scholarly journals Cultural background and chronology of the multisegment populated settlement Salekhard-4 located in the Lower Ob River region

2019 ◽  
Vol 8 (4) ◽  
pp. 131-138
Author(s):  
Olga Sergeevna Tupakhina ◽  
Daniel Sergeevich Tupakhin
Keyword(s):  
Bronze Age ◽  
Middle Ages ◽  
Northern Taiga ◽  
The Arctic ◽  
Late Bronze Age ◽  
13Th Century ◽  
Ob River ◽  
Taiga Forest ◽  
River Region ◽  
Cultural Layers

In this paper the authors study the issues of the cultural and chronological attribution of the Salekhard-4 settlement, the historic site, which was studied during the field works in 2017 for the first time. The site is located within the Salekhard city territory. Considering the vast historical and landscape context it should be noted that the territory of the Lower Ob River region (within the area of the modern Yamalo-Nenets Autonomous Okrug) includes several natural ranges: Northern taiga, forest tundra and tundra, and geographically spreads up to the Arctic coast. Moreover, it should be outlined that the historical retrospective displays multiple shifts of borders of the abovesaid nature and climatic ranges both, south and the northward, and such shifts affected migration of the ancient population considerably, which is clearly reflected on the archaeological remains. For instance the lower cultural layers of the Salekhard-4 settlement should be referred to the Chalcolithic Period (end of the 4th - beginning of the 3rd thousand years AD); this can be confirmed by the found ceramics referred to the Gorny Samotnel settlement. The cultural layers discovered above and containing the settlement and the burial complexes can be attributed to the Heyakh culture of the Late Bronze age (approx. 13th century AD). One of the tombs partially containing relics and remains is the subject of special interest as it contains the unviolated funeral accessories. The unique nature of this finding is that for today it is the only Late Bronze age burial located in the region under study. Undamaged condition of the antropological material made it possible to establish the sex and the race of the buried, as well as to determine the approximate age at death. The upper cultural layers of the site under study can be referred to the culture of the Lower Ob River region of the early Middle Ages (1st-4th centuries DC), they contain residuals of a wooden flooring, a fire-forge, and some amount of ceramics.

scholarly journals THE BEGINNING OF THE IRON AGE AT ARSLANTEPE: A 14C PERSPECTIVE

Radiocarbon ◽  
2021 ◽  
pp. 1-19
Author(s):  
Federico Manuelli ◽  
Cristiano Vignola ◽  
Fabio Marzaioli ◽  
Isabella Passariello ◽  
Filippo Terrasi
Keyword(s):  
Mass Spectrometry ◽  
Bronze Age ◽  
High Precision ◽  
Iron Age ◽  
Accelerator Mass Spectrometry ◽  
Late Bronze Age ◽  
13Th Century ◽  
Historical Events ◽  
Preliminary Results ◽  
Archaeological Data

ABSTRACT The Iron Age chronology at Arslantepe is the result of the interpretation of Luwian hieroglyphic inscriptions and archaeological data coming from the site and its surrounding region. A new round of investigations of the Iron Age levels has been conducted at the site over the last 10 years. Preliminary results allowed the combination of the archaeological sequence with the historical events that extended from the collapse of the Late Bronze Age empires to the formation and development of the new Iron Age kingdoms. The integration into this picture of a new set of radiocarbon (14C) dates is aimed at establishing a more solid local chronology. High precision 14C dating by accelerator mass spectrometry (AMS) and its correlation with archaeobotanical analysis and stratigraphic data are presented here with the purpose of improving our knowledge of the site’s history and to build a reliable absolute chronology of the Iron Age. The results show that the earliest level of the sequence dates to ca. the mid-13th century BC, implying that the site started developing a new set of relationships with the Levant already before the breakdown of the Hittite empire, entailing important historical implications for the Syro-Anatolian region at the end of the 2nd millennium BC.

scholarly journals Alalakh: an account of the excavations at Tell Atchana in the Hatay, 1937–1949

2004 ◽  
Author(s):  
Leonard Woolley
Keyword(s):  
Bronze Age ◽  
Large Scale ◽  
River Valley ◽  
Early Bronze Age ◽  
Late Bronze Age ◽  
13Th Century ◽  
Gold Silver

