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

• Published in: Archaeological and Anthropological Sciences
• Main Authors: Lemanik, Anna, Baca, Mateusz, Wertz, Krzysztof, Socha, Paweł, Popović, Danijela, Tomek, Teresa, Lipecki, Grzegorz, Kraszewska, Anna, Miękina, Barbara, Żeromska, Aleksandra, Pereswiet-Soltan, Andrea, Szyndlar, Zbigniew, Cieśla, Magda, Valde-Nowak, Paweł, Mackiewicz, Paweł, Nadachowski, Adam
• Format: Other/Unknown Material
• Language: English
• Published: 2020
• Subjects: Palaeoenvironmental reconstruction; Faunal succession; Obłazowa Cave; Magdalenian; Global warming; change; Greenland; Western Entrance; Microtus arvalis
• Online Access: https://ruj.uj.edu.pl/xmlui/handle/item/153294; https://doi.org/10.1007/s12520-020-01020-6

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 theWestern 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; minimumnumber 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.