Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)

Autores
Olhendorf, C.; Fey, Michael; Massaferro, Julieta; Haberzettl, Torsten; Laprida, Cecilia; Lücke, A.; Maidana, Nora Irene; Mayr, Christoph; Oehlerich, M.; Ramón Mercau, María Josefina; Wille, Michael; Corbella, Hugo; St Onge, G.; Schäbitz, F.; Zolitschka, Bernd
Año de publicación
2014
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-proxy analyses of sediment cores from the volcanic crater lake of Laguna Cháltel (50°S, 71°W). The chronology is based on AMS 14C age modeling constrained by paleomagnetic secular variations. Chemical and physical properties of the lake water together with results of lake-water surface-temperature monitoring, as well as sediment characteristics reveal conspicuous features archived as different sedimentary carbonate phases and morphologies which are attributed to lake-level changes. Sedimentological, geochemical and biological proxies together suggest the development from an initial playa lake-phase towards a system with progressively rising lake level. In detail, proxies indicate the existence of an ephemeral lake since 4700 cal BP until a glauberite-bearing carbonate crust formed around 4040 cal BP which probably is associated to the globally recognized 4.2 ka event. This crust is interpreted as a desiccation event terminating the ephemeral lake phase. Following this desiccation a shift towards conditions with a positive hydrological balance of Laguna Cháltel occurs, which leads to the development of a saline lake with ooid formation between 4040 and 3200 cal BP. Further lake-level increase with initially high minerogenic input until 2700 cal BP resulted in a lake freshening which allowed the preservation of diatoms. Sigmoidal and star shaped carbonate crystals occurred until 1720 cal BP indicating a syn- or post-depositional formation of ikaite. Anoxic conditions and increased deposition of clay and sand through fluvial and eolian input are interpreted as a further lake-level rise and/or a prolonged winter ice cover culminating during the Little Ice Age. The highest lake level was probably reached at that time and since then dropped to its present day height. Previous studies have shown that the southern hemisphere westerly winds (SWW) exert an oppositional control on hydrological regimes at the eastern and the western sides of the Patagonian Andes. At Laguna Cháltel SWW forcing is changing evaporation rates by varying wind intensities, air temperatures and lake ice coverages as well as by precipitation rates (easterly vs. westerly sources of moisture). Our data suggests that the lake-level history of Laguna Cháltel reflects changes in the SWW during the last 4.7 ka on the eastern side of the Andes. However, the elevated location of Laguna Cháltel on an 800 m high plateau at the leeward side of the Andes potentially leads to a local overprint of the SWW influence on the hydrological balance.
Fil: Olhendorf, C.. Universitat Bremen; Alemania
Fil: Fey, Michael. Universitat Bremen; Alemania
Fil: Massaferro, Julieta. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Administracion de Parques Nacionales; Argentina
Fil: Haberzettl, Torsten. Universitat Jena; Alemania
Fil: Laprida, Cecilia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Lücke, A.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania
Fil: Maidana, Nora Irene. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Mayr, Christoph. Universitat Erlangen-Nuremberg; Alemania. Ludwig Maximilians Universitat; Alemania
Fil: Oehlerich, M.. Ludwig Maximilians Universitat; Alemania
Fil: Ramón Mercau, María Josefina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Wille, Michael. Universitat Zu Köln; Alemania
Fil: Corbella, Hugo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentina
Fil: St Onge, G.. Institut Des Sciences de la Mer de Rimouski; Canadá
Fil: Schäbitz, F.. Universitat Zu Köln; Alemania
Fil: Zolitschka, Bernd. Universitat Bremen; Alemania
Materia
Lacustrine Ooids And Pseudomorphs After Ikaite
Multiple Dating
Bioproxies
Xrf Scanning
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:11336/29593

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oai_identifier_str oai:ri.conicet.gov.ar:11336/29593
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network_name_str CONICET Digital (CONICET)
