scholarly journals Postglacial history of East European boreal forests in the mid‐Kama region, pre‐Urals, Russia

Boreas ◽  
2020 ◽  
Vol 49 (3) ◽  
pp. 526-543 ◽  
Author(s):  
Lyudmila S. Shumilovskikh ◽  
Monika Schmidt ◽  
Mikhail Pereskokov ◽  
Pavel Sannikov
Keyword(s):  
Boreal Forests ◽  
East European ◽  
Postglacial History ◽  
History Of

Muscovy and the Tatars

2020 ◽  
Vol 54 (4) ◽  
pp. 403-431
Author(s):  
Bulat R. Rakhimzianov
Keyword(s):  
Seventeenth Century ◽  
Social Institutions ◽  
The Political ◽  
East European ◽  
Central Eurasia ◽  
History Of ◽  
Mutual Relations ◽  
Forest Line ◽  
The Relationship

Abstract This article explores relations between Muscovy and the so-called Later Golden Horde successor states that existed during the fifteenth and sixteenth centuries on the territory of Desht-i Qipchaq (the Qipchaq Steppe, a part of the East European steppe bounded roughly by the Oskol and Tobol rivers, the steppe-forest line, and the Caspian and Aral Seas). As a part of, and later a successor to, the Juchid ulus (also known as the Golden Horde), Muscovy adopted a number of its political and social institutions. The most crucial events in the almost six-century-long history of relations between Muscovy and the Tatars (13–18th centuries) were the Mongol invasion of the Northern, Eastern and parts of the Southern Rus’ principalities between 1237 and 1241, and the Muscovite annexation of the Kazan and Astrakhan khanates between 1552 and 1556. According to the model proposed here, the Tatars began as the dominant partner in these mutual relations; however, from the beginning of the seventeenth century this role was gradually inverted. Indicators of a change in the relationship between the Muscovite grand principality and the Golden Horde can be found in the diplomatic contacts between Muscovy and the Tatar khanates. The main goal of the article is to reveal the changing position of Muscovy within the system of the Later Golden Horde successor states. An additional goal is to revisit the role of the Tatar khanates in the political history of Central Eurasia in the fifteenth and sixteenth centuries.

Palestine and Genocide: An International Historical Perspective Revisited

2013 ◽  
Vol 12 (1) ◽  
pp. 1-7 ◽  
Author(s):  
Martin Shaw
Keyword(s):  
Historical Perspective ◽  
Settler Colonialism ◽  
Holy Land ◽  
Unique Combination ◽  
East European ◽  
History Of

This commentary reviews the responses to an earlier article, ‘Palestine in an International Historical Perspective on Genocide’ (Holy Land Studies, 9:1, 1–25), arguing that they illustrate both the possibilities and the limitations of serious debate about these issues. The responses mostly neglected the analytical core of the argument relating to 1948, which is therefore restated, emphasising Palestine's unique combination of elements that were parts of three general patterns implicated in genocide production (settler colonialism, East European nationalism, conflicts of decolonisation). The paper also gives further attention to the implications of the perspective for understanding the ‘genocide’ question in the subsequent history of the Israel-Palestine conflict.

scholarly journals History of sports medicine in east European countries

2015 ◽  
Vol 68 (1-2) ◽  
pp. 59-65
Author(s):  
Biljana Lazovic ◽  
Sanja Mazic ◽  
Marina Djelic ◽  
Jelena Suzic-Lazic ◽  
Radmila Sparic ◽  
...  
Keyword(s):  
Sports Medicine ◽  
Medical Knowledge ◽  
European Countries ◽  
Historical Background ◽  
Eastern European ◽  
Cultural Changes ◽  
East European ◽  
Psychological Pressure ◽  
History Of ◽  
Eastern European Countries

The purpose of this article is to provide a historical background of medicine, science and sports with the focus on the development of modern sports medicine in European countries, with an accent on Eastern European countries that have a long sports medicine tradition. The development of modern sports medicine began at the end of 19th and the beginning of 20th century, and it has been associated with social and cultural changes in the world of medicine, science and sports. Advanced medical knowledge, skills and practices, and the progress of scientific achievements enabled sports people to improve their performance level. Increased popularisation and commercialisation of sports have resulted from urbanization and city lifestyle, leading to the lack of physical activity and increased psychological pressure. In addition, the growing need and interest in sports and successes in professional sports have become a symbol of international recognition and prestige for the nations.

Going West

2011 ◽  
Vol 25 (4) ◽  
pp. 785-791 ◽  
Author(s):  
Tara Zahra
Keyword(s):  
Twentieth Century ◽  
Eastern Europe ◽  
Minority Rights ◽  
European History ◽  
East European ◽  
European Context ◽  
The World ◽  
History Of

“Going West” explores the potential of integrating East European History into broader histories of Europe and the world. Placing the history of Eastern Europe in a European context, I argue, may enable us to challenge the tropes of backwardness, pathology, and violence that still dominate the field. I also suggest that historians explore the extent to which conceptions of minority rights, development, and humanitarianism first developed in Eastern Europe radiated beyond the region in the twentieth century.

