Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium

Autores
Peña Monné, José Luis; Sancho Marcén, Carlos; Sampietro Vattuone, Maria Marta; Rivelli, Felipe; Rhodes, Edwards J.; Osácar Soriano, María Cinta; Rubio Fernández, Virginia; García Giménez, Rosario
Año de publicación
2015
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Cafayate depression is a dry valley located in the Pre-Andean region of northwest Argentina. The area shows the development of a large dune field. Its significance has been established from geomorphological and mineralogical evidence, grain shape characteristics and chronological data (OSL dating, archaeological remains, and historical data). The dating results were between 1000–1100 AD to1740–1830 AD showing that the aeolian dynamics remained active during the last millennium. It was not possible to identify stabilised phases marked by ruptures or paleosol development. Nevertheless, other regional and local proxies from Northwest Argentina (archaeological, documentary, etc.) were used to complete the interpretative framework to propose the paleoenvironmental evolution of the area. In addition, human activity and land use must be considered as a complementary factor affecting aeolian dynamics during the most recent stage.
Fil: Peña Monné, José Luis. Universidad de Zaragoza; España
Fil: Sancho Marcén, Carlos. Universidad de Zaragoza; 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
Fil: Rivelli, Felipe. Universidad Nacional de Salta. Facultad de Ciencias Naturales; Argentina
Fil: Rhodes, Edwards J.. University of California at Los Angeles; Estados Unidos. University Of Manchester; Reino Unido
Fil: Osácar Soriano, María Cinta. Universidad de Zaragoza; España
Fil: Rubio Fernández, Virginia. Universidad Autónoma de Madrid; España
Fil: García Giménez, Rosario. Universidad Autónoma de Madrid; España
Materia
Aeolian Dynamics
Osl Dating
Last Millenium
Nw Argentina Drylands
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/12593
Acceder
id CONICETDig_0ba45f21f1f85114d20bb7018ff343a5
oai_identifier_str oai:ri.conicet.gov.ar:11336/12593
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millenniumPeña Monné, José LuisSancho Marcén, CarlosSampietro Vattuone, Maria MartaRivelli, FelipeRhodes, Edwards J.Osácar Soriano, María CintaRubio Fernández, VirginiaGarcía Giménez, RosarioAeolian DynamicsOsl DatingLast MilleniumNw Argentina Drylandshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1https://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1https://purl.org/becyt/ford/6.1https://purl.org/becyt/ford/6The Cafayate depression is a dry valley located in the Pre-Andean region of northwest Argentina. The area shows the development of a large dune field. Its significance has been established from geomorphological and mineralogical evidence, grain shape characteristics and chronological data (OSL dating, archaeological remains, and historical data). The dating results were between 1000–1100 AD to1740–1830 AD showing that the aeolian dynamics remained active during the last millennium. It was not possible to identify stabilised phases marked by ruptures or paleosol development. Nevertheless, other regional and local proxies from Northwest Argentina (archaeological, documentary, etc.) were used to complete the interpretative framework to propose the paleoenvironmental evolution of the area. In addition, human activity and land use must be considered as a complementary factor affecting aeolian dynamics during the most recent stage.Fil: Peña Monné, José Luis. Universidad de Zaragoza; EspañaFil: Sancho Marcén, Carlos. Universidad de Zaragoza; 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; ArgentinaFil: Rivelli, Felipe. Universidad Nacional de Salta. Facultad de Ciencias Naturales; ArgentinaFil: Rhodes, Edwards J.. University of California at Los Angeles; Estados Unidos. University Of Manchester; Reino UnidoFil: Osácar Soriano, María Cinta. Universidad de Zaragoza; EspañaFil: Rubio Fernández, Virginia. Universidad Autónoma de Madrid; EspañaFil: García Giménez, Rosario. Universidad Autónoma de Madrid; EspañaElsevier Science2015-11info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/12593Peña Monné, José Luis; Sancho Marcén, Carlos; Sampietro Vattuone, Maria Marta; Rivelli, Felipe; Rhodes, Edwards J.; et al.; Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium; Elsevier Science; Palaeogeography, Palaeoclimatology, Palaeoecology; 438; 11-2015; 352-3630031-0182enginfo:eu-repo/semantics/altIdentifier/url/http://dx.doi.org/10.1016/j.palaeo.2015.08.028info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0031018215004642info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T12:19:47Zoai:ri.conicet.gov.ar:11336/12593instacron: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:34982025-10-22 12:19:47.955CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium
title Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium
spellingShingle Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium
Peña Monné, José Luis
Aeolian Dynamics
Osl Dating
Last Millenium
Nw Argentina Drylands
title_short Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium
title_full Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium
title_fullStr Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium
title_full_unstemmed Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium
title_sort Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium
dc.creator.none.fl_str_mv Peña Monné, José Luis
Sancho Marcén, Carlos
Sampietro Vattuone, Maria Marta
Rivelli, Felipe
Rhodes, Edwards J.
