dc.creatorVoldman, Gustavo Gabriel
dc.creatorAlbanesi, Guillermo Luis
dc.creatorOrtega, Gladys del Carmen
dc.creatorGiuliano, María Eugenia
dc.creatorMonaldi, Cesar Ruben
dc.date.accessioned2018-05-04T17:54:21Z
dc.date.accessioned2018-11-06T14:34:05Z
dc.date.available2018-05-04T17:54:21Z
dc.date.available2018-11-06T14:34:05Z
dc.date.created2018-05-04T17:54:21Z
dc.date.issued2017-05
dc.identifierVoldman, Gustavo Gabriel; Albanesi, Guillermo Luis; Ortega, Gladys del Carmen; Giuliano, María Eugenia; Monaldi, Cesar Ruben; New conodont taxa and biozones from the Lower Ordovician of the Cordillera Oriental, NW Argentina; John Wiley & Sons Ltd; Geological Journal (Chichester); 52; 3; 5-2017; 394-414
dc.identifier0072-1050
dc.identifierhttp://hdl.handle.net/11336/44167
dc.identifier1099-1034
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1887796
dc.description.abstractThe upper strata of the Santa Rosita and the Acoite formations (Lower Ordovician) exposed at Chulpíos Creek in the Santa Victoria study area of the Cordillera Oriental, NW Argentina, are analysed by means of conodont biostratigraphy. Four conodont zones are analysed for the referred formations, i.e. the Acodus apex, Acodus triangularis, Gothodus vetus and Gothodus andinus zones, on the basis of a collection with ca. 2800 conodont specimens that includes new conodont taxa. Acodus apex Albanesi and Zeballo, Acodus triangularis (Ding), Acodus zeballus n. sp., Gothodus andinus (Rao et al.), Gothodus vetus n. sp., and Paltodus cf. inaequalis (Pander) are described herein. The conodont genus Zentagnathus is diagnosed including two previously known species: Zentagnathus argentinensis (Rao et al.) and Zentagnathus primitivus (Voldman et al.). The Tetragraptus akzharensis and Baltograptus cf. deflexus graptolite zones were identified as well in the ∼1800‐m‐thick stratigraphic section. The incertae sedis Phosphannulus universalis Müller et al. is discussed for the Cordillera Oriental for the first time. The lower part of the Chulpíos section that involves the contact between the Santa Rosita and the Acoite formations is not able to be dated with precision either as upper Tremadocian or lower Floian because the ranges of the index taxa recorded in that interval of the study section span the stage boundary.
dc.languageeng
dc.publisherJohn Wiley & Sons Ltd
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://onlinelibrary.wiley.com/doi/abs/10.1002/gj.2766
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1002/gj.2766
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectCONODONTS
dc.subjectBIOSTRATIGRAPHY
dc.subjectLOWER ORDOVICIAN
dc.subjectCORDILLERA ORIENTAL
dc.subjectARGENTINA
dc.titleNew conodont taxa and biozones from the Lower Ordovician of the Cordillera Oriental, NW Argentina
dc.typeArtículos de revistas
dc.typeArtículos de revistas
dc.typeArtículos de revistas


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