Last glacial ecology and geoarchaeology of the Central Trans-Ural area: the Sosva River Upper Palaeolithic Complex, western Siberia

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F70883521%3A28160%2F11%3A00000894" target="_blank" >RIV/70883521:28160/11:00000894 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.1111/j.1502-3885.2010.00166.x" target="_blank" >http://dx.doi.org/10.1111/j.1502-3885.2010.00166.x</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1111/j.1502-3885.2010.00166.x" target="_blank" >10.1111/j.1502-3885.2010.00166.x</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Last glacial ecology and geoarchaeology of the Central Trans-Ural area: the Sosva River Upper Palaeolithic Complex, western Siberia

Popis výsledku v původním jazyce

Quaternary and geoarchaeology studies from the eastern limits of the Ural Mountains provide multiple lines of evidence of the Palaeolithic peopling of this geographically marginal and still poorly explored territory of western Siberia following the mid-last glacial (MIS 3) warming. A complex of investigated open-air localities in the Sosva River basin (the north-central Trans-Ural area) at the periphery of the western Siberian Plain, distinguished by very high concentrations of Pleistocene megafaunal remains previously regarded as "mammoth cemeteries", indicate, in conjunction with the associated diagnostic ivory/bone and stone industry, open occupation sites during the Last Glacial (MIS 2). Fossil faunal remains, dominated by mammoth (98%) together with bird and fish species, indicate various methods of exploitation of the Late Pleistocene natural resources and successful behavioural adaptation to the last glacial sub-polar tundra-steppe environment. The taphonomy and composition of t

Název v anglickém jazyce

Last glacial ecology and geoarchaeology of the Central Trans-Ural area: the Sosva River Upper Palaeolithic Complex, western Siberia

Popis výsledku anglicky

Quaternary and geoarchaeology studies from the eastern limits of the Ural Mountains provide multiple lines of evidence of the Palaeolithic peopling of this geographically marginal and still poorly explored territory of western Siberia following the mid-last glacial (MIS 3) warming. A complex of investigated open-air localities in the Sosva River basin (the north-central Trans-Ural area) at the periphery of the western Siberian Plain, distinguished by very high concentrations of Pleistocene megafaunal remains previously regarded as "mammoth cemeteries", indicate, in conjunction with the associated diagnostic ivory/bone and stone industry, open occupation sites during the Last Glacial (MIS 2). Fossil faunal remains, dominated by mammoth (98%) together with bird and fish species, indicate various methods of exploitation of the Late Pleistocene natural resources and successful behavioural adaptation to the last glacial sub-polar tundra-steppe environment. The taphonomy and composition of t

Druh

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

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

—

Projekt

—

Návaznosti

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Rok uplatnění

2011

Kód důvěrnosti údajů

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

Název periodika

BOREAS

ISSN

0300-9483

e-ISSN

—

Svazek periodika

40

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

US - Spojené státy americké

Počet stran výsledku

15

Strana od-do

146-160

Kód UT WoS článku

000285752900011

EID výsledku v databázi Scopus

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