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The impact of major warming at 14.7 ka on environmental changes and activity of Final Palaeolithic hunters at a local scale (Orawa-Nowy Targ Basin, Western Carpathians, Poland

Bibliographic Data

ID21196329
AuthorsAnna Lemanik (0000-0002-2523-0940, Institute of Systematics and Evolution of Animals), M Baca (0000-0003-2174-3914, University of Warsaw), Krzysztof Wertz (0000-0001-5993-7330, Institute of Systematics and Evolution of Animals), Paweł Socha (0000-0002-6405-6201), Danijela Popović (0000-0003-1025-3776, University of Warsaw), Teresa Tomek (0000-0002-8278-3031, Institute of Systematics and Evolution of Animals), Grzegorz Lipecki (0000-0003-2650-9385, Institute of Systematics and Evolution of Animals), Anna Kraszewska (0000-0002-3940-9570, Jagiellonian University), Barbara Miękina (0000-0002-1256-3922, Institute of Systematics and Evolution of Animals), Aleksandra Żeromska (0000-0001-5243-6509, University of Wrocław), Andrea Pereswiet-Soltan (0000-0002-2083-0648), Zbigniew Szyndlar (0000-0002-8645-7225, Institute of Systematics and Evolution of Animals), Magda Cieśla (0000-0002-8401-0411, Jagiellonian University), Paweł Valde-Nowak (0000-0003-1023-7389, University of Hradec Králové), Paweł Mackiewicz (0000-0003-4855-497X, University of Wrocław), Adam Nadachowski (0000-0001-6452-3028, Institute of Systematics and Evolution of Animals)
Year2020
Volume12
Issue3
Publication date2020-03-01
Open AccessYes
TypeARTICLE
VenueArchaeological and Anthropological Sciences (JOURNAL)
Journal identifiersISSN: 1866-9557 • E-ISSN: 1866-9565
PublisherSpringer Science and Business Media LLC (PUBLISHER)
DOI10.1007/s12520-020-01020-6
OpenAlexW3005148172
LanguageEN
Citations received7
References cited56

There is a widespread belief that the abrupt warming at 14.7 ka had a profound impact on the environment. However, the direct correlation between the global climatic event and changes in local environments is not obvious. We examined faunal succession in an intra-mountain basin of the Western Carpathians to assess the potential influence of the climatic change between Greenland Stadial-2a and Greenland Interstadial-1e on the local environment. We investigated three vertebrate assemblages (total number of identified specimens = 18,745; minimum number of individuals = 7515; 138 taxa) from Obłazowa Cave (western entrance) and a Rock overhang in Cisowa Rock, radiocarbon dated to the period before and after the global warming, between ca. 17.0 and 14.0 ka. Our data revealed that the major abrupt warming that occurred 14.7 ka had little impact on the local environment, which could suggest that ecosystems in Central Europe were resilient to the abrupt global climate changes. The increase in fauna population sizes and species diversities in local biotopes was gradual and began long before the temperature increase. This was supported by the analysis of ancient DNA of Microtus arvalis , which showed a gradual increase in effective population size after 19.0 ka. The results of palaeoclimatic reconstruction pointed out that the compared sites were characterized by similar climatic conditions. According to our calculations, the differences in the annual mean temperatures did not exceed 0.5 °C and mean annual thermal amplitude changed from 22.9 to 22.4 °C. The environmental changes before 14.7 ka had no impact on the activity of Final Palaeolithic hunters in the studied area

Biology · Cave · Climate change · Ecological succession · Ecosystem · Environmental change · Fauna · Geography · Global warming · Holocene · Holocene climatic optimum · Physical geography · Population · Radiocarbon dating · Stadial · Structural basin · Archaeology and ancient environmental studies · Geology and Paleoclimatology Research · Pleistocene-Era Hominins and Archaeology · Ecology · Geology · Oceanography · Paleontology

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Citations per year1.17
Citation span2020 - 2022 (3)
Highly citedNo

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