Changing environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones

Abstract Environmental change has been proposed as a factor that contributed to the extinction of the Neanderthals in Europe during MIS3. Currently, the different local environmental conditions experienced at the time when Anatomically Modern Humans (AMH) met Neanderthals are not well known. In the...

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Autores principales: Jennifer R. Jones, Michael P. Richards, Lawrence G. Straus, Hazel Reade, Jesús Altuna, Koro Mariezkurrena, Ana B. Marín-Arroyo
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Publicado: Nature Portfolio 2018
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spelling oai:doaj.org-article:5e9e5a7c5ef24d5ea3b9033011c7d2f02021-12-02T11:40:26ZChanging environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones10.1038/s41598-018-32493-02045-2322https://doaj.org/article/5e9e5a7c5ef24d5ea3b9033011c7d2f02018-10-01T00:00:00Zhttps://doi.org/10.1038/s41598-018-32493-0https://doaj.org/toc/2045-2322Abstract Environmental change has been proposed as a factor that contributed to the extinction of the Neanderthals in Europe during MIS3. Currently, the different local environmental conditions experienced at the time when Anatomically Modern Humans (AMH) met Neanderthals are not well known. In the Western Pyrenees, particularly, in the eastern end of the Cantabrian coast of the Iberian Peninsula, extensive evidence of Neanderthal and subsequent AMH activity exists, making it an ideal area in which to explore the palaeoenvironments experienced and resources exploited by both human species during the Middle to Upper Palaeolithic transition. Red deer and horse were analysed using bone collagen stable isotope analysis to reconstruct environmental conditions across the transition. A shift in the ecological niche of horses after the Mousterian demonstrates a change in environment, towards more open vegetation, linked to wider climatic change. In the Mousterian, Aurignacian and Gravettian, high inter-individual nitrogen ranges were observed in both herbivores. This could indicate that these individuals were procured from areas isotopically different in nitrogen. Differences in sulphur values between sites suggest some variability in the hunting locations exploited, reflecting the human use of different parts of the landscape. An alternative and complementary explanation proposed is that there were climatic fluctuations within the time of formation of these archaeological levels, as observed in pollen, marine and ice cores.Jennifer R. JonesMichael P. RichardsLawrence G. StrausHazel ReadeJesús AltunaKoro MariezkurrenaAna B. Marín-ArroyoNature PortfolioarticleCantabrian RegionMiddle-Upper Paleolithic TransitionMarine Isotope Stage (MIS3)Archaeological LevelsAnatomically Modern Humans (AMH)MedicineRScienceQENScientific Reports, Vol 8, Iss 1, Pp 1-20 (2018)
institution DOAJ
collection DOAJ
language EN
topic Cantabrian Region
Middle-Upper Paleolithic Transition
Marine Isotope Stage (MIS3)
Archaeological Levels
Anatomically Modern Humans (AMH)
Medicine
R
Science
Q
spellingShingle Cantabrian Region
Middle-Upper Paleolithic Transition
Marine Isotope Stage (MIS3)
Archaeological Levels
Anatomically Modern Humans (AMH)
Medicine
R
Science
Q
Jennifer R. Jones
Michael P. Richards
Lawrence G. Straus
Hazel Reade
Jesús Altuna
Koro Mariezkurrena
Ana B. Marín-Arroyo
Changing environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones
description Abstract Environmental change has been proposed as a factor that contributed to the extinction of the Neanderthals in Europe during MIS3. Currently, the different local environmental conditions experienced at the time when Anatomically Modern Humans (AMH) met Neanderthals are not well known. In the Western Pyrenees, particularly, in the eastern end of the Cantabrian coast of the Iberian Peninsula, extensive evidence of Neanderthal and subsequent AMH activity exists, making it an ideal area in which to explore the palaeoenvironments experienced and resources exploited by both human species during the Middle to Upper Palaeolithic transition. Red deer and horse were analysed using bone collagen stable isotope analysis to reconstruct environmental conditions across the transition. A shift in the ecological niche of horses after the Mousterian demonstrates a change in environment, towards more open vegetation, linked to wider climatic change. In the Mousterian, Aurignacian and Gravettian, high inter-individual nitrogen ranges were observed in both herbivores. This could indicate that these individuals were procured from areas isotopically different in nitrogen. Differences in sulphur values between sites suggest some variability in the hunting locations exploited, reflecting the human use of different parts of the landscape. An alternative and complementary explanation proposed is that there were climatic fluctuations within the time of formation of these archaeological levels, as observed in pollen, marine and ice cores.
format article
author Jennifer R. Jones
Michael P. Richards
Lawrence G. Straus
Hazel Reade
Jesús Altuna
Koro Mariezkurrena
Ana B. Marín-Arroyo
author_facet Jennifer R. Jones
Michael P. Richards
Lawrence G. Straus
Hazel Reade
Jesús Altuna
Koro Mariezkurrena
Ana B. Marín-Arroyo
author_sort Jennifer R. Jones
title Changing environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones
title_short Changing environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones
title_full Changing environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones
title_fullStr Changing environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones
title_full_unstemmed Changing environments during the Middle-Upper Palaeolithic transition in the eastern Cantabrian Region (Spain): direct evidence from stable isotope studies on ungulate bones
title_sort changing environments during the middle-upper palaeolithic transition in the eastern cantabrian region (spain): direct evidence from stable isotope studies on ungulate bones
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/5e9e5a7c5ef24d5ea3b9033011c7d2f0
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