Classification of alder forests on sandy massifs in the Rostov region

2015 ◽  
pp. 108-128 ◽  
Author(s):  
T. A. Sokolova

The results of geobotanical survey of Alnus glu­ti­nosa arena forests at three sandy areas within the North of the Rostov and the West of the Volgograd regions of the Russian Federation are given. The territory is situated at the East European Plain where steppes are zonal type of vegetation. This territory is well developed agricultural region with highly transformed lands. Nevertheless, the fragments of natural vegetation support rather high floristic and phytocoenotic diversity and they contain a number of endemic species also (Fedyaeva, 2002). Small patches of alder forest stands generally occur in roundish and tape-like depressions on the second and third sandy terraces of the Don River. These woods were in a focus of interest of many scientists, e.g. G. M. Zozulin (1992) who studied these more than 30 years. But the special papers including the ecologo-floristic characteristic of natural arena alder forests were missing up to now. According to vegetation classification based on the Braun-Blanquet approach (Braun-Blanquet, 1964) the alder forests are referred to four formerly described associations of the alliances Alnion incanae and Alnion glutinosae: Aceri tatarici–Alnetum glutinosae, Urtico dioicae–Alnetum glutinosae, Ficario–Ulmetum minoris and Carici elongatae–Alnetum glutinosae. Proposed 4 subassociations and 10 variants reveal the syntaxonomical structure of these associations. The comparative analysis of syntaxa of the forests of the alliances Alnion incanae and Alnion glutinosae within the Rostov region, in the Russian Southern Nechernozemje, in Ukraine and the Central Europe was done. It is emphasized that the differentiation of the alder communities is complicated due to their intrazonal positions in a landscape. There are a very few character species at the association level. At the same time a lot of plant communities reflect the ecotone features between the meso-hygrophyte forests of the class Querco-Fagetea and the mire woods of the class Alnetea glutinosae. Therefore we had to apply both the classical and nonclassical syntaxonomical analysis (Mirkin et al., 2009). It is obvious that the alder forests syntaxonomy at the lowest level will be specified in the nearest future. There are noticeable differences in species composition of studied communities depen­ding on their position in landscape. For example, there are communities with a large amount of species of the class Querco-Fagetea occurring in the forest margins and on slopes. The role of species of the class Alnetea glutinosae increases on the gradient from the outskirts of wood massifs to their central parts in lowlands also. Species of the alliance Alnion incanae are widely presented in all communities. Although the described communities are small in size and rather rare on the territory studied they contain 27 vascular plant species included in the Red Data Book of the Rostov region (Krasnaya…, 2004). These woods considerably increase the biodiversity within the steppe zone as well. The organization of a number of nature reserves is necessary to protect the certain types of alder forests.

Vita Antiqua ◽  
2021 ◽  
pp. 43-54
Author(s):  
V.N. Stepanchuk ◽  

The purpose of this article is to present data on the surface structure identified in the upper layer of the Mira site in the Dnieper valley. The occupation of layer I, based on a set of consistent data, constitutes the remains of a seasonal winter camp of Pleistocene horse hunters. Ten available radiocarbon dates place the calibrated age of layer I between 31,000 to 28,000 cal BP. The rapid albeit gentle overlapping of the settlement remains with alluvial sediments ensured that the original settlement and dwelling patterns and their elements survived well. Thanks to this, it is possible to reconstruct some significant aspects of the construction process, as well as details of the arrangement of the dwelling’s interior space. A 30,000-year-old, permanent skeleton cylindrical yaranga type surface construction from Mira layer I is currently representing the oldest dwelling known in the Upper Palaeolithic of Ukraine and a broader context of the steppe zone of the East European plain. Keywords: Upper Palaeolithic, surface dwelling, Eastern Europe


2010 ◽  
Vol 36 (-1) ◽  
pp. 47-54 ◽  
Author(s):  
Anto Raukas ◽  
Wojciech Stankowski ◽  
Vitālijs Zelčs ◽  
Petras Šinkunas

Chronology of the Last Deglaciation in the Southeastern Baltic Region on the Basis of Recent OSL DatesThe study of the deglaciation chronology in the south-eastern Baltic Region belonging to the outer zone of the last Pleistocene glaciation has a long history. The Finnish investigator H. Hausen (1913) who worked in the north-western portion of the East-European Plain at the beginning of the 20thcentury was the first to attempt a reconstruction of the course of glacial retreat during the last glaciation. At that time investigators had no physical dating methods and the time scale based on varvometric method, introduced by the Swedish geologist G. de Geer (1912) who divided the deglaciation history of Scandinavia into Daniglacial, Gotiglacial and Finiglacial, each of which had different palaeoglaciological conditions. During last decades different dating methods, including14C, ESR, luminescence methods and10Be techniques have been used, but they could not help essentially improve the existing stratigraphical charts and many problems of topical interest in the history of deglaciation have not been solved yet. During last years the first two authors have studied the suitability of OSL method for the geochronological purposes, paying the most attention to the waterlaid sediments. In the first step they have found the most promising genetical varieties of glaciofluvial sediments (glaciofluvial deltas and sandurs) and in this paper they widened the study area to all three Baltic states with close cooperation with Latvian and Lithuanian colleagues. The obtained results demonstrated, that not all mineral grains in the uppermost glaciofluvial and glaciolacustrine sediments were fully bleached during the last deglaciation. Probably the older sediments also influenced to the luminescence results. It means, that stratigraphic conclusions based on single dates or their small sets are inadmissible and in each case luminiscence dating requires a verification using other methods.


