A.A. Sementsov
Russian Academy of Sciences
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Featured researches published by A.A. Sementsov.
Radiocarbon | 2001
A.Yu. Alekseev; N.A. Bokovenko; Yu. Boltrik; K.A. Chugunov; Gordon Cook; V. A. Dergachev; N. Kovalyukh; G. Possnert; van der Johannes Plicht; E.M. Scott; A.A. Sementsov; Vadim Skripkin; Sergei K. Vasiliev; G.I. Zaitseva
The paper is compares the chronology of the monuments of the Scythian epoch located in the east and west of the Eurasian steppe zone on the basis of both archaeological and radiocarbon data. The lists of 14 C dates for the monuments located in different parts of Eurasia are presented according to the periods of their existence. Generally, the 14 C dates are confirmed the archaeological point of view and allow us to compare the chronological position of the European and Asian Scythian monuments on the united 14 C time scale.
Radiocarbon | 1997
G.I. Zaitseva; S.S. Vasiliev; L.S Marsadolov; van der Johannes Plicht; A.A. Sementsov; V. A. Dergachev; L.M. Lebedeva
We present a radiocarbon chronology of key Sayan-Altai monuments from the Scythian period, based on a statistical analysis of dates produced in the 1980s and now supplemented with new dates. These new (super 14) C dates were produced for samples from the Tuekta-1 barrows (burial mounds) and were measured both in St. Petersburg and Groningen. These tree-ring samples were fitted to the calibration curve. Chronologies were established for the Arzhan, Tuekta-1 and Pazyryk-5 barrows. The time of the construction of the Arzhan and Pazyryk-5 barrows is the 9th and late 5th-4th centuries BC, respectively, and agrees with archaeology. According to new data obtained, the time of the Tuekta-1 barrow construction is some years older than has been accepted thus far by archaeologists.
Radiocarbon | 1997
A.A. Sementsov; G.I. Zaitseva; J. Görsdorf; A. Nagler; H. Parzinger; N.A. Bokovenko; K.V. Chugunov; L.M. Lebedeva
We present here new radiocarbon dates for the different barrows (burial mounds) of the nomadic tribes of the Scythian period in the Khakassia and Tuva regions (Central Asia). The time scale of these barrows is compared with the elite barrows of the Sayan-Altai. In agreement with archaeological evidence, some barrows in Khakassia are chronologically close in time to the Arzhan barrow. The first (super 14) C dates produced for the barrows from the Tuva region belong to a later Scythian period, compared with the elite Arzhan barrow. We determined the final stage of the barrow construction, but to establish the starting time, more dates are necessary (both by dendrochronology and (super 14) C).
Radiocarbon | 2007
V.G. Dirksen; B. van Geel; M.A. Koulkova; G.I. Zaitseva; A.A. Sementsov; E.M. Scott; Gordon Cook; van der Johannes Plicht; L.M. Lebedeva; N.D. Bourova; N.A. Bokovenko
Two sediment sequences from Big Kyzykul Lake and the Shushenskoe paleolake in the Minusinsk depression, Southern Siberia, were studied by pollen, microfossil, and geochemical analyses, as well as radiocarbon dating. The records indicate the persistence of an arid period between ~11.77.6 cal kyr BP, increased effective moisture since ~7.6 cal kyr BP, 2 humid impulses at ~5.1 and 2.8 cal kyr BP separated by a dry interval, and the return to generally drier conditions after ~1.5 cal kyr BP. This is contrary to the findings noted for the Eurasian temperate zone, but agrees with proxy data reported for arid and semi-arid zones of Central Asia. Reconstructed changes in climate and environment are in good agreement with archaeological data. Almost no evidence of the Mesolithic-Neolithic cultures has been reported for the depression, which is consistent with a dry early and mid-Holocene. Effective moisture started to rise from ~7.6 cal kyr BP, followed by the beginning of human occupation at ~6 cal kyr BP. Two maxima of humidity are recorded in the late Holocene, corresponding to the arrival of trees in the depression. No gap was to be found from the Early Bronze to the Iron ages cultures at this time, with the exception of a dry interval at ~3.63.3 cal kyr BP, when the Minusinsk depression was sparsely occupied. The data obtained suggest a close relationship between climate change and cultural dynamics in the steppe zone of Southern Siberia.
