scholarly journals Scythian barrow № 4 of the «Sluiceway» group on the left bank of the Lower Dniester

2017 ◽  
Vol 6 (2) ◽  
pp. 108-113
Author(s):  
Vitalij Stepanovich Sinika ◽  
Nikolai Petrovich Telnov ◽  
Oksana Alexandrovna Zakordonets
Keyword(s):  
Black Sea ◽  
Forest Steppe ◽  
Left Bank ◽  
Black Sea Region ◽  
Funeral Rite ◽  
The North ◽  
Secondary Burial ◽  
North Western

The paper publishes materials obtained during the study of Scythian barrow 4 of the Sluiceway group on the left bank of the Lower Dniester in 2016. The main burial, almost completely robbed in antiquity, was surrounded by a ring ditch with two ruptures - in the northwest and southeast. At the western extremity of the northern arch of the ditch a horses skull was found. Secondary burial of the barrow remained undisturbed. It was done in an oblong pit. Such constructions have not been fixed in the Danube-Dniester steppes so far, except for a pit of similar proportions, excavated in the barrow 5 of the same cemetery as the published complex. The analysis of the funeral rite and a few preserved inventories demonstrates that both burials belonged to ordinary members of the Scythian community. At the same time, the gold holder and bronze earring from the secondary burial have practically no analogies in the Scythian complexes of the steppes of the North-Western Black Sea Region. A nail-shaped earring from the secondary grave testifies to the cultural impulse from the population of the Middle Dniester Region (forest-steppe), reflected in the finery of the Scythians on the left bank of the Lower Dniester in the second half of the 4th century BC.

scholarly journals BRONZE CROSS-SHAPED PLAQUES AS A CHRONOLOGY INDICATOR OF SKYTHIAN KURGANS OF THE NORTH PONTIC REGION OF THE SECOND — THIRD QUARTER OF THE 4th CENTURY BC

2019 ◽  
Vol 31 (2) ◽  
pp. 157-170
Author(s):  
S. V. Polin ◽  
М. N. Daragan
Keyword(s):  
Black Sea ◽  
Forest Steppe ◽  
Left Bank ◽  
Main Zone ◽  
The South ◽  
The West ◽  
Black Sea Region ◽  
The North ◽  
Made In

In the Scythian kurgans of the IVth century BC in the Northern Black Sea region, 31 bronze cruciform plaques were found. Such plaques are found mainly in male graves and much less often in female ones. These plaques were used as quiver buckles and for attaching the quiver to the belt. The main zone of concentration of cross-shaped plaques finds covers is the territory of the Lower Dnieper region, directly to the Dnieper. Apparently, this indicates that they were made in this region, where their place of manufacture could be only Kamenskoe hillfort, which was the center of metallurgy and metalworking in Steppe Scythia. From here they diverged south-east to Sivash within the present-day Kherson region, and much further north to the forest-steppe within the present-day right-bank Cherkasy and left-bank Kiev regions. Cross-shaped plaques are indicators of the advance of the steppe Scythians from the Lower Dnieper region to the north in the Ukrainian forest-steppe, to the west as far as the Lower Danube and very close to the south-east to Sivash. The latter direction, apparently, corresponds to migrations to winter pastures. More than half of all finds of cross-shaped plaques reliably date from within the second to third quarters of the IVth century BC, which gives every reason to assume the same dating for the complexes, where there are no own dating materials. In general, such bronze cross-shaped plaques are a reliable chronological indicator Scythian burials of the Northern Black Sea region of the second — third quarter of the IVth century BC, and also partly ethnic.

scholarly journals Sarmatian Barrow 1 of Kotlovina I Cemetery on the Left Bank of the Lower Danube

