A late Furongian trilobite assemblage from the eastern Cordillera Oriental (Santa Rosita Formation; Jujuy, Argentina) and its biostratigraphic significance

The trilobite Parabolina frequens argentina Zone is widely represented in the upper Furongian of northwestern Argentina. A fossil assemblage from the lower Santa Rosita Formation at Quebrada de Abra Blanca, Jujuy Province, is described herein. Parabolina frequens argentina (Kayser) and Parabolinella...

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Language:unknown
Published: 2018
Subjects:
Online Access:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_15145158_v20_n2_p271_Tortello
https://hdl.handle.net/20.500.12110/paper_15145158_v20_n2_p271_Tortello
id ftunibueairesbd:paper:paper_15145158_v20_n2_p271_Tortello
record_format openpolar
spelling ftunibueairesbd:paper:paper_15145158_v20_n2_p271_Tortello 2023-05-15T17:22:51+02:00 A late Furongian trilobite assemblage from the eastern Cordillera Oriental (Santa Rosita Formation; Jujuy, Argentina) and its biostratigraphic significance 2018 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_15145158_v20_n2_p271_Tortello https://hdl.handle.net/20.500.12110/paper_15145158_v20_n2_p271_Tortello unknown https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_15145158_v20_n2_p271_Tortello http://hdl.handle.net/20.500.12110/paper_15145158_v20_n2_p271_Tortello Argentina Formación Santa Rosita Furongiano tardío Jujuy Late Furongian Santa Rosita Formation Trilobites 2018 ftunibueairesbd https://doi.org/20.500.12110/paper_15145158_v20_n2_p271_Tortello 2023-02-16T01:55:22Z The trilobite Parabolina frequens argentina Zone is widely represented in the upper Furongian of northwestern Argentina. A fossil assemblage from the lower Santa Rosita Formation at Quebrada de Abra Blanca, Jujuy Province, is described herein. Parabolina frequens argentina (Kayser) and Parabolinella coelatifrons Harrington & Leanza have previously been reported from other localities of the biozone, whereas Lotagnostus hedini (Troedsson) is here described from South America for the first time. The latter provides high resolution data on the age of the P. frequens argentina Zone in the eastern Cordillera Oriental, where conodont-bearing strata have not been found yet. L. hedini exhibits a short biostratigraphic range, restricted to the latest Furongian of China (Xinjiang, Bulbolenus Zone; western Zhejiang, Lotagnostus hedini Zone), Kazakhstan (Euloma limitaris-Taoyuania Zone) and ?Canada (western Newfoundland, Phylacterus saylesi Fauna). In China and Kazakhstan, it occurs in association with, or a few meters below, the first appearance of the conodont Cordylodus proavus; a fact that increases the potential for global correlation. © 2018 Museo Argentino de Ciencias Naturales Bernardino Rivadavia. La Zona de trilobites de Parabolina frequens argentina está ampliamente representada en el Furongiano superior del noroeste argentino. En este trabajo se describe una asociación fosilífera del tramo inferior de la Formación Santa Rosita aflorante en la Quebrada de Abra Blanca, Provincia de Jujuy. Parabolina frequens argentina (Kayser) y Parabolinella coelatifrons Harrington & Leanza fueron previamente citados en otras localidades de la biozona, mientras que Lotagnostus hedini (Troedsson) es descripto aquí por primera vez para Sudamérica. Este último taxón aporta datos precisos sobre la edad de la Zona de P. frequens argentina en el sector este de la Cordillera Oriental, en donde aún no se han hallado rocas portadoras de faunas de conodontes. Lotagnostus hedini posee un rango bioestratigráfico corto, limitado al ... Other/Unknown Material Newfoundland Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires) Argentina Argentino Canada Corto ENVELOPE(-60.783,-60.783,-62.450,-62.450) Rocas ENVELOPE(-56.948,-56.948,-63.398,-63.398)
institution Open Polar
collection Biblioteca Digital FCEN-UBA (Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires)
op_collection_id ftunibueairesbd
language unknown
topic Argentina
Formación Santa Rosita
Furongiano tardío
Jujuy
Late Furongian
Santa Rosita Formation
Trilobites
