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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/12648
Ver los metadatos del registro completo
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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 Técnicas2025-09-03T09:50:45Zoai: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:34982025-09-03 09:50:45.346CONICET 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 |
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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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1842269050980270080 |
score |
13.13397 |