scholarly journals Mediaeval jewellery from the Volga-Kama area in the East-Baltic region

2021 ◽  
Vol 31 ◽  
pp. 227-251
Author(s):  
V. Kuznetsova ◽  
◽  
I. Stasyuk ◽  
Keyword(s):  
Archaeological Sites ◽  
Baltic Region ◽  
The South ◽  
13Th Century ◽  
Ladoga Region ◽  
Old Russian ◽  
North Western ◽  
North Sweden

This paper considers jewellery objects of the Volga-Kama provenience of the 9th–13th century revealed at archaeological sites in the territory of North-Western Russia, Latvia, Estonia, Finland and North Sweden. Groups of Kama and Volga imports are identified for the products characteristic of the Volga-Kama region in general, and for “syncretic” objects of the Old-Russian period combining artistic traditions and techniques of different regions. The article notes the concentration of finds of this kind in the South-East Ladoga region and in Novgorod

The Eastern Baltic

2018 ◽  
Author(s):  
Valter Lang
Keyword(s):  
Material Culture ◽  
Bronze Age ◽  
Iron Age ◽  
Archaeological Sites ◽  
Entire Region ◽  
Baltic Region ◽  
The South ◽  
Burial Practices ◽  
South West ◽  
The Baltic

This chapter examines Iron Age funerary and domestic archaeological sites, and economic and cultural developments from c.500 BC–AD 550/600, in the east Baltic region (present day Estonia, Latvia, and Lithuania). While the early pre-Roman Iron Age was to some extent a continuation of the late Bronze Age in material culture terms, many changes took place in the late pre-Roman Iron Age. At the change of era, new cultural trends spread over the east Baltic region, from the south-eastern shore of the Baltic to south-west Finland, which produced a remarkable unification of material culture over this entire region up to the Migration period. Differences in burial practices and ceramics, however, indicate the existence of two distinct ethnic groups, Proto-Finnic in the northern part of the region and Proto-Baltic to the south. Subsistence was based principally on agriculture and stock rearing, with minor variations in the economic orientation of different areas.

scholarly journals Absolute chronology of the Zedmar culture: Re-thinking radiocarbon dates

2017 ◽  
Vol 44 (1) ◽  
pp. 256-268
Author(s):  
Magdalena Kozicka
Keyword(s):  
Bayesian Analysis ◽  
Statistical Models ◽  
Archaeological Sites ◽  
Baltic Region ◽  
The South ◽  
Radiocarbon Dates ◽  
South Eastern ◽  
Calibration Methods ◽  
Eastern Baltic

Abstract The Zedmar culture is linked with the subneolithic circle of the South-Eastern Baltic region. So far, excavations have been carried out only on seven archaeological sites. Nonetheless, there are quite a lot of radiocarbon measurements. Most of them refer to the stratigraphic contexts. This allows to integrate all of the data into statistical models. With these, it is possible to query some statements about the Zedmar culture origin and its duration. At least as long as placing the Zedmar culture into an absolute timescale may offer any solution to those issues. The idea that radiocarbon dates could provide solutions or even final answers to some arguable questions in prehistorical studies was dropped, as soon as it became clear that in the whole approach the key role is played by calibration methods and the general variability of sampled material. However – thanks to including Bayesian analysis, a better understanding of dated materials and more complex examination of received results – it has been asserted again.

Associations of Sphagnum rubellum Wils. on the bogs of the south-east part of Baltic region

2003 ◽  
pp. 50-61 ◽  
Author(s):  
V. A. Smagin ◽  
M. G. Napreenko
Keyword(s):  
Baltic Sea ◽  
Plant Cover ◽  
Karelian Isthmus ◽  
Baltic Region ◽  
The South ◽  
The Baltic Sea ◽  
Kaliningrad Region ◽  
The Baltic ◽  
Typical Habitat ◽  
New Syntaxa

The paper characterizes the 3 associations comprising plant communities with Sphagnum rubellum in the south-eastern part of the Baltic region. The new syntaxa differ from each other both in their floristic characters and the pronounced affinity to definite regional mire types and particular habitats. The ass. Drosero-Sphagnetum rubelli is typical of the relatively most thorough ranges. It is observed from the Kaliningrad region to the Karelian Isthmus and, according to the published reference, occurs even throughout the whole area around the Baltic Sea. Its most typical habitat is that of margins of mire lakes and pools. The ass. Eriophoro-Sphagnetum rubelli occurs in central plateaus of convex plateau-like bogs, typical of the areas adjacent to the Baltic Sea coast. It occupies extended flat mire ecotopes with the water level 0.2–0.25 m deep. The ass. Empetro-Sphagnetum rubelli is characteristic of the retrogressive complex in the convex bogs of the East-Baltic Province. It is mostly observed along the coast of the Gulf of Finland. Its stands are rather dynamic and unstable in both space and time. The presence of communities comprised by these 3 associations is an important vegetation character of the series of regional mire types. Assuming an association level of the respective syntaxa seems rational for the purposes of adequate reflection of plant cover diversity.