spellingShingle Argentina
Formación Santa Rosita
Furongiano tardío
Jujuy
Late Furongian
Santa Rosita Formation
Trilobites
A late Furongian trilobite assemblage from the eastern Cordillera Oriental (Santa Rosita Formation; Jujuy, Argentina) and its biostratigraphic significance
topic_facet Argentina
Formación Santa Rosita
Furongiano tardío
Jujuy
Late Furongian
Santa Rosita Formation
Trilobites
description The trilobite Parabolina frequens argentina Zone is widely represented in the upper Furongian of northwestern Argentina. A fossil assemblage from the lower Santa Rosita Formation at Quebrada de Abra Blanca, Jujuy Province, is described herein. Parabolina frequens argentina (Kayser) and Parabolinella coelatifrons Harrington & Leanza have previously been reported from other localities of the biozone, whereas Lotagnostus hedini (Troedsson) is here described from South America for the first time. The latter provides high resolution data on the age of the P. frequens argentina Zone in the eastern Cordillera Oriental, where conodont-bearing strata have not been found yet. L. hedini exhibits a short biostratigraphic range, restricted to the latest Furongian of China (Xinjiang, Bulbolenus Zone; western Zhejiang, Lotagnostus hedini Zone), Kazakhstan (Euloma limitaris-Taoyuania Zone) and ?Canada (western Newfoundland, Phylacterus saylesi Fauna). In China and Kazakhstan, it occurs in association with, or a few meters below, the first appearance of the conodont Cordylodus proavus; a fact that increases the potential for global correlation. © 2018 Museo Argentino de Ciencias Naturales Bernardino Rivadavia. La Zona de trilobites de Parabolina frequens argentina está ampliamente representada en el Furongiano superior del noroeste argentino. En este trabajo se describe una asociación fosilífera del tramo inferior de la Formación Santa Rosita aflorante en la Quebrada de Abra Blanca, Provincia de Jujuy. Parabolina frequens argentina (Kayser) y Parabolinella coelatifrons Harrington & Leanza fueron previamente citados en otras localidades de la biozona, mientras que Lotagnostus hedini (Troedsson) es descripto aquí por primera vez para Sudamérica. Este último taxón aporta datos precisos sobre la edad de la Zona de P. frequens argentina en el sector este de la Cordillera Oriental, en donde aún no se han hallado rocas portadoras de faunas de conodontes. Lotagnostus hedini posee un rango bioestratigráfico corto, limitado al ...
title A late Furongian trilobite assemblage from the eastern Cordillera Oriental (Santa Rosita Formation; Jujuy, Argentina) and its biostratigraphic significance
title_short A late Furongian trilobite assemblage from the eastern Cordillera Oriental (Santa Rosita Formation; Jujuy, Argentina) and its biostratigraphic significance
title_full A late Furongian trilobite assemblage from the eastern Cordillera Oriental (Santa Rosita Formation; Jujuy, Argentina) and its biostratigraphic significance
title_fullStr A late Furongian trilobite assemblage from the eastern Cordillera Oriental (Santa Rosita Formation; Jujuy, Argentina) and its biostratigraphic significance
title_full_unstemmed A late Furongian trilobite assemblage from the eastern Cordillera Oriental (Santa Rosita Formation; Jujuy, Argentina) and its biostratigraphic significance
title_sort late furongian trilobite assemblage from the eastern cordillera oriental (santa rosita formation; jujuy, argentina) and its biostratigraphic significance
publishDate 2018
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_15145158_v20_n2_p271_Tortello
https://hdl.handle.net/20.500.12110/paper_15145158_v20_n2_p271_Tortello
long_lat ENVELOPE(-60.783,-60.783,-62.450,-62.450)
ENVELOPE(-56.948,-56.948,-63.398,-63.398)
geographic Argentina
Argentino
Canada
Corto
Rocas
geographic_facet Argentina
Argentino
Canada
Corto
Rocas
genre Newfoundland
genre_facet Newfoundland
op_relation https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_15145158_v20_n2_p271_Tortello
http://hdl.handle.net/20.500.12110/paper_15145158_v20_n2_p271_Tortello
op_doi https://doi.org/20.500.12110/paper_15145158_v20_n2_p271_Tortello
_version_ 1766109735725039616