This monograph describes large-scale excavations undertaken by Sir Leonard Woolley from 1937 to 1939, and again from 1946 to 1949, at the site of Alalakh (modern Tell Atchana) – a late Bronze Age city in the Amuq River valley of Turkey's Hatay Province. Described is the evidence of a series of superimposed palaces and temples, town defences, private houses and graves, in 17 archaeological levels reaching from late Early Bronze Age (Level XVII, c. 2200–2000 BC to Late Bronze Age (Level 0, 13th century BC). Supplementary reports describe the architecture and frescoes, sculptures, and portable objects in fired clay, gold, silver, ivory, stone, and glass.

CERAMICS OF THE PESTRYAKOVO LAKE SETTLEMENT (SOUTH OF WESTERN SIBERIA)

2021 ◽  
Vol 27 ◽  
pp. 205-212
Author(s):  
KIRYUSHIN K. ◽  
◽  
KIRYUSHIN Yu. ◽  
Keyword(s):  
Organic Matter ◽  
Bronze Age ◽  
Middle Ages ◽  
Iron Age ◽  
Western Siberia ◽  
Early Iron Age ◽  
Late Bronze Age ◽  
The South ◽  
Animal Hair ◽  
The Middle Ages

The article is devoted to the publication of finds of fragments of ceramic dishes discovered at the settlement of Pestryakovo Lake (Zavyalovsky district of Altai Territory). A group of ceramics which belongs to the early Iron Age and the Middle Ages, is pointed out. Single fragments find analogies in the materials of the sites of the Early and Late Bronze Age. The ceramic collection of the Pestryakovo Lake settlement includes groups of ceramics that belong to the Neolithic or Eneolithic. These are fragments of vessels ornamented with prints of a “string”, pricks, imprints of a short comb stamp, a dingle-dingle stamping. Linear-pricked and receding-pricked ceramics are quite informative. On the outer and inner surfaces, as well as in the fractures, traces of burnt-out organic matter (animal hair) are recorded. Such ceramics are widely represented in the south of Western Siberia and are associated with various settlement and burial complexes from the Ob to the Irtysh and various cultural formations of the Neolithic and Eneolithic. Keywords: settlement, ceramics, ornamentation technique, comparative typological analysis, neolithic, eneolithic

Holocene evolution of closed depressions and its relation to landscape dynamics in the loess areas of Poland

The Holocene ◽  
2019 ◽  
Vol 29 (4) ◽  
pp. 543-564 ◽  
Author(s):  
Renata Kołodyńska-Gawrysiak
Keyword(s):  
Land Use ◽  
Soil Erosion ◽  
Bronze Age ◽  
Middle Ages ◽  
Central Europe ◽  
Iron Age ◽  
Landscape Dynamics ◽  
Early Iron Age ◽  
Late Bronze Age ◽  
Atlantic Period

Past Pleistocene topography of the loess uplands is rich in local sinks (closed depressions (CDs)) influencing sediment fluxes. Soil-sediment sequences from CDs constituting geoarchives where landscape changes under natural and anthropogenic conditions have been recorded. Pedo-sedimentary archives from 10 CDs in the Polish loess belt and human settlements were analysed. Phases of the Holocene evolution of the CDs were correlated with landscape dynamics in loess areas in Poland and Central Europe. Phases of infilling of CDs occurring (2) from the late Boreal/early Atlantic Period until the (middle) late Bronze Age/early Iron Age and (4) since the early Middle Ages until today were documented. These were phases of long-term soil erosion and colluviation corresponding to the increasing agricultural land use of Polish loess uplands. Phases of soil formation related to geomorphic stabilization of CDs occurred (1) from the late Vistulian until the late Boreal/early Atlantic Period and (3) from the late Bronze Age/early Iron Age until the early/high Middle Ages. These were phases of decreased soil erosion and landform conservation in a considerable part of Poland’s loess areas. Pedo-sedimentary archives from the CDs have recorded soil erosion strongly related with human-induced land-use changes. The mean soil erosion rate in the catchment of CDs was 0.33 t·ha−1·yr−1 during prehistory and 4.0 t·ha−1·yr−1 during the last approximately 1000 years. Phases of CD evolution are representative for the main phases of sediment and landscape dynamics in Poland’s loess areas recorded in various archives, and are not synchronous with some of these phases in Central Europe.

