The Berelekh Mammoth “Graveyard”: New Chronological and Stratigraphical Data from the 2009 Field Season

To clarify unanswered questions of site formation, geology and the archaeology of the Berelekh geoarchaeological complex, a special survey was undertaken in 2009 of the area surrounding the site. Several geological units have been revealed. By establishing the spatial and temporal relationship of th...

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Published in:Geoarchaeology
Main Authors: Pitulko, Vladimir V., Basilyan, Aleksandr E., Pavlova, Elena Y.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2014
Subjects:
Online Access:http://dx.doi.org/10.1002/gea.21483
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spelling crwiley:10.1002/gea.21483 2024-06-09T07:45:38+00:00 The Berelekh Mammoth “Graveyard”: New Chronological and Stratigraphical Data from the 2009 Field Season Pitulko, Vladimir V. Basilyan, Aleksandr E. Pavlova, Elena Y. 2014 http://dx.doi.org/10.1002/gea.21483 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fgea.21483 https://onlinelibrary.wiley.com/doi/pdf/10.1002/gea.21483 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Geoarchaeology volume 29, issue 4, page 277-299 ISSN 0883-6353 1520-6548 journal-article 2014 crwiley https://doi.org/10.1002/gea.21483 2024-05-16T14:25:10Z To clarify unanswered questions of site formation, geology and the archaeology of the Berelekh geoarchaeological complex, a special survey was undertaken in 2009 of the area surrounding the site. Several geological units have been revealed. By establishing the spatial and temporal relationship of these deposits—as well as their age—we have reconstructed the formation history of the Berelekh bone bed. The mammoth bone deposit belongs to a paleochannel. Radiocarbon dating of mammoth remains at Berelekh demonstrates rapid accumulation during the Bølling warming. Human involvement in its formation is, at best, questionable, since there is no real overlap between the radiocarbon dates associated with past human activity, and those of the mammoth bone bed. This study confirms that humans used mammoth bone remains after the bone bed was deposited. Culturally, the Berelekh “site” does not have any relationship to the so‐called “Dyuktai culture.” Instead, the Berelekh archaeological finds (side notched stone pendants) show certain similarities to non‐microblade terminal Pleistocene assemblages found from Yenisei to Kamchatka. Additionally, the Berelekh complex presents a clear analogy with lithics found in Eastern Beringia. Teardrop‐shaped incomplete bifaces found in the assemblage are comparable to the Chindadn points of Alaska. The nature of this “Chindadn connection” is intriguing but it is the only visible cultural link between Western and Eastern Beringia. Article in Journal/Newspaper Dyuktai culture Kamchatka Alaska Beringia Wiley Online Library Teardrop ENVELOPE(163.917,163.917,-78.150,-78.150) Geoarchaeology 29 4 277 299
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description To clarify unanswered questions of site formation, geology and the archaeology of the Berelekh geoarchaeological complex, a special survey was undertaken in 2009 of the area surrounding the site. Several geological units have been revealed. By establishing the spatial and temporal relationship of these deposits—as well as their age—we have reconstructed the formation history of the Berelekh bone bed. The mammoth bone deposit belongs to a paleochannel. Radiocarbon dating of mammoth remains at Berelekh demonstrates rapid accumulation during the Bølling warming. Human involvement in its formation is, at best, questionable, since there is no real overlap between the radiocarbon dates associated with past human activity, and those of the mammoth bone bed. This study confirms that humans used mammoth bone remains after the bone bed was deposited. Culturally, the Berelekh “site” does not have any relationship to the so‐called “Dyuktai culture.” Instead, the Berelekh archaeological finds (side notched stone pendants) show certain similarities to non‐microblade terminal Pleistocene assemblages found from Yenisei to Kamchatka. Additionally, the Berelekh complex presents a clear analogy with lithics found in Eastern Beringia. Teardrop‐shaped incomplete bifaces found in the assemblage are comparable to the Chindadn points of Alaska. The nature of this “Chindadn connection” is intriguing but it is the only visible cultural link between Western and Eastern Beringia.
format Article in Journal/Newspaper
author Pitulko, Vladimir V.
Basilyan, Aleksandr E.
Pavlova, Elena Y.
spellingShingle Pitulko, Vladimir V.
Basilyan, Aleksandr E.
Pavlova, Elena Y.
The Berelekh Mammoth “Graveyard”: New Chronological and Stratigraphical Data from the 2009 Field Season
author_facet Pitulko, Vladimir V.
Basilyan, Aleksandr E.
Pavlova, Elena Y.
author_sort Pitulko, Vladimir V.
title The Berelekh Mammoth “Graveyard”: New Chronological and Stratigraphical Data from the 2009 Field Season
title_short The Berelekh Mammoth “Graveyard”: New Chronological and Stratigraphical Data from the 2009 Field Season
title_full The Berelekh Mammoth “Graveyard”: New Chronological and Stratigraphical Data from the 2009 Field Season
title_fullStr The Berelekh Mammoth “Graveyard”: New Chronological and Stratigraphical Data from the 2009 Field Season
title_full_unstemmed The Berelekh Mammoth “Graveyard”: New Chronological and Stratigraphical Data from the 2009 Field Season
title_sort berelekh mammoth “graveyard”: new chronological and stratigraphical data from the 2009 field season
publisher Wiley
publishDate 2014
url http://dx.doi.org/10.1002/gea.21483
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fgea.21483
https://onlinelibrary.wiley.com/doi/pdf/10.1002/gea.21483
long_lat ENVELOPE(163.917,163.917,-78.150,-78.150)
geographic Teardrop
geographic_facet Teardrop
genre Dyuktai culture
Kamchatka
Alaska
Beringia
genre_facet Dyuktai culture
Kamchatka
Alaska
Beringia
op_source Geoarchaeology
volume 29, issue 4, page 277-299
ISSN 0883-6353 1520-6548
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/gea.21483
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