integration of data on the intensity of vegetation transformation have been conducted. It was found that plant communities ІV (the highest) and III degrees of transformation cover an area more than 0.6 hectares (one third of the total plot area). These communities were occurred mainly in phanerophyte-type biotopes (aspen, willow, birch, and, partly, pine), which have been affected by pyrogenic and biogenic factors. The GIS-project created as a result of the study serves as a geo-information base that can be further improved and used to solve other applied problems.


Author(s):  
Andrey Belov ◽  
Andrey Rybin

Based on the records of management documentation, periodicals, memoirs of contemporaries, the article presents an overall picture of the daily life of virgin lands (tselina). The study showed that upon arrival to the new land volunteers were often forced to live in the severe conditions of lack of infrastructure. They had to live in tents or field trailers. At the same time, settlers themselves could improve their living conditions by building state-farm (sovkhoz) settlements. Such work required a lot of effort. The average working time was 12–14 hours a day, regardless of the age, length of service and experience of a volunteer who arrived to the virgin lands. Earnings ranged between 500–1400 rubles per month in average. Food supply system in the new land development areas was essential to support the physical strength of the volunteers. However, as contemporaries remember, the food was unsatisfactory. The diet, as a rule, was monotonous, in view of which workers often staged strikes. In the end, gradually the infrastructure in the virgin lands acquired the level usual for the Central Russia. In particular, leisure time outside the virgin lands was spent in cinemas, clubs, libraries, amateur circles, holding sports competitions. However, social security was in poor condition as well as medical care. Not all medical centers worked; there was a constant lack of doctors, which led to increased injuries. Many volunteers who came to the new lands had no experience in agriculture – in this regard, medicine played an important role in the daily life of virgin lands. New settlers also faced a number of problems, which led to disruption of the usual daily life. In particular, cases of hooliganism caused by alcoholism, fights with lethal outcomes were frequent in the new lands. The indigenous population was often hostile to visitors. In addition, the residents of virgin lands were harmed by the military, who conducted nuclear weapons tests in the vicinity of new farms. In the end, the new settlers were able to cope with the difficulties they were facing and in a short time established a large-scale production of grain crops. Due to this, the country was able to temporarily overcome the food issue that had become urgent in the post-war period. Key words: living conditions, working process, wages, leisure, daily life, virgin and fallow lands.


2019 ◽  
Vol 16 ◽  
pp. 00047
Author(s):  
Irina Safronova ◽  
Tatiana Yurkovsksya

The latitudinal changes of vegetation cover on the plains of Siberia are observed. In Western Siberia there are 4 zones (tundra and taiga, and forest-steppe and steppe only here), in Central and North-Eastern Siberia − only 2 zones (tundra and taiga).Tundra zone is represented by 4 subzones in Central Siberia; in Western and North-Eastern Siberia − by 3 subzones (there are no polar subzone). All 5 subzones of the taiga zone are distinguished both in Western Siberia and in the Central Siberia, but in the Central Siberia, forests are found in very high latitudes. The feature of the taiga zone of Western Siberia is high paludification. As a result, the vegetation of mires dominates over the zonal vegetation. Zonal West Siberian types are dark coniferous forests. Light coniferous forests predominate in the taiga zone of Central and North-Eastern Siberia. In the forest-steppe zone in Western Siberia forests are small-leaved − birch, aspen-birch (Betula pendula, Populus tremula). The abundance of mires is the feature of this zone, as well as in the taiga.