Revisiting the Fosse Temple at Tel Lachish

2017 ◽  
Vol 17 (1) ◽  
pp. 64-75 ◽  
Author(s):  
Ido Koch
Keyword(s):  
Bronze Age ◽  
The Self ◽  
Late Bronze Age ◽  
13Th Century ◽  
History Of ◽  
Cultural World

This paper reconsiders the Late Bronze Age history of the Fosse Temple at Lachish and reconstructs its context vis-à-vis the broader role of the local Canaanite cult. During the reign of Amenhotep iii the structure’s plan was modified to conform to Egyptian-style and there was a profusion of Egyptian imports to the site, primarily associated with the cult of Hathor. These facts reflect the cultic innovations that were taking place in Egypt itself—the self-deification of Amenhotep iii and his consort, Tiye, including her depiction and worship as Hathor. It is consequently argued that the translation of Hathor/Tiye into the local goddess, Elat, and its continuous practice until the late 13th century bc echo the integration of Egypt within the indigenous cultural world.

scholarly journals Sedimentation and vegetation history of a buried Meuse terrace during the Holocene in relation to the human occupation history (Limburg, the Netherlands)

2016 ◽  
Vol 96 (2) ◽  
pp. 131-163 ◽  
Author(s):  
Frieda S. Zuidhoff ◽  
Johanna A.A. Bos
Keyword(s):  
Bronze Age ◽  
Middle Ages ◽  
Human Activities ◽  
Vegetation History ◽  
Roman Period ◽  
Early Holocene ◽  
Late Bronze Age ◽  
The Holocene ◽  
River Terraces ◽  
Main River Channel

AbstractDuring several archaeological excavations on a river terrace of the river Meuse near the village of Lomm (southeast Netherlands) information was gathered for a reconstruction of the sedimentation and vegetation history during the Holocene. Various geoarchaeological methods – geomorphological, micromorphological and botanical analyses – were applied, while accelerator mass spectrometry (AMS) 14C and optically stimulated luminescence (OSL) dating provided an accurate chronology for the sediments.During the Early Holocene, many former braided river channels were deepened due to climate amelioration. Later, river flow concentrated in one main river channel to the west, at the location of the modern Meuse. The other channels were only active during floods, and infilling continued until the Bronze Age. Because of the higher setting of the Lomm terrace, it was only occasionally flooded and therefore formed an excellent location for habitation. Humans adapted to the changing landscape, as most remains were found on the higher river terraces or their slopes, a short distance from the Maas river. The Lomm terrace was more or less continuously inhabited from the Mesolithic onwards.During the Early Holocene, river terraces were initially densely forested with birch and pine. From the Boreal (Mesolithic) onwards, dense mixed forests with deciduous shrubs and trees such as hazel, oak, elm and lime developed. During the Atlantic (Meso/Neolithic), the deciduous forests became dominated by oak. Due to human activities from the Late Subboreal (Late Bronze Age) onwards, forests slowly became more open, yet remained relatively dense in comparison to other Dutch areas. The botanical data, however, show that within the Lomm study area there was a large difference in the composition, distribution and openness of the vegetation. The spatial variation in openness came into existence during the Late Bronze Age, as soon as the higher areas started to be used for human activities (i.e. habitation, agriculture and livestock herding). Due to human activities, the northern part of the study area became very open during the Early Roman period. In the lower-situated areas of the southern part, however, forests remained present much longer, until the Early Middle Ages. Due to large-scale deforestation in the Lomm area and hinterland during the Roman period and Middle Ages, the sediment load of the river increased, large floods occurred and overbank sediments were deposited, burying the archaeological remains. The largest increase in sedimentation occurred after the Middle Ages.