2020 ◽  
pp. 168-180
Author(s):  
Sergey Simonenko ◽  
Sergey Lysenko ◽  
Sergey Razumov ◽  
Vitalij Sinika
Keyword(s):  
Black Sea ◽  
The Body ◽  
Left Bank ◽  
Red Clay ◽  
Black Sea Region ◽  
North West ◽  
Funeral Rite ◽  
The North ◽  
Roman Time ◽  
Western Shore

Introduction. The paper deals with analyzing the Sarmatian burial complex investigated in 1990 in the barrow 1 of Kotlovina I cemetery located on the western shore of the lake Yalpug, 3 km from the village of the same name in Reni district of Odessa region. Materials. The mound was surrounded by a circular ditch with a single gap in the south. Similar ditches were recorded on the Sarmatian sites of the North-Western Black Sea region, as well as on the territory of Hungary and in the Don region. The burial was made with an offset from the geometric center of the mound, apparently, in order to avoid robbery. The main and only grave was done in a pit with an undercut. The buried man laid under the western wall of the funeral chamber in an elongated position on his back, his head to the north. The accompanying inventory is represented by a red clay pottery jug, which was covered by a handmade lid-bowl, as well as a large handmade pot. A large onehanded red clay pottery jug is of particular interest. Such vessels were widespread in the North Black Sea region, and their findings are known both in funeral complexes and in ancient settlements of the Roman time. The large size of the handmade lid-bowl, as well as the presence of traces of fuliginosity makes it possible to assume its dual purpose: as tableware during life and as a lid of the pottery vessel for the internment. The handmade pot is distinguished by an ornament in the form of impressions on the upper part of the body, forming a triangle. Conclusions. The analysis of the features of the funeral rite and the time of the inventorys existence make it possible to date the barrow to the 2nd – 3rd centuries AD. Grave 1 from barrow 1 of Kotlovina I cemetery clarifies the historical picture of the stay of Sarmatian tribes in the North-West Black Sea region, in particular, on the left bank of the Lower Danube.

scholarly journals Barrow 11 of the “Garden” Group in the Lower Dniester Region and Contemporary “Mythmaking” About Scythian “Amazons”

2020 ◽  
pp. 64-101
Author(s):  
Vitalij Sinika ◽  
Sergey Lysenko ◽  
Sergey Razumov ◽  
Nikolaj Telnov ◽  
Sylwia Łukasik
Keyword(s):  
Material Culture ◽  
Black Sea ◽  
The Body ◽  
Left Bank ◽  
Women Warriors ◽  
Black Sea Region ◽  
Scientific Methods ◽  
North West ◽  
The North ◽  
Stone Slab

The article publishes and analyzes materials obtained during the study of the Scythian barrow 11 of the “Garden” group excavated in 2018 near village Glinoe, Slobodzeya district, on the left bank of the Lower Dniester, for the first time.The barrow was surrounded by a circular ditch and contained four burials – one infant and three female. The tools from the barrow are represented by knives, spindle-whorls, needle. The only piece of tableware was found and it was a wooden bowl. The adornments (a pair of earrings, two bead necklaces, one bead bracelet, two “elbow bracelets”) were also discovered. Earrings with conical bulges on one of the endings testify to the Thracian influence on the material culture of the Scythians of the North-West Black Sea region. All female graves contained mirrors. Two of them are identical, and both were laid under the body of the buried. One of the mirrors has handle aforethoughtly broken in antiquity. The cult objects are a pendant made of a dog’s tooth and a stone slab, the arrowheads are the only weapons. The barrow dates back to the second half (preferably the third quarter) of the 4th century BC. Finding a quiver set in the grave 4 of barrow 11 of Glinoe/”Garden” group made the authors to analyze the burials of the so-called Scythian “amazons” of the North Black Sea region. It turned out that many of them were attributed with flagrant violations of scientific methods as burials of women-warriors, which is nothing more than modern “myth-making”. As a result, the authors claim that an open-minded analysis allows us to distinguish three groups of Scythian burials with weapons: 1) containing weapons, placement of which reflects certain “ethnographic” features of the rite or the special status of buried; 2) containing arrowheads that may indicate hunting; 3) the burials of warriors with diverse and numerous weapons.

