Some Results of New Investigations at the Kapova Cave in the Southern Urals

1989 ◽  
Vol 55 (1) ◽  
pp. 181-191 ◽  
Author(s):  
V. E. Shchelinsky

In 1982 investigations were resumed at the Kapova Cave in the Urals, which was already widely known for its rock paintings dating from the Upper Palaeolithic period. It is, to date, the only authentic site of its kind in Eastern Europe.The cave is situated on the western slopes of the southern Urals in the valley of the Belaya River 200 km south of the city of Ufa (fig. 1). It is a cave of a karst type that evolved in limestones of the Devonian and Carboniferous periods. The enormous entrance to the cave facing south-east is in the narrow gorge of the canyon of a U-shaped valley at a distance of 150 m from the Belaya River at a height of 7–8 m above its low-water level (pl. 31). The total length of the cave's passages investigated is 2 km (fig. 2).

2011 ◽  
Vol 45 ◽  
pp. 223-236 ◽  
Author(s):  
I. N. Urbanavichene

The first data on the lichen flora of Zyuratkul National Park (Chelyabinsk Region) are provided. The preliminary list includes 263 species of lichens and allied fungi. Parmelia barrenoae and Pyxine sorediata were found for the first time for the Eastern Europe, 22 species are new for the Urals and 23 for the Southern Urals.


2012 ◽  
Vol 18 (1) ◽  
pp. 29-50
Author(s):  
Sergeï Gutsalov

Abstract This article publishes interesting burials of ancient nomads dating from the end of the 3rd, 2nd or 1st centuries BC from the Dongulyuk II and Volodarka I tumuli necropoleis in the West of Kazakhstan. Materials from these funerary sites include some quite rare finds: phalerae, belt plates bearing depictions of confronting winged dragons, two-handled infantry swords used by warriors on foot and other objects relating to the life of nomads. The funerary rite – including such elements as burials in pits with ledges or in catacombs, the laying out of horses’ skulls on ledges, the arrangement of the deceased with their heads pointing to the north or south – indicates that the cultural links of the nomads from the southern foothills of the Urals at the end of the 1st millennium BC were orientated towards Central Asia. If it is borne in mind that many objects among the accompanying grave goods can also be associated with the eastern half of the Eurasian steppes, then it would seem highly likely that the nomads had originally come from northern China, moving west and migrating into eastern Europe including the southern Urals.


2021 ◽  
Vol 2 (44) ◽  
pp. 3-3
Author(s):  
Alexander Saakian ◽  
◽  

The article presents the results of a bioindication study of atmospheric air pollution on the condition of pine needles (Pinus sylvestris L.) on the example of the city of Orsk, Orenburg region. The city of Orsk is a major industrial center of the Southern Urals. The research was carried out on 6 sites located within the city with different anthropogenic loads. The research method is based on the direct dependence of damage to Pinus sylvestris L. needles (necrosis and desiccation) on the level of atmospheric air pollution. Analyzed the morphological characteristics of the needles of Pinus sylvestris L. in the studied areas. The result of the study is an assessment of the state of atmospheric air. Keywords: BIOINDICATION, SCOTS PINE, NEEDLES, AIR POLLUTION, ORSK CITY, ORENBURG REGION


2019 ◽  
Vol 488 (4) ◽  
pp. 413-419
Author(s):  
A. A. Krasnobaev ◽  
V. N. Puchkov ◽  
N. D. Sergeeva ◽  
S. V. Busharina

New age determinations of detrital zircons of sandstones augmented the possibilities of interpretation of their provenance. This interpretation is often restricted by a formal comparison of age-and-composition characteristics of detrital crystals with any very distant model objects. A different situation arises when the role of a source of a detritus is claimed by local objects. The analysis of SHRIMP and TIMS - datеs of zircons and U and Th concentrations in them, and also a comparison of histograms of primary zircons from Riphean volcanics and rocks of the Taratash complex on one hand and the detrital zircons from the sandstones of Vendian (Asha series) and Lower Riphean (Ai Formation) on the other, have shown that the age variations of sources and clastics are comparable in many aspects. It means that the age characteristics of primary zircons from the Riphean volcanics and rocks of the Taratash complex as sources of zircon clastics for the Riphean and Vendian sandstones in the Southern Urals are regulated by processes of resedimentation, though the influence of distant sources is not excluded.