Osácar Soriano, María Cinta
Rubio Fernández, Virginia
García Giménez, Rosario
author Peña Monné, José Luis
author_facet Peña Monné, José Luis
Sancho Marcén, Carlos
Sampietro Vattuone, Maria Marta
Rivelli, Felipe
Rhodes, Edwards J.
Osácar Soriano, María Cinta
Rubio Fernández, Virginia
García Giménez, Rosario
author_role author
author2 Sancho Marcén, Carlos
Sampietro Vattuone, Maria Marta
Rivelli, Felipe
Rhodes, Edwards J.
Osácar Soriano, María Cinta
Rubio Fernández, Virginia
García Giménez, Rosario
author2_role author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Aeolian Dynamics
Osl Dating
Last Millenium
Nw Argentina Drylands
topic Aeolian Dynamics
Osl Dating
Last Millenium
Nw Argentina Drylands
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
https://purl.org/becyt/ford/6.1
https://purl.org/becyt/ford/6
dc.description.none.fl_txt_mv The Cafayate depression is a dry valley located in the Pre-Andean region of northwest Argentina. The area shows the development of a large dune field. Its significance has been established from geomorphological and mineralogical evidence, grain shape characteristics and chronological data (OSL dating, archaeological remains, and historical data). The dating results were between 1000–1100 AD to1740–1830 AD showing that the aeolian dynamics remained active during the last millennium. It was not possible to identify stabilised phases marked by ruptures or paleosol development. Nevertheless, other regional and local proxies from Northwest Argentina (archaeological, documentary, etc.) were used to complete the interpretative framework to propose the paleoenvironmental evolution of the area. In addition, human activity and land use must be considered as a complementary factor affecting aeolian dynamics during the most recent stage.
Fil: Peña Monné, José Luis. Universidad de Zaragoza; España
Fil: Sancho Marcén, Carlos. Universidad de Zaragoza; 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
Fil: Rivelli, Felipe. Universidad Nacional de Salta. Facultad de Ciencias Naturales; Argentina
Fil: Rhodes, Edwards J.. University of California at Los Angeles; Estados Unidos. University Of Manchester; Reino Unido
Fil: Osácar Soriano, María Cinta. Universidad de Zaragoza; España
Fil: Rubio Fernández, Virginia. Universidad Autónoma de Madrid; España
Fil: García Giménez, Rosario. Universidad Autónoma de Madrid; España
description The Cafayate depression is a dry valley located in the Pre-Andean region of northwest Argentina. The area shows the development of a large dune field. Its significance has been established from geomorphological and mineralogical evidence, grain shape characteristics and chronological data (OSL dating, archaeological remains, and historical data). The dating results were between 1000–1100 AD to1740–1830 AD showing that the aeolian dynamics remained active during the last millennium. It was not possible to identify stabilised phases marked by ruptures or paleosol development. Nevertheless, other regional and local proxies from Northwest Argentina (archaeological, documentary, etc.) were used to complete the interpretative framework to propose the paleoenvironmental evolution of the area. In addition, human activity and land use must be considered as a complementary factor affecting aeolian dynamics during the most recent stage.
publishDate 2015
dc.date.none.fl_str_mv 2015-11
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/11336/12593
Peña Monné, José Luis; Sancho Marcén, Carlos; Sampietro Vattuone, Maria Marta; Rivelli, Felipe; Rhodes, Edwards J.; et al.; Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium; Elsevier Science; Palaeogeography, Palaeoclimatology, Palaeoecology; 438; 11-2015; 352-363
0031-0182
url http://hdl.handle.net/11336/12593
identifier_str_mv Peña Monné, José Luis; Sancho Marcén, Carlos; Sampietro Vattuone, Maria Marta; Rivelli, Felipe; Rhodes, Edwards J.; et al.; Geomorphological study of the Cafayate dune field (Northwest Argentina) during the last millennium; Elsevier Science; Palaeogeography, Palaeoclimatology, Palaeoecology; 438; 11-2015; 352-363
0031-0182
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://dx.doi.org/10.1016/j.palaeo.2015.08.028
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0031018215004642
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier Science
publisher.none.fl_str_mv Elsevier Science
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
_version_ 1846782639729541120
score 12.982451

Publicaciones similares