Detailed Information on Publication Record
2015
Dolní Věstonice IIa: Gravettian microstratigraphy, environment, and the origin of baked clay production in Moravia
SVOBODA, Jiří, Šárka HLADILOVÁ, Ivan HORÁČEK, Jozef KAISER, Miroslav KRÁLÍK et. al.Basic information
Original name
Dolní Věstonice IIa: Gravettian microstratigraphy, environment, and the origin of baked clay production in Moravia
Authors
SVOBODA, Jiří (203 Czech Republic, guarantor, belonging to the institution), Šárka HLADILOVÁ (203 Czech Republic, belonging to the institution), Ivan HORÁČEK (203 Czech Republic), Jozef KAISER (203 Czech Republic), Miroslav KRÁLÍK (203 Czech Republic, belonging to the institution), Jan NOVÁK (203 Czech Republic), Martin NOVÁK (703 Slovakia), Petr POKORNÝ (203 Czech Republic), Sandra SÁZELOVÁ (203 Czech Republic, belonging to the institution), Libuše SMOLÍKOVÁ (203 Czech Republic) and Tomáš ZIKMUND (203 Czech Republic)
Edition
Quaternary International, 2015, 1040-6182
Other information
Language
English
Type of outcome
Článek v odborném periodiku
Field of Study
Archaeology, anthropology, ethnology
Country of publisher
United Kingdom of Great Britain and Northern Ireland
Confidentiality degree
není předmětem státního či obchodního tajemství
Impact factor
Impact factor: 2.067
RIV identification code
RIV/00216224:14310/15:00082059
Organization unit
Faculty of Science
UT WoS
000350997500017
Keywords in English
Dolní Věstonice; Early Gravettian; Microstratigraphy; Environment; Burnt clay; Czech Republic
Tags
International impact, Reviewed
Změněno: 5/4/2016 16:03, Ing. Andrea Mikešková
Abstract
V originále
Creating an overall scheme of Gravettian stratigraphy and chronology in the Middle Danube area is a matter of current debate. This paper addresses the formation of microstratigraphies at large open-air sites, evidence of the earliest Gravettian occupation in the Dolní Vestonice-Pavlov area, and occurrence of early ceramics from this context. The case presented here is a complex early Gravettian microstratigraphy of charcoal deposits at Dolní Vestonice IIa with a sequence of AMS dates between 28.4 and 31.7 ka uncal BP (30-33 ka cal BC) and two middle Gravettian (Pavlovian) dates from the nearby living floor. The associated environmental evidence of charcoal, pollen, molluscs, and vertebrates shows that climatic development through the six horizons was relatively stable, but with a certain variability in moisture and extension of forest. In horizon 3c, the molluscs and both small and large vertebrates indicate an episode of restricted forest formation around 28.4 ka uncal BP (30-31 ka cal BC). Baked clay (ceramic) fragments from horizon 3c represent the earliest dated items of this kind in the Gravettian. Microstratigraphies of this type demonstrate the complexity of cultural deposits at the large Gravettian sites and throw light on the hitherto poorly understood time-period of the early Gravettian in Moravia.
Links
ED1.1.00/02.0068, research and development project |
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EE2.3.20.0181, research and development project |
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