Large scale and regional demographic responses to climatic changes in Europe during the Final Palaeolithic
Jazyk angličtina Země Spojené státy americké Médium electronic-ecollection
Typ dokumentu časopisecké články, historické články
PubMed
40173400
PubMed Central
PMC11964466
DOI
10.1371/journal.pone.0310942
PII: PONE-D-24-39812
Knihovny.cz E-zdroje
- MeSH
- archeologie MeSH
- dějiny starověku MeSH
- hustota populace MeSH
- klimatické změny * dějiny MeSH
- lidé MeSH
- populační dynamika * MeSH
- Check Tag
- dějiny starověku MeSH
- lidé MeSH
- Publikační typ
- časopisecké články MeSH
- historické články MeSH
- Geografické názvy
- Evropa MeSH
The European Final Palaeolithic witnessed marked changes in almost all societal domains. Despite a rich body of evidence, our knowledge of human palaeodemographic processes and regional population dynamics still needs to be improved. In this study, we present regionally differentiated population estimates for the Greenland Interstadial 1d-a (GI-1d-a; 14-12.7 ka cal BP) and the Greenland Stadial 1 (GS-1; 12.7-11.6 ka cal BP) for Southern, Western, Northern and Central Europe. The data were obtained by applying the Cologne Protocol, a geostatistical approach for estimating prehistoric population size and density, to a newly compiled dataset of Final Palaeolithic sites. On a large spatio-temporal scale and compared to preceding Upper Palaeolithic phases, areas north of the Alps become the dominant demographic growth area for the first time since the dispersal of anatomically modern humans into Europe. At smaller scales, we observe divergent regional trends, with a conspicuous lack of archaeological evidence appearing in previously occupied areas of central France and Germany. Our study also shows that during the Final Palaeolithic, the climatic cooling of GS-1 coincides with a pronounced population decline in most parts of the study area. An apparent increase in population density occurs only in north-eastern Central Europe and north-eastern Italy. Our estimates suggest that the total population was reduced by half. Similar results, with a relationship between decreasing temperatures and decreasing populations, have already been observed for the late phase of the Gravettian, when populations were reduced to only one third of those estimated for the early phase. Yet, in contrast to the collapse of local populations during the late Gravettian, the increase in population densities in Central Europe during GS-1 indicates population movements eastwards, possibly in response to deteriorating climatic conditions, particularly in western regions during the Younger Dryas.
Centre for Cultural Anthropology Moravian Museum Brno Czech Republic
CNRS Laboratoire PACEA UMR 5199 Université de Bordeaux Bordeaux France
CNRS UMR 8068 TEMPS MSH MONDES Nanterre France
Department of Archaeology and Heritage Studies Aarhus University Aarhus Denmark
Department of Archaeology Prehistory Research Unit Ghent University Ghent Belgium
Department of Archaeology University of York York United Kingdom
Department of Old World and Asian Studies University Erlangen Nürnberg Erlangen Germany
Faculty of Archaeology Adam Mickiewicz University Poznań Poland
Faculty of Archaeology Leiden University Leiden The Netherlands
Institute of Archaeology of the Czech Academy of Sciences Prague Czech Republic
Institute of Environmental Geology and Geoengineering National Council of Research Milano Italy
Institute of Prehistoric Archaeology University of Cologne Cologne Germany
Leibniz Zentrum für Archäologie Schleswig Germany
Museum for Archaeology Schleswig Holstein State Museums Foundation Schloss Gottorf Schleswig Germany
Muséum national d'Histoire naturelle CNRS HNHP UMR 7194 Paris France
Research bureau Old Land Eindhoven The Netherlands
Stichting STONE Foundation for Stone Age Research in the Netherlands Groningen The Netherlands
University of the Basque Country Faculty of Arts Vitoria Gasteiz Spain
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