Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina
- Autores
- Gogorza, Claudia Susana; Lirio, J. M.; Nuñez, H.; Chaparro, Marcos Adrián Eduardo; Bertorello, Hector Raul; Sinito, Ana Maria
- Año de publicación
- 2004
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Relative changes in geomagnetic field intensity over the last 16,000 years BP were recovered from the study of four cores obtained from Lake Escondido (South Argentina). Rock magnetic analysis shows that the main magnetic mineral is magnetite, the concentrations being mainly between 0.01 and 0.1%, and the grain size between 1 and 8_m. In order to fulfil the criteria for assessing the reliability of paleointensity data derived from sediments [Rev. Geophys. 31 (1993) 319], the samples whose concentrations and size are beyond this range were rejected. The remanent magnetisation at 20mT(NRM20mT)was normalised using the anhysteric remanent magnetisation (ARM100mT), the saturation of the isothermal remanent magnetisation (SIRM) and the low field magnetic susceptibility (k). Coherence function analysis indicates that the records are not significantly affected by local environmental conditions. This suggests that the variations in normalised remanence are mostly likely due to geomagnetic paleointensity fluctuations. ARM100mT is the best normaliser for the Lake Escondido sediments. The record of relative paleointensity (NRM20mT/ARM100mT) shows peaks and troughs whose amplitudes are similar to those in the St. Lawrence Estuary, Lake Baikal, Lake Pepin and Larsen-A Ice shelf data set and a stack of archeomagnetic data given as virtual axial dipole moment (VADM).
Fil: Gogorza, Claudia Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; Argentina
Fil: Lirio, J. M.. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina
Fil: Nuñez, H.. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina
Fil: Chaparro, Marcos Adrián Eduardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; Argentina
Fil: Bertorello, Hector Raul. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía y Física; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba; Argentina
Fil: Sinito, Ana Maria. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; Argentina - Materia
-
RELATIVE PALEOINTENSITY
HOLOCENE
SOUTH AMERICA
LAKE ESCONDIDO
COHERENCE - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/242567
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Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, ArgentinaGogorza, Claudia SusanaLirio, J. M.Nuñez, H.Chaparro, Marcos Adrián EduardoBertorello, Hector RaulSinito, Ana MariaRELATIVE PALEOINTENSITYHOLOCENESOUTH AMERICALAKE ESCONDIDOCOHERENCEhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Relative changes in geomagnetic field intensity over the last 16,000 years BP were recovered from the study of four cores obtained from Lake Escondido (South Argentina). Rock magnetic analysis shows that the main magnetic mineral is magnetite, the concentrations being mainly between 0.01 and 0.1%, and the grain size between 1 and 8_m. In order to fulfil the criteria for assessing the reliability of paleointensity data derived from sediments [Rev. Geophys. 31 (1993) 319], the samples whose concentrations and size are beyond this range were rejected. The remanent magnetisation at 20mT(NRM20mT)was normalised using the anhysteric remanent magnetisation (ARM100mT), the saturation of the isothermal remanent magnetisation (SIRM) and the low field magnetic susceptibility (k). Coherence function analysis indicates that the records are not significantly affected by local environmental conditions. This suggests that the variations in normalised remanence are mostly likely due to geomagnetic paleointensity fluctuations. ARM100mT is the best normaliser for the Lake Escondido sediments. The record of relative paleointensity (NRM20mT/ARM100mT) shows peaks and troughs whose amplitudes are similar to those in the St. Lawrence Estuary, Lake Baikal, Lake Pepin and Larsen-A Ice shelf data set and a stack of archeomagnetic data given as virtual axial dipole moment (VADM).Fil: Gogorza, Claudia Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; ArgentinaFil: Lirio, J. M.. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; ArgentinaFil: Nuñez, H.. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; ArgentinaFil: Chaparro, Marcos Adrián Eduardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; ArgentinaFil: Bertorello, Hector Raul. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía y Física; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba; ArgentinaFil: Sinito, Ana Maria. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; ArgentinaElsevier Science2004-07info: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/11336/242567Gogorza, Claudia Susana; Lirio, J. M.; Nuñez, H.; Chaparro, Marcos Adrián Eduardo; Bertorello, Hector Raul; et al.; Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina; Elsevier Science; Physics of the Earth and Planetary Interiors; 145; 1-4; 7-2004; 219-2380031-9201CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0031920104001670info:eu-repo/semantics/altIdentifier/doi/10.1016/j.pepi.2004.03.010info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:33:07Zoai:ri.conicet.gov.ar:11336/242567instacron: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 09:33:07.448CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina |
title |
Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina |
spellingShingle |
Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina Gogorza, Claudia Susana RELATIVE PALEOINTENSITY HOLOCENE SOUTH AMERICA LAKE ESCONDIDO COHERENCE |
title_short |
Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina |
