Cosmic spherules from the Ordovician of Argentina
- Autores
- Voldman, Gustavo Gabriel; Genge, G. L.; Albanesi, Guillermo Luis; Barnes, C. R.; Ortega, Gladys del Carmen
- Año de publicación
- 2013
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The discovery of magnetic spherules in acid-insoluble residues from conodont samples encouraged a systematic search for Ordovician micrometeorites from Northwestern Argentina. Some 220 melted micrometeorites were recovered from the magnetic fraction of 6 samples (total rock weight: 23 kg) from the Cordillera Oriental (Santa Rosita Formation) and 17 from 5 samples (total rock weight: 8.9 kg) from the Argentine Precordillera (Las Aguaditas, Gualcamayo and Las Vacas formations). The specimens resemble I-type cosmic spherules, in their chemistry and distinct dendritic and polygonal crystalline structures. They represent a flux of micrometeorites several orders of magnitude greater than present. The wide differences in spherule abundance between the Precordillera and the Cordillera Oriental samples could reflect uncertainties in the sedimentary rates or temporal variations in the flux of extraterrestrial matter to Earth. The micrometeorite-bearing formations span the late Tremadocian to the late Darriliwian (~480-460 Ma), which is consistent with a period of elevated flux of extraterrestrial material, as recorded several thousand kilometres away from coeval horizons in Scotland, Sweden and central China.
Fil: Voldman, Gustavo Gabriel. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Genge, G. L.. Imperial College London; Reino Unido
Fil: Albanesi, Guillermo Luis. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina
Fil: Barnes, C. R.. Scholl Of Earth And Ocean Sciences; Canadá
Fil: Ortega, Gladys del Carmen. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Museo de Paleontología; Argentina - Materia
-
MICROSPHERULES
COSMIC DUST
ORDOVICIAN
CORDILLERA ORIENTAL
PRECORDILLERA
ARGENTINA - 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:11336/181476
Ver los metadatos del registro completo
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Cosmic spherules from the Ordovician of ArgentinaVoldman, Gustavo GabrielGenge, G. L.Albanesi, Guillermo LuisBarnes, C. R.Ortega, Gladys del CarmenMICROSPHERULESCOSMIC DUSTORDOVICIANCORDILLERA ORIENTALPRECORDILLERAARGENTINAhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The discovery of magnetic spherules in acid-insoluble residues from conodont samples encouraged a systematic search for Ordovician micrometeorites from Northwestern Argentina. Some 220 melted micrometeorites were recovered from the magnetic fraction of 6 samples (total rock weight: 23 kg) from the Cordillera Oriental (Santa Rosita Formation) and 17 from 5 samples (total rock weight: 8.9 kg) from the Argentine Precordillera (Las Aguaditas, Gualcamayo and Las Vacas formations). The specimens resemble I-type cosmic spherules, in their chemistry and distinct dendritic and polygonal crystalline structures. They represent a flux of micrometeorites several orders of magnitude greater than present. The wide differences in spherule abundance between the Precordillera and the Cordillera Oriental samples could reflect uncertainties in the sedimentary rates or temporal variations in the flux of extraterrestrial matter to Earth. The micrometeorite-bearing formations span the late Tremadocian to the late Darriliwian (~480-460 Ma), which is consistent with a period of elevated flux of extraterrestrial material, as recorded several thousand kilometres away from coeval horizons in Scotland, Sweden and central China. Fil: Voldman, Gustavo Gabriel. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; ArgentinaFil: Genge, G. L.. Imperial College London; Reino UnidoFil: Albanesi, Guillermo Luis. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; ArgentinaFil: Barnes, C. R.. Scholl Of Earth And Ocean Sciences; CanadáFil: Ortega, Gladys del Carmen. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Museo de Paleontología; ArgentinaJohn Wiley & Sons Ltd2013-03-01info: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/11336/181476Voldman, Gustavo Gabriel; Genge, G. L.; Albanesi, Guillermo Luis; Barnes, C. R.; Ortega, Gladys del Carmen; Cosmic spherules from the Ordovician of Argentina; John Wiley & Sons Ltd; Geological Journal (Chichester); 48; 2-3; 1-3-2013; 222-2350072-10501099-1034CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/gj.2418/abstractinfo:eu-repo/semantics/altIdentifier/doi/10.1002/gj.2418/abstractinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:04:48Zoai:ri.conicet.gov.ar:11336/181476instacron: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:34982025-09-03 10:04:48.818CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Cosmic spherules from the Ordovician of Argentina |
title |
Cosmic spherules from the Ordovician of Argentina |
spellingShingle |
Cosmic spherules from the Ordovician of Argentina Voldman, Gustavo Gabriel MICROSPHERULES COSMIC DUST ORDOVICIAN CORDILLERA ORIENTAL PRECORDILLERA ARGENTINA |
title_short |
Cosmic spherules from the Ordovician of Argentina |
title_full |
Cosmic spherules from the Ordovician of Argentina |
title_fullStr |
Cosmic spherules from the Ordovician of Argentina |
title_full_unstemmed |
Cosmic spherules from the Ordovician of Argentina |
