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Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe
The study of local extinction times, together with the associated environmental and human population changes in the last glacial termination, provides insights into the causes of mega- and microfauna extinctions. In East-Central (EC) Europe, groups of Palaeolithic humans were present throughout the...
Autores principales: | , , , , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Nature Publishing Group UK
2022
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9043214/ https://www.ncbi.nlm.nih.gov/pubmed/35474321 http://dx.doi.org/10.1038/s41598-022-10714-x |
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author | Magyari, Enikő Katalin Gasparik, Mihály Major, István Lengyel, György Pál, Ilona Virág, Attila Korponai, János Haliuc, Aritina Szabó, Zoltán Pazonyi, Piroska |
author_facet | Magyari, Enikő Katalin Gasparik, Mihály Major, István Lengyel, György Pál, Ilona Virág, Attila Korponai, János Haliuc, Aritina Szabó, Zoltán Pazonyi, Piroska |
author_sort | Magyari, Enikő Katalin |
collection | PubMed |
description | The study of local extinction times, together with the associated environmental and human population changes in the last glacial termination, provides insights into the causes of mega- and microfauna extinctions. In East-Central (EC) Europe, groups of Palaeolithic humans were present throughout the last glacial maximum, but disappeared suddenly around 15,200 cal BP. In this study cave sediment profiles dated using radiocarbon techniques and a large set of mammal bones dated directly by AMS (14)C were used to determine local extinction times. These were, in turn, compared to changes in the total megafauna population of EC Europe derived from coprophilous fungi, the Epigravettian population decline, quantitative climate models, pollen and plant macrofossil inferred climate, as well as to biome reconstructions. The results suggest that the population size of large herbivores decreased in the area after 17,700 cal BP, when temperate tree abundance and warm continental steppe cover both increased in the lowlands. Boreal forest expansion started around 16,200 cal BP. Cave sediments show the decline of narrow-headed vole and arctic lemming populations specifically associated with a tundra environment at the same time and the expansion of the common vole, an inhabitant of steppes. The last dated appearance of arctic lemming was at ~ 16,640 cal BP, while that of the narrow-headed vole at ~ 13,340, and the estimated extinction time of woolly mammoth was either at 13,830 (GRIWM) or 15,210 (PHASE), and reindeer at 11,860 (GRIWM) or 12,550 cal BP (PHASE). The population decline of the large herbivore fauna slightly preceded changes in terrestrial vegetation, and likely facilitated it via a reduction in the intensity of grazing and the concomitant accumulation of plant biomass. Furthermore, it is possible to conclude that the Late Epigravettian population had high degree of quarry-fidelity; they left the basin when these mammals vanished. |
format | Online Article Text |
id | pubmed-9043214 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2022 |
publisher | Nature Publishing Group UK |
record_format | MEDLINE/PubMed |
spelling | pubmed-90432142022-04-28 Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe Magyari, Enikő Katalin Gasparik, Mihály Major, István Lengyel, György Pál, Ilona Virág, Attila Korponai, János Haliuc, Aritina Szabó, Zoltán Pazonyi, Piroska Sci Rep Article The study of local extinction times, together with the associated environmental and human population changes in the last glacial termination, provides insights into the causes of mega- and microfauna extinctions. In East-Central (EC) Europe, groups of Palaeolithic humans were present throughout the last glacial maximum, but disappeared suddenly around 15,200 cal BP. In this study cave sediment profiles dated using radiocarbon techniques and a large set of mammal bones dated directly by AMS (14)C were used to determine local extinction times. These were, in turn, compared to changes in the total megafauna population of EC Europe derived from coprophilous fungi, the Epigravettian population decline, quantitative climate models, pollen and plant macrofossil inferred climate, as well as to biome reconstructions. The results suggest that the population size of large herbivores decreased in the area after 17,700 cal BP, when temperate tree abundance and warm continental steppe cover both increased in the lowlands. Boreal forest expansion started around 16,200 cal BP. Cave sediments show the decline of narrow-headed vole and arctic lemming populations specifically associated with a tundra environment at the same time and the expansion of the common vole, an inhabitant of steppes. The last dated appearance of arctic lemming was at ~ 16,640 cal BP, while that of the narrow-headed vole at ~ 13,340, and the estimated extinction time of woolly mammoth was either at 13,830 (GRIWM) or 15,210 (PHASE), and reindeer at 11,860 (GRIWM) or 12,550 cal BP (PHASE). The population decline of the large herbivore fauna slightly preceded changes in terrestrial vegetation, and likely facilitated it via a reduction in the intensity of grazing and the concomitant accumulation of plant biomass. Furthermore, it is possible to conclude that the Late Epigravettian population had high degree of quarry-fidelity; they left the basin when these mammals vanished. Nature Publishing Group UK 2022-04-26 /pmc/articles/PMC9043214/ /pubmed/35474321 http://dx.doi.org/10.1038/s41598-022-10714-x Text en © The Author(s) 2022 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
spellingShingle | Article Magyari, Enikő Katalin Gasparik, Mihály Major, István Lengyel, György Pál, Ilona Virág, Attila Korponai, János Haliuc, Aritina Szabó, Zoltán Pazonyi, Piroska Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe |
title | Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe |
title_full | Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe |
title_fullStr | Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe |
title_full_unstemmed | Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe |
title_short | Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe |
title_sort | mammal extinction facilitated biome shift and human population change during the last glacial termination in east-central europe |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9043214/ https://www.ncbi.nlm.nih.gov/pubmed/35474321 http://dx.doi.org/10.1038/s41598-022-10714-x |
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