Lower Cretaceous ammonites from the Neuquén Basin, Argentina: A new heteromorph fauna from the uppermost Agrio Formation

Although the Agrio Formation (Valanginian-Early Barremian) yields rich ammonite faunas at many levels, the highest beds are very sparsely fossiliferous. However, intensive collecting over the years has yielded a sparse fauna of heteromorph ammonites that are completely new to Argentina. Three taxa a...

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Publicado: 2012
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01956671_v35_n_p208_AguirreUrreta
http://hdl.handle.net/20.500.12110/paper_01956671_v35_n_p208_AguirreUrreta
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spelling paper:paper_01956671_v35_n_p208_AguirreUrreta2023-06-08T15:20:14Z Lower Cretaceous ammonites from the Neuquén Basin, Argentina: A new heteromorph fauna from the uppermost Agrio Formation Ammonites Argentina Barremian Biostratigraphy Hauterivian Neuquén Basin ammonite Barremian biostratigraphy fauna fossil Hauterivian taxonomy Argentina Neuquen Basin Ammonoidea Heteromorpha Sabaudiella Although the Agrio Formation (Valanginian-Early Barremian) yields rich ammonite faunas at many levels, the highest beds are very sparsely fossiliferous. However, intensive collecting over the years has yielded a sparse fauna of heteromorph ammonites that are completely new to Argentina. Three taxa are represented, Sabaudiella riverorum sp. nov., Curacoites rotundus gen. et sp. nov. and Hamulinites? sp. The fauna is placed in a new ammonite zone of Sabaudiella riverorum and dated as latest Hauterivian-Early Barremian. © 2012 Elsevier Ltd. 2012 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01956671_v35_n_p208_AguirreUrreta http://hdl.handle.net/20.500.12110/paper_01956671_v35_n_p208_AguirreUrreta
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Ammonites
Argentina
Barremian
Biostratigraphy
Hauterivian
Neuquén Basin
ammonite
Barremian
biostratigraphy
fauna
fossil
Hauterivian
taxonomy
Argentina
Neuquen Basin
Ammonoidea
Heteromorpha
Sabaudiella
spellingShingle Ammonites
Argentina
Barremian
Biostratigraphy
Hauterivian
Neuquén Basin
ammonite
Barremian
biostratigraphy
fauna
fossil
Hauterivian
taxonomy
Argentina
Neuquen Basin
Ammonoidea
Heteromorpha
Sabaudiella
Lower Cretaceous ammonites from the Neuquén Basin, Argentina: A new heteromorph fauna from the uppermost Agrio Formation
topic_facet Ammonites
Argentina
Barremian
Biostratigraphy
Hauterivian
Neuquén Basin
ammonite
Barremian
biostratigraphy
fauna
fossil
Hauterivian
taxonomy
Argentina
Neuquen Basin
Ammonoidea
Heteromorpha
Sabaudiella
description Although the Agrio Formation (Valanginian-Early Barremian) yields rich ammonite faunas at many levels, the highest beds are very sparsely fossiliferous. However, intensive collecting over the years has yielded a sparse fauna of heteromorph ammonites that are completely new to Argentina. Three taxa are represented, Sabaudiella riverorum sp. nov., Curacoites rotundus gen. et sp. nov. and Hamulinites? sp. The fauna is placed in a new ammonite zone of Sabaudiella riverorum and dated as latest Hauterivian-Early Barremian. © 2012 Elsevier Ltd.
title Lower Cretaceous ammonites from the Neuquén Basin, Argentina: A new heteromorph fauna from the uppermost Agrio Formation
title_short Lower Cretaceous ammonites from the Neuquén Basin, Argentina: A new heteromorph fauna from the uppermost Agrio Formation
title_full Lower Cretaceous ammonites from the Neuquén Basin, Argentina: A new heteromorph fauna from the uppermost Agrio Formation
title_fullStr Lower Cretaceous ammonites from the Neuquén Basin, Argentina: A new heteromorph fauna from the uppermost Agrio Formation
title_full_unstemmed Lower Cretaceous ammonites from the Neuquén Basin, Argentina: A new heteromorph fauna from the uppermost Agrio Formation
title_sort lower cretaceous ammonites from the neuquén basin, argentina: a new heteromorph fauna from the uppermost agrio formation
publishDate 2012
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_01956671_v35_n_p208_AguirreUrreta
http://hdl.handle.net/20.500.12110/paper_01956671_v35_n_p208_AguirreUrreta
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