Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales
Lynx Cave is one of a handful of locations in North Wales that provide evidence of Late Upper Palaeolithic huntergatherers at the end of the last ice-age. With the region being recolonized at a time of rapid environmental change there is a need to develop on-site palaeoenvironmental records that are...
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ftuglasgow:oai:eprints.gla.ac.uk:260298 2023-05-15T16:37:45+02:00 Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales Stevens, Rhiannon E. Reade, Hazel Tripp, Jennifer Sayle, Kerry L. Walker, Elizabeth A. Gaudzinski-Windheuser, Sabine Jöris, Olaf 2021-12-06 text http://eprints.gla.ac.uk/260298/ http://eprints.gla.ac.uk/260298/1/260298.pdf https://doi.org/10.11588/propylaeum.950.c12581 en eng Römisch-Germanischen Zentralmuseums http://eprints.gla.ac.uk/260298/1/260298.pdf Stevens, R. E., Reade, H., Tripp, J., Sayle, K. L. <http://eprints.gla.ac.uk/view/author/8948.html> and Walker, E. A. (2021) Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales. In: Gaudzinski-Windheuser, S. and Jöris, O. (eds.) The Beef behind all Possible Pasts: The Tandem-Festschrift in Honour of Elaine Turner and Martin Street. Römisch-Germanischen Zentralmuseums, pp. 589-607. ISBN 9783884673423 (doi:10.11588/propylaeum.950.c12581) cc_by_sa_4 CC-BY-SA Book Sections NonPeerReviewed 2021 ftuglasgow https://doi.org/10.11588/propylaeum.950.c12581 2022-03-03T23:17:49Z Lynx Cave is one of a handful of locations in North Wales that provide evidence of Late Upper Palaeolithic huntergatherers at the end of the last ice-age. With the region being recolonized at a time of rapid environmental change there is a need to develop on-site palaeoenvironmental records that are directly linked to the archaeology in order to further understanding of the environments and landscapes that these hunter-gatherer groups experienced. Through carbon (δ13C), nitrogen (δ15N) and sulphur (δ34S) stable isotope analysis of animal bones we explore the environmental conditions during the human occupation of Lynx Cave. Analysis of the data indicates the faunal isotope results cluster into three distinct groupings, which when considered in light of the species composition, radiocarbon dates, sample layer provenance and known temporal patterns in herbivore isotope data from Northern Europe, are likely to relate to GI-1cba (the Allerød period) around 13,700-13,000 cal BP, GI-1cba/GS-1 (the Late Allerød/ early Younger Dryas period) around 13,100-12,800 cal BP, and the Bronze Age. The isotope data indicates that the Late Upper Palaeolithic or Late Palaeolithic occupations occurred in an open landscape in which soils were undergoing changing hydrological conditions linked to ice sheet melt and permafrost thaw process and subsequent recovery. The evidence of butchery marks on the faunal remains from both Late Glacial isotope clusters, along with the disparate radiocarbon dates and the presence of three hearths, support the idea of very short-term episodic use of the cave over an extended time period. Book Part Ice Ice Sheet permafrost Lynx University of Glasgow: Enlighten - Publications |
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Open Polar |
collection |
University of Glasgow: Enlighten - Publications |
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ftuglasgow |
language |
English |
description |
Lynx Cave is one of a handful of locations in North Wales that provide evidence of Late Upper Palaeolithic huntergatherers at the end of the last ice-age. With the region being recolonized at a time of rapid environmental change there is a need to develop on-site palaeoenvironmental records that are directly linked to the archaeology in order to further understanding of the environments and landscapes that these hunter-gatherer groups experienced. Through carbon (δ13C), nitrogen (δ15N) and sulphur (δ34S) stable isotope analysis of animal bones we explore the environmental conditions during the human occupation of Lynx Cave. Analysis of the data indicates the faunal isotope results cluster into three distinct groupings, which when considered in light of the species composition, radiocarbon dates, sample layer provenance and known temporal patterns in herbivore isotope data from Northern Europe, are likely to relate to GI-1cba (the Allerød period) around 13,700-13,000 cal BP, GI-1cba/GS-1 (the Late Allerød/ early Younger Dryas period) around 13,100-12,800 cal BP, and the Bronze Age. The isotope data indicates that the Late Upper Palaeolithic or Late Palaeolithic occupations occurred in an open landscape in which soils were undergoing changing hydrological conditions linked to ice sheet melt and permafrost thaw process and subsequent recovery. The evidence of butchery marks on the faunal remains from both Late Glacial isotope clusters, along with the disparate radiocarbon dates and the presence of three hearths, support the idea of very short-term episodic use of the cave over an extended time period. |
author2 |
Gaudzinski-Windheuser, Sabine Jöris, Olaf |
format |
Book Part |
author |
Stevens, Rhiannon E. Reade, Hazel Tripp, Jennifer Sayle, Kerry L. Walker, Elizabeth A. |
spellingShingle |
Stevens, Rhiannon E. Reade, Hazel Tripp, Jennifer Sayle, Kerry L. Walker, Elizabeth A. Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales |
author_facet |
Stevens, Rhiannon E. Reade, Hazel Tripp, Jennifer Sayle, Kerry L. Walker, Elizabeth A. |
author_sort |
Stevens, Rhiannon E. |
title |
Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales |
title_short |
Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales |
title_full |
Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales |
title_fullStr |
Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales |
title_full_unstemmed |
Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales |
title_sort |
changing environment at the late upper palaeolithic ite of lynx cave, north wales |
publisher |
Römisch-Germanischen Zentralmuseums |
publishDate |
2021 |
url |
http://eprints.gla.ac.uk/260298/ http://eprints.gla.ac.uk/260298/1/260298.pdf https://doi.org/10.11588/propylaeum.950.c12581 |
genre |
Ice Ice Sheet permafrost Lynx |
genre_facet |
Ice Ice Sheet permafrost Lynx |
op_relation |
http://eprints.gla.ac.uk/260298/1/260298.pdf Stevens, R. E., Reade, H., Tripp, J., Sayle, K. L. <http://eprints.gla.ac.uk/view/author/8948.html> and Walker, E. A. (2021) Changing environment at the Late Upper Palaeolithic ite of Lynx Cave, North Wales. In: Gaudzinski-Windheuser, S. and Jöris, O. (eds.) The Beef behind all Possible Pasts: The Tandem-Festschrift in Honour of Elaine Turner and Martin Street. Römisch-Germanischen Zentralmuseums, pp. 589-607. ISBN 9783884673423 (doi:10.11588/propylaeum.950.c12581) |
op_rights |
cc_by_sa_4 |
op_rightsnorm |
CC-BY-SA |
op_doi |
https://doi.org/10.11588/propylaeum.950.c12581 |
_version_ |
1766028052946485248 |