Tupinambine teiids from the middle Miocene of north-western Patagonia (Argentina)

2008 ◽  
Vol 29 (3) ◽  
pp. 425-431 ◽  
Author(s):  
Santiago Brizuela ◽  
Adriana María Albino
Keyword(s):  
Geographical Distribution ◽  
Middle Miocene ◽  
First Record ◽  
South American ◽  
The South ◽  
North Western

Abstract Remains of teiids assignable to the Tupinambinae (Tupinambis sp. or Crocodilurus sp.) are here described from the middle Miocene Collón Curá Formation at Cañadón del Tordillo, in Neuquén province, Argentina. No tupinambine species presently inhabits the region of the fossil locality. The fossils represent the westernmost distribution of fossil tupinambine teiids in Patagonia, enlarging the known geographical distribution of the teiids through the Miocene in a longitudinal range. Also, they constitute the first record of lizards from the Colloncuran SALMA, partially filling the record of tupinambine teiids for the South American Miocene.

scholarly journals Old Russian Graffito Inscription in the Abbey of Saint-Gilles, South of France

Slovene ◽  
2014 ◽  
Vol 3 (2) ◽  
pp. 110-129 ◽  
Author(s):  
Anne-Sophie Brun ◽  
Andreas Hartmann-Virnich ◽  
Estelle Ingrand-Varenne ◽  
Savva M. Mikheev
Keyword(s):  
Western Europe ◽  
Linguistic Analysis ◽  
The South ◽  
Archaeological Investigation ◽  
Southern France ◽  
Santiago De Compostela ◽  
Old Russian ◽  
Medieval Europe

The abbey of Saint-Gilles-du-Gard near Arles in the south of France was one of the most prominent pilgrimage sites in medieval Europe. Recent archaeological investigation has shown that construction of the abbey church, one of the most significant Romanesque pilgrimage churches in southern France, began ca. 1170/1180. The lower church (crypt) with the tomb of St. Giles (Lat. Aegidius, Fr. Gilles) and some of the walls of the upper church belong to that period. A well-preserved Cyrillic graffito was discovered on a pier of the upper church, close to the spot where the tomb of St. Giles is located in the crypt below. The text contains a prayer with a common formula: GI POMЪZI | RABU SVЪ|EMU SЬMKЪ|VI NINOSLA|VICHIU ‘Lord, help your servant Semko, son of Ninoslav.’ Palaeographic and linguistic analysis shows that the graffito is of Russian origin. It was probably made at some time between 1180 and 1250 by a pilgrim travelling from Russia to Santiago de Compostela, and it is the most geographically remote Old Russian graffito inscription discovered so far in western Europe.

scholarly journals Geochronology of granites of the western Korosten AMCG complex (Ukrainian Shield): implications for the emplacement history and origin of miarolitic pegmatites

2021 ◽  
Vol 33 (6) ◽  
pp. 703-716
Author(s):  
Leonid Shumlyanskyy ◽  
Gerhard Franz ◽  
Sarah Glynn ◽  
Oleksandr Mytrokhyn ◽  
Dmytro Voznyak ◽  
...  
Keyword(s):  
Economic Value ◽  
Ukrainian Shield ◽  
Western Region ◽  
The South ◽  
Anorthosite Massif ◽  
Granitic Intrusion ◽  
Plutonic Complex ◽  
Flow Through ◽  
Basic Rocks ◽  
North Western

Abstract. The origin of large miarolitic (also known as “chamber”) pegmatites is not fully understood although they may have great economic value. The formation of cavities in magmatic bodies is related to melt degassing and gas or fluid flow through partially solidified magma. In this paper, the origin of the Volyn pegmatite field, located in the Palaeoproterozoic Korosten anorthosite–mangerite–charnockite–granite (AMCG) complex, North-Western region of the Ukrainian Shield, is discussed. Pegmatites of the field host deposits of piezoelectric quartz that is accompanied by gem-quality beryl and topaz. The Volyn pegmatite field is confined to granites located in the south-western part of the Korosten complex and extends for 22 km along the contact with the anorthosite massif within the Korosten plutonic complex. Geological data indicate hybridization of basic melts and partly crystallized granites, as well as direct impact of fluids derived from basic melts on the chamber pegmatites. The new U–Pb zircon ages obtained for granites and pegmatites of the Korosten complex confirm that the rock assemblage in the northern part of the complex crystallized between 1800 and 1780 Ma, whereas rocks in the southern part intruded mainly between 1768 and 1755 Ma. U–Pb zircon ages for granites from the south-western part of the Korosten complex indicate that granites were emplaced at 1770–1765 Ma, a few million years prior to the intrusion of the gabbro–anorthosite massif (1762–1758 Ma), while chamber pegmatites in these granites crystallized at 1760 ± 3 Ma, coevally with the basic rocks. Ultimately, the formation of the chamber pegmatites was related to the reheating of the semi-crystallized granitic intrusion and to fluids migrating from the underlying gabbro–anorthosite massif.

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