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Littérature scientifique sur le sujet « Russification – Volga River Region (Russia) »

Auteur : Grafiati
Publié le 10 mars 2023

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Articles de revues sur le sujet "Russification – Volga River Region (Russia)"

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Baranov, D. V., A. O. Utkina et A. V. Panin. « Tver proglacial lake (Tver region, Russia) : myth or reality ». Limnology and Freshwater Biology, no 4 (2022) : 1383–84. http://dx.doi.org/10.31951/2658-3518-2022-a-4-1383.

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Abstract. In this study we aimed to find a Tver proglacial lake in the Upper Volga low land at the Late Valdai that it have been reconstructed by D.D. Kvasov. Our field studies did not verify previously reconstructed lake terraces at 135 140 and 120 125 m a.s.l., though at 140 m a.s.l. we found the Volga River terrace near Seslavie (Tver region, Russia). According to OSL data from this terrace, the Volga River has existed in the Upper Volga lowland ever since the LGM.
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Schletterer, Martin, Leopold Füreder, Vyacheslav Viktorovich Kuzovlev, Kyrill Yuryevich Zhenikov et Yuri Nikolayevich Zhenikov. « REFCOND-VOLGA : a monitoring programme for water quality in the headwaters of the Volga River (Tver region, Russia) ». Revista Eletrônica de Gestão e Tecnologias Ambientais 4, no 1 (23 novembre 2016) : 18. http://dx.doi.org/10.9771/gesta.v4i1.16288.

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<p>Within the research expedition “Upper Volga 2005” an assessment of hydrological, limnochemical and biological parameters was carried out in the Volga River upstream of Tver, including the main channel as well as major tributaries. This assessment revealed that the headwaters of the Volga River represent conditions which are either reference or least disturbed and stipulated the establishment of the monitoring programme “REFCOND_VOLGA”, which is in operation since 2006 and includes stretches along the Volga River (Rzhev, Staritsa, Tver) as well as along the tributary Tudovka.</p>This paper summarizes the “first 10 years” of this joint Russia-Austrian research project, focusing on a sound description of the research area and providing a complementary view on the available data as well as a view ahead.
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Ugleva, S. V., et S. V. Shabalina. « Ricketsioses in the Lower Volga region ». Journal of microbiology, epidemiology and immunobiology 98, no 2 (5 mai 2021) : 231–38. http://dx.doi.org/10.36233/0372-9311-60.

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The aim of this work was to describe the features of the epidemiology and clinic of rickettsioses at the Lower Volga region.Materials and methods. Scientific papers on searchable electronic databases (Web of Science, PubMed, eLIBRARY and ResearchGate) were selected and analyzed. Of the 256 found sources, the authors selected 87, taking into account the keywords, after an analysis of the selected literature, 30 sources were included in the present study in accordance with the topic of the work.Results. On the territory of the Lower Volga region, including the Astrakhan region, two rickettsioses are recorded: rickettsiosis from the tick-borne spotted fevers group — Astrakhan spotted fever (APL) and Q fever (coxiellosis). APL is a relatively new rickettsiosis common in the Caspian Sea basin, along the floodplain of the river Volga to Volgograd, capturing the steppes of Kalmykia. Q fever is recorded in many countries of the world, and in Russia, in terms of its importance and distribution, it occupies one of the first places among endemic diseases. The clinical characteristics of these rickettsioses are also presented.Conclusions. The study of the epidemiology and clinic of rickettsial infections remains relevant.
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Karmazina, Inessa O., Stanislav K. Korb, Andrey P. Mikhailenko, Alexander B. Ruchin, Nikolai V. Shulaev, Leonid V. Egorov et Victor V. Aleksanov. « The last Pleistocene glaciations phylogeography episode of Phaneroptera falcata (Poda, 1761) (Orthoptera : Tettigoniidae) in the Volga River basin based on the mtDNA Cytochrome C Oxidase subunit 1 (COI) gene fragment ». Acta Biologica Sibirica 6 (18 septembre 2020) : 279–91. http://dx.doi.org/10.3897/abs.6.e56139.

