Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina
- Autores
- Vennari, Verónica Vanesa; Aguirre-Urreta, Maria Beatriz
- Año de publicación
- 2014
- Idioma
- inglés
- Tipo de recurso
- documento de conferencia
- Estado
- versión publicada
- Descripción
- Marine successions of the Vaca Muerta Formation (early Tithonian-late Berriasian) in the Neuquén Basin, west-central Argentina, are worldwide known by their abundant and well preserved ammonoid content. A systematic revision of the ammonoid groups contained in the first portion (late early Tithonian - early middle Tithonian) of the Vaca Muerta Formation was performed. This study aims to clarify the stratigraphic distribution of the involved species, their relative abundance and diversity and their palaeobiogeographical affinities. Sampling was performed over eighteen stratigraphic sections, placed along a north-south transect in the basin, from the Aconcagua in northern Mendoza to Picún Leufú in southern Neuquén. Over 600 specimens were selected for the taxonomic analysis which resulted in the identification of thirteen species and one subspecies of ammonoids that, in turn, were grouped into six genera, four subfamilies and three families. Among them, a new genus and two new species are proposed. Members of the Family Ataxioceratidae, which encompass 86% of the species, dominated the faunal association, whereas the Families Aspidoceratidae and Simoceratidae grouped the 14% of the remaining species. Concerning Subfamilies, Virgatosphinctinae (65%) was the best represented, followed by Lithacoceratinae (21%), Physodoceratinae (7%) and Simoceratinae (7%). Subfamily Virgatosphinctinae comprises three genera: Virgatosphinctes Uhlig, with two species, Virgatosphinctes andesensis (Douvillé) and Virgatosphinctes (?) densistriatus (Steuer); Pseudinvoluticeras Spath with three species, Pseudinvoluticeras douvillei Spath, Pseudinvoluticeras windhauseni (Weaver) and Pseudinvoluticeras (?) n. sp.?; and Choicensisphinctes Leanza with four species, Choicensisphinctes choicensis (Burckhardt), Choicensisphinctes erinoides (Burckhardt), Choicensisphinctes n. sp. aff. erinoides and Choicensisphinctes n. sp. Subfamily Lithacoceratinae was found to be well represented by abundant specimens of ¨Subplanites Spath, which hitherto has been found to encompass only one species, ¨Subplanites¨ malarguensis Spath. Subfamilies Physodoceratinae and Simoceratinae include one genus each: Schaireria Checa, with Schaireria neoburgensis (Oppel) and Pseudovolanoceras Cecca, with Pseudovolanoceras sp. cf. Pseudovolanoceras aesinense krantzense (Cantú-Chapa), respectively. The identification of a taxonomically homogeneous ammonoid assemblage in the lower portion of each of the studied Vaca Muerta Formation sections enables to support the hypothesis of a synchronous Tithonian transgression in the Neuquén Basin. Typical Indo-Pacific elements such as Virgatosphinctes, as well as Mediterranean forms like Pseudovolanoceras, confirm the well established marine connections of the Neuquén Basin with the Mediterranean and Indo-Pacific Subrealms, atleast since the Tithonian. Endemic (e.g. Choicensisphinctes) and pandemic genera (e.g. Schaireria)have also been recorded in the analyzed stratigraphic interval.