2019 ◽  
pp. 39-56 ◽  
Author(s):  
E. A. Volkova ◽  
V. N. Khramtsov

The article is devoted to the vegetation mapping of the “Levashovskiy les”— a large forest-mire massif located in the northern part of St. Petersburg (Fig. 1). It continues a series of articles on the vegetation of existing and proposed specially protected natural areas of St. Petersburg (Volkova, Khramtsov, 2018). Large-scale map of modern vegetation (Fig. 2) is presented; the map legend includes 67 main numbers, the signs and numeric indexes at the numbers made it possible to show 93 mapping units (associations and their variants). Brief description of the main types of plant communities (spruce, pine, birch, aspen, gray alder and black alder forests; raised bogs, transitional mires and fens, floodplain and upland meadows) reveals the content of the legend. Vegetation cover is characterized by the dominance of secondary communities. The main anthropogenic impacts on modern vegetation are following: drainage reclamation, deforestation and former agricultural use, forest fires, gas pipelines, highways. Most of the forest communities are secondary ones; they have grown under the pressure of various anthropogenic factors and at different time. Nowadays an active process of natural regeneration of conife­rous (mainly spruce) trees goes in the forests. Plant community structure and species composition were taken into account as well as their dynamic state. To assess the degree of disturbance of plant communities and the potential for their restoration, the analysis of all mapped vegetation categories with respect to their position in the ranks of restorative successions was made. Then an assessment map “Dynamic state of plant communities” (Fig. 3) was compiled. The map shows following categories of dynamic types of communities: conventionally primary; relatively long-term secondary and stable long-term secondary (Sukachev, 1938; Isachenko, 1964; Karpenko, 1965; Gribova, Isachenko, 1972); short-term secondary that were divided into 3 categories representing different stages of restorative series. Present state of the vegetation cover of the “Levashovskiy les” can be determined by the ratio of the areas of conventionally primary and secondary communities. Areal analysis of dynamic categories of plant communities showed that only a bit more than 20 % of the territory is occupied by conventionally primary communities and about 60 % – by short-term secondary ones with good restorative potential. Without strong anthropogenic and natural disturbances, a significant part of the disturbed plant communities will be able to self-restore to their natural state. The establishment of a specially protected natural area as well as the regulation of conservation regime will support restoration process of nature ecosystems.


2015 ◽  
pp. 94-119 ◽  
Author(s):  
I. A. Lavrinenko

A typological scheme of territorial units of vegetation (TUV) developed on the basis of the large-scale map of theKolguev Island is presented. Four basic rank typological units (division, class, group and type) define TUV positions in the hierarchical system of vegetation cover. The concepts of diagnostic syntaxon and combination of diagnostic syntaxa that occur exclusively or primarily within these typological units are introduced. Prodromus of the Kolguev Island vegetation consists of 42 syntaxa (association / subassociation / type of community). 38 types of TUV from 22 groups (8 homogeneous and 14 heterogeneous – serial and ecological ranks, complexes and combinations), assigned to 15 classes and 3 divisions are allocated on the vegetation map in 1 : 50 000 scale. The categories of different rank can be used as dynamic elements of the map legend. This approach gives us a possibility to combine the syntaxonomic diversity of plant communities and typology of TUV.


2015 ◽  
pp. 129-147
Author(s):  
M. P. Tishchenko ◽  
A. Yu. Korolyuk ◽  
N. I. Makunina