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This study is to research the phylogeography of Phaneroptera falcata (Poda, 1761) in the Volga river basin based on the mtDNA Cytochrome C Oxidase subunit 1 (COI) gene fragment at the last Pleistocene glaciation episode. The studied location is the Volga river basin, a territory within the central and partially southern parts of European Russia; it includes the rivers Volga, Oka, Khoper and Don basins. We used the traditional molecular phylogeography methods: mtDNA COI gene fragment from the key locations within the studied area was sequenced and then analyzed (cladogram topology, haplotype diversity, cladogram calibration etc.). The phylogenetic tree shows the dispersion of our samples over the following regions: Lower Volga, Middle Volga, Lower Oka, Middle Oka, Upper Oka, Don basin, Khoper basin. Nine haplotypes determined from our samples; they are grouped into 7 haplogroups. Six of them are in the basins of the main rivers of the Volga region: three haplogroups - on the Oka (Upper, Middle and Lower Oka respectively), haplogroups of the Khoper and Don basins, and the haplogroup of the Middle Volga combining two subgroups – Lower and Middle Volga basins. The distribution of found haplogroups correlates with big river basins in the Volga area (Volga, Oka, Khoper, Don).
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Korolev, Alexey A., Djamila F. Amirova et Maxim V. Tokarev. « SOME ASPECTS OF THE ISLAMIC «RENAISSANCE» IN POST-SOVIET RUSSIA IN THE LATE 1980s – 1990s (based on materials from the Central Volga Region) ». Historical Search 1, no 4 (25 décembre 2020) : 45–51. http://dx.doi.org/10.47026/2712-9454-2020-1-4-45-51.

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The article describes the content and forms of the «revival» of Islam in the Middle Volga region – an increase in the number of mosques, the training and training of ministers of the Islamic cult, the restoration of the system of Muslim education and education, etc.; the practice of interaction between authorities and believers in the conditions of post-Soviet Russia is considered. The significant role of the Muslim mass media in the process of the revival of Islam is analyzed. The newspapers in the Tatar language, for the most part, were of a cultural and educational nature and were intended for a reader who is actively interested in the traditions of his people. Compact living with the Russians and, as a result, some Russification of the Tatars on the territory of the Middle Volga region became the main reason that Muslim newspapers were published in whole or in part in Russian. Initially, there were virtually no analytical materials in the Muslim publications, the information was presented somewhat one-sided, the bulk of the publications were devoted to the description or explanation of religious rites, etc. Virtually all Islamic newspapers were loyal to federal and local authorities. The process of reviving Muslim education is also considered. Almost in all regions of compact residence of Muslims, secondary, higher and special religious educational institutions were established. The Islamic «renaissance» proceeded at a slower pace than the Orthodox, and, first of all, in the Middle Volga region, since the local party and Soviet authorities were characterized by strong inertia, misunderstanding of the processes taking place; there were no corresponding serious spiritual structures and organizations that could become the initiators and implementers of new tasks. Islam in post-Soviet Russia existed fundamentally in different conditions than in the Russian Empire or the USSR. The relationship between the muftis – leaders of the Spiritual Directorates of Muslims and the federal authorities – was characterized by constancy and certainty. Representatives of the Islamic cult were represented in almost all high government levels in the country. At the turn of 20th – 21st centuries. Islam in the Middle Volga region did not become a serious factor of political socialization and a component of the political culture of the Tatar-Muslim ethno-confessional groups.
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Seleznevа, A. V., et I. S. Dedovа. « Morphogenetic analysis of erosion topography the right Volga river bank (Volgograd region, Russia) ». Geomorphology RAS, no 4 (8 novembre 2019) : 88–101. http://dx.doi.org/10.31857/s0435-42812019488-101.

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The article is devoted to a detailed morphogenetic analysis of erosion topography of the right Volga river bank (Volgograd region, Russia). The estimation of the factors in the development of erosion processes: lithological, geomorphological, climatic, biotic. It is established that the general trends of the development and the propagation of gully systems depend on the zonal conditions, and their specificity from structural-lithological and geomorphological features of the area. The actual basis for the work, based on data from field observations, interpretation of satellite imagery, morphometric processing of topographic maps. The obtained results were used for compiling maps, morphometric characteristics of the relief and zoning of the right bank of the Volgograd city according to the intensity of erosion processes. It was established that the studied area is among the most erosion-affected territories in the European part of Russia with the average erosion density of the network from 0.10.3 up to 34 km/km2. Comparison of factors determining the intensity of the evolution and morphology of gully systems led to the conclusion that modern intensification of erosion is the result of economic activities.
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Podshivalina, V. N., et N. G. Sheveleva. « First record of Sinodiaptomus sarsi (Copepoda : Calanoida) from the East European Plain ». Zoosystematica Rossica 29, no 1 (28 avril 2020) : 60–69. http://dx.doi.org/10.31610/zsr/2020.29.1.60.

