<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
    <record>
        <controlfield tag="001">58394</controlfield>
        <controlfield tag="005">20170327111934.0</controlfield>
        <datafield tag="024" ind1="8" ind2=" ">
            <subfield code="2">sideral</subfield>
            <subfield code="a">97276</subfield>
        </datafield>
        <datafield tag="037" ind1=" " ind2=" ">
            <subfield code="a">ART-2016-97276</subfield>
        </datafield>
        <datafield tag="041" ind1=" " ind2=" ">
            <subfield code="a">eng</subfield>
        </datafield>
        <datafield tag="100" ind1=" " ind2=" ">
            <subfield code="a">Castanera, D</subfield>
        </datafield>
        <datafield tag="245" ind1=" " ind2=" ">
            <subfield code="a">An overview of the lower cretaceous dinosaur tracksites from the mirambel formation in the iberian range (ne spain)</subfield>
        </datafield>
        <datafield tag="260" ind1=" " ind2=" ">
            <subfield code="c">2016</subfield>
        </datafield>
        <datafield tag="506" ind1="0" ind2=" ">
            <subfield code="a">Access copy available to the general public</subfield>
            <subfield code="f">Unrestricted</subfield>
        </datafield>
        <datafield tag="520" ind1="3" ind2=" ">
            <subfield code="a">Up to now, the ichnological vertebrate record from the Barremian Mirambel Formation (NE Spain) has remained completely unknown despite the fact that osteological findings have been reported in recent years. Here we provide an overview of 11 new dinosaur tracksites found during a fieldwork campaign in the year 2011. The majority of these tracksites (seven) preserve small- to medium-sized tridactyl tracks here assigned to indeterminate theropods. Only one footprint presents enough characters to classify it as Megalosauripus isp. Ornithopod tracks identified as Caririchnium isp. and Iguanodontipodidae indet. and sauropod tracks are recorded at two tracksites. The footprints are preserved in a variety of paleoenvironmental conditions and thus display different kinds of preservation (true tracks, shallow undertracks, natural casts and undertrack casts). The ichnological record from the Mirambel Formation seems to be theropod dominated. This is a clear discrepancy with the osteological record identified in this formation, which shows a predominance of ornithopod dinosaurs.</subfield>
        </datafield>
        <datafield tag="536" ind1=" " ind2=" ">
            <subfield code="9">info:eu-repo/grantAgreement/ES/MINECO/CGL2014-53548</subfield>
        </datafield>
        <datafield tag="540" ind1=" " ind2=" ">
            <subfield code="9">info:eu-repo/semantics/openAccess</subfield>
            <subfield code="a">by-nc-nd</subfield>
            <subfield code="u">http://creativecommons.org/licenses/by-nc-nd/3.0/es/</subfield>
        </datafield>
        <datafield tag="655" ind1=" " ind2="4">
            <subfield code="a">info:eu-repo/semantics/article</subfield>
            <subfield code="v">info:eu-repo/semantics/publishedVersion</subfield>
        </datafield>
        <datafield tag="700" ind1=" " ind2=" ">
            <subfield code="a">Díaz-Martínez, I</subfield>
        </datafield>
        <datafield tag="700" ind1=" " ind2=" ">
            <subfield code="0">(orcid)0000-0002-7210-1033</subfield>
            <subfield code="a">Moreno-Azanza, M</subfield>
        </datafield>
        <datafield tag="700" ind1=" " ind2=" ">
            <subfield code="0">(orcid)0000-0003-1732-9155</subfield>
            <subfield code="a">Canudo, JI</subfield>
            <subfield code="u">Universidad de Zaragoza</subfield>
        </datafield>
        <datafield tag="700" ind1=" " ind2=" ">
            <subfield code="0">(orcid)0000-0002-8427-6199</subfield>
            <subfield code="a">Gasca JM</subfield>
        </datafield>
        <datafield tag="710" ind1="2" ind2=" ">
            <subfield code="1">2000</subfield>
            <subfield code="2">655</subfield>
            <subfield code="a">Universidad de Zaragoza</subfield>
            <subfield code="b">Departamento de Ciencias de la Tierra</subfield>
            <subfield code="c">Paleontología</subfield>
        </datafield>
        <datafield tag="773" ind1=" " ind2=" ">
            <subfield code="g">71 (2016), 65-74</subfield>
            <subfield code="p">Bull. - N.M. Mus. Nat. Hist. Sci.</subfield>
            <subfield code="t">Bulletin - New Mexico Museum of Natural History and Science</subfield>
            <subfield code="x">1524-4156</subfield>
        </datafield>
        <datafield tag="856" ind1="4" ind2="1">
            <subfield code="u">https://www.researchgate.net/publication/305636600_AN_OVERVIEW_OF_THE_LOWER_CRETACEOUS_DINOSAUR_TRACKSITES_FROM_THE_MIRAMBEL_FORMATION_IN_THE_IBERIAN_RANGE_NE_SPAIN</subfield>
            <subfield code="z">Texto completo de la revista</subfield>
        </datafield>
        <datafield tag="856" ind1="4" ind2=" ">
            <subfield code="s">7998580</subfield>
            <subfield code="u">http://zaguan.unizar.es/record/58394/files/texto_completo.pdf</subfield>
            <subfield code="y">Versión publicada</subfield>
        </datafield>
        <datafield tag="856" ind1="4" ind2=" ">
            <subfield code="s">143153</subfield>
            <subfield code="u">http://zaguan.unizar.es/record/58394/files/texto_completo.jpg?subformat=icon</subfield>
            <subfield code="x">icon</subfield>
            <subfield code="y">Versión publicada</subfield>
        </datafield>
        <datafield tag="909" ind1="C" ind2="O">
            <subfield code="o">oai:zaguan.unizar.es:58394</subfield>
            <subfield code="p">articulos</subfield>
            <subfield code="p">driver</subfield>
        </datafield>
        <datafield tag="951" ind1=" " ind2=" ">
            <subfield code="a">2017-01-03-12:03:42</subfield>
        </datafield>
        <datafield tag="980" ind1=" " ind2=" ">
            <subfield code="a">ARTICLE</subfield>
        </datafield>
    </record>

    
</collection>