title_sort |
Cosmic spherules from the Ordovician of Argentina |
dc.creator.none.fl_str_mv |
Voldman, Gustavo Gabriel Genge, G. L. Albanesi, Guillermo Luis Barnes, C. R. Ortega, Gladys del Carmen |
author |
Voldman, Gustavo Gabriel |
author_facet |
Voldman, Gustavo Gabriel Genge, G. L. Albanesi, Guillermo Luis Barnes, C. R. Ortega, Gladys del Carmen |
author_role |
author |
author2 |
Genge, G. L. Albanesi, Guillermo Luis Barnes, C. R. Ortega, Gladys del Carmen |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
MICROSPHERULES COSMIC DUST ORDOVICIAN CORDILLERA ORIENTAL PRECORDILLERA ARGENTINA |
topic |
MICROSPHERULES COSMIC DUST ORDOVICIAN CORDILLERA ORIENTAL PRECORDILLERA ARGENTINA |
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 discovery of magnetic spherules in acid-insoluble residues from conodont samples encouraged a systematic search for Ordovician micrometeorites from Northwestern Argentina. Some 220 melted micrometeorites were recovered from the magnetic fraction of 6 samples (total rock weight: 23 kg) from the Cordillera Oriental (Santa Rosita Formation) and 17 from 5 samples (total rock weight: 8.9 kg) from the Argentine Precordillera (Las Aguaditas, Gualcamayo and Las Vacas formations). The specimens resemble I-type cosmic spherules, in their chemistry and distinct dendritic and polygonal crystalline structures. They represent a flux of micrometeorites several orders of magnitude greater than present. The wide differences in spherule abundance between the Precordillera and the Cordillera Oriental samples could reflect uncertainties in the sedimentary rates or temporal variations in the flux of extraterrestrial matter to Earth. The micrometeorite-bearing formations span the late Tremadocian to the late Darriliwian (~480-460 Ma), which is consistent with a period of elevated flux of extraterrestrial material, as recorded several thousand kilometres away from coeval horizons in Scotland, Sweden and central China. Fil: Voldman, Gustavo Gabriel. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina Fil: Genge, G. L.. Imperial College London; Reino Unido Fil: Albanesi, Guillermo Luis. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina Fil: Barnes, C. R.. Scholl Of Earth And Ocean Sciences; Canadá Fil: Ortega, Gladys del Carmen. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Departamento de Geologia Básica y Aplicada; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas, Físicas y Naturales. Museo de Paleontología; Argentina |
description |
The discovery of magnetic spherules in acid-insoluble residues from conodont samples encouraged a systematic search for Ordovician micrometeorites from Northwestern Argentina. Some 220 melted micrometeorites were recovered from the magnetic fraction of 6 samples (total rock weight: 23 kg) from the Cordillera Oriental (Santa Rosita Formation) and 17 from 5 samples (total rock weight: 8.9 kg) from the Argentine Precordillera (Las Aguaditas, Gualcamayo and Las Vacas formations). The specimens resemble I-type cosmic spherules, in their chemistry and distinct dendritic and polygonal crystalline structures. They represent a flux of micrometeorites several orders of magnitude greater than present. The wide differences in spherule abundance between the Precordillera and the Cordillera Oriental samples could reflect uncertainties in the sedimentary rates or temporal variations in the flux of extraterrestrial matter to Earth. The micrometeorite-bearing formations span the late Tremadocian to the late Darriliwian (~480-460 Ma), which is consistent with a period of elevated flux of extraterrestrial material, as recorded several thousand kilometres away from coeval horizons in Scotland, Sweden and central China. |
publishDate |
2013 |
dc.date.none.fl_str_mv |
2013-03-01 |
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/11336/181476 Voldman, Gustavo Gabriel; Genge, G. L.; Albanesi, Guillermo Luis; Barnes, C. R.; Ortega, Gladys del Carmen; Cosmic spherules from the Ordovician of Argentina; John Wiley & Sons Ltd; Geological Journal (Chichester); 48; 2-3; 1-3-2013; 222-235 0072-1050 1099-1034 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/181476 |
identifier_str_mv |
Voldman, Gustavo Gabriel; Genge, G. L.; Albanesi, Guillermo Luis; Barnes, C. R.; Ortega, Gladys del Carmen; Cosmic spherules from the Ordovician of Argentina; John Wiley & Sons Ltd; Geological Journal (Chichester); 48; 2-3; 1-3-2013; 222-235 0072-1050 1099-1034 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://onlinelibrary.wiley.com/doi/10.1002/gj.2418/abstract info:eu-repo/semantics/altIdentifier/doi/10.1002/gj.2418/abstract |
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 |
John Wiley & Sons Ltd |
publisher.none.fl_str_mv |
John Wiley & Sons Ltd |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
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CONICET Digital (CONICET) |
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CONICET Digital (CONICET) |
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Consejo Nacional de Investigaciones Científicas y Técnicas |
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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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1842269877214117888 |
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13.13397 |