Raw material as fossile directeur? A case study of the use of Stránská skála-type chert
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68081758%3A_____%2F21%3A00551210" target="_blank" >RIV/68081758:_____/21:00551210 - isvavai.cz</a>
Výsledek na webu
<a href="https://doi.org/10.31577/szausav.2021.suppl.2.14" target="_blank" >https://doi.org/10.31577/szausav.2021.suppl.2.14</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.31577/szausav.2021.suppl.2.14" target="_blank" >10.31577/szausav.2021.suppl.2.14</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Raw material as fossile directeur? A case study of the use of Stránská skála-type chert
Popis výsledku v původním jazyce
The Stránská skála-type chert is a local Moravian chert of Jurassic age, which is available only within a limited area restricted to the Stránská skála rock outcrop and secondary sources in nearby gravels. As this raw material has been well-studied petrographically, its distribution is easy to trace. Its use and proportions within individual archaeological assemblages in particular vary over time – ranging from the dominant raw material during several chrono-cultural periods to a complete absence of this raw material in other periods. Periods of significant use include the Initial and Early Upper Palaeolithic, Late Neolithic and Early Eneolithic. Less pronounced evidence of distribution is also known from the Late/Final Eneolithic and from the Early Bronze Age. Periods of no use include the Middle to Late Upper Palaeolithic, Early – Middle Neolithic and Middle Eneolithic. This raw material was mostly used locally with a limited distribution – the maximum extent of its occurrence is a few tens of kilometres from the source outcrop. The Stránská skála-type chert should be accepted as a fossile directeur sensu lato thanks to its easy determination and the isolation of the outcrop in combination with the techno-typological analysis.
Název v anglickém jazyce
Raw material as fossile directeur? A case study of the use of Stránská skála-type chert
Popis výsledku anglicky
The Stránská skála-type chert is a local Moravian chert of Jurassic age, which is available only within a limited area restricted to the Stránská skála rock outcrop and secondary sources in nearby gravels. As this raw material has been well-studied petrographically, its distribution is easy to trace. Its use and proportions within individual archaeological assemblages in particular vary over time – ranging from the dominant raw material during several chrono-cultural periods to a complete absence of this raw material in other periods. Periods of significant use include the Initial and Early Upper Palaeolithic, Late Neolithic and Early Eneolithic. Less pronounced evidence of distribution is also known from the Late/Final Eneolithic and from the Early Bronze Age. Periods of no use include the Middle to Late Upper Palaeolithic, Early – Middle Neolithic and Middle Eneolithic. This raw material was mostly used locally with a limited distribution – the maximum extent of its occurrence is a few tens of kilometres from the source outcrop. The Stránská skála-type chert should be accepted as a fossile directeur sensu lato thanks to its easy determination and the isolation of the outcrop in combination with the techno-typological analysis.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
60102 - Archaeology
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2021
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Študijné zvesti Archeologického ústavu Slovenskej akadémie vied
ISSN
0560-2793
e-ISSN
—
Svazek periodika
2021
Číslo periodika v rámci svazku
Supplementum 2
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
18
Strana od-do
213-230
Kód UT WoS článku
000756151800014
EID výsledku v databázi Scopus
2-s2.0-85123777047