Introduction

2016 ◽  
pp. 1-8
Author(s):  
Paul Huddie
Keyword(s):  
Black Sea ◽  
Russian Empire ◽  
The Black Sea ◽  
Western Balkans ◽  
Crimean War ◽  
Black Sea Region ◽  
The North ◽  
The Russian Empire ◽  
North Western

The year 2014 marked the 160th anniversary of the beginning of the Crimean War, 1854–6. It was during that anniversary year that the names of Crimea, Sevastopol, Simferopol and the Black Sea re-entered the lexicon of Ireland, and so did the terms ‘Russian aggression’, ‘territorial violation’ and ‘weak neighbour’. Coincidentally, those same places and terms, and the sheer extent to which they perpetuated within Irish and even world media as well as popular parlance, had not been seen nor heard since 1854. It was in that year that the British and French Empires committed themselves to war in the wider Black Sea region and beyond against the Russian Empire. The latter had demonstrated clear aggression, initially diplomatic and later military, against its perceived-to-be-weak neighbour and long-term adversary in the region, the Ottoman Empire, or Turkey. As part of that aggression Russia invaded the latter’s vassal principalities in the north-western Balkans, namely Wallachia and Moldavia (part of modern-day Romania), collectively known as the Danubian Principalities. Russia had previously taken Crimea from the Ottomans in 1783....

The colour/pattern polymorphism of Philaenus spumarius (Hemiptera: Cercopidae) in the north-western Black Sea region of Turkey

Biologia ◽  
2010 ◽  
Vol 65 (2) ◽  
Author(s):  
Selcuk Yurtsever ◽  
Nilgun Akdeniz ◽  
Burcu Karahalil
Keyword(s):  
Black Sea ◽  
Colour Pattern ◽  
Black Sea Region ◽  
Philaenus Spumarius ◽  
The North ◽  
The Common ◽  
Pattern Polymorphism ◽  
North Western

AbstractThe heritable elytral colour/pattern polymorphism of Philaenus spumarius in north-western Black Sea region of Turkey was investigated. A total of 2,530 adult spittlebugs, 1,020 females and 1,510 males were collected and analysed in terms of the 11 most common colour forms. Nine different phenotypes, expressed by six different alleles, were determined: populi (POP), typicus (TYP), trilineatus (TRI), marginellus (MAR), flavicollis (FLA), leucocephalus (LCE), gibbus (GIB), albomaculatus (ALB), and leucophtalmus (LOP). The common phenotypes lateralis (LAT) and quadrimaculatus (QUA) of previous studies were not encountered at all. The predominant phenotype was TYP (63%) in females and males followed by POP (31%). TRI (4%) and melanics (5%) were at close proportions. However, only one site had nine phenotypes altogether. The majority of the sites had only the POP and TYP morphs. The melanic forms were found only in females.

scholarly journals Scythian barrow 12 of the «Sluiceway» Group in the Lower Dniester

Eminak ◽  
2021 ◽  
pp. 253-267
Author(s):  
Vitalij Sinika ◽  
Nicolai Telnov ◽  
Sergey Lysenko ◽  
Sergey Razumov
Keyword(s):  
Material Culture ◽  
Black Sea ◽  
Type I ◽  
Left Bank ◽  
Black Sea Region ◽  
North West ◽  
The North ◽  
West Black Sea ◽  
West Black Sea Region