Fil: Vennari, Verónica Vanesa. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
Fil: Aguirre-Urreta, Maria Beatriz. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina
4th International Palaeontological Congress
Mendoza
Argentina
Asociación Internacional de Paleontología - Materia
-
Bioestratigraphy
Ammonoids
Neuquen Basin
Late Jurassic - 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:11336/220464
Ver los metadatos del registro completo
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Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, ArgentinaVennari, Verónica VanesaAguirre-Urreta, Maria BeatrizBioestratigraphyAmmonoidsNeuquen BasinLate Jurassichttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Marine successions of the Vaca Muerta Formation (early Tithonian-late Berriasian) in the Neuquén Basin, west-central Argentina, are worldwide known by their abundant and well preserved ammonoid content. A systematic revision of the ammonoid groups contained in the first portion (late early Tithonian - early middle Tithonian) of the Vaca Muerta Formation was performed. This study aims to clarify the stratigraphic distribution of the involved species, their relative abundance and diversity and their palaeobiogeographical affinities. Sampling was performed over eighteen stratigraphic sections, placed along a north-south transect in the basin, from the Aconcagua in northern Mendoza to Picún Leufú in southern Neuquén. Over 600 specimens were selected for the taxonomic analysis which resulted in the identification of thirteen species and one subspecies of ammonoids that, in turn, were grouped into six genera, four subfamilies and three families. Among them, a new genus and two new species are proposed. Members of the Family Ataxioceratidae, which encompass 86% of the species, dominated the faunal association, whereas the Families Aspidoceratidae and Simoceratidae grouped the 14% of the remaining species. Concerning Subfamilies, Virgatosphinctinae (65%) was the best represented, followed by Lithacoceratinae (21%), Physodoceratinae (7%) and Simoceratinae (7%). Subfamily Virgatosphinctinae comprises three genera: Virgatosphinctes Uhlig, with two species, Virgatosphinctes andesensis (Douvillé) and Virgatosphinctes (?) densistriatus (Steuer); Pseudinvoluticeras Spath with three species, Pseudinvoluticeras douvillei Spath, Pseudinvoluticeras windhauseni (Weaver) and Pseudinvoluticeras (?) n. sp.?; and Choicensisphinctes Leanza with four species, Choicensisphinctes choicensis (Burckhardt), Choicensisphinctes erinoides (Burckhardt), Choicensisphinctes n. sp. aff. erinoides and Choicensisphinctes n. sp. Subfamily Lithacoceratinae was found to be well represented by abundant specimens of ¨Subplanites Spath, which hitherto has been found to encompass only one species, ¨Subplanites¨ malarguensis Spath. Subfamilies Physodoceratinae and Simoceratinae include one genus each: Schaireria Checa, with Schaireria neoburgensis (Oppel) and Pseudovolanoceras Cecca, with Pseudovolanoceras sp. cf. Pseudovolanoceras aesinense krantzense (Cantú-Chapa), respectively. The identification of a taxonomically homogeneous ammonoid assemblage in the lower portion of each of the studied Vaca Muerta Formation sections enables to support the hypothesis of a synchronous Tithonian transgression in the Neuquén Basin. Typical Indo-Pacific elements such as Virgatosphinctes, as well as Mediterranean forms like Pseudovolanoceras, confirm the well established marine connections of the Neuquén Basin with the Mediterranean and Indo-Pacific Subrealms, atleast since the Tithonian. Endemic (e.g. Choicensisphinctes) and pandemic genera (e.g. Schaireria)have also been recorded in the analyzed stratigraphic interval.Fil: Vennari, Verónica Vanesa. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; ArgentinaFil: Aguirre-Urreta, Maria Beatriz. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina4th International Palaeontological CongressMendozaArgentinaAsociación Internacional de PaleontologíaAsociación Internacional de Paleontología2014info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/conferenceObjectCongresoBookhttp://purl.org/coar/resource_type/c_5794info:ar-repo/semantics/documentoDeConferenciaapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/220464Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina; 4th International Palaeontological Congress; Mendoza; Argentina; 2014; 631-631CONICET DigitalCONICETengInternacionalinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:37:09Zoai:ri.conicet.gov.ar:11336/220464instacron: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 09:37:09.543CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina |
