"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin
- Autores
- Cisterna, Gabriela Adriana; Sterren, Andrea Fabiana
- Año de publicación
- 2010
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The Levipustula Fauna (included in the Levipustula levis Zone) is a relatively diversified fossil assemblage composed of brachiopods, bivalves, bryozoans, gastropods, and crinoids. This fauna usually is associated with glaciomarine sequences related to the Carboniferous glacial event that affected the southwestern Gondwanan margin. The Levipustula Fauna has been identified in different units (e.g., Hoyada Verde, La Capilla, Leoncito, and Yalguaraz Formations) exposed in the Calingasta-Uspallata Basin. The Hoyada Verde Formation, herein proposed as a key section, contains the most complete record of the Levipustula Fauna. A detailed compositional, taphonomic, and paleoecological study of this section allows us to propose two associations within the so-called Levipustula Zone: the "Intraglacial Levipustula Fauna," present in the diamictite-dominated lower part, and the "Postglacial Levipustula Fauna," dominant in the upper part of section. The fossils of the "Intraglacial Levipustula Fauna" are scarce and poorly diversified. These two features suggest environmentally stressed conditions, probably related to low temperatures in areas close to glaciers. In comparison, the "Postglacial Levipustula Fauna," relatively more abundant and diverse, exhibits compositional variations that could be explained by paleoenvironmental changes associated with fluctuations in substratum and food supply, such as those identified in modern ecosystems. The identification of the "Intraglacial Levipustula Fauna" and the "Postglacial Levipustula Fauna" may constitute a new tool for understanding the particular relationship between faunal assemblages and climatic variations linked to the Gondwanan glaciation in the Calingasta-Uspallata Basin. Also, the new "Intraglacial Levipustula Fauna" identified in the Hoyada Verde Formation would have biostratigraphical and paleogeographical implications in intra-and interbasinal correlations.
Fil: Cisterna, Gabriela Adriana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Fundación Miguel Lillo; Argentina
Fil: Sterren, Andrea Fabiana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones Paleobiológicas; Argentina - Materia
-
Levipustula Fauna
Carboniferous
Glacial Event
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:11336/54903
Ver los metadatos del registro completo
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spelling |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan marginCisterna, Gabriela AdrianaSterren, Andrea FabianaLevipustula FaunaCarboniferousGlacial EventArgentinahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Levipustula Fauna (included in the Levipustula levis Zone) is a relatively diversified fossil assemblage composed of brachiopods, bivalves, bryozoans, gastropods, and crinoids. This fauna usually is associated with glaciomarine sequences related to the Carboniferous glacial event that affected the southwestern Gondwanan margin. The Levipustula Fauna has been identified in different units (e.g., Hoyada Verde, La Capilla, Leoncito, and Yalguaraz Formations) exposed in the Calingasta-Uspallata Basin. The Hoyada Verde Formation, herein proposed as a key section, contains the most complete record of the Levipustula Fauna. A detailed compositional, taphonomic, and paleoecological study of this section allows us to propose two associations within the so-called Levipustula Zone: the "Intraglacial Levipustula Fauna," present in the diamictite-dominated lower part, and the "Postglacial Levipustula Fauna," dominant in the upper part of section. The fossils of the "Intraglacial Levipustula Fauna" are scarce and poorly diversified. These two features suggest environmentally stressed conditions, probably related to low temperatures in areas close to glaciers. In comparison, the "Postglacial Levipustula Fauna," relatively more abundant and diverse, exhibits compositional variations that could be explained by paleoenvironmental changes associated with fluctuations in substratum and food supply, such as those identified in modern ecosystems. The identification of the "Intraglacial Levipustula Fauna" and the "Postglacial Levipustula Fauna" may constitute a new tool for understanding the particular relationship between faunal assemblages and climatic variations linked to the Gondwanan glaciation in the Calingasta-Uspallata Basin. Also, the new "Intraglacial Levipustula Fauna" identified in the Hoyada Verde Formation would have biostratigraphical and paleogeographical implications in intra-and interbasinal correlations.Fil: Cisterna, Gabriela Adriana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Fundación Miguel Lillo; ArgentinaFil: Sterren, Andrea Fabiana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones Paleobiológicas; ArgentinaGeological Society of America2010-08-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/54903Cisterna, Gabriela Adriana; Sterren, Andrea Fabiana; "Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin; Geological Society of America; Special Paper of the Geological Society of America; 468; 1-8-2010; 133-1470016-7606CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://pubs.geoscienceworld.org/books/book/622/chapter/3805392/info:eu-repo/semantics/altIdentifier/doi/10.1130/2010.2468(06)info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:01:48Zoai:ri.conicet.gov.ar:11336/54903instacron: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 10:01:49.022CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin |
title |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin |
spellingShingle |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin Cisterna, Gabriela Adriana Levipustula Fauna Carboniferous Glacial Event Argentina |
title_short |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin |
title_full |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin |
