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
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/220464

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network_name_str CONICET Digital (CONICET)
spelling 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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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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