scholarly journals Distribution of Yellow Wagtail Forms Motacilla flava – Complex in the North of Western Siberia, Russia

2017 ◽  
Vol 10 (1) ◽  
pp. 1-9
Author(s):  
Mikhail G. Golovatin ◽  
Vasiliy A. Sokolov
Keyword(s):  
Western Siberia ◽  
Northern Taiga ◽  
Yamal Peninsula ◽  
Yellow Wagtail ◽  
Forest Tundra ◽  
Ob River ◽  
North East ◽  
The North ◽  
Taiga Forest ◽  
Shrub Tundra

On the basis of the materials obtained from the studies carried out from 2000 to 2015, we present the data on distribution of the Yellow Wagtail forms in the north of Western Siberia, i.e. within the overlapping boundaries of the ranges of a complex set of several polytypical forms – Motacilla flava sensu lato. Four forms have been identified here: two forms from the group of Western Yellow Wagtails (M. f. thunbergi and M. f. beema & flava) and two forms from the group of Eastern Yellow Wagtails (M. t. plexa and M. t. tschutschensis). Western “black-headed” form M. f. thunbergi is spread in the area of the northern taiga, forest tundra and south shrub tundra within the Ob River basin, while eastern “black-headed” form M. t. plexa is found in the shrubby tundra and further to the east from the Ob River in forest tundra and northern taiga. Western “light headed” wagtails M. f. beema & flava spread as far as 65º05'N along the floodplain of the Ob River. Eastern “light-headed” wagtail M. t. tschutschensis penetrates the Taz peninsula and, through the anthropogenic sites, the north-east coast of the Yamal Peninsula, i.e. the Sabetta area as far as 71º14'N. The entire range of the Yellow Wagtail is characterized by the interchange of zones inhabited by “black-headed” (without the expressed eyebrows on males) and “light-headed” (with notable eyebrows on males or white-headed) forms from the north to the south.

New cereal grain finds from southern Satakunta, Finland, dated from the Late Bronze Age to the Middle Ages

2020 ◽  
pp. 145-154
Author(s):  
Terttu Lempiäinen ◽  
Maija Helamaa ◽  
Heli Lehto ◽  
Ulla Moilanen ◽  
Markku Oinonen ◽  
...  
Keyword(s):  
Bronze Age ◽  
Middle Ages ◽  
Late Bronze Age ◽  
Cereal Grain ◽  
The Middle Ages

scholarly journals SETTLEMENT BARSOVA GORA II/42 (NEOLITHIC, ENEOLITHIC AND BRONZE AGE COMPLEXES)

2021 ◽  
Vol 3 (2) ◽  
pp. 122-136
Author(s):  
Е.N. Dubovtseva ◽  
Keyword(s):  
Bronze Age ◽  
River Bank ◽  
Oil Companies ◽  
Ob River ◽  
Neolithic Age ◽  
Unique Object ◽  
Cultural Layers ◽  
Cultural Types ◽  
High Bank ◽  
The Neolithic Age

The settlement Barsova Gora II/42 is located in Khanty-Mansiysk Autonomous Okrug-Yugra, 15 km west of Surgut, on the high bank of the Ob' River. The settlement is being actively destroyed due to the activities of oil companies. More than 20 objects and structures were investigated in 2011 during rescue excavations, some of them are pits of ancient dwellings (sites 1, 2, 6, 15, 19), some are household outbuildings and pits (sites 3, 4, 7, 8, 9, 10, 11, 13, 14, 16, 17, 18, 20), two objects have a cult purpose (sites 5, 12). An important feature of the monument is that archaeological structures of different epochs and cultures overlap each other, allowing us to trace the sequence of settlement of this part of the Ob River bank. During the Neolithic Age the constructions of Bystrinsky and Barsovogorsky cultural types were located here, the cultural layers containing ceramics of Vakhovsky type belong to the Eneolithic Age, and the constructions and household pits of Kulugansky type belong to the Bronze Age. An ochre storage pit and a ring ochre structure represent a unique object, which is probably related to ancient rituals. The revealed objects (Nos. 15, 19, 18, 2, 1, 5, 17, 13) are partially investigated and require further excavations.

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