Nouveau regard sur la paléobiogéographie de la faune de graptolites de l’Ordovicien inférieur de l’Argentine nord-occidentale

dc.creatorVento, Barbara
dc.creatorToro, Blanca Azucena
dc.creatorMaletz, Jörg
dc.date.accessioned2019-02-18T19:25:55Z
dc.date.accessioned2022-10-14T23:04:30Z
dc.date.available2019-02-18T19:25:55Z
dc.date.available2022-10-14T23:04:30Z
dc.date.created2019-02-18T19:25:55Z
dc.date.issued2012-07
dc.identifierVento, Barbara; Toro, Blanca Azucena; Maletz, Jörg; New insights into the paleobiogeography of the Early Ordovician graptolite fauna of northwestern Argentina; Elsevier France-editions Scientifiques Medicales Elsevier; Comptes Rendus Palevol; 11; 5; 7-2012; 345-355
dc.identifier1631-0683
dc.identifierhttp://hdl.handle.net/11336/70394
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4317297
dc.description.abstractA multivariate analysis was used to determine the faunistic relationships of the northwestern Argentinean graptolite faunas of Floian age to faunas from Baltica, Avalonia, Laurentia and SW China. A statistical analysis at the species level of the five geographic regions for the Lower Floian was performed with the classic Jaccard's index. The resulting affinity dendrogram shows stronger relationships between Early Floian graptolite faunas of northwestern Argentina and those from Baltica, with less obvious similarities to Great Britain (Avalonia) faunas and only weak affinities to North American (Laurentia) and Chinese (SW China) graptolite faunas. The statistical analysis confirms the paleobiogeographic relationships previously observed in other areas of the Cordillera Oriental, and supports the hypothesis that during the Early Ordovician, northwestern Argentina was located at middle to high latitudes, corresponding to the Atlantic Faunal Realm of cold water graptolite biofacies. The studied graptolite material from the Quinilicán and Agua Chica sections is preserved in shales and siltstones interbedded with fine to medium-grained sandstones corresponding to the lower part of the Acoite Formation. The biostratigraphic implications of the associated graptolites are briefly discussed, and Trichograptus dilaceratus (Herrmann), Acrograptus gracilis (Törnquist), Expansograptus latus (T.S. Hall) and Corymbograptus v-fractus tullbergi (Monsen) are described from the Argentine Cordillera Oriental for the first time. © 2012 Académie des sciences.
dc.languageeng
dc.publisherElsevier France-editions Scientifiques Medicales Elsevier
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1631068312000772
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1016/j.crpv.2012.02.002
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectFLOIAN PALEOBIOGEOGRAPHY
dc.subjectGRAPTOLITES
dc.subjectNORTHWESTERN ARGENTINA
dc.subjectSTATISTICAL ANALYSIS
dc.titleNew insights into the paleobiogeography of the Early Ordovician graptolite fauna of northwestern Argentina
dc.titleNouveau regard sur la paléobiogéographie de la faune de graptolites de l’Ordovicien inférieur de l’Argentine nord-occidentale
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion


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