2018 ◽  
Vol 90 (3) ◽  
pp. 439-456 ◽  
Author(s):  
Adam Nadachowski ◽  
Grzegorz Lipecki ◽  
Mateusz Baca ◽  
Michał Żmihorski ◽  
Jarosław Wilczyński

AbstractThe woolly mammoth (Mammuthus primigenius) was widespread in almost all of Europe during the late Pleistocene. However, its distribution changed because of population fluctuations and range expansions and reductions. During Marine Oxygen Isotope Stage 2 (MIS 2), these processes were highly dynamic. Our analyses of 318 radiocarbon dates from 162 localities, obtained directly from mammoth material, confirmed important changes in mammoth range between ~28.6 and ~14.1 ka. The Greenland stadial 3 interval (27.5–23.3 ka) was the time of maximum expansion of the mammoth in Europe during MIS 2. The continuous range was soon fragmented and reduced, resulting in the disappearance of Mammuthus during the last glacial maximum from ~21.4 to ~19.2 ka in all parts of the North European Plain. It is not clear whether mammoths survived in the East European Plain. The mammoth returned to Europe soon after ~19.0 ka, and for the next 3–4 millennia played an important role in the lifeways of Epigravettian societies in eastern Europe. Mammoths became extinct in most of Europe by ~14.0 ka, except for core areas such as the far northeast of Europe, where they survived until the beginning of the Holocene. No significant correlation was found between the distribution of the mammoth in Europe and human activity.


Author(s):  
A. G. Granovsky ◽  
N. V. Granovskya

The tectonic structure in the junction zone of the East European and Scythian platforms of Rostov region has been considered. Different ages and ranks of Precambrian and Phanerozoic tectonic structures, their correlation within the studied area and tectonic zoning scheme are presented. The structure and composition of rock complexes, formation conditions and their tectonic development stages are characterized. The East European platform within the described territory is represented by two disconnected fragments of the Russian Plate. The northern fragment is the south-eastern part of the Voronezh anteclise, located to the north of the Donetsk-Astrakhan tectonic suture. The southern fragment corresponds to the eastern dipping of the Pre-Paleozoic rocks of the Ukrainian shield, forming the buried Rostov ledge. The Scythian (Epihercynian) platform located to the south of the Donetsk-Astrakhan tectonic suture, is represented by a folded Paleozoic (in some places pre-middle-Jurassic) base and a platform cover of Mesozoic-Cenozoic rocks. The part of the Scythian platform is the exposed Donbass area, where Paleozoic rocks of the base of the platform protrude to the surface and form the Donetsk ledge. The northern part of the Scythian plate, which extends over the buried folds system of Donbass, is allocated from the south by Manych over-fault deflections and called «Karpinsky shaft». The system of the Manych deflections and the territory located to the south compile the Ciscaucasian part of the Scythian plate.


2019 ◽  
Vol 70 (3) ◽  
pp. 198-210
Author(s):  
Nikolay Khitrov ◽  
Maria Smirnova ◽  
Nikolai Lozbenev ◽  
Ekaterina Levchenko ◽  
Vasiliy Gribov ◽  
...  

Abstract The soil cover of the forest-steppe and steppe zones of the East European Plain is characterized by diverse soil combinations revealed during large-scale and detailed soil mapping against the background of a traditional zonal sequence of dominant automorphic soils alternating from the north to the south and clearly displayed on small-scale soil maps. The composition, configuration and functioning of particular soil cover patterns are determined by the soil forming factors acting within a given area. The elementary soil areas (detailed scale) and elementary soil cover patterns maps (large scale) of the Central Russian, Kalach, and Volga Uplands are created by both traditional and digital soil mapping methods. Low-contrasting soil combinations with the background Haplic Chernozems (Loamic or Clayic, Pachic) alternating with zooturbated Haplic Chernozems (Loamic or Clayic, Pachic) on convex elements of the microtopography and Luvic Chernozems (Loamic or Clayic, Pachic) on concave elements of the microtopography prevails under conditions of thick clay loamy parent materials and free drainage. Under conditions of shallow embedding by low-permeable clayey sediments, the soil cover includes Chernozems or Chernic Phaeozems with stagnic features in some part of the soil profile or even Mollic Stagnosols. The presence of shrink-swell clays of different ages leads to the formation of Bathyvertic Chernozems, Vertic Chernozems, Vertic Chernic Phaeozems and/or Pellic Vertisols. The presence of soluble salts in the parent material leads to the development of solonetzic soil complexes consisting of Protosodic or Sodic Chernozems and different types of Solonetzes.


2020 ◽  
Vol 4 (7) ◽  
pp. 52-60
Author(s):  
Tatiana Sokolova ◽  

The paper presents the data on new locations in forest communities of the Rostov Region of vascular plant spe-cies listed in the regional Red Data Book. More than 200 new localities were recorded for 42 species between 2008 and 2020. Matteucia struthiopteris is recorded for the first time in the Rostov Region. 22 species are rec-ommended for inclusion into the new edition of the Red Data Book of the Rostov Region.


Data in Brief ◽  
2020 ◽  
Vol 30 ◽  
pp. 105555
Author(s):  
Fatima Kurbanova ◽  
Tatiana Puzanova ◽  
Olga Rudenko ◽  
Gennadiy Starodubtsev

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