title |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina |
spellingShingle |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina Vennari, Verónica Vanesa Bioestratigraphy Ammonoids Neuquen Basin Late Jurassic |
title_short |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina |
title_full |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina |
title_fullStr |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina |
title_full_unstemmed |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina |
title_sort |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina |
dc.creator.none.fl_str_mv |
Vennari, Verónica Vanesa Aguirre-Urreta, Maria Beatriz |
author |
Vennari, Verónica Vanesa |
author_facet |
Vennari, Verónica Vanesa Aguirre-Urreta, Maria Beatriz |
author_role |
author |
author2 |
Aguirre-Urreta, Maria Beatriz |
author2_role |
author |
dc.subject.none.fl_str_mv |
Bioestratigraphy Ammonoids Neuquen Basin Late Jurassic |
topic |
Bioestratigraphy Ammonoids Neuquen Basin Late Jurassic |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Marine successions of the Vaca Muerta Formation (early Tithonian-late Berriasian) in the Neuquén Basin, west-central Argentina, are worldwide known by their abundant and well preserved ammonoid content. A systematic revision of the ammonoid groups contained in the first portion (late early Tithonian - early middle Tithonian) of the Vaca Muerta Formation was performed. This study aims to clarify the stratigraphic distribution of the involved species, their relative abundance and diversity and their palaeobiogeographical affinities. Sampling was performed over eighteen stratigraphic sections, placed along a north-south transect in the basin, from the Aconcagua in northern Mendoza to Picún Leufú in southern Neuquén. Over 600 specimens were selected for the taxonomic analysis which resulted in the identification of thirteen species and one subspecies of ammonoids that, in turn, were grouped into six genera, four subfamilies and three families. Among them, a new genus and two new species are proposed. Members of the Family Ataxioceratidae, which encompass 86% of the species, dominated the faunal association, whereas the Families Aspidoceratidae and Simoceratidae grouped the 14% of the remaining species. Concerning Subfamilies, Virgatosphinctinae (65%) was the best represented, followed by Lithacoceratinae (21%), Physodoceratinae (7%) and Simoceratinae (7%). Subfamily Virgatosphinctinae comprises three genera: Virgatosphinctes Uhlig, with two species, Virgatosphinctes andesensis (Douvillé) and Virgatosphinctes (?) densistriatus (Steuer); Pseudinvoluticeras Spath with three species, Pseudinvoluticeras douvillei Spath, Pseudinvoluticeras windhauseni (Weaver) and Pseudinvoluticeras (?) n. sp.?; and Choicensisphinctes Leanza with four species, Choicensisphinctes choicensis (Burckhardt), Choicensisphinctes erinoides (Burckhardt), Choicensisphinctes n. sp. aff. erinoides and Choicensisphinctes n. sp. Subfamily Lithacoceratinae was found to be well represented by abundant specimens of ¨Subplanites Spath, which hitherto has been found to encompass only one species, ¨Subplanites¨ malarguensis Spath. Subfamilies Physodoceratinae and Simoceratinae include one genus each: Schaireria Checa, with Schaireria neoburgensis (Oppel) and Pseudovolanoceras Cecca, with Pseudovolanoceras sp. cf. Pseudovolanoceras aesinense krantzense (Cantú-Chapa), respectively. The identification of a taxonomically homogeneous ammonoid assemblage in the lower portion of each of the studied Vaca Muerta Formation sections enables to support the hypothesis of a synchronous Tithonian transgression in the Neuquén Basin. Typical Indo-Pacific elements such as Virgatosphinctes, as well as Mediterranean forms like Pseudovolanoceras, confirm the well established marine connections of the Neuquén Basin with the Mediterranean and Indo-Pacific Subrealms, atleast since the Tithonian. Endemic (e.g. Choicensisphinctes) and pandemic genera (e.g. Schaireria)have also been recorded in the analyzed stratigraphic interval. Fil: Vennari, Verónica Vanesa. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina Fil: Aguirre-Urreta, Maria Beatriz. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina 4th International Palaeontological Congress Mendoza Argentina Asociación Internacional de Paleontología |
