Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes
- Autores
- Fernández, Marilén; San Martín, Cristina Natalia; Ponce, Juan Federico; Bigler, C.; Rydberg, J.
- Año de publicación
- 2022
- Idioma
- inglés
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- In order to analyze environmental and climatic changes during the late Holocene, a lacustrine sediment core was obtained from Laguna Ceniza (54˚ 40’ 38” S; 68˚ 13’ 13” O) located in a hanging valley in the Fuegian Andes (Argentina). The lake is fed by a stream originating from a small cirque glacier located in the valley head. The core (75 cm) was taken close to a delta of the stream and covers the last 2775 cal years BP. Here, we present the preliminary results based on sedimentological, geochemical and diatom data from the upper part of the core (last 1500 cal years BP). The sedimentological analysis shows the presence of six lithofacies: grey silty-sand, reddle silty-sand, laminated sandy-silt, laminated silt, grey clay-silt and white clay-silt. These lithofacies are likely associated to variations in the relative importance of glacier dynamics and mass movement processes from the valley slopes. The geochemical data (ITRAX core scanner) show a general decrease in the Al-Ti towards the top, and throughout the core there are several distinct peaks in Ca-Sr (possibly indicating input from the glacier). The diatom assemblages show a variety of species mainly dominated by Pinnularia microstauron (60 %) and P. interrupta, P. viridiformis, Aulacoseira alpigena, Brachysira huitatorum, Encyonema difficilis, Frustulia aff fuegiana, F. rhomboides and Veigaludwigia urbana in lower frequency (20%). In general, these taxa indicate a freshwater basin with oligotrophic conditions. At 16-17 cm of the core (900 cal years BP), Achnanthidium minutisimum reaches a frequency of 40%, together with an increase of Psammothidium incognitum (28%) and P. confusum (9%). The clear rise in the mentioned diatoms is associated to the reddle silty sand lithofacie, suggesting the occurrence of a highenergy flow event into the lake.
Fil: Fernández, Marilén. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: San Martín, Cristina Natalia. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Ponce, Juan Federico. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina
Fil: Bigler, C.. Universidad de Umea; Suecia
Fil: Rydberg, J.. Universidad de Umea; Suecia
IAL-IPA 2022 meeting: Lagos, Memorias del Territorio
San Carlos de Bariloche
Argentina
International Assosiation of Limnology
International Paleolimnology Assosiation
Municipio de Bariloche
Ministerio de Ciencia y Tecnología e innovación de la Republica Argentina - Materia
-
Diatoms
Geochemestry
Sedimentology
Lakes - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/234780
Ver los metadatos del registro completo
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CONICET Digital (CONICET) |
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Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian AndesFernández, MarilénSan Martín, Cristina NataliaPonce, Juan FedericoBigler, C.Rydberg, J.DiatomsGeochemestrySedimentologyLakeshttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1In order to analyze environmental and climatic changes during the late Holocene, a lacustrine sediment core was obtained from Laguna Ceniza (54˚ 40’ 38” S; 68˚ 13’ 13” O) located in a hanging valley in the Fuegian Andes (Argentina). The lake is fed by a stream originating from a small cirque glacier located in the valley head. The core (75 cm) was taken close to a delta of the stream and covers the last 2775 cal years BP. Here, we present the preliminary results based on sedimentological, geochemical and diatom data from the upper part of the core (last 1500 cal years BP). The sedimentological analysis shows the presence of six lithofacies: grey silty-sand, reddle silty-sand, laminated sandy-silt, laminated silt, grey clay-silt and white clay-silt. These lithofacies are likely associated to variations in the relative importance of glacier dynamics and mass movement processes from the valley slopes. The geochemical data (ITRAX core scanner) show a general decrease in the Al-Ti towards the top, and throughout the core there are several distinct peaks in Ca-Sr (possibly indicating input from the glacier). The diatom assemblages show a variety of species mainly dominated by Pinnularia microstauron (60 %) and P. interrupta, P. viridiformis, Aulacoseira alpigena, Brachysira huitatorum, Encyonema difficilis, Frustulia aff fuegiana, F. rhomboides and Veigaludwigia urbana in lower frequency (20%). In general, these taxa indicate a freshwater basin with oligotrophic conditions. At 16-17 cm of the core (900 cal years BP), Achnanthidium minutisimum reaches a frequency of 40%, together with an increase of Psammothidium incognitum (28%) and P. confusum (9%). The clear rise in the mentioned diatoms is associated to the reddle silty sand lithofacie, suggesting the occurrence of a highenergy flow event into the lake.Fil: Fernández, Marilén. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; ArgentinaFil: San Martín, Cristina Natalia. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Ponce, Juan Federico. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; ArgentinaFil: Bigler, C.. Universidad de Umea; SueciaFil: Rydberg, J.. Universidad de Umea; SueciaIAL-IPA 2022 meeting: Lagos, Memorias del TerritorioSan Carlos de BarilocheArgentinaInternational Assosiation of LimnologyInternational Paleolimnology AssosiationMunicipio de BarilocheMinisterio de Ciencia y Tecnología e innovación de la Republica ArgentinaDigital2022info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectEncuentroBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/234780Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes; IAL-IPA 2022 meeting: Lagos, Memorias del Territorio; San Carlos de Bariloche; Argentina; 2022; 310CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://zenodo.org/records/7305148Internacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T10:24:19Zoai:ri.conicet.gov.ar:11336/234780instacron: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 10:24:19.463CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes |
title |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes |
spellingShingle |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes Fernández, Marilén Diatoms Geochemestry Sedimentology Lakes |
title_short |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes |
