Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina

Autores
Toms, Phillip S.; King, Matthew; Zárate, Marcelo Arístides; Kemp, Rob A.; Foit Jr., Franklin F.
Año de publicación
2004
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The synthesis of paleoclimatic archives provided by loess and alluvial sequences of central Argentina has been hindered by the lack of a cohesive lithostratigraphic framework extending across the Chaco-Pampean plains and catchments of the Rios Desaguadero, Colorado, and Negro. This condition originates in part from the dearth of absolute chronological controls. The occurrence of discrete tephra layers across this region may provide an opportunity to address this deficiency if a tephrochronological framework can be established. The potential of such a project is assessed within the context of a pilot study constrained within alluvial sequences of central western Argentina proximal to potential source vents in the Southern Volcanic Zone. The intersite discrimination and correlation of tephra layers on a geochemical basis is examined, with indirect chronological control for the eruption of each generated by optical dating. Alluvial sediments on either side of each of five tephra units at a type site were dated using the optically stimulated luminescence of fine-silt-sized quartz, thus providing an age control on each tephra (ca. 24,000, 30,000, 32,000, 39,000, and 48,000 yr). The geochemical composition of each tephra was derived. Using these data, tephra layers at other sites in the study area were geochemically analyzed and, in instances of statistical concordance in major oxide structure, correlated to the type site and therefore ascribed ages. This methodology identified a further sixth volcanic event between ca. 24,000 and 30,000 yr not registered by type-site tephras. The extension of this initial tephrochronological framework beyond the alluvial sequences of central western Argentina is encouraged by the occurrence of geochemically distinct tephra verified and dated in this study.
Fil: Toms, Phillip S.. University of London; Reino Unido
Fil: King, Matthew. University of London; Reino Unido
Fil: Zárate, Marcelo Arístides. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa; Argentina
Fil: Kemp, Rob A.. University of London; Reino Unido
Fil: Foit Jr., Franklin F.. Washington State University; Estados Unidos
Materia
Alluvial Sequences
Argentina
Mendoza
Optical Dating
Tephrochronology
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:11336/81803

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network_name_str CONICET Digital (CONICET)
spelling Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western ArgentinaToms, Phillip S.King, MatthewZárate, Marcelo ArístidesKemp, Rob A.Foit Jr., Franklin F.Alluvial SequencesArgentinaMendozaOptical DatingTephrochronologyhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The synthesis of paleoclimatic archives provided by loess and alluvial sequences of central Argentina has been hindered by the lack of a cohesive lithostratigraphic framework extending across the Chaco-Pampean plains and catchments of the Rios Desaguadero, Colorado, and Negro. This condition originates in part from the dearth of absolute chronological controls. The occurrence of discrete tephra layers across this region may provide an opportunity to address this deficiency if a tephrochronological framework can be established. The potential of such a project is assessed within the context of a pilot study constrained within alluvial sequences of central western Argentina proximal to potential source vents in the Southern Volcanic Zone. The intersite discrimination and correlation of tephra layers on a geochemical basis is examined, with indirect chronological control for the eruption of each generated by optical dating. Alluvial sediments on either side of each of five tephra units at a type site were dated using the optically stimulated luminescence of fine-silt-sized quartz, thus providing an age control on each tephra (ca. 24,000, 30,000, 32,000, 39,000, and 48,000 yr). The geochemical composition of each tephra was derived. Using these data, tephra layers at other sites in the study area were geochemically analyzed and, in instances of statistical concordance in major oxide structure, correlated to the type site and therefore ascribed ages. This methodology identified a further sixth volcanic event between ca. 24,000 and 30,000 yr not registered by type-site tephras. The extension of this initial tephrochronological framework beyond the alluvial sequences of central western Argentina is encouraged by the occurrence of geochemically distinct tephra verified and dated in this study.Fil: Toms, Phillip S.. University of London; Reino UnidoFil: King, Matthew. University of London; Reino UnidoFil: Zárate, Marcelo Arístides. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa; ArgentinaFil: Kemp, Rob A.. University of London; Reino UnidoFil: Foit Jr., Franklin F.. Washington State University; Estados UnidosAcademic Press Inc Elsevier Science2004-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/81803Toms, Phillip S.; King, Matthew; Zárate, Marcelo Arístides; Kemp, Rob A.; Foit Jr., Franklin F.; Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina; Academic Press Inc Elsevier Science; Quaternary Research; 62; 1; 7-2004; 60-750033-5894CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2004.05.005info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/quaternary-research/article/geochemical-characterization-correlation-and-optical-dating-of-tephra-in-alluvial-sequences-of-central-western-argentina/A3A8DE4F94C415CCC7875125B9EDD55Ainfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-10T13:19:18Zoai:ri.conicet.gov.ar:11336/81803instacron: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:34982025-09-10 13:19:18.32CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
title Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
spellingShingle Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
Toms, Phillip S.
Alluvial Sequences
Argentina
Mendoza
Optical Dating
Tephrochronology
title_short Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
title_full Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
title_fullStr Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
title_full_unstemmed Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
title_sort Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina
dc.creator.none.fl_str_mv Toms, Phillip S.
