scholarly journals Chronology of Prehistoric Cultural Complexes of Sakhalin Island (Russian Far East)

Radiocarbon ◽  
2004 ◽  
Vol 46 (1) ◽  
pp. 353-362 ◽  
Author(s):  
Yaroslav V Kuzmin ◽  
Alexander A Vasilevski ◽  
Sergei V Gorbunov ◽  
G S Burr ◽  
A J Timothy Jull ◽  
...  

A chronological framework for the prehistoric cultural complexes of Sakhalin Island is presented based on 160 radiocarbon dates from 74 sites. The earliest 14C-dated site, Ogonki 5, corresponds to the Upper Paleolithic, about 19,500–17,800 BP. According to the 14C data, since about 8800 BP, there is a continuous sequence of Neolithic, Early Iron Age, and Medieval complexes. The Neolithic existed during approximately 8800–2800 BP. Transitional Neolithic-Early Iron Age complexes are dated to about 2800–2300 BP. The Early Iron Age may be dated to about 2500–1300 BP. The Middle Ages period is dated to approximately 1300–300 BP (VII–XVII centuries AD).

Radiocarbon ◽  
2018 ◽  
Vol 60 (5) ◽  
pp. 1611-1620 ◽  
Author(s):  
Yaroslav V Kuzmin ◽  
Vsevolod S Panov ◽  
Viacheslav V Gasilin ◽  
Sergei V Batarshev

ABSTRACTNew paleodietary data were obtained after the discovery and excavation in 2015–2017 of the Cherepakha 13 site in the southern part of Primorye (Maritime) Province in far eastern Russia. The site is located near the coast of Ussuri Bay (Sea of Japan) and belongs to the Yankovsky cultural complex of the Early Iron Age 14C-dated to ca. 3000 BP (ca. 1200 cal BC). The stable isotope composition of the bone collagen for 11 humans and 30 animals was determined. For humans, the following values (with±1 sigma) were yielded: δ13C=–10.2±0.8‰; and δ15N=+12.4±0.3‰. The majority of terrestrial animals show the usual isotopic signals: δ13C=–19.4 ÷ –23.3‰; and δ15N=+4.6÷+6.6‰ (for wolves, up to +10.1‰); dogs, however, have an isotopic composition similar to humans: δ13C= –11.7±1.2‰; and δ15N=+12.4±0.4‰. Marine mammals have common values for pinnipeds: δ13C=–13.7 ÷ –14.6‰; and δ15N=+17.4 ÷ +18.0‰. The main food resources for the population of Cherepakha 13 site were (1) marine mollusks, fish, and mammals; and (2) terrestrial mammals; and possibly C4 plants (domesticated millets).


Author(s):  
KIRYUSHIN K. ◽  
◽  
KIRYUSHIN Yu. ◽  

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


2013 ◽  
pp. 111-118
Author(s):  
Darko Radmanovic ◽  
Desanka Kostic ◽  
Jelena Lujic ◽  
Svetlana Blazic

After decades-long vertebrate fauna research, out of 42 archaeological sites in Vojvodina (Serbia) from different periods ranging from the Neolithic to the Middle Ages, remains of birds were registered at 17 sites (4 from the Neolithic, 1 from the Early Iron Age, 7 from the Late Iron Age, 5 from the Roman Period, 1 from the Migration Period, and 4 from the Middle Ages). A total of 14 species and 4 genera were registered for this vertebrate class. The richest ornithofauna is from the Neolithic, where 9 species and 3 genera were registered. The Migration and Medieval periods are next with 4 registered species and one genus each. There were 3 species registered from the Roman Period, and 2 species from the Late Iron Age. The poorest ornitofauna was registered from the Early Iron Age, only one species.


Radiocarbon ◽  
1997 ◽  
Vol 40 (2) ◽  
pp. 675-686 ◽  
Author(s):  
Yaroslav V. Kuzmin ◽  
A. J. T. Jull ◽  
Lyobov A. Orlova ◽  
Leopold D. Sulerzhitsky

Ca. 150 unequivocal 14C dates from the prehistoric cultures in the Russian Far East can be used to elucidate chrono-cultural boundaries in that region. Microblade technology started as early as ca. 20,000 bp, and continued to exist in the middle Amur River basin until ca. 10,500 bp, and in Primorye until ca. 7800 bp. The emergence of pottery-making in the lower Amur River basin goes back to ca. 13,300 bp. The transition from Upper Paleolithic to Neolithic took place during the time interval 13,300–7800 bp and pottery was widely spread in the Russian Far East by ca. 6700–8400 bp. The first evidence of shellfish collection is estimated to ca. 6400 bp at Peter the Great Gulf coast, Sea of Japan. The beginning of agriculture in Primorye, based on finding of both millet seeds (Setaria italica L.) and pollen of cultivated cereals (Cerealia), is 14C-dated to ca. 4200–3700 bp (ca. 1980–2900 cal BC). The Neolithic/Early Iron Age boundary was estimated at ca. 3100–3300 bp (1400–1600 cal BC) in the mainland Russian Far East, and to ca. 1800–2300 bp (400 cal BC–200 cal ad) on the Sakhalin and southern Kuril Islands.


