scholarly journals СИНАНТРОПІЗАЦІЯ ФЛОРИ ВОЛИНСЬКОЇ ОБЛАСТІ

Author(s):  
L.О. Kotsun ◽  
I.I. Kuzmishyna

<span>Volyn region is located in North-Western Ukraine. Its territory is plain in the North and poorly hilly in the South with a total obliquely in a Northerly direction. The climate is temperate continental with mild winters and moderately warm enough wet summer. Sod-podzolic and meadow soils is predominate, sod, forest-steppe podzolized soils, typical black less common. According to physical and geographic zone, the area belongs to the zone of mixed coniferous-deciduous forests; by geobotanical zoning of Ukraine – the European broadleaved forest region, East European and Central provinces. Some 1272 species of vascular plants of natural flora were registered in the Volyn region during filed surveys in 1999-2015 together with retrospective data and herbarium collections. Among them the synanthropic group was isolated, which includes 507 species (over 38% of all the species). Local synanthropic apophytes species (ca. 287) are dominated over antropophytes (220 species). The ratio between these two groups is 1.3:1. This is the evidence that the synanthropic flora was formed with domination of local explerent apophytes followed by adventive plant species. Species with active dissemination strategy in seminatural and transformed ecosystems like hemiapophytes (149 species) are dominated among the apophytes by the degree of adaptation to the anthropogenically transformed conditions. It was found that 220 species belong to antropophytes among which the kenophytes (111 species) dominate by time of invasion. We also registered some 109 species of arheophytes. The ratio between these two groups is 0.9:1.0, which indicates the moderate degree of invasion of alien species to the study area. The xenophytes (111 species) are dominated by the method of invasion. The epekophytes (159 species) – species that which grow in communities that would disappear with the cessation of human activities dominate by the degree of naturalization. We distinguished the group of alien species with high phytocoenotic activities that are the herbaceous annuals or milticarpos with the core root system without underground shoots of North American origin.</span>

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.


Radiocarbon ◽  
2009 ◽  
Vol 51 (2) ◽  
pp. 783-793 ◽  
Author(s):  
Pavel M Dolukhanov ◽  
Anvar Shukurov ◽  
Kate Davison ◽  
Graeme Sarson ◽  
Natalia P Gerasimenko ◽  
...  

Newly available radiocarbon dates show the early signs of pottery-making in the North Caspian area, the Middle-Lower Volga, and the Lower Don at 8–7 kyr cal BC. Stable settlements, as indicated by “coeval subsamples,” are recognized in the Middle-Lower Volga (Yelshanian) at 6.8 kyr cal BC and the Caspian Lowland at about 6 kyr cal BC. The ages of the Strumel-Gostyatin, Surskian, and Bug-Dniesterian sites are in the range of 6.6–4.5 kyr BC, overlapping with early farming entities (Starčevo-Körös-Criş and Linear Pottery), whose influence is perceptible in archaeological materials. Likewise, the 14C-dated pollen data show that the spread of early pottery-making coincided with increased precipitation throughout the forest-steppe area.


2020 ◽  
Vol 85-86 ◽  
Author(s):  
O.I. Shynder ◽  
Y.M. Negrash

Objective – to study the current distribution of Sedum pallidum in Ukraine, to analyze its state in the alien flora of Ukraine. Material and methods. The studies were conducted in 2008–2019 in the plain part of Ukraine and in the Mountain Crimea. Literature information, several national herbarium collections and other sources were analyzed. Special attention was paid to the delimitation of synantropic locations of S. pallidum from cultural ones. Results. S. pallidum is a sub-euxine species, which range occupies the Mountain Crimea. It is widely cultivated throughout Ukraine and is prone to naturalization, thanks to its vegetative and generative reproduction. In general, about 30 synantropic locations of S. pallidum have been recorded, mainly in the Middle Prydniprovia and Western Ukraine. Urban lawns and roadsides on light substrates are favorable ecological niches for S. pallidum. Соnclusions. S. pallidum is the alien species in the flora of the plain part of Ukraine and ergasiophyte in its origin. A potential secondary synanthropic range of this species occupies the whole country except the Carpathian highlands. It has been established that S. pallidum in the culture of the Forest-Steppe is a perennial herb. Two races identified in its composition (var. pallidum and var. bithynicum) are probably ecads, and have no systematic importance. In the culture, S. pallidum is characterized by successful vegetative and generative reproduction, which contributes to its naturalization. S. pallidum is often confused with other species of the genus, what does not contribute to its study in adventive floras. A key for S. pallidum determination has been proposed.