Inner Asia ◽  
1999 ◽  
Vol 1 (2) ◽  
pp. 267-282 ◽  
Author(s):  
V. A. Shnirelman

AbstractArkaim is the name given to the site of an ancient town in the Southern Urals, dated to the 17th–16th centuries BC. Discovered in 1987, Arkaim rapidly became more than an archaeological site. It became the focus for an extraordinary congolmeration of ideas linked to ecological and political movements, in particular those of Russian nationalists. Threatened with flooding because of a dam project, Arkaim was made a ‘Museum Reserve’. Soon it became the focus for theories that this was a sacred place and furthermore the home of proto-Slavs. The break-up of the Soviet Union was followed by attempts by Russian nationalists to demonstrate the legitimacy of their domination of the former empire. The article shows how quasi historical claims expanded into myth and fantasy, linked to the emergence of new cults. Arkaim became the city not only of proto Slavs but of Zarathustra and the Aryans too. Such inventions are related to local politics and ethnic tensions as well as to wider Russian nationalism.


Author(s):  
Н. Л. Моргунова ◽  
М. А. Кулькова ◽  
А. М. Кульков

Среди курганов ямной культуры Среднего Поволжья и Южного Приуралья особое место занимают монументальные сооружения с находками изделий из железа. Выделяются предметы как производственного, так и ритуального назначения. По данным радиоуглеродного анализа курганы датируются в пределах первой половины III тыс. до н. э. В 2019 г. авторами на современном оборудовании проведены новые исследования химического состава поверхности металлических предметов, изотопный анализ свинца, а также реставрация железных предметов. Дополнительные исследования позволили подтвердить метеоритное происхождение железа, уточнить форму и функциональное назначение изделий. Анализ погребального обряда и инвентаря из меди и метеоритного железа позволяет сделать вывод, что курганы были предназначены для «супер-лидеров». При жизни они могли выполнять управленческие, военные и сакрально-ритуальные функции. Наличие предметов из железа свидетельствует об обожествлении власти вождей и о распространенном представлении связи лидерства и небесных сил. Large burial constructions that have yielded items made from iron occupy a special place among the Yamnaya kurgans in the Middle Volga region and the Southern Urals. It is possible to single out both production items and artifacts used for religious purposes. The radiocarbon data put the kurgans around the first half of III mill. BC. In 2019 the authors conducted new research of the chemical composition of the metal item surface, using modern equipment, performed the stable isotope analysis of the lead and carried out the restoration works of the iron objects. The additional studies provided an opportunity to confirm the meteoric origin of the iron, clarify the shape and the functional purpose of the artifacts. It can be inferred from the analysis of the funerary rite and the offerings made from copper and meteoric iron that the kurgans were intended to bury super leaders. During their lifetime such chieftains could perform management, military and sacral ritual functions. Presence of iron items suggests that the power of the chieftains was deified and the idea of the links between the leadership and heavenly forces was quite common.


2016 ◽  
Author(s):  
Victor Puchkov

Abstract. The period of an official activity of the EUROPROBE commission was inconnected in the Urals with implementation of the URALIDES Program, that stimulated many qualified geologists from the Western research institutes and Universities to come to the region and work with local geologists at actual problems of the Uralian geology. The author tries to answer a question: what interesting results had been obtained in the Southern Urals in the last decade, when the most of foreign researchers left the Urals, and how these results correspond to the scientific conclusions that had been done before.


2021 ◽  
Vol 20 (2) ◽  
pp. 192-204
Author(s):  
Vladimir N. Zemtsov

The article identifies the features of the Ural region in terms of preserving and updating the memory of the epoch of 1812-1814. Based on the analysis of various options for preserving images of the epoch (through living memory, materialized memory, festive events and other means), the author comes to the conclusion that the Ural region, despite its remoteness from the theater of war, organically fit into the all-Russian memorial context. At the same time the memory is shaped by the regions focus on military production, and by its providing a significant part of the irregular cavalry recruited from the Orenburg Cossacks and non-Russian peoples. The latter circumstance, through images of Northern cupids, gave the Urals an exotic fame abroad. Forms of preserving Urals memory of the events of 1812-1814 range from variants of living memory, which includes elements left over from the communicative memory, to purposeful activities of central and local authorities to organize mass events at anniversary dates. A significant role in memory preservation is traditionally played by educational institutions, which, starting from the school level, form the memory of childhood. The greatest concentration of memory elements related to the epoch is observed in the Southern Urals, which is predetermined, to a large extent, by the presence of compactly living non-Russian peoples who seek to emphasize their role in the events of all-Russian and even global history. Unlike a number of other national regions of the Russian Federation, the appeal to historical memory in the Urals takes place within the framework of a unifying and reconciling tradition. Despite some commemorative gaps, the three epochs (pre-Soviet, Soviet and post-Soviet) in relation to the historical memory in the Urals about the events of 1812-1814 look quite organic. Images of this great time continue to act as a unifying factor, thus preserving the sense of a common past not only with the all-Russian, but also with common European and global history.


