<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" 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:creator>Vasilyan, Davit</dc:creator>
  <dc:date>2018-08-27</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Background Amphibians, due to their ecophysiological peculiarities, have a physiology  dependent on environmental conditions and sensitively respond to their changes.  Here, the oldest record of the genus Thaumastosaurus is described, whose fossil  record known exclusively from Western Europe is discussed in the scope of the  climatic changes of 33.5–40.5 Ma. Results In the present paper, the fossil remains of  the genus from three localities in Switzerland (11 samples overall) have been studied  and referred to the species Thaumastosaurus bottii. Its stratigraphic distribution has  been revised and summarised. The studied localities present the stratigraphically  oldest and the most eastern occurrences of the genus Thaumastosaurus. Eocene  probable ranids (Ranidae indet./Rana sp./? Rana sp.) from Europe could be referred  to Thaumastosaurus. Discussion Their first occurrence of ranids most likely coincides  with a warm phase of the global climate at 40 Ma, as tropical conditions were  prevailing in Europe. As a result of the gradual cooling of the global climate, the  tropical conditions in Europe were replaced by drier open habitats towards the latest  Eocene at 34 Ma, when the latest occurrence of the European endemic genus  Thaumastosaurus is known. Taking the fossil record and the climate evolution of that  time into account, it can be concluded that Thaumastosaurus represents one of the  groups among the vertebrates that disappeared during the large extinction event at  the Eo–Oligocene transition, known as the Grande Coupure. The fossil finds of the  genus from the studied localities allow to refer the previously suggested Eocene true  frogs to the genus Thaumastosaurus, hereby stating the arrival of the true frog family  Ranidae by the genus Pelophylax in Europe from the east at the earliest Oligocene.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/307224</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307224/files/vas_ewe.pdf</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307224/files/vas_ewe_sm.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.7717/peerj.5511</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>PeerJ. - 2018, vol. 6, p. e5511</dc:source>
  <dc:subject>info:eu-repo/classification/udc/56</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Eocene Western European endemic genus Thaumastosaurus: new insights into the question “Are the Ranidae known prior to the Oligocene?”</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