2018 ◽  
pp. 149-154

Vera Antonovna Martynenko (17.02.1936–06.01.2018) — famous specialist in the field of studying vascular plant flora and vegetation of the Far North, the Honored worker of the Komi Republic (2006), The Komi Republic State Scientific Award winner (2000). She was born in the town Likhoslavl of the Kali­nin (Tver) region. In 1959, Vera Antonovna graduated from the faculty of soil and biology of the Leningrad State University and then moved to the Komi Branch of USSR Academy of Science (Syktyvkar). From 1969 to 1973 she passed correspondence postgraduate courses of the Komi Branch of USSR Academy of ­Science. In 1974, she received the degree of candidate of biology (PhD) by the theme «Comparative analysis of the boreal flora at the Northeast European USSR» in the Botanical Institute (St. Petersburg). In 1996, Vera Antonovna received the degree of doctor of biology in the Institute of plant and animal ecology (Ekaterinburg) «Flora of the northern and mid subzones of the taiga of the European North-East». The study and conservation of species and coenotical diversity of the plant world, namely the vascular plants flora of the Komi Republic and revealing its transformation under the anthropogenic influence, was in the field of V. A. Martynenko’ scientific interests. She made great contribution to the study of the Komi Republic meadow flora and the pool of medi­cinal plants. She performed inventorying and mapping the meadows of several agricultural enterprises of the Republic, revealed the species composition and places for harvesting medicinal plants and studied their productivity in the natural flora of the boreal zone. The results of her long-term studies were used for making the NPA system and the Red Book of the Komi Republic (1998 and 2009). Vera Antonovna participated in the research of the influence of placer gold mining and oil development on the natural ecosystems of the North, and developed the method of long-term monitoring of plant cover. Results of these works are of high practical value. V. A. Martynenko is an author and coauthor of more than 130 scientific publications. The most important jnes are «Flora of Northeast European USSR» (1974, 1976, and 1977), «Floristic composition of fodder lands of the Northeast Europe» (1989), «The forests of the Komi Republic» (1999), «Forestry of forest resources of the Komi Republic» (2000), «The list of flora of the Yugyd va national park» (2003), «The guide for vascular plants of the Syktyvkar and its vicinities» (2005), «Vascular plants of the Komi Republic» (2008), and «Resources of the natural flora of the Komi Republic» (2014). She also was an author of «Encyclopedia of the Komi Republic» (1997, 1999, and 2000), «Historical and cultural atlas of the Komi Republic» (1997), «Atlas of the Komi Republic» (2001, 2011). V. A. Martynenko made a great contribution to the development of the botanical investigations in the North. Since 1982, during more than 10 years, she was the head of the Department of the Institute of Biology. Three Ph. D. theses have been completed under her leadership. Many years, she worked actively in the Dissertation Council of the Institute of biology Komi Scientific Centre UrB RAS.  The death of Vera Antonovna Martynenko is a heavy and irretrievable loss for the staff of the Institute of Biology. The memory of Vera Antonovna will live in her numerous scientific works, the hearts of students and colleagues.


2018 ◽  
Vol 51 (1) ◽  
pp. 66-72 ◽  
Author(s):  
A. T. Barabanov ◽  
S. V. Dolgov ◽  
N. I. Koronkevich ◽  
V. I. Panov ◽  
A. I. Petel’ko

2019 ◽  
Vol 8 (2) ◽  
pp. 215-220
Author(s):  
Andrey Mikhailovich Skorobogatov

For a long time, the Eneolithic of the Don forest-steppe remained one of the least studied epochs in the archaeological scheme of the region. However, since the late 1960s, sites with materials of the Eneolithic have been actively explored on the territory of the Voronezh and Lipetsk Regions. By the 1980s, researchers had a concept for the development of copper-stone age cultures within the system of the Mariupol cultural-historical region of the Dnieper-Don-Ural interfluve, which is still relevant today. The criteria for distinguishing the Eneolithic era in the steppe and forest-steppe spaces of the East European steppe and forest-steppe were substantiated. The idea of their synchronization with complexes of the Tripolye A period was designated. The early Eneolithic in the Don forest-steppe was marked by the appearance of a population with specific ceramics of Nizhnedonskaya culture. Questions of the chronology of the early Eneolithic were solved exclusively by methods of analogies with the materials of neighboring territories and synchronization with the local Neolithic complexes. The paper deals with the problems of chronology, periodization and synchronization of materials from the early Aeneolithic of the territory of the Don forest-steppe. The focus is on the absolute dating of the Nizhnedonskaya culture of the Mariupol cultural-historical region and its synchronization with the early Tripolye Culture. According to all the data available to date, the regions early Eneolithic can be dated from 5300 to 4250 BC.


2021 ◽  
Vol 29 (6) ◽  
pp. 627-640
Author(s):  
E. Yu. Golubkova ◽  
O. F. Kuzmenkova ◽  
E. A. Kushim ◽  
A. G. Laptsevich ◽  
S. S. Mankievič ◽  
...  

Abstract— The complete sections of the Lower and Upper Vendian of the East European Platform were opened in the boreholes of Belarus. This allows us to consider this region as a stratotype area. In order to update the paleontological characteristics of the Vendian, organic-walled microfossils from the Bogushevsk-1, Bogushevsk-2 (Liozno), and Lepel-1 reference boreholes drilled in the north of the Orsha Depression were studied. The transitive assemblage I with Leiosphaeridia minutissima–Leiosphaeridia tenuissima was recognized in the Lower Vendian Liozno Formation of the Volyn Series and the Upper Vendian Kotlin Formation. The Redkino microfossil assemblages were identified at three stratigraphic levels in the Nizy, Selyava, and Chernitsa formations: assemblage II with Morania zinkovi, assemblage III with Morania zinkovi–Tynnia precambrica, and assemblage IV with Morania zinkovi–Tynnia precambrica–Striatella coriacea, respectively. The Kotlin assemblage V with Vendotaenia antiqua–Primoflagella speciosa was distinguished in the upper part of the Kotlin Formation (Bogushevsk-1 borehole). On the basis of the taxonomic composition, assemblages III and IV are correlated with the first Redkino biota of the Starorusskaya Formation; assemblage V is correlated with the third Kotlin biota of the Vasileostrovskaya Formation of the northwestern part of Russia. Our data show a high biostratigraphic potential of organic-walled microfossils, which should be used to substantiate regional stratigraphic units of the Upper Vendian in the updated stratigraphic scheme of the East European Platform.


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