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The calanoid copepod species Sinodiaptomus sarsi (Rylov, 1923) is recorded from the East European Plain (the Sura River floodplain, Middle Volga Region, Russia) for the first time. A brief description and illustrations of the species are provided, and some differences between its European and Asian populations are revealed. The studied population of S. sarsi from the Sura River basin is mostly similar in morphological characters to populations from China and Japan.
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Dronin, G. « PLANTS FROM RED BOOK OF RUSSIA IN THE SYZRANKA RIVER BASIN (MIDDLE VOLGA REGION) ». Bulletin of the Moscow State Regional University (Natural sciences), no 5 (2015) : 20–25. http://dx.doi.org/10.18384/2310-7189-2015-5-20-25.

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Vakalova, E. V., A. M. Butenko, T. V. Vishnevskaya, T. E. Dorofeeva, A. K. Gitelman, L. N. Kulikova, D. K. Lvov et S. V. Alkhovsky. « Results of investigation of ticks in Volga river delta (Astrakhan region, 2017) for Crimean-Congo hemorrhagic fever virus (Nairoviridae, Orthonairovirus, CCHFV) and other tick-borne arboviruses ». Problems of Virology, Russian journal 64, no 5 (20 octobre 2019) : 221–28. http://dx.doi.org/10.36233/0507-4088-2019-64-5-221-228.

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Introduction. There are natural foci of Crimean-Congo hemorrhagic fever (CCHF) that vectored by Hyalomma marginatum ticks in Volga river delta (Astrakhan region, South of Russia). The circulation of Dhori virus (DHOV) (Thogotovirus: Orthomyxoviridae) has been also shown here. We hypothesized that other tick-borne arboviruses are also likely to circulate in the region. In particular, Bhanja virus (Phlebovirus: Phenuiviridae), Wad Medani virus (Orbivirus: Reoviridae), and Tamdy virus (Orthonairovirus: Nairoviridae), which were found to circulate in neighboring regions and are vectored by Haemaphysalis spp., Dermacenter spp., and Hyalomma spp. ticks.Goals and objectives. The aim of the study was to examine ixodid ticks in Volga river delta for the presence of CCHFV, DHOV, Bhanja virus, Wad Medani virus, and Tamdy virus.Material and methods. Ticks were collected in Volga river delta in 2017. We used molecular genetic methods for the detection and analysis of nucleic acids (PCR, sequencing, phylogenetic analysis).Results. We detect CCHFV and DHOV RNA in H. marginatum ticks. The rate of infected H. marginatum ticks was 1.98% for CCHFV and 0.4% for DHOV. The results of genetic analysis showed that found DHOV strains are almost identical (99- 100% in the M gene) and forms a separate genetic lineage alongside of Batken virus from Central Asia. At the same time, Bhanja virus, Wad Medani virus, and Tamdy virus were not found in ticks, collected in this region.Conclusions. DHOV is circulating in the natural foci of CCHF in the Volga river delta. The ratio of infection of H. marginatum with CCHFV and DHOV was determined for the first time.
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Boldyreva, Ekaterina. « Glazed pottery of the Eastern origin in the South part of the Eastern Europe. The main types and sourses of production ». Rossiiskaia arkheologiia, no 4 (décembre 2021) : 82–92. http://dx.doi.org/10.31857/s086960630015281-8.

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The article focuses on the analysis of glazed ware imported into the southern regions of Russia from the Early Middle Ages to the Golden Horde period. The author studied most common types of glazed ware and their sources. In order to compare, the paper considers the groups of ware brought to the Pontic and the Volga River regions. From the 7th century in the northern Pontic region, vessels produced in Constantinople appeared. Various groups of Byzantine pottery were recorded there till the beginning of the Golden Horde period. In the Caspian region, glazed ware appeared not earlier than the middle-late 9th – early 10th century coming there from Central Asia and the Middle East. In the 11th century, there were no significant changes in the sources and number of imported products in the Pontic, while the Volga River region falls under the influence of the North-Eastern Caucasus, Transcaucasia and the Middle East (mainly Iran). In the second half – end of the 12th century, the Volga region was becoming one of the key areas points in the trade of kashi ware of Middle Eastern origin. In the 14th century, Byzantine ware first appeared there. The same period was marked with the rise in local pottery production in the Pontic and Azov littoral which contributed to the spread of these products throughout Eastern Europe.
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Thèses sur le sujet "Russification – Volga River Region (Russia)"

