Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)

Autores
Pérez Lambán, Fernando; Peña Monné, José Luis; Fanlo Loras, Javier; Picazo Millán, Jesús V.; Badía Villas, David; Rubio Fernández, Virginia; García Giménez, Rosario; Sampietro Vattuone, Maria Marta
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Slope deposits in semiarid regions are known to be very sensitive environments, especially those that occurred during the minor fluctuations of the late Holocene. In this paper we analyse Holocene colluvium genesis, composition, and paleoenvironmental meaning through the study of slope deposits in NE Spain. Two cumulative slope stages are described during this period. In the study area, both slope accumulations are superimposed and this has enabled an excellent preservation of the aggregative sequence and the paleosols corresponding to stabilisation stages. 14C and TL dating, as well as archaeological remains, provide considerable chronological precision for this sequence. The origin of the accumulation of the lower unit is placed around 4295–4083 cal yr BP/2346–2134 cal yr BC (late Chalcolithic) and it developed until the Iron Age in a cooler and wetter climate (Cold Iron Age). Under favourable conditions, a soil A-horizon was formed on top of this unit. A new slope accumulation was formed during the Little Ice Age. Within the slope two morphogenetic periods ending with A-horizons are distinguished and related with two main cold–wet climatic events. The study of these slopes provides a great amount of data for the paleoenvironmental and geoarchaeological reconstruction of the late Holocene in NE Spain.
Fil: Pérez Lambán, Fernando. Universidad de Zaragoza; España
Fil: Peña Monné, José Luis. Universidad de Zaragoza; España
Fil: Fanlo Loras, Javier. Universidad de Zaragoza; España
Fil: Picazo Millán, Jesús V.. Universidad de Zaragoza; España
Fil: Badía Villas, David. Universidad de Zaragoza; España
Fil: Rubio Fernández, Virginia. Universidad Autónoma de Madrid; España
Fil: García Giménez, Rosario . Universidad Autónoma de Madrid; España
Fil: Sampietro Vattuone, Maria Marta. Universidad Nacional de Tucuman. Facultad de Cs.naturales E Instituto Miguel Lillo. Laboratorio de Geoarqueologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Materia
Geoarchaeology
Slope Morpho-Dynamic
Paleosol
Paleoenvironment
Late Holocene
Cold Iron Age
Warm Roman Period
Medieval Climatic Anomaly
Little Ice Age
Ebro Depression
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/12648
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/12648
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)Pérez Lambán, FernandoPeña Monné, José LuisFanlo Loras, JavierPicazo Millán, Jesús V.Badía Villas, DavidRubio Fernández, VirginiaGarcía Giménez, Rosario Sampietro Vattuone, Maria MartaGeoarchaeologySlope Morpho-DynamicPaleosolPaleoenvironmentLate HoloceneCold Iron AgeWarm Roman PeriodMedieval Climatic AnomalyLittle Ice AgeEbro Depressionhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Slope deposits in semiarid regions are known to be very sensitive environments, especially those that occurred during the minor fluctuations of the late Holocene. In this paper we analyse Holocene colluvium genesis, composition, and paleoenvironmental meaning through the study of slope deposits in NE Spain. Two cumulative slope stages are described during this period. In the study area, both slope accumulations are superimposed and this has enabled an excellent preservation of the aggregative sequence and the paleosols corresponding to stabilisation stages. 14C and TL dating, as well as archaeological remains, provide considerable chronological precision for this sequence. The origin of the accumulation of the lower unit is placed around 4295–4083 cal yr BP/2346–2134 cal yr BC (late Chalcolithic) and it developed until the Iron Age in a cooler and wetter climate (Cold Iron Age). Under favourable conditions, a soil A-horizon was formed on top of this unit. A new slope accumulation was formed during the Little Ice Age. Within the slope two morphogenetic periods ending with A-horizons are distinguished and related with two main cold–wet climatic events. The study of these slopes provides a great amount of data for the paleoenvironmental and geoarchaeological reconstruction of the late Holocene in NE Spain.Fil: Pérez Lambán, Fernando. Universidad de Zaragoza; EspañaFil: Peña Monné, José Luis. Universidad de Zaragoza; EspañaFil: Fanlo Loras, Javier. Universidad de Zaragoza; EspañaFil: Picazo Millán, Jesús V.. Universidad de Zaragoza; EspañaFil: Badía Villas, David. Universidad de Zaragoza; EspañaFil: Rubio Fernández, Virginia. Universidad Autónoma de Madrid; EspañaFil: García Giménez, Rosario . Universidad Autónoma de Madrid; EspañaFil: Sampietro Vattuone, Maria Marta. Universidad Nacional de Tucuman. Facultad de Cs.naturales E Instituto Miguel Lillo. Laboratorio de Geoarqueologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaWashington State Univ2014-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/12648Pérez Lambán, Fernando; Peña Monné, José Luis; Fanlo Loras, Javier; Picazo Millán, Jesús V.; Badía Villas, David; et al.; Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain); Washington State Univ; Quaternary Research; 81; 1; 1-2014; 1-140033-5894enginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2013.10.011info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/quaternary-research/article/div-classtitlepaleoenvironmental-and-geoarchaeological-reconstruction-from-late-holocene-slope-records-lower-huerva-valley-ebro-basin-ne-spaindiv/B201E72A06C7B447340E92C4DAEF46A8info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:46:08Zoai:ri.conicet.gov.ar:11336/12648instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-29 09:46:08.763CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)
title Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)
spellingShingle Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)
Pérez Lambán, Fernando
Geoarchaeology
Slope Morpho-Dynamic
Paleosol
Paleoenvironment
Late Holocene
Cold Iron Age
Warm Roman Period
Medieval Climatic Anomaly
Little Ice Age
Ebro Depression
title_short Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)
title_full Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)
title_fullStr Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)
title_full_unstemmed Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)
title_sort Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain)
dc.creator.none.fl_str_mv Pérez Lambán, Fernando
Peña Monné, José Luis
Fanlo Loras, Javier
Picazo Millán, Jesús V.
