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The Oxfordian-Kimmeridgian boundary in the Puerto Lorente section (External Prebetic) revisited

dc.contributor.authorOlóriz, F.
dc.contributor.authorRodríguez Tovar, F. J.
dc.description.abstractIn the Puerto Lorente section at the Sierra de Cazorla (External Prebetic), the uppermost Oxfordian is made up of limestones with recognizable traces of increasing condensation. O verlayin gare marls, marly-limestones and limestones of the Lower Kimmeridgian. The surface boundary between the Oxfordian and the Kimmeridgian has been traditionally referred to the cephalopod rich “hardground" which precedes deposition of the lowerm ost Kimmeridgian marls. Nevertheless, careful studies on this surface allowed us to identify rare specimens of Sutneria platynota (REINECKE) and therefore to improve the previous biostratigraphic interpretations. The obtained data will be valuable for the updated interpretation of the eco-sedimentary evolution in epicontinental areas of the Southlberian paleomargin around the Oxfordian-Kimmeridgian boundaryes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherOxfordian-Kimmeridgian boundaryes_ES
dc.subject.otherExternal Prebetices_ES
dc.subject.otherSouthern Spaines_ES
dc.titleReconsideración del límite Oxfordiense-Kimmeridgiense en el perfil de Puerto Lorente (Prebético Externo)es_ES
dc.titleThe Oxfordian-Kimmeridgian boundary in the Puerto Lorente section (External Prebetic) revisitedeng

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Atribución-NoComercial-SinDerivadas 3.0 España
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