King, Matthew
Zárate, Marcelo Arístides
Kemp, Rob A.
Foit Jr., Franklin F.
author Toms, Phillip S.
author_facet Toms, Phillip S.
King, Matthew
Zárate, Marcelo Arístides
Kemp, Rob A.
Foit Jr., Franklin F.
author_role author
author2 King, Matthew
Zárate, Marcelo Arístides
Kemp, Rob A.
Foit Jr., Franklin F.
author2_role author
author
author
author
dc.subject.none.fl_str_mv Alluvial Sequences
Argentina
Mendoza
Optical Dating
Tephrochronology
topic Alluvial Sequences
Argentina
Mendoza
Optical Dating
Tephrochronology
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The synthesis of paleoclimatic archives provided by loess and alluvial sequences of central Argentina has been hindered by the lack of a cohesive lithostratigraphic framework extending across the Chaco-Pampean plains and catchments of the Rios Desaguadero, Colorado, and Negro. This condition originates in part from the dearth of absolute chronological controls. The occurrence of discrete tephra layers across this region may provide an opportunity to address this deficiency if a tephrochronological framework can be established. The potential of such a project is assessed within the context of a pilot study constrained within alluvial sequences of central western Argentina proximal to potential source vents in the Southern Volcanic Zone. The intersite discrimination and correlation of tephra layers on a geochemical basis is examined, with indirect chronological control for the eruption of each generated by optical dating. Alluvial sediments on either side of each of five tephra units at a type site were dated using the optically stimulated luminescence of fine-silt-sized quartz, thus providing an age control on each tephra (ca. 24,000, 30,000, 32,000, 39,000, and 48,000 yr). The geochemical composition of each tephra was derived. Using these data, tephra layers at other sites in the study area were geochemically analyzed and, in instances of statistical concordance in major oxide structure, correlated to the type site and therefore ascribed ages. This methodology identified a further sixth volcanic event between ca. 24,000 and 30,000 yr not registered by type-site tephras. The extension of this initial tephrochronological framework beyond the alluvial sequences of central western Argentina is encouraged by the occurrence of geochemically distinct tephra verified and dated in this study.
Fil: Toms, Phillip S.. University of London; Reino Unido
Fil: King, Matthew. University of London; Reino Unido
Fil: Zárate, Marcelo Arístides. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de La Pampa; Argentina
Fil: Kemp, Rob A.. University of London; Reino Unido
Fil: Foit Jr., Franklin F.. Washington State University; Estados Unidos
description The synthesis of paleoclimatic archives provided by loess and alluvial sequences of central Argentina has been hindered by the lack of a cohesive lithostratigraphic framework extending across the Chaco-Pampean plains and catchments of the Rios Desaguadero, Colorado, and Negro. This condition originates in part from the dearth of absolute chronological controls. The occurrence of discrete tephra layers across this region may provide an opportunity to address this deficiency if a tephrochronological framework can be established. The potential of such a project is assessed within the context of a pilot study constrained within alluvial sequences of central western Argentina proximal to potential source vents in the Southern Volcanic Zone. The intersite discrimination and correlation of tephra layers on a geochemical basis is examined, with indirect chronological control for the eruption of each generated by optical dating. Alluvial sediments on either side of each of five tephra units at a type site were dated using the optically stimulated luminescence of fine-silt-sized quartz, thus providing an age control on each tephra (ca. 24,000, 30,000, 32,000, 39,000, and 48,000 yr). The geochemical composition of each tephra was derived. Using these data, tephra layers at other sites in the study area were geochemically analyzed and, in instances of statistical concordance in major oxide structure, correlated to the type site and therefore ascribed ages. This methodology identified a further sixth volcanic event between ca. 24,000 and 30,000 yr not registered by type-site tephras. The extension of this initial tephrochronological framework beyond the alluvial sequences of central western Argentina is encouraged by the occurrence of geochemically distinct tephra verified and dated in this study.
publishDate 2004
dc.date.none.fl_str_mv 2004-07
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/11336/81803
Toms, Phillip S.; King, Matthew; Zárate, Marcelo Arístides; Kemp, Rob A.; Foit Jr., Franklin F.; Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina; Academic Press Inc Elsevier Science; Quaternary Research; 62; 1; 7-2004; 60-75
0033-5894
CONICET Digital
CONICET
url http://hdl.handle.net/11336/81803
identifier_str_mv Toms, Phillip S.; King, Matthew; Zárate, Marcelo Arístides; Kemp, Rob A.; Foit Jr., Franklin F.; Geochemical characterization, correlation, and optical dating of tephra in alluvial sequences of central western Argentina; Academic Press Inc Elsevier Science; Quaternary Research; 62; 1; 7-2004; 60-75
0033-5894
CONICET Digital
CONICET
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.2004.05.005
info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/quaternary-research/article/geochemical-characterization-correlation-and-optical-dating-of-tephra-in-alluvial-sequences-of-central-western-argentina/A3A8DE4F94C415CCC7875125B9EDD55A
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
dc.publisher.none.fl_str_mv Academic Press Inc Elsevier Science
publisher.none.fl_str_mv Academic Press Inc 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)
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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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