spelling Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)Olhendorf, C.Fey, MichaelMassaferro, JulietaHaberzettl, TorstenLaprida, CeciliaLücke, A.Maidana, Nora IreneMayr, ChristophOehlerich, M.Ramón Mercau, María JosefinaWille, MichaelCorbella, HugoSt Onge, G.Schäbitz, F.Zolitschka, BerndLacustrine Ooids And Pseudomorphs After IkaiteMultiple DatingBioproxiesXrf Scanninghttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-proxy analyses of sediment cores from the volcanic crater lake of Laguna Cháltel (50°S, 71°W). The chronology is based on AMS 14C age modeling constrained by paleomagnetic secular variations. Chemical and physical properties of the lake water together with results of lake-water surface-temperature monitoring, as well as sediment characteristics reveal conspicuous features archived as different sedimentary carbonate phases and morphologies which are attributed to lake-level changes. Sedimentological, geochemical and biological proxies together suggest the development from an initial playa lake-phase towards a system with progressively rising lake level. In detail, proxies indicate the existence of an ephemeral lake since 4700 cal BP until a glauberite-bearing carbonate crust formed around 4040 cal BP which probably is associated to the globally recognized 4.2 ka event. This crust is interpreted as a desiccation event terminating the ephemeral lake phase. Following this desiccation a shift towards conditions with a positive hydrological balance of Laguna Cháltel occurs, which leads to the development of a saline lake with ooid formation between 4040 and 3200 cal BP. Further lake-level increase with initially high minerogenic input until 2700 cal BP resulted in a lake freshening which allowed the preservation of diatoms. Sigmoidal and star shaped carbonate crystals occurred until 1720 cal BP indicating a syn- or post-depositional formation of ikaite. Anoxic conditions and increased deposition of clay and sand through fluvial and eolian input are interpreted as a further lake-level rise and/or a prolonged winter ice cover culminating during the Little Ice Age. The highest lake level was probably reached at that time and since then dropped to its present day height. Previous studies have shown that the southern hemisphere westerly winds (SWW) exert an oppositional control on hydrological regimes at the eastern and the western sides of the Patagonian Andes. At Laguna Cháltel SWW forcing is changing evaporation rates by varying wind intensities, air temperatures and lake ice coverages as well as by precipitation rates (easterly vs. westerly sources of moisture). Our data suggests that the lake-level history of Laguna Cháltel reflects changes in the SWW during the last 4.7 ka on the eastern side of the Andes. However, the elevated location of Laguna Cháltel on an 800 m high plateau at the leeward side of the Andes potentially leads to a local overprint of the SWW influence on the hydrological balance.Fil: Olhendorf, C.. Universitat Bremen; AlemaniaFil: Fey, Michael. Universitat Bremen; AlemaniaFil: Massaferro, Julieta. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Administracion de Parques Nacionales; ArgentinaFil: Haberzettl, Torsten. Universitat Jena; AlemaniaFil: Laprida, Cecilia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Lücke, A.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; AlemaniaFil: Maidana, Nora Irene. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Mayr, Christoph. Universitat Erlangen-Nuremberg; Alemania. Ludwig Maximilians Universitat; AlemaniaFil: Oehlerich, M.. Ludwig Maximilians Universitat; AlemaniaFil: Ramón Mercau, María Josefina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Wille, Michael. Universitat Zu Köln; AlemaniaFil: Corbella, Hugo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; ArgentinaFil: St Onge, G.. Institut Des Sciences de la Mer de Rimouski; CanadáFil: Schäbitz, F.. Universitat Zu Köln; AlemaniaFil: Zolitschka, Bernd. Universitat Bremen; AlemaniaElsevier Science2014-07info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/29593Olhendorf, C.; Fey, Michael; Massaferro, Julieta; Haberzettl, Torsten; Laprida, Cecilia; et al.; Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina); Elsevier Science; Palaeogeography, Palaeoclimatology, Palaeoecology; 411; 7-2014; 229-2480031-0182CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.palaeo.2014.06.030info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0031018214003423info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:35:26Zoai:ri.conicet.gov.ar:11336/29593instacron: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 10:35:27.068CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
title Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
spellingShingle Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
Olhendorf, C.
