Ordovician conodonts of the Devendeus Formation at the Angosto de La Quesera (Cordillera Oriental of Salta, Argentina): Taxonomic considerations and biostratigraphic significance

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Main Author: J. CARLOROSI
Format: Artículo científico
Language:en
Published: Universitat de Barcelona 2011
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author J. CARLOROSI
author_facet J. CARLOROSI
contents Ordovician conodonts of the Devendeus Formation at the Angosto de La Quesera (Cordillera Oriental of Salta, Argentina): Taxonomic considerations and biostratigraphic significance J. CARLOROSI S. HEREDIA G. ACEÑOLAZA Ciencias de la Tierra Conodonts Ordovician Devendeus Formation Northwestern Argentina Conodonts recovered from the Devendeus Formation at the Angosto de La Quesera locality (Cordillera Oriental of Salta) in northwestern Argentina include Nogamiconus sp., Problematoconites perforatus, Drepanoistodus sp., Oneotodus sp., Scolopodus filosus, Teridontus nakamurai and Variabiloconus sp., as a part of an association that defines a pre-Paltodus deltifer Zone. The material most likely represents the Cordylodus angulatus and/or the lower part of the Rossodus manitouensis Zone. These microfossils support the dating of the Devendeus Formation as Tremadocian (Early Ordovician). 2011 artículo científico 1695-6133 https://www.redalyc.org/articulo.oa?id=50521609005 en http://www.redalyc.org/revista.oa?id=505 Geologica Acta: an international earth science journal application/pdf Universitat de Barcelona Geologica Acta: an international earth science journal (España) Num.2 Vol.9
format Artículo científico
id redalyc_50521609005
institution Redalyc
language en
publishDate 2011
publisher Universitat de Barcelona
spellingShingle Ordovician conodonts of the Devendeus Formation at the Angosto de La Quesera (Cordillera Oriental of Salta, Argentina): Taxonomic considerations and biostratigraphic significance
J. CARLOROSI
Ciencias de la Tierra
Conodonts
Ordovician
Devendeus Formation
Northwestern Argentina
Ordovician conodonts of the Devendeus Formation at the Angosto de La Quesera (Cordillera Oriental of Salta, Argentina): Taxonomic considerations and biostratigraphic significance J. CARLOROSI S. HEREDIA G. ACEÑOLAZA Ciencias de la Tierra Conodonts Ordovician Devendeus Formation Northwestern Argentina Conodonts recovered from the Devendeus Formation at the Angosto de La Quesera locality (Cordillera Oriental of Salta) in northwestern Argentina include Nogamiconus sp., Problematoconites perforatus, Drepanoistodus sp., Oneotodus sp., Scolopodus filosus, Teridontus nakamurai and Variabiloconus sp., as a part of an association that defines a pre-Paltodus deltifer Zone. The material most likely represents the Cordylodus angulatus and/or the lower part of the Rossodus manitouensis Zone. These microfossils support the dating of the Devendeus Formation as Tremadocian (Early Ordovician). 2011 artículo científico 1695-6133 https://www.redalyc.org/articulo.oa?id=50521609005 en http://www.redalyc.org/revista.oa?id=505 Geologica Acta: an international earth science journal application/pdf Universitat de Barcelona Geologica Acta: an international earth science journal (España) Num.2 Vol.9
title Ordovician conodonts of the Devendeus Formation at the Angosto de La Quesera (Cordillera Oriental of Salta, Argentina): Taxonomic considerations and biostratigraphic significance
topic Ciencias de la Tierra
Conodonts
Ordovician
Devendeus Formation
Northwestern Argentina
url https://www.redalyc.org/articulo.oa?id=50521609005