description |
Marine successions of the Vaca Muerta Formation (early Tithonian-late Berriasian) in the Neuquén Basin, west-central Argentina, are worldwide known by their abundant and well preserved ammonoid content. A systematic revision of the ammonoid groups contained in the first portion (late early Tithonian - early middle Tithonian) of the Vaca Muerta Formation was performed. This study aims to clarify the stratigraphic distribution of the involved species, their relative abundance and diversity and their palaeobiogeographical affinities. Sampling was performed over eighteen stratigraphic sections, placed along a north-south transect in the basin, from the Aconcagua in northern Mendoza to Picún Leufú in southern Neuquén. Over 600 specimens were selected for the taxonomic analysis which resulted in the identification of thirteen species and one subspecies of ammonoids that, in turn, were grouped into six genera, four subfamilies and three families. Among them, a new genus and two new species are proposed. Members of the Family Ataxioceratidae, which encompass 86% of the species, dominated the faunal association, whereas the Families Aspidoceratidae and Simoceratidae grouped the 14% of the remaining species. Concerning Subfamilies, Virgatosphinctinae (65%) was the best represented, followed by Lithacoceratinae (21%), Physodoceratinae (7%) and Simoceratinae (7%). Subfamily Virgatosphinctinae comprises three genera: Virgatosphinctes Uhlig, with two species, Virgatosphinctes andesensis (Douvillé) and Virgatosphinctes (?) densistriatus (Steuer); Pseudinvoluticeras Spath with three species, Pseudinvoluticeras douvillei Spath, Pseudinvoluticeras windhauseni (Weaver) and Pseudinvoluticeras (?) n. sp.?; and Choicensisphinctes Leanza with four species, Choicensisphinctes choicensis (Burckhardt), Choicensisphinctes erinoides (Burckhardt), Choicensisphinctes n. sp. aff. erinoides and Choicensisphinctes n. sp. Subfamily Lithacoceratinae was found to be well represented by abundant specimens of ¨Subplanites Spath, which hitherto has been found to encompass only one species, ¨Subplanites¨ malarguensis Spath. Subfamilies Physodoceratinae and Simoceratinae include one genus each: Schaireria Checa, with Schaireria neoburgensis (Oppel) and Pseudovolanoceras Cecca, with Pseudovolanoceras sp. cf. Pseudovolanoceras aesinense krantzense (Cantú-Chapa), respectively. The identification of a taxonomically homogeneous ammonoid assemblage in the lower portion of each of the studied Vaca Muerta Formation sections enables to support the hypothesis of a synchronous Tithonian transgression in the Neuquén Basin. Typical Indo-Pacific elements such as Virgatosphinctes, as well as Mediterranean forms like Pseudovolanoceras, confirm the well established marine connections of the Neuquén Basin with the Mediterranean and Indo-Pacific Subrealms, atleast since the Tithonian. Endemic (e.g. Choicensisphinctes) and pandemic genera (e.g. Schaireria)have also been recorded in the analyzed stratigraphic interval. |
publishDate |
2014 |
dc.date.none.fl_str_mv |
2014 |
dc.type.none.fl_str_mv |
info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/conferenceObject Congreso Book http://purl.org/coar/resource_type/c_5794 info:ar-repo/semantics/documentoDeConferencia |
status_str |
publishedVersion |
format |
conferenceObject |
dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/220464 Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina; 4th International Palaeontological Congress; Mendoza; Argentina; 2014; 631-631 CONICET Digital CONICET |
url |
http://hdl.handle.net/11336/220464 |
identifier_str_mv |
Ammonoids of the basal section of the Vaca Muerta Formation, Neuquén Basin, Argentina; 4th International Palaeontological Congress; Mendoza; Argentina; 2014; 631-631 CONICET Digital CONICET |
dc.language.none.fl_str_mv |
eng |
language |
eng |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
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application/pdf application/pdf application/pdf |
dc.coverage.none.fl_str_mv |
Internacional |
dc.publisher.none.fl_str_mv |
Asociación Internacional de Paleontología |
publisher.none.fl_str_mv |
Asociación Internacional de Paleontología |
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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 |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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