Vegetation and climate history of Quebec’s mixed boreal forest suggests greater abundance of temperate species during the early- and mid-Holocene

Botany ◽  
2018 ◽  
Vol 96 (7) ◽  
pp. 437-448 ◽  
Author(s):  
Émilie Larochelle ◽  
Martin Lavoie ◽  
Pierre Grondin ◽  
Pierre-Luc Couillard
Keyword(s):  
Boreal Forests ◽  
Regional Scale ◽  
Plant Macrofossils ◽  
Habitat Characteristics ◽  
Temperate Species ◽  
White Pine ◽  
Yellow Birch ◽  
Climate History ◽  
History Of ◽  
Suitable Habitats

Today, scattered disjunct stands of two temperate species, yellow birch and white pine, are present north of their continuous distributional range in southern Quebec (Canada) at topographical locations that offer protection from severe fires. This study tested whether these species had populations more numerous and widespread millennia ago when the climate was presumably warmer. Specifically, this research involved the analyses of pollen, plant macrofossils, and charcoal fragments of two sites within the western part of Quebec’s balsam fir – paper birch bioclimatic domain: a forest humus deposit from a yellow birch stand (local scale), and a peatland (regional scale). Fossil data suggest that white pine was more abundant regionally between 7500 and 5000 cal. BP, before coming rare under subsequent cooler conditions. Likewise, yellow birch was more abundant regionally between 7700 and 1500 cal BP. Its subsequent decline and the local disappearance of white pine by ∼200 cal. BP may both be explained by the severe fires that occurred in recent centuries, as well as the rarity of suitable habitats for these species. The sustained presence of temperate species in mixed boreal forests is the result of the combined action of climate, natural disturbances and habitat characteristics.

scholarly journals Montenegro as perceived by a British diplomat: The Hugh Rose's report of 1852.

Balcanica ◽  
2002 ◽  
pp. 211-226
Author(s):  
Cedomir Antic
Keyword(s):  
Nineteenth Century ◽  
British Empire ◽  
Foreign Relations ◽  
Balance Of Power ◽  
Political Elite ◽  
Crimean War ◽  
East European ◽  
Short Period ◽  
History Of ◽  
European Periphery

The following article deals with the image of Montenegro, a little country from the south-east European periphery, as perceived by a member of the nineteenth century British political elite. The history of this petty entity, less populated than an average English city, became especially important on the eve of the Holly Places Crises (of Palestine, 1853). A single dispute over the Montenegro-Ottoman border threatened to turn into European war, just a year before the Crimean War commenced. In regard the Montenegrin question, the always sensitive European "balance of power" was upset with the appearance of the unexpected alliance between Russia and Austria. The unique interest of the British Empire then started, for a short period of time, to be tied in with this almost unknown principality. The attitude of British diplomacy to Montenegro, image of the principality reconstructed in the Colonel Hugh Rose's report and its sources, could contribute not only to the advance the history of British foreign relations, but also to the development of the history of Montenegro.

scholarly journals Chronology of the Last Deglaciation in the Southeastern Baltic Region on the Basis of Recent OSL Dates

2010 ◽  
Vol 36 (-1) ◽  
pp. 47-54 ◽  
Author(s):  
Anto Raukas ◽  
Wojciech Stankowski ◽  
Vitālijs Zelčs ◽  
Petras Šinkunas
Keyword(s):  
Outer Zone ◽  
East European Plain ◽  
Last Deglaciation ◽  
Baltic Region ◽  
East European ◽  
The North ◽  
Dating Methods ◽  
History Of ◽  
Close Cooperation ◽  
The Last Deglaciation

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.

Palynology and Paleoecology of Postglacial Sediments from the Lower Fraser River Canyon of British Columbia

1975 ◽  
Vol 12 (5) ◽  
pp. 745-756 ◽  
Author(s):  
R. W. Mathewes ◽  
G. E. Rouse
Keyword(s):  
Tsuga Heterophylla ◽  
Climatic Conditions ◽  
Douglas Fir ◽  
Fraser River ◽  
Pollen Assemblage ◽  
Glacial Ice ◽  
Transitional Area ◽  
Postglacial History ◽  
History Of Vegetation ◽  
History Of

The postglacial history of vegetation in the Yale area of the lower Fraser River Canyon is described from sediments of two lakes using percentage pollen analysis supplemented with macrofossil evidence and radiocarbon dating. Deposition of postglacial sediments, ranging from basal clays to gyttjas, began about 11 500 y B.P. Three distinct pollen assemblage zones are distinguished, reflecting in part the main climatic conditions for the intervals. The oldest zone, with high percentages of pine (Pinus) and alder (Alnus) pollen, suggests cool and moist conditions following withdrawal of glacial ice. This is followed by marked increases in Douglas-fir (Pseudotsuga), grasses and other nonarboreal pollen, suggesting in part, warmer and drier conditions. The third zone, ranging from about the Mt. Mazama ash at 6600 y B.P. to the present, is marked by high alder and Douglas-fir, and increasing cedar (Thuja-Chamaecyparis type), western hemlock (Tsuga heterophylla), fir (Abies) and birch; an assemblage indicating a return to wetter conditions. This sequence contrasts with previously described successions that recognized the classical Hypsithermal in adjacent areas. The sequence of inferred vegetational changes, although similar to those described for the Haney area to the west, suggests that the Yale area has been a biogeoclimatically transitional area for much of postglacial time.

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