2021 ◽  
Vol 20 (5) ◽  
pp. 69-81
Author(s):  
Nikolay I. Drozdov ◽  
Victor P. Leontev ◽  
Dmitry A. Gurulev ◽  
Kseniya V. Biryuleva

Purpose. As a result of preparations for the flooding of the Boguchan Hydroelectric Power Station reservoir bed, the Lower Angara region has witnessed increased activity as an archeological source base in recent years. It initiated the development of studies on the taxonomy of pottery traditions, both in the region and in adjacent territories, their chronology and interaction models. A number of informative archaeological sites at the estuary of the Kova River were excavated in large-scale horizontal exposures. Morphological analysis of the most informative part of the collection of surveys of 2008–2011, its comparative studies and the subsequent analysis of the spatial and stratigraphic context of the wares were the object of this paper. Results. A number of pottery groups were identified and their cultural-chronological attribution was proposed. Pottery of the Middle Ages predominate – Ust’-Kova type vessels, wares decorated with thin and smearing cordons, combed decorated pottery. The period of the Early Iron Age is represented by the Tsepan’ culture pottery, vessels with ‘wisp’ cordons and thin cordons decorated with finger pinches. Morphologically heterogeneous ‘pearl-ribbed’ pottery is attributed to the Bronze Age. Among the Neolithic ceramics, ‘net-impressed’ pottery (including the Aplin type), wares of Posol’sk and Ust’-Belaya types, as well as vessels close to Serovo pottery were presented. The complexes of the Early Iron Age – the Middle Ages have little information content due to the fact that the upper culture-bearing sediments are largely disturbed. There is a tendency toward a shift of site zones from the Angara coast in the Neolithic and Bronze Age to the right bank of the Kova River in subsequent periods. Conclusion. The collection includes wares dating from the Neolithic to the ‘Russian’ time. Conclusions about the information content of materials of cultural layers for further research are made. A subsequent collation of observations on settlement location trends will be able to reveal mobility patterns among carriers of various pottery traditions.


Author(s):  
E. Ershova ◽  
◽  
E. Ponomarenko ◽  
A. Alexandrovskiy ◽  
N. Krenke ◽  
...  

The horizons of slash-and-burn agriculture were distinguished by pedological, anthracological, phytolithic and palynological features. Radiocarbon dates were obtained from the coals. Most of the dates refer to the time of the Great Migration and the Middle Ages. Some of the slash horizons are dated to the Early Iron Age, the earliest are from the Bronze Age and, presumably, the Neolithic.


1994 ◽  
Vol 9 (6) ◽  
pp. 503-513 ◽  
Author(s):  
Natalya B. Verkhovskaya ◽  
Aleksandr S. Kundyshev ◽  
Nikolay A. Kliuev

Radiocarbon ◽  
2007 ◽  
Vol 49 (2) ◽  
pp. 757-766 ◽  
Author(s):  
Yaroslav V Kuzmin

In Siberia, the accumulation of radiocarbon dates from archaeological sites since the 1960s makes it possible to compile a general Paleolithic 14C database, which contains about 440 entries as of late 2005. With these data, we can reveal the main chronological patterns of Paleolithic complexes, with a focus on the late Middle Paleolithic (Mousterian) and Upper Paleolithic. The 14C dates for late Middle Paleolithic industries in Siberia are quite “young,” up to about 30,000–28,500 BP and perhaps ∼27,000 BP. The emergence of the Upper Paleolithic in Siberia took place relatively early compared with Eastern Europe. At about 43,000–35,000 BP, blade-dominated industries existed in the Altai Mountains and Lake Baikal region, and numerous adornments are known from several sites of that age. The late Upper Paleolithic complexes with microblade technology from the Altai Mountains are 14C dated to about 35,000–28,000 BP, and represent the earliest unequivocal evidence of microblade manufacture in northern Eurasia. The end of the Paleolithic in Siberia is related to the appearance of pottery, which indicates the beginning of the Neolithic period. In northern Transbaikal, the earliest pottery complexes are dated to about 12,000–11,000 BP and in the Russian Far East even to ∼13,000 BP, while in most of Siberia they date to approximately 8000–6000 BP. The most important features of the Siberian Paleolithic chronology are: a) the long persistence of Middle Paleolithic complexes, until about 30,000–27,000 BP; b) very early Middle to Upper Paleolithic transition, ∼43,000 BP, closely connected with the emergence of art and symbolic behavior in the earliest Upper Paleolithic at this time; c) the very early origin of microblade complexes, at least at about 35,000 BP; and d) a gradual Paleolithic–Neolithic transition, beginning in the Russian Far East at ∼13,000 BP and in Transbaikal about 12,000–11,000 BP, in most of Siberia at about 8000–6000 BP, and even later in some northern regions.


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