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   <dc:title>Middle Devonian reef‑derived calciturbidites of western Ossa‑Morena Zone (Portugal): conodont biostratigraphy of the Eifelian Pedreira da Engenharia Limestone</dc:title>
   <dc:creator>Silvério,  Gonçalo</dc:creator>
   <dc:creator>Liao Chen, Jau-Chyn</dc:creator>
   <dc:creator>Valenzuela-Ríos, José Ignacio</dc:creator>
   <dc:creator>Machado, Gil</dc:creator>
   <dc:creator>Barreto, Pedro</dc:creator>
   <dc:creator>Moreira, Noel</dc:creator>
   <dc:subject>56:551.734(469)</dc:subject>
   <dc:subject>Eifelian</dc:subject>
   <dc:subject>Conodonts</dc:subject>
   <dc:subject>Calciturbidites</dc:subject>
   <dc:subject>Pedreira da Engenharia limestone</dc:subject>
   <dc:subject>Cabrela Basin</dc:subject>
   <dc:subject>Ossa-Morena Zone</dc:subject>
   <dc:subject>Paleontología</dc:subject>
   <dc:subject>2416.02 Paleontología de Los Invertebrados</dc:subject>
   <dc:description>The first biostratigraphical study on the complete Pedreira da Engenharia quarry section (Middle Devonian, SW Portugal) is presented. A total of 32 samples were collected from the three subsections (PE-A, quarry floor; PE-B and PE-C). This led to the identification of 15 species belonging to the genera Icriodus, Polygnathus and Tortodus. Four index species were identified: P. costatus; T. australis; T. kockelianus; and P. ensensis. The age for the Pedreira da Engenharia section was updated from the costatus zone (Boogaard, 1972) to the costatus-ensensis zones (lower to uppermost Eifelian). There is a thin part of the succession representing the kockelianus and, possibly, eiflius zones, together being represented by 1,5 m. A CAI value of 5-5.5 for the conodont elements indicates a maximum temperature of over 300 ºC. The Pedreira da Engenharia Limestone, together with the Odivelas Limestone, are evidence of the development of calciturbidite sedimentation associated with atoll-like structures (only preserved in Odivelas) along the SW boundary of Ossa-Morena Zone, being probably associated with the beginning of the subduction of the Rheic Ocean during Early to Middle Devonian times.</dc:description>
   <dc:description>Fundação para a Ciência e a Tecnologia (Portugal)</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>2024-07-09T18:14:57Z</dc:date>
   <dc:date>2024-07-09T18:14:57Z</dc:date>
   <dc:date>2024</dc:date>
   <dc:type>journal article</dc:type>
   <dc:identifier>https://hdl.handle.net/20.500.14352/105882</dc:identifier>
   <dc:identifier>1698-6180</dc:identifier>
   <dc:identifier>10.1007/s41513-024-00242-0</dc:identifier>
   <dc:identifier>1886-7995</dc:identifier>
   <dc:language>eng</dc:language>
   <dc:relation>UIDB/04683/2020  MICCIN-MIU, CAS22/00148</dc:relation>
   <dc:relation>UIDP/04683/2020</dc:relation>
   <dc:relation>MIU Next Generation EU, ZA21-005</dc:relation>
   <dc:relation>UIDB/04683/2020</dc:relation>
   <dc:relation>ALT20-03-0145-FEER-000028</dc:relation>
   <dc:relation>2020.08450.BD</dc:relation>
   <dc:relation>UNESCO-IGCP 652</dc:relation>
   <dc:relation>PALPALPAL (GIUV2017-395)</dc:relation>
   <dc:relation>PERIGONDWANA (UCM 910231)</dc:relation>
   <dc:rights>Attribution 4.0 International</dc:rights>
   <dc:rights>http://creativecommons.org/licenses/by/4.0/</dc:rights>
   <dc:rights>open access</dc:rights>
   <dc:format>application/pdf</dc:format>
   <dc:publisher>Springer</dc:publisher>
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