Dolní Věstonice IIa: Gravettian microstratigraphy, environment, and the origin of baked clay production in Moravia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10313973" target="_blank" >RIV/00216208:11310/15:10313973 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/68081758:_____/15:00453287 RIV/60076658:12310/15:43888827 RIV/00216224:14310/15:00082059 RIV/00216208:11620/15:10313973 a 2 dalších

Výsledek na webu

<a href="http://dx.doi.org/10.1016/j.quaint.2014.06.048" target="_blank" >http://dx.doi.org/10.1016/j.quaint.2014.06.048</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1016/j.quaint.2014.06.048" target="_blank" >10.1016/j.quaint.2014.06.048</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Dolní Věstonice IIa: Gravettian microstratigraphy, environment, and the origin of baked clay production in Moravia

Popis výsledku v původním jazyce

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 Dolni 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 Dolni 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 ca

Název v anglickém jazyce

Dolní Věstonice IIa: Gravettian microstratigraphy, environment, and the origin of baked clay production in Moravia

Popis výsledku anglicky

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 Dolni 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 Dolni 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 ca

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

AC - Archeologie, antropologie, etnologie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2015

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Quaternary International

ISSN

1040-6182

e-ISSN

—

Svazek periodika

359

Číslo periodika v rámci svazku

2 March 2015

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

16

Strana od-do

195-210

Kód UT WoS článku

000350997500017

EID výsledku v databázi Scopus

2-s2.0-84923535121