Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill

Atxurra Cave (Berriatua, Northern Spain) contains an important Magdalenian archaeological assemblage comprising evidence of ephemeral occupation in the lower cave level and a unique assemblage of rock art. With the aim of understanding the palaeoenvironmental conditions and the nature of the human o...

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Autores: Aranbarri, J., Arriolabengoa, M., Rios-Garaizar, Joseba, Aranburu-Mendizabal, Ainhoa, Uzquiano, Paloma, Arranz-Otaegui, Amaia, González-Sampériz, Penélope, Garate, Diego
Tipo de recurso: artículo
Estado:Versión aceptada para publicación
Fecha de publicación:2024
País:España
Institución:Consejo Superior de Investigaciones Científicas (CSIC)
Repositorio:DIGITAL.CSIC. Repositorio Institucional del CSIC
OAI Identifier:oai:digital.csic.es:10261/354465
Acceso en línea:http://hdl.handle.net/10261/354465
Access Level:acceso abierto
Palabra clave:Archaeological context
Palynology
Anthracology
Micromorphology
Karstic caves
Magdalenian
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spelling Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fillAranbarri, J.Arriolabengoa, M.Rios-Garaizar, JosebaAranburu-Mendizabal, AinhoaUzquiano, PalomaArranz-Otaegui, AmaiaGonzález-Sampériz, PenélopeGarate, DiegoArchaeological contextPalynologyAnthracologyMicromorphologyKarstic cavesMagdalenianAtxurra Cave (Berriatua, Northern Spain) contains an important Magdalenian archaeological assemblage comprising evidence of ephemeral occupation in the lower cave level and a unique assemblage of rock art. With the aim of understanding the palaeoenvironmental conditions and the nature of the human occupation, detailed micromorphological, mineralogical, palynological and anthracological analyses were undertaken near the entrance of the cave. The lower part of the excavated sequence comprises almost unfossiliferous silty units deposited over a thick speleothem deposit, which alternates with a sandy-silt matrix-supported microfacies dated about 33.4 kyr B.P. Palynological assemblage in this unit suggest regional vegetation was formed by montane pines, junipers and broadleaved elements like birch and hazel. Overlying units of brown clayey material, dated to ca. 19.7–18.4 kyr B.P., contain evidence of a Gravettian occupation with Noailles burins, and a palynoflora indicative of localized conifers with a dense herbaceous steppe understory, in an arid and cold climate. At ca. 15.5–14.5 kyr B.P. there is a return to meso-thermophilous tree and shrub taxa within a warmer and humid climate background, which may have favored the regional development of the Magdalenian culture. The uppermost unit, dated ca. 7.7–7 kyr B.P., reveals postglacial expansion of a mixed Atlantic forest with no signals of anthropization before the start of the Neolithic.This research has been benefited from the financial support provided by DINAMO3 (CGL2015-69160-R), funded by the Spanish Inter-Ministry Commission of Science and Technology (CICYT). Archaeological research in Atxurra was funded by Bizkaiko Foru Aldundia between 2014 and 2015 for the excavation, between 2016 and 2020 for the rock art study, and by the Basque Government in 2014 for the analysis of archaeological material.Peer reviewedElsevierComisión Interministerial de Ciencia y Tecnología, CICYT (España)Diputación Foral de BizkaiaEusko JaurlaritzaMinisterio de Economía y Competitividad (España)Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]202420242024info:eu-repo/semantics/articlehttp://purl.org/coar/resource_type/c_6501Postprintinfo:eu-repo/semantics/acceptedVersionapplication/pdfhttp://hdl.handle.net/10261/354465reponame:DIGITAL.CSIC. Repositorio Institucional del CSICinstname:Consejo Superior de Investigaciones Científicas (CSIC)Inglés#PLACEHOLDER_PARENT_METADATA_VALUE#info:eu-repo/grantAgreement/MINECO//CGL2015-69160-RThe underlying dataset has been published as supplementary material of the article in the publisher platform at https://doi.org/10.1016/j.palaeo.2023.111996https://doi.org/10.1016/j.palaeo.2023.111996Síinfo:eu-repo/semantics/openAccessoai:digital.csic.es:10261/3544652026-05-22T06:33:51Z
dc.title.none.fl_str_mv Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
title Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