Lacustrine Ooids And Pseudomorphs After Ikaite
Multiple Dating
Bioproxies
Xrf Scanning
title_short Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
title_full Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
title_fullStr Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
title_full_unstemmed Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
title_sort Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
dc.creator.none.fl_str_mv Olhendorf, C.
Fey, Michael
Massaferro, Julieta
Haberzettl, Torsten
Laprida, Cecilia
Lücke, A.
Maidana, Nora Irene
Mayr, Christoph
Oehlerich, M.
Ramón Mercau, María Josefina
Wille, Michael
Corbella, Hugo
St Onge, G.
Schäbitz, F.
Zolitschka, Bernd
author Olhendorf, C.
author_facet Olhendorf, C.
Fey, Michael
Massaferro, Julieta
Haberzettl, Torsten
Laprida, Cecilia
Lücke, A.
Maidana, Nora Irene
Mayr, Christoph
Oehlerich, M.
Ramón Mercau, María Josefina
Wille, Michael
Corbella, Hugo
St Onge, G.
Schäbitz, F.
Zolitschka, Bernd
author_role author
author2 Fey, Michael
Massaferro, Julieta
Haberzettl, Torsten
Laprida, Cecilia
Lücke, A.
Maidana, Nora Irene
Mayr, Christoph
Oehlerich, M.
Ramón Mercau, María Josefina
Wille, Michael
Corbella, Hugo
St Onge, G.
Schäbitz, F.
Zolitschka, Bernd
author2_role author
author
author
author
author
author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv Lacustrine Ooids And Pseudomorphs After Ikaite
Multiple Dating
Bioproxies
Xrf Scanning
topic Lacustrine Ooids And Pseudomorphs After Ikaite
Multiple Dating
Bioproxies
Xrf Scanning
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-proxy analyses of sediment cores from the volcanic crater lake of Laguna Cháltel (50°S, 71°W). The chronology is based on AMS 14C age modeling constrained by paleomagnetic secular variations. Chemical and physical properties of the lake water together with results of lake-water surface-temperature monitoring, as well as sediment characteristics reveal conspicuous features archived as different sedimentary carbonate phases and morphologies which are attributed to lake-level changes. Sedimentological, geochemical and biological proxies together suggest the development from an initial playa lake-phase towards a system with progressively rising lake level. In detail, proxies indicate the existence of an ephemeral lake since 4700 cal BP until a glauberite-bearing carbonate crust formed around 4040 cal BP which probably is associated to the globally recognized 4.2 ka event. This crust is interpreted as a desiccation event terminating the ephemeral lake phase. Following this desiccation a shift towards conditions with a positive hydrological balance of Laguna Cháltel occurs, which leads to the development of a saline lake with ooid formation between 4040 and 3200 cal BP. Further lake-level increase with initially high minerogenic input until 2700 cal BP resulted in a lake freshening which allowed the preservation of diatoms. Sigmoidal and star shaped carbonate crystals occurred until 1720 cal BP indicating a syn- or post-depositional formation of ikaite. Anoxic conditions and increased deposition of clay and sand through fluvial and eolian input are interpreted as a further lake-level rise and/or a prolonged winter ice cover culminating during the Little Ice Age. The highest lake level was probably reached at that time and since then dropped to its present day height. Previous studies have shown that the southern hemisphere westerly winds (SWW) exert an oppositional control on hydrological regimes at the eastern and the western sides of the Patagonian Andes. At Laguna Cháltel SWW forcing is changing evaporation rates by varying wind intensities, air temperatures and lake ice coverages as well as by precipitation rates (easterly vs. westerly sources of moisture). Our data suggests that the lake-level history of Laguna Cháltel reflects changes in the SWW during the last 4.7 ka on the eastern side of the Andes. However, the elevated location of Laguna Cháltel on an 800 m high plateau at the leeward side of the Andes potentially leads to a local overprint of the SWW influence on the hydrological balance.
