Siberia: Paleolithic

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F70883521%3A28160%2F14%3A43872427" target="_blank" >RIV/70883521:28160/14:43872427 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.1007/978-1-4419-0465-2" target="_blank" >http://dx.doi.org/10.1007/978-1-4419-0465-2</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/978-1-4419-0465-2" target="_blank" >10.1007/978-1-4419-0465-2</a>

Result language
angličtina
Original language name
Siberia: Paleolithic
Original language description
Siberia is a territory of 13.1 mil km2 encompassing the northern part of Asia east of the Ural Mountains to the Pacific coast (the Far East). This vast area has major significance for documenting the evolutionary processes of initial human settlement inthe frame of past climates and climate change in the boreal and (circum-)polar regions of the Northern Hemisphere. Particularly, the central continental areas in the transitional subarctic zone between the northern Siberian lowlands south of the Arctic Ocean and the southern Siberian mountain systems characterized by a strongly continental climate regime have been subjected to multidisciplinary Quaternary (palaeoecological and geoarchaeological) investigations during the last decades. Siberia is also the principal territory for trans-continental studies and correlations of geological climate proxy records across Eurasia following the East-West and South-North geographic transects. Among them, loess (fine aeolian dust) represents, togeth
Czech name
—
Czech description
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Publication year
2014
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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