<?xml version="1.0" encoding="UTF-8"?><?xml-stylesheet type="text/xsl" href="static/style.xsl"?><OAI-PMH xmlns="http://www.openarchives.org/OAI/2.0/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd"><responseDate>2026-06-29T09:34:08Z</responseDate><request verb="GetRecord" identifier="oai:docta.ucm.es:20.500.14352/58914" metadataPrefix="oai_dc">https://docta.ucm.es/rest/oai/request</request><GetRecord><record><header><identifier>oai:docta.ucm.es:20.500.14352/58914</identifier><datestamp>2023-08-27T09:46:23Z</datestamp><setSpec>com_20.500.14352_14</setSpec><setSpec>col_20.500.14352_15</setSpec></header><metadata><oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:doc="http://www.lyncode.com/xoai" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
   <dc:title>Lower Bathonian ammonites of Serra de la Creu
(Tivissa, Catalan Basin, Spain)</dc:title>
   <dc:creator>Fernández López, Sixto Rafael</dc:creator>
   <dc:subject>564.53(234.1)</dc:subject>
   <dc:subject>Middle Jurassic</dc:subject>
   <dc:subject>Ammonoids</dc:subject>
   <dc:subject>Taphonomy</dc:subject>
   <dc:subject>Biostratigraphy</dc:subject>
   <dc:subject>Chronostratigraphy</dc:subject>
   <dc:subject>Palaeobiogeography</dc:subject>
   <dc:subject>Iberia</dc:subject>
   <dc:subject>Paleontología</dc:subject>
   <dc:subject>2416 Paleontología</dc:subject>
   <dc:description>The study of ammonites of the Bajocian/Bathonian boundary from Serra de la Creu (Tivissa, province of Tarragona), a locality of the
Catalan Basin, allows to recognize several bio- and chronostratigraphic units commonly missing in the Iberian Basin. The Parkinsoni
Zone (Upper Bajocian) and the lowermost Zigzag Zone (Lower Bathonian) established for NW Europe areas can be identified in the
Catalan and Iberian basins (Spain), although the ammonite fossil assemblages are composed by Submediterranean taxa.</dc:description>
   <dc:description>Depto. de Geodinámica, Estratigrafía y Paleontología</dc:description>
   <dc:description>Fac. de Ciencias Geológicas</dc:description>
   <dc:description>TRUE</dc:description>
   <dc:description>pub</dc:description>
   <dc:date>2023-06-20T18:54:49Z</dc:date>
   <dc:date>2023-06-20T18:54:49Z</dc:date>
   <dc:date>2000</dc:date>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/58914</dc:identifier>
   <dc:identifier>0253-6730</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:rights>open access</dc:rights>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Muséum d'histoire naturelle de Genève</dc:publisher>
</oai_dc:dc></metadata></record></GetRecord></OAI-PMH>