Fil: Olhendorf, C.. Universitat Bremen; Alemania
Fil: Fey, Michael. Universitat Bremen; Alemania
Fil: Massaferro, Julieta. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Administracion de Parques Nacionales; Argentina
Fil: Haberzettl, Torsten. Universitat Jena; Alemania
Fil: Laprida, Cecilia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Lücke, A.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania
Fil: Maidana, Nora Irene. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Mayr, Christoph. Universitat Erlangen-Nuremberg; Alemania. Ludwig Maximilians Universitat; Alemania
Fil: Oehlerich, M.. Ludwig Maximilians Universitat; Alemania
Fil: Ramón Mercau, María Josefina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Wille, Michael. Universitat Zu Köln; Alemania
Fil: Corbella, Hugo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentina
Fil: St Onge, G.. Institut Des Sciences de la Mer de Rimouski; Canadá
Fil: Schäbitz, F.. Universitat Zu Köln; Alemania
Fil: Zolitschka, Bernd. Universitat Bremen; Alemania
description Hydrological changes that occurred during the last 4700 years have been reconstructed using multi-proxy analyses of sediment cores from the volcanic crater lake of Laguna Cháltel (50°S, 71°W). The chronology is based on AMS 14C age modeling constrained by paleomagnetic secular variations. Chemical and physical properties of the lake water together with results of lake-water surface-temperature monitoring, as well as sediment characteristics reveal conspicuous features archived as different sedimentary carbonate phases and morphologies which are attributed to lake-level changes. Sedimentological, geochemical and biological proxies together suggest the development from an initial playa lake-phase towards a system with progressively rising lake level. In detail, proxies indicate the existence of an ephemeral lake since 4700 cal BP until a glauberite-bearing carbonate crust formed around 4040 cal BP which probably is associated to the globally recognized 4.2 ka event. This crust is interpreted as a desiccation event terminating the ephemeral lake phase. Following this desiccation a shift towards conditions with a positive hydrological balance of Laguna Cháltel occurs, which leads to the development of a saline lake with ooid formation between 4040 and 3200 cal BP. Further lake-level increase with initially high minerogenic input until 2700 cal BP resulted in a lake freshening which allowed the preservation of diatoms. Sigmoidal and star shaped carbonate crystals occurred until 1720 cal BP indicating a syn- or post-depositional formation of ikaite. Anoxic conditions and increased deposition of clay and sand through fluvial and eolian input are interpreted as a further lake-level rise and/or a prolonged winter ice cover culminating during the Little Ice Age. The highest lake level was probably reached at that time and since then dropped to its present day height. Previous studies have shown that the southern hemisphere westerly winds (SWW) exert an oppositional control on hydrological regimes at the eastern and the western sides of the Patagonian Andes. At Laguna Cháltel SWW forcing is changing evaporation rates by varying wind intensities, air temperatures and lake ice coverages as well as by precipitation rates (easterly vs. westerly sources of moisture). Our data suggests that the lake-level history of Laguna Cháltel reflects changes in the SWW during the last 4.7 ka on the eastern side of the Andes. However, the elevated location of Laguna Cháltel on an 800 m high plateau at the leeward side of the Andes potentially leads to a local overprint of the SWW influence on the hydrological balance.
publishDate 2014
dc.date.none.fl_str_mv 2014-07
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/11336/29593
Olhendorf, C.; Fey, Michael; Massaferro, Julieta; Haberzettl, Torsten; Laprida, Cecilia; et al.; Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina); Elsevier Science; Palaeogeography, Palaeoclimatology, Palaeoecology; 411; 7-2014; 229-248
0031-0182
CONICET Digital
CONICET
url http://hdl.handle.net/11336/29593
identifier_str_mv Olhendorf, C.; Fey, Michael; Massaferro, Julieta; Haberzettl, Torsten; Laprida, Cecilia; et al.; Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina); Elsevier Science; Palaeogeography, Palaeoclimatology, Palaeoecology; 411; 7-2014; 229-248
0031-0182
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.palaeo.2014.06.030
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0031018214003423
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/
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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)
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repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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