title_fullStr |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin |
title_full_unstemmed |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin |
title_sort |
"Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin |
dc.creator.none.fl_str_mv |
Cisterna, Gabriela Adriana Sterren, Andrea Fabiana |
author |
Cisterna, Gabriela Adriana |
author_facet |
Cisterna, Gabriela Adriana Sterren, Andrea Fabiana |
author_role |
author |
author2 |
Sterren, Andrea Fabiana |
author2_role |
author |
dc.subject.none.fl_str_mv |
Levipustula Fauna Carboniferous Glacial Event Argentina |
topic |
Levipustula Fauna Carboniferous Glacial Event 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 Levipustula Fauna (included in the Levipustula levis Zone) is a relatively diversified fossil assemblage composed of brachiopods, bivalves, bryozoans, gastropods, and crinoids. This fauna usually is associated with glaciomarine sequences related to the Carboniferous glacial event that affected the southwestern Gondwanan margin. The Levipustula Fauna has been identified in different units (e.g., Hoyada Verde, La Capilla, Leoncito, and Yalguaraz Formations) exposed in the Calingasta-Uspallata Basin. The Hoyada Verde Formation, herein proposed as a key section, contains the most complete record of the Levipustula Fauna. A detailed compositional, taphonomic, and paleoecological study of this section allows us to propose two associations within the so-called Levipustula Zone: the "Intraglacial Levipustula Fauna," present in the diamictite-dominated lower part, and the "Postglacial Levipustula Fauna," dominant in the upper part of section. The fossils of the "Intraglacial Levipustula Fauna" are scarce and poorly diversified. These two features suggest environmentally stressed conditions, probably related to low temperatures in areas close to glaciers. In comparison, the "Postglacial Levipustula Fauna," relatively more abundant and diverse, exhibits compositional variations that could be explained by paleoenvironmental changes associated with fluctuations in substratum and food supply, such as those identified in modern ecosystems. The identification of the "Intraglacial Levipustula Fauna" and the "Postglacial Levipustula Fauna" may constitute a new tool for understanding the particular relationship between faunal assemblages and climatic variations linked to the Gondwanan glaciation in the Calingasta-Uspallata Basin. Also, the new "Intraglacial Levipustula Fauna" identified in the Hoyada Verde Formation would have biostratigraphical and paleogeographical implications in intra-and interbasinal correlations. Fil: Cisterna, Gabriela Adriana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Fundación Miguel Lillo; Argentina Fil: Sterren, Andrea Fabiana. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones Paleobiológicas; Argentina |
description |
The Levipustula Fauna (included in the Levipustula levis Zone) is a relatively diversified fossil assemblage composed of brachiopods, bivalves, bryozoans, gastropods, and crinoids. This fauna usually is associated with glaciomarine sequences related to the Carboniferous glacial event that affected the southwestern Gondwanan margin. The Levipustula Fauna has been identified in different units (e.g., Hoyada Verde, La Capilla, Leoncito, and Yalguaraz Formations) exposed in the Calingasta-Uspallata Basin. The Hoyada Verde Formation, herein proposed as a key section, contains the most complete record of the Levipustula Fauna. A detailed compositional, taphonomic, and paleoecological study of this section allows us to propose two associations within the so-called Levipustula Zone: the "Intraglacial Levipustula Fauna," present in the diamictite-dominated lower part, and the "Postglacial Levipustula Fauna," dominant in the upper part of section. The fossils of the "Intraglacial Levipustula Fauna" are scarce and poorly diversified. These two features suggest environmentally stressed conditions, probably related to low temperatures in areas close to glaciers. In comparison, the "Postglacial Levipustula Fauna," relatively more abundant and diverse, exhibits compositional variations that could be explained by paleoenvironmental changes associated with fluctuations in substratum and food supply, such as those identified in modern ecosystems. The identification of the "Intraglacial Levipustula Fauna" and the "Postglacial Levipustula Fauna" may constitute a new tool for understanding the particular relationship between faunal assemblages and climatic variations linked to the Gondwanan glaciation in the Calingasta-Uspallata Basin. Also, the new "Intraglacial Levipustula Fauna" identified in the Hoyada Verde Formation would have biostratigraphical and paleogeographical implications in intra-and interbasinal correlations. |
publishDate |
2010 |
dc.date.none.fl_str_mv |
2010-08-01 |
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/11336/54903 Cisterna, Gabriela Adriana; Sterren, Andrea Fabiana; "Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin; Geological Society of America; Special Paper of the Geological Society of America; 468; 1-8-2010; 133-147 0016-7606 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/54903 |
identifier_str_mv |
Cisterna, Gabriela Adriana; Sterren, Andrea Fabiana; "Levipustula Fauna" in central-western Argentina and its relationships with the Carboniferous glacial event in the southwestern Gondwanan margin; Geological Society of America; Special Paper of the Geological Society of America; 468; 1-8-2010; 133-147 0016-7606 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://pubs.geoscienceworld.org/books/book/622/chapter/3805392/ info:eu-repo/semantics/altIdentifier/doi/10.1130/2010.2468(06) |
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 |
dc.publisher.none.fl_str_mv |
Geological Society of America |
publisher.none.fl_str_mv |
Geological Society of America |
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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1842269719167500288 |
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13.13397 |