Badía Villas, David
Rubio Fernández, Virginia
García Giménez, Rosario
Sampietro Vattuone, Maria Marta
author Pérez Lambán, Fernando
author_facet Pérez Lambán, Fernando
Peña Monné, José Luis
Fanlo Loras, Javier
Picazo Millán, Jesús V.
Badía Villas, David
Rubio Fernández, Virginia
García Giménez, Rosario
Sampietro Vattuone, Maria Marta
author_role author
author2 Peña Monné, José Luis
Fanlo Loras, Javier
Picazo Millán, Jesús V.
Badía Villas, David
Rubio Fernández, Virginia
García Giménez, Rosario
Sampietro Vattuone, Maria Marta
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Geoarchaeology
Slope Morpho-Dynamic
Paleosol
Paleoenvironment
Late Holocene
Cold Iron Age
Warm Roman Period
Medieval Climatic Anomaly
Little Ice Age
Ebro Depression
topic Geoarchaeology
Slope Morpho-Dynamic
Paleosol
Paleoenvironment
Late Holocene
Cold Iron Age
Warm Roman Period
Medieval Climatic Anomaly
Little Ice Age
Ebro Depression
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Slope deposits in semiarid regions are known to be very sensitive environments, especially those that occurred during the minor fluctuations of the late Holocene. In this paper we analyse Holocene colluvium genesis, composition, and paleoenvironmental meaning through the study of slope deposits in NE Spain. Two cumulative slope stages are described during this period. In the study area, both slope accumulations are superimposed and this has enabled an excellent preservation of the aggregative sequence and the paleosols corresponding to stabilisation stages. 14C and TL dating, as well as archaeological remains, provide considerable chronological precision for this sequence. The origin of the accumulation of the lower unit is placed around 4295–4083 cal yr BP/2346–2134 cal yr BC (late Chalcolithic) and it developed until the Iron Age in a cooler and wetter climate (Cold Iron Age). Under favourable conditions, a soil A-horizon was formed on top of this unit. A new slope accumulation was formed during the Little Ice Age. Within the slope two morphogenetic periods ending with A-horizons are distinguished and related with two main cold–wet climatic events. The study of these slopes provides a great amount of data for the paleoenvironmental and geoarchaeological reconstruction of the late Holocene in NE Spain.
Fil: Pérez Lambán, Fernando. Universidad de Zaragoza; España
Fil: Peña Monné, José Luis. Universidad de Zaragoza; España
Fil: Fanlo Loras, Javier. Universidad de Zaragoza; España
Fil: Picazo Millán, Jesús V.. Universidad de Zaragoza; España
Fil: Badía Villas, David. Universidad de Zaragoza; España
Fil: Rubio Fernández, Virginia. Universidad Autónoma de Madrid; España
Fil: García Giménez, Rosario . Universidad Autónoma de Madrid; España
Fil: Sampietro Vattuone, Maria Marta. Universidad Nacional de Tucuman. Facultad de Cs.naturales E Instituto Miguel Lillo. Laboratorio de Geoarqueologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
description Slope deposits in semiarid regions are known to be very sensitive environments, especially those that occurred during the minor fluctuations of the late Holocene. In this paper we analyse Holocene colluvium genesis, composition, and paleoenvironmental meaning through the study of slope deposits in NE Spain. Two cumulative slope stages are described during this period. In the study area, both slope accumulations are superimposed and this has enabled an excellent preservation of the aggregative sequence and the paleosols corresponding to stabilisation stages. 14C and TL dating, as well as archaeological remains, provide considerable chronological precision for this sequence. The origin of the accumulation of the lower unit is placed around 4295–4083 cal yr BP/2346–2134 cal yr BC (late Chalcolithic) and it developed until the Iron Age in a cooler and wetter climate (Cold Iron Age). Under favourable conditions, a soil A-horizon was formed on top of this unit. A new slope accumulation was formed during the Little Ice Age. Within the slope two morphogenetic periods ending with A-horizons are distinguished and related with two main cold–wet climatic events. The study of these slopes provides a great amount of data for the paleoenvironmental and geoarchaeological reconstruction of the late Holocene in NE Spain.
publishDate 2014
dc.date.none.fl_str_mv 2014-01
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/12648
Pérez Lambán, Fernando; Peña Monné, José Luis; Fanlo Loras, Javier; Picazo Millán, Jesús V.; Badía Villas, David; et al.; Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain); Washington State Univ; Quaternary Research; 81; 1; 1-2014; 1-14
0033-5894
url http://hdl.handle.net/11336/12648
identifier_str_mv Pérez Lambán, Fernando; Peña Monné, José Luis; Fanlo Loras, Javier; Picazo Millán, Jesús V.; Badía Villas, David; et al.; Paleoenvironmental and Geoarchaeological reconstruction from Late Holocene slope records (Lower Huerva Valley, Ebro Basin, NE Spain); Washington State Univ; Quaternary Research; 81; 1; 1-2014; 1-14
0033-5894
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2013.10.011
info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/quaternary-research/article/div-classtitlepaleoenvironmental-and-geoarchaeological-reconstruction-from-late-holocene-slope-records-lower-huerva-valley-ebro-basin-ne-spaindiv/B201E72A06C7B447340E92C4DAEF46A8
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Washington State Univ
publisher.none.fl_str_mv Washington State Univ
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 13.069144

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