The Tobol and the Irtysh watershed occupy the western part of West-Siberian plain. Area studied covers latitudinal band between 55° and 57° n. l. It includes the southern part of subtaiga subzone and northern part of forest-steppe zone. This territory has been used for agriculture since XVIIth century. In the middle of XXth century the local landscapes were represented by endless arable lands alternated with tiny patches of forests on the watersheds and swamps and solonchaks prevailing at lowlands. In the end of XXth century the large areas of arable lands, especially in northern part of mentioned area, were abandoned. Nowadays this area is covered by fallow meadows on different stages of demutation. Vegetation studies of the region have started in the end of XIXth century. One of the best scientific works on local grasslands was written by B. N. Gorodkov (1915). The spectrum of natural plant communities demonstrates some changes fr om south to north. These changes enclose both zonal and intrazonal vegetation. The southern part of the area studied belongs to forest-steppe zone. Its zonal vegetation is represented by small-leaved forests, grasslands (steppe meadows) and meadow steppes. Zonal vegetation of northern part — subtaiga subzone — includes only small-leaved forests. The watershed grasslands replace the cut-off forests. Intrazonal vegetation of southern part consists of various grasslands on salty soils and swamps predominated in the northern part. The border of forest-steppe and subtaiga represents a combination of zonal and intrazonal communities disturbed by man. The goal of this article is to reveal the diversity of grasslands on drained soils of mentioned area. The analysis of 151 geobotanical relevйs obtained fr om subtaiga and northern forest-steppe of Omskaya and Tyumenskaya administrative districts has been carried out. The syntaxonomy of the Tobol-and-the Irtysh watershed grasslands is represented by 6 associations, 4 subassociations and 2 communities of 4 alliances, 4 order and 2 classes. Subtaiga and northern forest steppe are charac­terized by different spectra of grasslands. This can be explained by a presence of wide range of saline soils in forest-steppe and their absence in subtaiga. The floristic composition of grasslands of forest-steppes zone includes the plants tolerant to soil salinity such as Artemisia pontica, Galatella biflora, Plantago maxi­ma, Eryngium planum, Saussurea amara, Limonium gmelinii. The listed species are rare in subtaiga grasslands while Festuca pratensis, Phleum pratense, Agrostis gigantea of alliance Festucion pratensis are dominated in subtaiga grassland meadows. Steppe meadows of this territory are represented by two classes. Northern forest-steppe subzone demonstrates the northern lim it of Festuco-Brometea (alliance Galatellion biflorae of order Festucetalia valesiacae). The associations Galatello biflorae–Calamagrostietum epigeii and Galio borealis–Artemisietum ponticae occupy the zonal positions. Their communities are characterize by high activity of meadow-steppe mesoxerophytes that are the diagnostic of the class Festuco-Brometea. The meadow mesophytes dominate in subtaiga steppe meadows absolutely; meadow-steppe species are rare. They are marked with a lack of diagnostic species of alliance Galatellion biflorae. They are ascribed to the class Molinio–Arrhenatheretea, order Galietalia veri and alliance Trifolion montani as the communities Filipendula stepposa–Cenolophium denudatum and Astragalus danicus–Potentilla anserinа. Forest steppe meadows of alliance Aconito barbati–Vicion unijugae (order Carici macrou­rae–Crepidetalia sibiricae, class Molinio-Arrhena­theretea) are usual for northern, subtaiga subzone of the Tobol and the Irtysh watershed. Diagnostic species list of the communities belonging to the order Carici macrourae–Crepidetalia sibiricae on West-Siberian plain is impoverished in comparison with the uplands and the mountains of South Siberia wh ere this order was described by Ermakov et al. (1999). We have revealed 2 new associations of alliance Aconito barbati–Vicion unijugae: Aegopodio podagrariae–Brachypodietum pinnati and Dracocephalo ruyschiani–Heracleetum sibiricae. In subtaiga subzone communities of these associations occupy the small well drained habitats between mesophytic forests and arable lands. The first association unites the xerophytic forest meadows with Aegopodium podagraria dominance, occurring only on right bank of the Ishim River. The second one includes forest meadows of subtaiga widely spread on the Tobol and the Irtysh watershed. Association Dracocephalo ruyschiani–Heracleetum sibiricae comprises two subassociations: D. r.–H. s. typicum and D. r.–H. s.molinietosum caeruleae. One of diagnostic species of the last mentioned subassociation is Molinia caerulea that is a common species of boreal wet meadows of Europe. The eastern border of this species distribution is on the left riverside of the Ishim River. Meadows of alliance Festucion pratensis of order Arrhenatheretalia are characteristic only for subtaiga, they belong to two associations. Meadows of subassociation Cirsio setosi–Phleetum pratensis pastinacetosum sylvestris are widespread. They are wide spread over the abandoned arable lands and rather monotonous by their floristic composition. The floristic peculiarity of plant communities is abundance of diagnostic species of classes Artemisietea и Chenopodietea. Meadows of Agrostio tenuis–Festucetum pratensis Yamalov 2005 occur on sandy soils; they present one of the first stages of pine forest demutation. Some of species are not characteristic for typical subassociation described by S. M. Yamalov (2005), therefore the meadows of this association on the Tobol and the Irtysh watershed are referred to a new subassociation A. t.–F. p. senecionetosum jacobaea.