Radiocarbon | 2007
G.I. Zaitseva; K.V. Chugunov; A.Yu. Alekseev; V. A. Dergachev; S.S. Vasiliev; A.A. Sementsov; Gordon Cook; E.M. Scott; van der Johannes Plicht; H. Parzinger; A. Nagler; H. Jungner; E Sonninen; N.D. Bourova
This paper focuses on the chronological study of 2 Scythian period monuments that are the key to the chronology of the entire Eurasian Scythian culture. These are the unique monuments of Arzhan-1 and Arzhan-2 in Central Asia (Tuva Republic). The dating of both these monuments began immediately after their discovery, but discussion about their chronological position is still current. Both monuments contained considerable wooden material from their construction suitable for dendrochronology and radiocarbon dating. The first results for the Arzhan-1 barrow were obtained by wiggle-matching in 20042005, while the Arzhan-2 barrow was first dated in 2003. It is now possible to compare the chronological position of these barrows using the same methods. As postulated earlier, Arzhan-1 is the oldest Scythian period monument and is dated to the boundary of the 89th centuries BC. The position of the Arzhan-2 monument stretches to the middle of the 7th century BC. d13C values for annual tree rings in logs from both barrows were also determined to gain a better understanding of the climatic conditions at the time of barrow construction.
Radiocarbon | 2004
G.I. Zaitseva; K.V. Chugunov; V. A. Dergachev; A. Nagler; G Parzinger; E.M. Scott; A.A. Sementsov; Sergei K. Vasiliev; B. van Geel; van der Johannes Plicht; L.M. Lebedeva
The first radiocarbon dates from the unique early Scythian monument Arzhan-2, discovered in 2001, are presented. The monument contained a royal burial (grave nr 5). Unfortunately, precise dating is hampered by the Hallstatt plateau in the calibration curve. However, using both accelerator mass spectrometry measurements from buried materials and conventional dates for floating tree rings from the burial chamber, we were able to date the construction of the monument to the 7th century BC. This is consistent with archaeological expectations. Other graves located inside the barrow were also dated. Grave nr 11, located on the edge of the barrow, is younger, showing that the monument was a place of burial ritual for many years for this ancient population.
Radiocarbon | 1997
G.I. Zaitseva; Göran Possnert; Andrey Yu. Alekseev; V. A. Dergachev; A.A. Sementsov
The first radiocarbon dates for the famous monuments of European Scythia were produced for the Kelermes, Seven Brothers, Solocha and Chertomlyk barrows (burial mounds) by both accelerator mass spectrometry (AMS) and conventional methods. The obtained (super 14) C dates confirmed the traditional archaeological chronology, which was based on the analysis of written data and typological comparisons of Scythian artifacts with similar objects found in the Ancient East and Greece. The (super 14) C dates for the European Scythian monuments are compared with the Asian ones. The (super 14) C chronology of the European Scythian monuments shows chronological synchronisms between the Asiatic and European monuments. The calibrated ages for the investigated barrows generally agree with the archaeological data.
Radiocarbon | 1997
G.I. Zaitseva; V. A. Dergachev; Vladimir L. Timofeev; A.A. Sementsov
A large number of (super 14) C dates for archaeological sites in European Russia have been entered into a new database. The database includes >1500 dates for ca. 500 archaeological sites. Because European Russia is a very large area, the database includes subdivisions of territories and regions. We analyzed our (super 14) C dates according to archaeological periods (Paleolithic through Medieval period) and made a comparison with environmental (climatic) parameters. Our database for archaeological sites and monuments offers new possibilities for correlation between the development of ancient cultures and natural-climatic processes.
Radiocarbon | 2009
G.I. Zaitseva; S V Pankova; S.S. Vasiliev; V. A. Dergachev; E.M. Scott; A.A. Sementsov; H. Jungner; E Sonninen
The present research is focused on the dating of the Oglakhty burial ground, the key site of stage I of the Tashtyk culture. Despite the numerous well-preserved burials of that type investigated at the Oglakhty complexes, their chronological position has remained unclear. From the early 20th century until the present, 2 different time periods had been identified for the Tashtyk burials: (1) from the 1st century BC until the 1st century AD and (2) from the 1st until the 2nd century AD. New data obtained in the 1990s suggested a different age for Tashtyk burials, namely the 3rd-4th centuries AD. This considerable shift in chronology needed to be checked with independent data. The chronological position of one of the Oglakhty burials, tomb 4, has been investigated with the use of wiggle-matching, applied to wooden logs used in the construction of tomb 4. The resulting dates for this burial strongly suggest its age as being limited to the 3rd-4th centuries AD, which is corroborated by the archaeological dates of the imported artifacts found in the grave and which is in agreement with the chronological position of the Oglakhty site, as proposed by previous investigations.
Geochronometria | 2002
A.Yu. Alekseev; N.A. Bokovenko; Yu. Boltrik; K.A. Chugunov; Gordon Cook; V. A. Dergachev; N. Kovaliukh; G. Possnert; van der Johannes Plicht; E.M. Scott; A.A. Sementsov; V. Skripkin; S.S. Vasiliev; G.I. Zaitseva