<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>Song, Yi-Gang</dc:creator>
  <dc:creator>Li, Ying</dc:creator>
  <dc:creator>Meng, Hong-Hu</dc:creator>
  <dc:creator>Fragnière, Yann</dc:creator>
  <dc:creator>Ge, Bin-Jie</dc:creator>
  <dc:creator>Sakio, Hitoshi</dc:creator>
  <dc:creator>Yousefzadeh, Hamed</dc:creator>
  <dc:creator>Bétrisey, Sébastien</dc:creator>
  <dc:creator>Kozlowski, Gregor</dc:creator>
  <dc:date>2020-11-09</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">Relict species play an important role in understanding the biogeography of  intercontinental disjunctions. Pterocarya (a relict genus) is the valuable model taxon  for studying the biogeography of East Asian versus southern European/West Asian  disjunct patterns. This disjunction has not been as well studied as others (e.g.,  between Eastern Asia and North America). Several phylogenetic studies on  Pterocarya have been conducted, but none have provided a satisfactory phylogenetic  resolution. Here, we report the first well-resolved phylogeny of Pterocarya using  restriction site-associated DNA sequencing data based on the sampling of all taxa  across the entire distribution area of the genus. Taxonomic treatments were also  clarified by combining morphological traits. Furthermore, fossil-calibrated phylogeny  was used to explore the biogeography of Pterocarya. Our results support the  existence of two sections in Pterocarya, which is in accordance with morphological  taxonomy. Section Platyptera comprises three species: P. rhoifolia, P. macroptera, and  P. delavayi. Section Pterocarya also comprises three species: P. fraxinifolia, P.  hupehensis, and P. stenoptera. The divergence between the two sections took place  during the early Miocene (20.5 Ma). The formation of the Gobi Desert and climate  cooling of northern Siberia in the Middle Miocene (15.7 Ma) might have caused the  split of the continuous distribution of this genus and the formation of the East Asian  versus southern European/West Asian disjunct pattern. Lastly, the divergence  between P. hupehensis and P. stenoptera as well as between P. rhoifolia and P.  macroptera/P. delavayi (10.0 Ma) supports the late Miocene diversification hypothesis  in East Asia.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/308982</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308982/files/koz_ptb.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.3390/plants9111524</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Plants. - 2020, vol. 9, no. 11, p. 1524</dc:source>
  <dc:subject>info:eu-repo/classification/udc/57</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Phylogeny, taxonomy, and biogeography of Pterocarya (Juglandaceae)</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