The article publishes and analyzes the materials obtained in the study of the barrow 12 of the «Sluiceway» («Vodovod») group near the Glinoe village, Slobodzeya district, on the left bank of the Lower Dniester. The grave in a catacomb of the type I (undercut) was the main under the mound, and three other in the pits were secondary. A similar situation is extremely rarely recorded in the North-West Black Sea region. The construction of round cult pits accompanying the main burial is also noteworthy. The handmade pot with a beak from the children’s burial indicates the manufacture of special dishes designed for dispensing food during feeding. The finding of the miniature bracelet with a plate receiver in the burial of a child, apparently, indicates the Thracian influence on the material culture of the Scythians of the North-West Black Sea Region, at least from the second half of the 4th century BC. It was at this time that the published mound was built and graves were made under its mound. Materials from the barrow Glinoe / «Sluiceway» 12 and other, later, Scythian burials on the left bank of the Lower Dniester demonstrate that the Scythian culture of the North-West Black Sea region continues to maintain its originality not only in the second half of the 4th century BC, but also in the next two centuries.

scholarly journals Black Soils Degradation in the South-Western Black Sea Region at Irrigation and in the Post-Irrigation Period

2012 ◽  
Vol 7 (1) ◽  
pp. 107-109
Author(s):  
Yaroslav Bilanchyn ◽  
Svetlana Rezvaya ◽  
Volodymyr Medinets
Keyword(s):  
Black Sea ◽  
Physical State ◽  
The South ◽  
Black Sea Region ◽  
The North ◽  
Irrigation Period ◽  
Composition Properties ◽  
Sea Area ◽  
North Western

Many years’ studies of process of changes in composition, properties and fertility of the black soils of the North-Western Black Sea area in Ukraine with irrigation have revealed mobility of carbonates and humus in them, decrease of capacity of cationic consumption and content of consumed calcium, increase of share of consumed magnesium and sodium. Indicators of agro-physical state of soils under irrigation conditions are worsening significantly.

scholarly journals Mesoscale numerical modeling of the boundary atmospheric layer adapted to the north-western Black Sea region. Part 1. Mathematical problem formulation

2019 ◽  
pp. 5-22
Author(s):  
E. V. Ivanova
Keyword(s):  
Boundary Layer ◽  
Numerical Modeling ◽  
Kinetic Energy ◽  
Free Boundary ◽  
Black Sea ◽  
Meteorological Parameters ◽  
Velocity Fluctuations ◽  
Black Sea Region ◽  
The North ◽  
North Western

The article presents a complete mathematical formulation of the problem of the boundary layer of the atmosphere and the interacting surface layers of the soil with the active layer of the sea adapted to the North-Western Black Sea Region through the inclusion of the coastline shape, relief elevation angles and climatic characteristics of soil moisture. The numerical model is a three-dimensional, unsteady, hydrostatic model with one- or two-parameter closure. The paper presents a detailed description of the applied sub-grid processes parameterizations such as cloudiness in the lower tier, flows of short- and long-wave radiation throughout thickness of the boundary layer and near the Earth, antigradient migration for basic meteorological variables in the presence of neutral or weakly stable stratification, components of water, heat and radiation balance, phase transitions of moisture in the atmosphere, and different parameterizations of turbulent processes used in the model. The possibilities of the model include description of neutral and stable boundary layers with consideration of the kinetic energy of vertical velocity fluctuations instead of the kinetic energy of longitudinal and transverse velocity fluctuations. Identification of the type of the boundary layer at a particular point in time is estimated using values of the Richardson number. In addition, in case of convective conditions presence, parameterization of dry convection and wet-convective adaptation may be implemented. At the boundaries of "free boundary layer – surface or near-water layer of air, air-soil and air-water" certain bonding conditions are to be set to ensure continuity of meteorological parameters or their flows. On the upper boundary of the free boundary layer actual values of meteorological parameters and necessary parameters, or corresponding values from the global atmospheric model are to set. At the lower boundary of the deep soil layer the invariance of the vertical temperature gradient of the active layer of the sea – the value of temperature which is equal to the value of the latter according to its climatic values in the considered season of the year is to be set. The presented model is the first approximation in numerical modeling of the boundary layer over the adapted territory and is designed for studying the thermodynamic structure of the boundary layer of the adapted territory, as well as for identifying the breeze effects over the terrain.

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