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dc.contributor.author
Olhendorf, C.
dc.contributor.author
Fey, Michael
dc.contributor.author
Massaferro, Julieta
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Haberzettl, Torsten
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Laprida, Cecilia
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Lücke, A.
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Maidana, Nora Irene
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Mayr, Christoph
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Oehlerich, M.
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Ramón Mercau, María Josefina
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Wille, Michael
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Corbella, Hugo
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St Onge, G.
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Schäbitz, F.
dc.contributor.author
Zolitschka, Bernd
dc.date.available
2017-12-04T18:42:46Z
dc.date.issued
2014-07
dc.identifier.citation
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
dc.identifier.issn
0031-0182
dc.identifier.uri
http://hdl.handle.net/11336/29593
dc.description.abstract
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.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Elsevier Science
dc.rights
info:eu-repo/semantics/openAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
dc.subject
Lacustrine Ooids And Pseudomorphs After Ikaite
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Multiple Dating
dc.subject
Bioproxies
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Xrf Scanning
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Meteorología y Ciencias Atmosféricas
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Ciencias de la Tierra y relacionadas con el Medio Ambiente
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CIENCIAS NATURALES Y EXACTAS
dc.title
Late Holocene hydrology inferred from lacustrine sediments of Laguna Cháltel (southeastern Argentina)
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2017-06-19T17:27:56Z
dc.journal.volume
411
dc.journal.pagination
229-248
dc.journal.pais
Países Bajos
dc.journal.ciudad
Amsterdam
dc.description.fil
Fil: Olhendorf, C.. Universitat Bremen; Alemania
dc.description.fil
Fil: Fey, Michael. Universitat Bremen; Alemania
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Fil: Massaferro, Julieta. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Administracion de Parques Nacionales; Argentina
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Fil: Haberzettl, Torsten. Universitat Jena; Alemania
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Fil: Laprida, Cecilia. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
dc.description.fil
Fil: Lücke, A.. Helmholtz Gemeinschaft. Forschungszentrum Jülich; Alemania
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Fil: Maidana, Nora Irene. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
dc.description.fil
Fil: Mayr, Christoph. Universitat Erlangen-Nuremberg; Alemania. Ludwig Maximilians Universitat; Alemania
dc.description.fil
Fil: Oehlerich, M.. Ludwig Maximilians Universitat; Alemania
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Fil: Ramón Mercau, María Josefina. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
dc.description.fil
Fil: Wille, Michael. Universitat Zu Köln; Alemania
dc.description.fil
Fil: Corbella, Hugo. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Parque Centenario. Museo Argentino de Ciencias Naturales "Bernardino Rivadavia"; Argentina
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Fil: St Onge, G.. Institut Des Sciences de la Mer de Rimouski; Canadá
dc.description.fil
Fil: Schäbitz, F.. Universitat Zu Köln; Alemania
dc.description.fil
Fil: Zolitschka, Bernd. Universitat Bremen; Alemania
dc.journal.title
Palaeogeography, Palaeoclimatology, Palaeoecology
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.palaeo.2014.06.030
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0031018214003423
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