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Description of chelonian remains from the Upper Maastrichtian of Aren and Seraduy (Huesca)

dc.contributor.authorMurelaga, Xabier
dc.contributor.authorCanudo, José Ignacio
dc.date.accessioned2014-08-07T09:21:18Z
dc.date.available2014-08-07T09:21:18Z
dc.date.issued2005
dc.identifier.urihttp://hdl.handle.net/10272/8708
dc.description.abstractChelonian plates from the uppermost Maastrichtian of the Huesca Province are described. The remains have been found in the transitional and fluvial Tremp Group. The bothremydid turtle plates are well preserved and represent the most abundant elements. Only one eroded plate fragment of the solemydid turtle has been discovered. This difference is possibly due to tafonomic factors, but does not discard that the solmydids ones were more scarce because it was a group in decrease at end of Cretaceousen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherCheloniansen_US
dc.subject.otherBothremydidaeen_US
dc.subject.otherSolemydidaeen_US
dc.subject.otherUpper Cretaceousen_US
dc.subject.otherHuescaen_US
dc.titleDescripción de los restos de quelonios del Maastrichtiense superior de Aren y Serraduy (Huesca)en_US
dc.titleDescription of chelonian remains from the Upper Maastrichtian of Aren and Seraduy (Huesca)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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