Late Cambrian acritarchs from the Santa Rosita Formation: implications for the Cambrian-Ordovician boundary in the eastern Cordillera of northwest Argentina

Marine phytoplankton from the Late Cambrian are described for the first time in the Eastern Cordillera of northwest Argentina. The acritarch assemblage was recovered from an offshore lower mudstone unit towards the base of the Casa Colorada Member (Santa Rosita Formation) in the Quebrada de Moya sec...

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Detalles Bibliográficos
Autores: Rubinstein, Claudia Viviana, Mangano, Maria Gabriela, Buatois, Luis Alberto
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2003
País:Argentina
Institución:Consejo Nacional de Investigaciones Científicas y Técnicas
Repositorio:CONICET Digital (CONICET)
Idioma:inglés
OAI Identifier:oai:ri.conicet.gov.ar:11336/40886
Acceso en línea:http://hdl.handle.net/11336/40886
Access Level:acceso abierto
Palabra clave:Palynology
acritarchs
Upper Cambrian
Cambrian/Ordovician boundary
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Descripción
Sumario:Marine phytoplankton from the Late Cambrian are described for the first time in the Eastern Cordillera of northwest Argentina. The acritarch assemblage was recovered from an offshore lower mudstone unit towards the base of the Casa Colorada Member (Santa Rosita Formation) in the Quebrada de Moya section, Jujuy Province. The presence of Vulcanisphaera africana, Saharidia fragilis, Granomarginata squamacea and Celtiberium sp. 1, together with the absence of Tremadocian acritarch species and the scarcity and low diversity of diacrodian acritarchs suggest an age not younger than Late Cambrian for this acritarch assemblage. This age<br />assignment is also supported by stratigraphic information and regional correlations.