<rdf:RDF xmlns:rdf="http://www.openarchives.org/OAI/2.0/rdf/" xmlns:ow="http://www.ontoweb.org/ontology/1#" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:ds="http://dspace.org/ds/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/rdf/ http://www.openarchives.org/OAI/2.0/rdf.xsd">
   <ow:Publication rdf:about="oai:digibug.ugr.es:10481/77080">
      <dc:title>Middle Miocene (Serravallian) rhodoliths and coralline algal debris in carbonate ramps (Betic Cordillera, S Spain)</dc:title>
      <dc:creator>Aguirre Rodríguez, Julio</dc:creator>
      <dc:creator>Braga Alarcón, Juan Carlos</dc:creator>
      <dc:subject>Rhodolith beds</dc:subject>
      <dc:subject>Autochthonous-allochthonous assemblages</dc:subject>
      <dc:subject>Carbonate ramps</dc:subject>
      <dc:subject>Guadalquivir Basin</dc:subject>
      <dc:subject>Jimena</dc:subject>
      <dc:subject>Jódar</dc:subject>
      <dc:subject>Betic Cordillera</dc:subject>
      <dc:description>Serravallian (middle Miocene) coralline algal assemblages at the southern&#xd;
margin of the Guadalquivir Basin (southern Spain) occur as rhodoliths&#xd;
preserved in situ or very close to their growth habitats&#xd;
(autochthonous–parautochthonous assemblages) and also as reworked&#xd;
remains (allochthonous assemblages). The former assemblages consist of&#xd;
spherical rhodoliths built up by encrusting to warty plants and also of large&#xd;
fragments of branches, whereas the latter are mostly unrecognizable small&#xd;
fragments occurring in channeled packstone–grainstone beds. In both cases,&#xd;
the most abundant components are members of the order Hapalidiales&#xd;
(Mesophyllum roveretoi, Mesophyllum sp., Lithothamnion ramosissimum,&#xd;
and less frequently Phymatolithon group calcareum and Lithothamnion&#xd;
group corallioides). Laminar growths of Lithoporella minus and branches of&#xd;
Spongites group fruticulosus and Sporolithon sp. occur very rarely. There are&#xd;
also anecdotal records of Subterraniphyllum thomasii, extending its upper&#xd;
stratigraphic range up to the Serravallian in the western Tethys. The&#xd;
autochthonous–parautochthonous coralline algal assemblages formed in a&#xd;
middle ramp, at several tens of meters of water depth, as suggested by the&#xd;
dominance of Hapalidiales. The allochthonous assemblages represent&#xd;
fragments of coralline algae derived from the middle ramp and redeposited&#xd;
in deeper settings, most likely the outer ramp, due to storm-generated currents.</dc:description>
      <dc:date>2022-09-29T12:12:48Z</dc:date>
      <dc:date>2022-09-29T12:12:48Z</dc:date>
      <dc:date>2022-08-26</dc:date>
      <dc:type>info:eu-repo/semantics/article</dc:type>
      <dc:identifier>Aguirre J and Braga JC (2022), Middle Miocene (Serravallian) rhodoliths and coralline algal debris in carbonate ramps (Betic Cordillera, S Spain). Front. Earth Sci. 10:958148. doi: [10.3389/feart.2022.958148]</dc:identifier>
      <dc:identifier>https://hdl.handle.net/10481/77080</dc:identifier>
      <dc:identifier>10.3389/feart.2022.958148</dc:identifier>
      <dc:language>eng</dc:language>
      <dc:rights>http://creativecommons.org/licenses/by/4.0/</dc:rights>
      <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
      <dc:rights>Atribución 4.0 Internacional</dc:rights>
      <dc:publisher>Frontiers</dc:publisher>
   </ow:Publication>
</rdf:RDF>