2020 ◽  
Vol 62 ◽  
pp. 70-76
Author(s):  
O. E. Merezhko ◽  
M. A. Mazunin ◽  
E. Z. Savin ◽  
A. I. Gridnev

The article presents tests of natural creeping apple trees and natural dwarfs, carried out in the in the conditions of the Orenburg region. There were from 50 to 100 trees in the experiment in each variant. Vigorous standard plantations were used as control. The aim of the research was to test natural creeping apple trees, natural dwarfs against the background of standard varieties bred in the South Urals (Chelyabinsk), as well as to determine their prospects for intensive horticulture in the extreme conditions of the region. The preservation of plantings for all variants of the experiment for 20 years of research is high and amounted to 92-99 %, their condition was estimated at 4.5-5.0 points. The highest yield was noted for natural dwarfs (457.2 c/ha), the smallest yield was obtained on vigorous standard plantings (control) – 238.7 c/ha. Naturally creeping apple trees in terms of productivity were higher than control by an average of 25 %. Of the naturally creeping varieties, the most productive were the varieties Podsnezhnik (348.3 c/ha), Chudnoe (335.2 c/ha), the least productive were the varieties Plastun and Kovrovoe (255.1 and 262.5 c/ha, respectively). On the natural dwarfs, the most productive variety was the variety Brat Chudnogo (461.2 c/ha). In the control, the most productive varieties were the varieties Symbol (295.9 c/ha) and Nadezhda (270.5 c/ha), less productive were the varieties Pamyat Zhavoronkova and Fevralskoe (208.0 and 224.1 c/ha, respectively). Low-growing plantations, in particular layer and natural varieties of the Urals, are distinguished by their early maturity and, in general, higher productivity per unit area. The highest labor costs are accounted for by natural dwarfs (485.4 person-day/ha) and the lowest in vigorous plantings (317.4 person-day/ha). This has a positive eff ect on the profit and rentability of production.


LITOSFERA ◽  
2021 ◽  
Vol 21 (5) ◽  
pp. 601-608
Author(s):  
A. A. Krasnobaev ◽  
V. N. Puchkov ◽  
N. D. Sergeeva ◽  
S. V. Busharina

Research subject. Magmatic complexes that are developed in the lower (volcanogenic-sedimentary) part of the Ai Formation of the Lower Riphean of the Taratash anticline in the Southern Urals. Results. For the frst time, the Lower Permian SHRIMP dating (288.6 ± 3.1 Ma by U-Pb method on zircon from monzogabbro) was obtained for a dike cutting the basalts of the Lower Paleozoic (420–450 Ma) age. Conclusions. On the eastern slope of the Urals there is a chain of massifs which are close in the age. The chain belongs to the Lower Permian Stepninsky monzogabbro-granosyenite-granite complex, represented by the Uiski, Vandyshevski, Biryukovski and Stepninski intrusions with the age of 281 ± 2, 280 ± 2 and 286 ± 2 Ma, correspondingly (U-Pb method after zircons, SHRIMP-II, VSEGEI) and earlier obtained dates 281 ± 4 Ma (Rb-Sr isochrone) and 283 ± 2 Ma (isotope Pb-Pb method after zircons). The Stepninsky complex was described earlier as plume-dependent. The monzogabbro dike, described in this paper, although being at a considerable distance from the Sepninsky complex, is situated at a strike of the chain of the stepninsky intrusions, is close to them by the composition and age and can be ascribed to the same plume episode. The idea of the plume character of the complex was ехрressed by us relatively long ago based on a superimposed character of the chain of the intrusions over the earlier, collisional Uralian structures. As for the geochemical character (monzogabbro) the dike conforms with one of two standard trends of the Stepninsky complex – monzonite (monzogabbro, monzodiorites, syenites).


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