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<dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:invenio="http://invenio-software.org/elements/1.0" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><dc:identifier>doi:10.1016/j.cretres.2021.104997</dc:identifier><dc:language>eng</dc:language><dc:creator>Aurell, M.</dc:creator><dc:creator>Bádenas, B.</dc:creator><dc:creator>Castanera, D.</dc:creator><dc:creator>Gasca, J.M.</dc:creator><dc:creator>Canudo, J.I.</dc:creator><dc:creator>Laita, E.</dc:creator><dc:creator>Liesa, C.L.</dc:creator><dc:title>Latest Jurassic–Early Cretaceous synrift evolution of the Torrelapaja Subbasin (Cameros Basin): implications for Northeast Iberia palaeogeography</dc:title><dc:identifier>ART-2021-126123</dc:identifier><dc:description>The reconstruction of the latest Jurassic–Early Cretaceous evolution of the Torrelapaja Subbasin (Cameros Basin, Spain) resulted in the characterization of three synrift sequences (SS-1, SS-2 and SS-3) bounded by major unconformities. Three major NW–SE normal faults combined with smaller scale faults of variable direction (around NE–SW) controlled the sedimentation. The complex geometry of the Torrelapaja Subbasin indicates a main extension direction of NE–SW, and a secondary NW–SE extension. Sedimentation of the Tithonian–middle Berriasian SS-1 occurred in alluvial fan systems, grading upwards to carbonate palustrine-lacustrine environments. A new vertebrate site with large size sauropod bones has been found in the middle part of SS-1. The lower boundary of the uppermost Hauterivian–lower Barremian SS-2 is locally a palaeokarst, with sedimentary infill including three new fossil sites with remains of ornithopod, sauropod and theropod dinosaurs. Sedimentation of SS-2 encompasses distal alluvial terrigenous facies with local palaeosoils and palustrine-lacustrine limestones grading upwards to middle-distal alluvial facies. After a late Barremian–early Albian stratigraphic gap, sedimentation resumed in coastal flat environments represented by the mudstones with intercalated skeletal (oyster-rich) sandy limestones with carbonaceous plant remains of the SS-3. A middle–late Albian age assignment of SS-3 based on regional correlation is supported by strontium isotopic data. This unit marks the first Early Cretaceous marine incursion in the area from the northern Atlantic realm. This is a notable change of the previous palaeogeographical reconstructions which established that the first marine encroachment occurred in the early Aptian and was sourced from Tethysian domains. © 2021 Elsevier Ltd</dc:description><dc:date>2021</dc:date><dc:source>http://zaguan.unizar.es/record/147762</dc:source><dc:doi>10.1016/j.cretres.2021.104997</dc:doi><dc:identifier>http://zaguan.unizar.es/record/147762</dc:identifier><dc:identifier>oai:zaguan.unizar.es:147762</dc:identifier><dc:relation>info:eu-repo/grantAgreement/ES/AEI/PID2019-108705GB-I00</dc:relation><dc:relation>info:eu-repo/grantAgreement/ES/DGA/E18-20R</dc:relation><dc:relation>info:eu-repo/grantAgreement/ES/DGA/E32-20R</dc:relation><dc:relation>info:eu-repo/grantAgreement/ES/MICINN/CGL2017-85038-P</dc:relation><dc:identifier.citation>Cretaceous Research 128 (2021), 104997 [27 pp]</dc:identifier.citation><dc:rights>by-nc-nd</dc:rights><dc:rights>http://creativecommons.org/licenses/by-nc-nd/3.0/es/</dc:rights><dc:rights>info:eu-repo/semantics/openAccess</dc:rights></dc:dc>

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