spellingShingle Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
Aranbarri, J.
Archaeological context
Palynology
Anthracology
Micromorphology
Karstic caves
Magdalenian
title_short Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
title_full Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
title_fullStr Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
title_full_unstemmed Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
title_sort Human colonisation and vegetation response to Late Pleistocene to mid-Holocene climate variability in Northern Iberia based on a multiproxy analysis of the Atxurra cave-fill
dc.creator.none.fl_str_mv Aranbarri, J.
Arriolabengoa, M.
Rios-Garaizar, Joseba
Aranburu-Mendizabal, Ainhoa
Uzquiano, Paloma
Arranz-Otaegui, Amaia
González-Sampériz, Penélope
Garate, Diego
author Aranbarri, J.
author_facet Aranbarri, J.
Arriolabengoa, M.
Rios-Garaizar, Joseba
Aranburu-Mendizabal, Ainhoa
Uzquiano, Paloma
Arranz-Otaegui, Amaia
González-Sampériz, Penélope
Garate, Diego
author_role author
author2 Arriolabengoa, M.
Rios-Garaizar, Joseba
Aranburu-Mendizabal, Ainhoa
Uzquiano, Paloma
Arranz-Otaegui, Amaia
González-Sampériz, Penélope
Garate, Diego
author2_role author
author
author
author
author
author
author
dc.contributor.none.fl_str_mv Comisión Interministerial de Ciencia y Tecnología, CICYT (España)
Diputación Foral de Bizkaia
Eusko Jaurlaritza
Ministerio de Economía y Competitividad (España)
Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72]
dc.subject.none.fl_str_mv Archaeological context
Palynology
Anthracology
Micromorphology
Karstic caves
Magdalenian
topic Archaeological context
Palynology
Anthracology
Micromorphology
Karstic caves
Magdalenian
description Atxurra Cave (Berriatua, Northern Spain) contains an important Magdalenian archaeological assemblage comprising evidence of ephemeral occupation in the lower cave level and a unique assemblage of rock art. With the aim of understanding the palaeoenvironmental conditions and the nature of the human occupation, detailed micromorphological, mineralogical, palynological and anthracological analyses were undertaken near the entrance of the cave. The lower part of the excavated sequence comprises almost unfossiliferous silty units deposited over a thick speleothem deposit, which alternates with a sandy-silt matrix-supported microfacies dated about 33.4 kyr B.P. Palynological assemblage in this unit suggest regional vegetation was formed by montane pines, junipers and broadleaved elements like birch and hazel. Overlying units of brown clayey material, dated to ca. 19.7–18.4 kyr B.P., contain evidence of a Gravettian occupation with Noailles burins, and a palynoflora indicative of localized conifers with a dense herbaceous steppe understory, in an arid and cold climate. At ca. 15.5–14.5 kyr B.P. there is a return to meso-thermophilous tree and shrub taxa within a warmer and humid climate background, which may have favored the regional development of the Magdalenian culture. The uppermost unit, dated ca. 7.7–7 kyr B.P., reveals postglacial expansion of a mixed Atlantic forest with no signals of anthropization before the start of the Neolithic.
publishDate 2024
dc.date.none.fl_str_mv 2024
2024
2024
dc.type.none.fl_str_mv info:eu-repo/semantics/article
http://purl.org/coar/resource_type/c_6501
Postprint
info:eu-repo/semantics/acceptedVersion
format article
status_str acceptedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/10261/354465
url http://hdl.handle.net/10261/354465
dc.language.none.fl_str_mv Inglés
language_invalid_str_mv Inglés
dc.relation.none.fl_str_mv #PLACEHOLDER_PARENT_METADATA_VALUE#
info:eu-repo/grantAgreement/MINECO//CGL2015-69160-R
The underlying dataset has been published as supplementary material of the article in the publisher platform at https://doi.org/10.1016/j.palaeo.2023.111996
https://doi.org/10.1016/j.palaeo.2023.111996

dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
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dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:DIGITAL.CSIC. Repositorio Institucional del CSIC
instname:Consejo Superior de Investigaciones Científicas (CSIC)
instname_str Consejo Superior de Investigaciones Científicas (CSIC)
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