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ZEMTSOVA, Oxana. « Russification and educational policies in the Middle Volga Region (1860-1914) ». Doctoral thesis, 2014. http://hdl.handle.net/1814/34847.

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Defence date: 13 January 2014
Examining Board: Professor Stephen Anthony Smith, University of Oxford /EUI (Supervisor); Professor Alexander Etkind, EUI Professor; Alexei Miller, CEU Budapest; Professor Boris Kolonitskii, European University in St. Petersburg.
First made available online on 26 February 2015.
The dissertation investigates the Russification policy of the late-imperial Russian state, as it related to educational policy in the Middle Volga region. It seeks to understand how the tsarist authorities sought to define Russianness and how they sought to craft relations with pagan minorities and Muslims in a region where the Slavic-Orthodox, the Turkic-Islamic and the Finno-pagan worlds interacted. It asks how far the educational projects of the Orthodox missions and the secular authorities brought about Russification. The analysis of the changes in imperial policy in the period between the 1860s to 1914 allows for the conclusion that the methods, instruments and aims of Russification policy continually changed and that policy was applied quite differently vis-à-vis the Muslim and pagan, or in most cases only superficially Orthodox , population of the region. When dealing with the educational project for the non-Muslim population in the region, also known as the project of N.Ilminskii, the dissertation aims to understand how the russifying and missionary components related to each other. Furthermore, it studies the alternative educational projects aiming at Russification of the non-Russian population of the region that the Ilminskii system had to compete with. A considerable amount of the dissertation is devoted the discussion of the Muslim reform movement and emergence of Jadidism. By analyzing and comparing the curricula of old-method madrasahs and the new-methods ones, the dissertation demonstrates the evolution that the Middle Volga Muslims underwent under the influence of both inner reforms and the actions of the authorities.
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Uriková, Lucie. « Role řeky Volhy v sebeidentifikaci obyvatel Horního Povolží v 19. století ». Master's thesis, 2021. http://www.nusl.cz/ntk/nusl-448814.

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In my master thesis I deal with the issue of the identity of 19th century Russian society and the role of the Volga River in it. I focus on the characterization of Russian identity in the broadest sense, on the relationship of human society to nature, and on two case studies from the Upper Volga region. In the theory of Russian identity I consider four of its characteristic features - ambivalence, patriotism, spirituality and sentimentalism - to be crucial. The analysis of the relationship between human society and nature includes a section devoted to the reasons for human attachment to landscape, discusses the concept of national landscapes, and presents the dominant idea of the Russian landscape at the end of the 19th century. The last section is devoted to research on the role of the Volga River in the self-identification of the inhabitants of the Upper Volga region. In a study of the worship of the source of the Volga and in research on folklore, I note the attitude of various influences towards this river and, on this basis, define the place of the Volga River in the life of different social classes. The conclusion of my study is that the role of the Volga River in the life of the Upper Volga inhabitants was in many ways the same as its role in the national social discourse, but quite out of...
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Livres sur le sujet "Russification – Volga River Region (Russia)"

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Ėtnokonfessionalʹnyĭ faktor v istorii Saratovskogo Povolzhʹi︠a︡ (1860--2000-e gody). Saratov : Saratovskiĭ gosudarstvennyĭ sot︠s︡ialʹno-ėkonomicheskiĭ universitet, 2013.

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Golod v Povolzhʹe, 1919-1925 gg. : Proiskhozhdenie, osobennosti, posledstvii︠a︡ : monografii︠a︡. Volgograd : Volgogradskoe nauchnoe izdatelʹstvo, 2007.

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Syzranov, A. V. Islam v Nizhnem Povolzhʹe : Monografii︠a︡. Astrakhanʹ : Izdatelʹskiĭ dom "Astrakhanskiĭ universitet', 2012.

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Trade and economic contacts between the Volga and Kama Rivers region and the classical world. Oxford, England : Archaeopress, 2015.

