"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
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/54903

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network_name_str CONICET Digital (CONICET)
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
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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