title_full |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes |
title_fullStr |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes |
title_full_unstemmed |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes |
title_sort |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes |
dc.creator.none.fl_str_mv |
Fernández, Marilén San Martín, Cristina Natalia Ponce, Juan Federico Bigler, C. Rydberg, J. |
author |
Fernández, Marilén |
author_facet |
Fernández, Marilén San Martín, Cristina Natalia Ponce, Juan Federico Bigler, C. Rydberg, J. |
author_role |
author |
author2 |
San Martín, Cristina Natalia Ponce, Juan Federico Bigler, C. Rydberg, J. |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
Diatoms Geochemestry Sedimentology Lakes |
topic |
Diatoms Geochemestry Sedimentology Lakes |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
In order to analyze environmental and climatic changes during the late Holocene, a lacustrine sediment core was obtained from Laguna Ceniza (54˚ 40’ 38” S; 68˚ 13’ 13” O) located in a hanging valley in the Fuegian Andes (Argentina). The lake is fed by a stream originating from a small cirque glacier located in the valley head. The core (75 cm) was taken close to a delta of the stream and covers the last 2775 cal years BP. Here, we present the preliminary results based on sedimentological, geochemical and diatom data from the upper part of the core (last 1500 cal years BP). The sedimentological analysis shows the presence of six lithofacies: grey silty-sand, reddle silty-sand, laminated sandy-silt, laminated silt, grey clay-silt and white clay-silt. These lithofacies are likely associated to variations in the relative importance of glacier dynamics and mass movement processes from the valley slopes. The geochemical data (ITRAX core scanner) show a general decrease in the Al-Ti towards the top, and throughout the core there are several distinct peaks in Ca-Sr (possibly indicating input from the glacier). The diatom assemblages show a variety of species mainly dominated by Pinnularia microstauron (60 %) and P. interrupta, P. viridiformis, Aulacoseira alpigena, Brachysira huitatorum, Encyonema difficilis, Frustulia aff fuegiana, F. rhomboides and Veigaludwigia urbana in lower frequency (20%). In general, these taxa indicate a freshwater basin with oligotrophic conditions. At 16-17 cm of the core (900 cal years BP), Achnanthidium minutisimum reaches a frequency of 40%, together with an increase of Psammothidium incognitum (28%) and P. confusum (9%). The clear rise in the mentioned diatoms is associated to the reddle silty sand lithofacie, suggesting the occurrence of a highenergy flow event into the lake. Fil: Fernández, Marilén. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina Fil: San Martín, Cristina Natalia. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Ponce, Juan Federico. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina. Universidad Nacional de Tierra del Fuego, Antártida e Islas del Atlántico Sur. Instituto de Ciencias Polares, Ambientales y Recursos Naturales; Argentina Fil: Bigler, C.. Universidad de Umea; Suecia Fil: Rydberg, J.. Universidad de Umea; Suecia IAL-IPA 2022 meeting: Lagos, Memorias del Territorio San Carlos de Bariloche Argentina International Assosiation of Limnology International Paleolimnology Assosiation Municipio de Bariloche Ministerio de Ciencia y Tecnología e innovación de la Republica Argentina |
description |
In order to analyze environmental and climatic changes during the late Holocene, a lacustrine sediment core was obtained from Laguna Ceniza (54˚ 40’ 38” S; 68˚ 13’ 13” O) located in a hanging valley in the Fuegian Andes (Argentina). The lake is fed by a stream originating from a small cirque glacier located in the valley head. The core (75 cm) was taken close to a delta of the stream and covers the last 2775 cal years BP. Here, we present the preliminary results based on sedimentological, geochemical and diatom data from the upper part of the core (last 1500 cal years BP). The sedimentological analysis shows the presence of six lithofacies: grey silty-sand, reddle silty-sand, laminated sandy-silt, laminated silt, grey clay-silt and white clay-silt. These lithofacies are likely associated to variations in the relative importance of glacier dynamics and mass movement processes from the valley slopes. The geochemical data (ITRAX core scanner) show a general decrease in the Al-Ti towards the top, and throughout the core there are several distinct peaks in Ca-Sr (possibly indicating input from the glacier). The diatom assemblages show a variety of species mainly dominated by Pinnularia microstauron (60 %) and P. interrupta, P. viridiformis, Aulacoseira alpigena, Brachysira huitatorum, Encyonema difficilis, Frustulia aff fuegiana, F. rhomboides and Veigaludwigia urbana in lower frequency (20%). In general, these taxa indicate a freshwater basin with oligotrophic conditions. At 16-17 cm of the core (900 cal years BP), Achnanthidium minutisimum reaches a frequency of 40%, together with an increase of Psammothidium incognitum (28%) and P. confusum (9%). The clear rise in the mentioned diatoms is associated to the reddle silty sand lithofacie, suggesting the occurrence of a highenergy flow event into the lake. |
publishDate |
2022 |
dc.date.none.fl_str_mv |
2022 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/conferenceObject Encuentro Book http://purl.org/coar/resource_type/c_5794 info:ar-repo/semantics/documentoDeConferencia |
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publishedVersion |
format |
conferenceObject |
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http://hdl.handle.net/11336/234780 Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes; IAL-IPA 2022 meeting: Lagos, Memorias del Territorio; San Carlos de Bariloche; Argentina; 2022; 310 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/234780 |
identifier_str_mv |
Diatoms, sedimentology and geochemistry study from a high altitude lake in the Fuegian Andes; IAL-IPA 2022 meeting: Lagos, Memorias del Territorio; San Carlos de Bariloche; Argentina; 2022; 310 CONICET Digital CONICET |
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eng |
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eng |
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https://creativecommons.org/licenses/by/2.5/ar/ |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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