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Lost and found in Russia : Encounters in the deep heartland. London : I.B. Tauris, 2009.

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Richards, Susan. Lost and found in Russia : Encounters in the deep heartland. London : I.B. Tauris, 2009.

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Susan, Richards. Lost and found in Russia : Encounters in the deep heartland. London : I.B. Tauris, 2009.

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Mendi︠u︡kov, A. V. Russkai︠a︡ pravoslavnai︠a︡ t︠s︡erkovʹ v Srednem Povolzhʹe na rubezhe XIX-XX vekov. Samara : Samarskiĭ gos. tekhnicheskiĭ universitet, 2007.

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Russkai︠a︡ pravoslavnai︠a︡ t︠s︡erkovʹ v Srednem Povolzhʹe na rubezhe XIX-XX vekov. Samara : Samarskiĭ gos. tekhnicheskiĭ universitet, 2007.

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Gábor, Bálint. Wolgatatarische Dialektstudien : Textkritische Neuausgabe der Originalsammlung von G. Bálint 1875-76. Budapest : Library of the Hungarian Academy of Sciences, 1988.

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Actes de conférences sur le sujet "Russification – Volga River Region (Russia)"

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КУЗНЕЦОВА, В. Н. « Zoomorphic Pendants of the First Third of the II Millenium A.D. from Upper Volga Region ». Dans Тверь, тверская земля и сопредельные территории в эпоху средневековья. Crossref, 2019. http://dx.doi.org/10.25681/iaras.2018.978-5-9906508-3-1.12-22.

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В статье рассматриваются полые и пластинчатые зооморфные подвески, найденные на памятниках Верхнего Поволжья первой трети II тыс. н.э. Отмечается сходство значительного количества типов, распространенных в Верхневолжье и на северных окраинах Древней Руси. Стилистика некоторых находок является синкретичной; выделяются элементы близкие прикамской и прибалтийской изобразительным традициям. The article deals with hollow and open-work zoomorphic pendants of the first third of the II millenium A.D. found in cultural property sites of Upper Volga region. There is certain resemblance between a considerable amount of types which prevail in Upper Volga region and northern regions of Old Russia. Some of the findings have stylistics of syncretic nature. They include elements similar to decorative traditions of the Kama River area and Baltic.
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Trunilina, Vera. « VOLCANOGENIC FORMATION OF THE UYANDINO-YASACHNAYA MAGMATIC ARC IN THE MIDSTREAM OF THE INDIGIRKA RIVER (VERKHOYANSK-KOLYMA OROGENIC REGION) ». Dans 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/1.1/s01.007.

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The Uyandino-Yasachnaya magmatic arc is the largest volcanic-plutonic belt in the north-east of Russia. However, there is yet to be a consensus on the nature of the arc, despite a long study of the rocks composing it. Most researchers consider it to be an island arc formation, however, some researchers also believe that it of a riftogenic or heterogeneous nature. The arc is composed of volcanogenic-sedimentary strata of variegated composition and associated subvolcanic formations. The rocks were formed during the Oxfordian-Volgian stage; their formation either preceded that of the Late Jurassic-Early Cretaceous granitoid massifs, or was synchronous with it. The research focused on volcanogenic and subvolcanic formations of the southeastern part of the arc in the midstream of the Indigirka River. The purpose of the research was to determine their composition and geodynamic conditions of formation. For this purpose, the study of the structure of volcanogenic strata and sub-volcanoes, their petrographic and chemical compositions, relations with granitoids was carried out. The volcanogenic strata within the territory are represented by two formations of rhyolite and their clastolavas: low-alkaline tholeiitic Oxfordian-Kimmeridgian formation and calcalkaline Medium Kimmeridgian � Early Volgian formation. The lower formation developed in the island-arc setting the upper formation developed under transitional conditions of the island-arc to the marginal-continental regime. The subvolcanic massifs have a dacite-rhyodacite composition; they intrude volcanogenic strata of both these suites and are metamorphosed near the contacts of the Early Cretaceous massifs. Their parental melt was produced at the boundary of amphibolite and dacite-tonalite substrates at maximum temperature (up to 1050oC) and pressure (up to 11.1 kbar). They are of Middle or Late Volga age and formed in the initial stages of the development of the active margin of the continent.
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