title_full |
Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina |
title_fullStr |
Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina |
title_full_unstemmed |
Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina |
title_sort |
Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina |
dc.creator.none.fl_str_mv |
Gogorza, Claudia Susana Lirio, J. M. Nuñez, H. Chaparro, Marcos Adrián Eduardo Bertorello, Hector Raul Sinito, Ana Maria |
author |
Gogorza, Claudia Susana |
author_facet |
Gogorza, Claudia Susana Lirio, J. M. Nuñez, H. Chaparro, Marcos Adrián Eduardo Bertorello, Hector Raul Sinito, Ana Maria |
author_role |
author |
author2 |
Lirio, J. M. Nuñez, H. Chaparro, Marcos Adrián Eduardo Bertorello, Hector Raul Sinito, Ana Maria |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
RELATIVE PALEOINTENSITY HOLOCENE SOUTH AMERICA LAKE ESCONDIDO COHERENCE |
topic |
RELATIVE PALEOINTENSITY HOLOCENE SOUTH AMERICA LAKE ESCONDIDO COHERENCE |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Relative changes in geomagnetic field intensity over the last 16,000 years BP were recovered from the study of four cores obtained from Lake Escondido (South Argentina). Rock magnetic analysis shows that the main magnetic mineral is magnetite, the concentrations being mainly between 0.01 and 0.1%, and the grain size between 1 and 8_m. In order to fulfil the criteria for assessing the reliability of paleointensity data derived from sediments [Rev. Geophys. 31 (1993) 319], the samples whose concentrations and size are beyond this range were rejected. The remanent magnetisation at 20mT(NRM20mT)was normalised using the anhysteric remanent magnetisation (ARM100mT), the saturation of the isothermal remanent magnetisation (SIRM) and the low field magnetic susceptibility (k). Coherence function analysis indicates that the records are not significantly affected by local environmental conditions. This suggests that the variations in normalised remanence are mostly likely due to geomagnetic paleointensity fluctuations. ARM100mT is the best normaliser for the Lake Escondido sediments. The record of relative paleointensity (NRM20mT/ARM100mT) shows peaks and troughs whose amplitudes are similar to those in the St. Lawrence Estuary, Lake Baikal, Lake Pepin and Larsen-A Ice shelf data set and a stack of archeomagnetic data given as virtual axial dipole moment (VADM). Fil: Gogorza, Claudia Susana. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; Argentina Fil: Lirio, J. M.. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina Fil: Nuñez, H.. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina Fil: Chaparro, Marcos Adrián Eduardo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; Argentina. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; Argentina Fil: Bertorello, Hector Raul. Universidad Nacional de Córdoba. Facultad de Matemática, Astronomía y Física; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba; Argentina Fil: Sinito, Ana Maria. Universidad Nacional del Centro de la Provincia de Buenos Aires. Facultad de Ciencias Exactas. Instituto de Física Arroyo Seco; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tandil; Argentina |
description |
Relative changes in geomagnetic field intensity over the last 16,000 years BP were recovered from the study of four cores obtained from Lake Escondido (South Argentina). Rock magnetic analysis shows that the main magnetic mineral is magnetite, the concentrations being mainly between 0.01 and 0.1%, and the grain size between 1 and 8_m. In order to fulfil the criteria for assessing the reliability of paleointensity data derived from sediments [Rev. Geophys. 31 (1993) 319], the samples whose concentrations and size are beyond this range were rejected. The remanent magnetisation at 20mT(NRM20mT)was normalised using the anhysteric remanent magnetisation (ARM100mT), the saturation of the isothermal remanent magnetisation (SIRM) and the low field magnetic susceptibility (k). Coherence function analysis indicates that the records are not significantly affected by local environmental conditions. This suggests that the variations in normalised remanence are mostly likely due to geomagnetic paleointensity fluctuations. ARM100mT is the best normaliser for the Lake Escondido sediments. The record of relative paleointensity (NRM20mT/ARM100mT) shows peaks and troughs whose amplitudes are similar to those in the St. Lawrence Estuary, Lake Baikal, Lake Pepin and Larsen-A Ice shelf data set and a stack of archeomagnetic data given as virtual axial dipole moment (VADM). |
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/11336/242567 Gogorza, Claudia Susana; Lirio, J. M.; Nuñez, H.; Chaparro, Marcos Adrián Eduardo; Bertorello, Hector Raul; et al.; Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina; Elsevier Science; Physics of the Earth and Planetary Interiors; 145; 1-4; 7-2004; 219-238 0031-9201 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/242567 |
identifier_str_mv |
Gogorza, Claudia Susana; Lirio, J. M.; Nuñez, H.; Chaparro, Marcos Adrián Eduardo; Bertorello, Hector Raul; et al.; Paleointensity studies on Holocene–Pleistocene sediments from lake Escondido, Argentina; Elsevier Science; Physics of the Earth and Planetary Interiors; 145; 1-4; 7-2004; 219-238 0031-9201 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0031920104001670 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.pepi.2004.03.010 |
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 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 |
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1844613015012376576 |
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13.070432 |