2005 ◽  
pp. 59-75 ◽  
Author(s):  
V. B. Golub ◽  
D. N. Karpov ◽  
A. N. Sorokin ◽  
L. F. Nikolaychuk

A survey and revision of the highest syntaxa of the class Festuco-Puccinellietea with the exception of plant communities attributed to the class Scorzonero—Juncetea gerardii are submitted. Communities of the Festuco-Puccinellietea are inland intrazonal stands of Eura­sia on solonetz soils, most common in flat lowlands as well on the rivers and lakes terraces that are briefly flooded in spring-time, and dry for the most part of the growing season. The diagnostic species combi­nation of the class is heterogeneous. It includes Arte­misia dwarf semi-shrubs of the Seriphidium section that are widely spread in the Iran-Turan subregion of the Sahara-Gobi area. These are also Limonium species that are mostly diverse in the Mediterranean region where from these taxa could move into inland areas with solonetz soils. The Festuca taxa of the section Festuca together with Poa bulbosa have probably moved on solonetz soils from adjoining steppes. The halophytic Puccinellia taxa of Xeratropis and Puc­cinellia sections could penetrate into Festuco-Puccinellietea communities from the banks saline pools. The floristic composition of the class in question gives the bright example of the net-shaped evolution of plant communities according to Whittaker (1980). The distri­bution area of Festuco-Puccinellietea communities lies within the Black Sea-Kazakhstan subregion of the Eurasian Steppe region according to the subdivision of the Ancient Mediterranean by Lavrenko (1962, 1970а). There are no communities that could be placed in Festuco-Puccinellietea in Central Asia, at least the authors were not lucky to find any signs of these in references. The closest to this class are the communities of Achnatheretea splendentis, however their floristic composition and ecology are significantly different. Within the whole area of their distribution the Festuco-Puccinellietea communities are neighboring with those of Scorzonero—Juncetea gerardii occupying shallow depressions, while in the steppe zone they occur close to zonal phytocenoses on placor belonging to Festuco-Brometea. There is no idea what kinds of semidesert zonal vegetation are contiguous with Festuco-Puccinellietea communities because it is still been poorly studied from the point of view of the Braun-Blanquet approach. Syntaxa that belong to Festuco-Puccinellietea are so far poorly studied on the vast area of Ukraine, as well as Krasnodar and Stavropol regions, the Don River basin, the territory between the Don and Volga rivers of Russia, and Northern Kazakhstan.


2013 ◽  
pp. 125-135
Author(s):  
N. A. Volkova

In order to study processes taking place in secondary overmoisturised ecosystems large-scale mapping of vegetation of the ecosystems was realized. The research was taken in the steppe zone in the Rostov region. 6 yearly maps (1997–2003) of plant communities were completed at the key plot. Plant communities distribution and dynamics mostly depend on soil moisturizing and salinization. Three main types of plant successions were distinguished: 1 – fluctuation changes of plant communities effected by soil moisture degree; 2 – plant successions influenced by intermittent overmoisturization; 3 – plant successions under antropogenic influence.


2011 ◽  
Vol 74 (2) ◽  
pp. 149-157 ◽  
Author(s):  
Beata Barabasz-Krasny

The studies of fallow lands were undertaken on the Przemyśl hills in the area of Cisowa locality which, till very recently, have been owned by a State Farm (PGR). The objective was to gain insight into the composition and diversification of plant communities on meadows, pastures and fields laid fallow, in context of habitat conditions prevailing after the use had ceased. The study utilised an old cadastral map showing the type of communities by category of use: meadows, pasture, and cultivated fields. The study material consisted of 180 relevés, obtained in the period 1998-2000 using the Braun-Blanquet method. By employing numerical classification, eight plant communities were distinguished, including only two of the association rank: Epilobio-Juncetum effusi, Arrhenatheretum elatioris. The analysis of Ellenberg’s habitat indices proved that all the communities belonged to the half-light vegetation group, occurring mostly on fresh soils, under intermediate moisture-content conditions, more rarely on moist soils which do not dry out. The soil reaction was most often neutral or slightly acidic, and in most of the soils the nitrogen content was in the intermediate range. The two principal trends in the succession of communities in the area, after its farming management has ceased, are: marked increase in species richness resulting from the expansion of species, and the process of overgrowing by woody vegetation.


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