<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>Antoine, Pierre-Olivier</dc:creator>
  <dc:creator>Made, Jan van der</dc:creator>
  <dc:creator>Métais, Grégoire</dc:creator>
  <dc:creator>Phuc, Laq The</dc:creator>
  <dc:creator>Quan, Quý Trương</dc:creator>
  <dc:creator>Schneider, Simon</dc:creator>
  <dc:creator>Tran, Dang Ngoc</dc:creator>
  <dc:creator>Vasilyan, Davit</dc:creator>
  <dc:creator>Viet, Luong The</dc:creator>
  <dc:creator>Böhme, Madelaine</dc:creator>
  <dc:date>2018-06-01</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Current scientific knowledge of Tertiary fossils from south of the Ailao Shan-Red River  shear zone is extremely poor, in sharp contrast with the situation nowadays, as the  area of Laos and Vietnam is regarded as a global hotspot of biodiversity. In this  context, the few localities that yielded fossil assemblages are of first importance for  the understanding of Cenozoic palaeobiogeography and the tectonic and  palaeogeographical evolution of the region. Hang Mon 1 (Son La Province, Northern  Vietnam) was the first site that provided evidence of Tertiary mammals, but its age  remained very controversial, interpretations ranging from Oligocene to Late Miocene.  Herein, we re-investigate the mammal fauna of the locality based on newly collected  material and previously published fossil mammals. A new outcrop, Hang Mon 2,  provides evidence of the rhinoceroses Pleuroceros blanfordi and Bugtirhinus sp.  Together with the earlier finds of uncommonly small-sized Protaceratherium, these  fossils allow a correlation to the earliest Miocene (most probably ranging from ~23 to  ~21 Ma; Aquitanian) based on faunal comparison with the Sulaiman Province of  Pakistan. The revision of the mammals from Hang Mon 1 is in agreement with this  stratigraphic proposal. In addition, the discoveries from Vietnam (the rhinocerotid  assemblage and Hyotherium) further support the hypothesis of strong biogeographical  and environmental affinities between Europe, the Indian Subcontinent and Southeast  Asia (Vietnam) during the Aquitanian.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/307047</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/307047/files/vas_bps.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s12549-017-0295-y</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Palaeobiodiversity and Palaeoenvironments. - 2018, vol. 98, no. 2, p. 287–313</dc:source>
  <dc:subject>info:eu-repo/classification/udc/56</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Biochronological and palaeobiogeographical significance of the earliest Miocene mammal fauna from Northern Vietnam</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
