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Title
  • en Multiple trans-Beringia dispersals of the barklouse genus Trichadenotecnum (Insecta: Psocodea: Psocidae)
Creator
    • en Johnson, Kevin P.
    • en Casasola González, José Arturo
    • en Bess, Emilie
    • en García Aldrete, Alfonso Neri
Accessrights open access
Rights
  • en This is a pre-copyedited, author-produced version of an article accepted for publication in Biological Journal of the Linnean Society following peer review. The version of record Volume 121, Issue 3, July 2017, Pages 501–513 is available online at: https://doi.org/10.1093/biolinnean/blx006.
Subject
  • Other en Arcto-Tertiary relict biota
  • Other en Beringia
  • Other en Isthmus of Panama
  • Other en molecular phylogeny
  • Other en molecular dating
  • Other en ancestral area reconstruction
  • NDC 486
Description
  • Abstract en The causes underlying disjunct distributions are of major importance in biogeography. Arcto-Tertiary relict biotas in the temperate northern hemisphere, which typically show disjunct distributions between Asia and the Nearctic region, are widely known, but often poorly understood examples of disjunct distributions. The distributional pattern of the barklouse genus Trichadenotecnum is an example of an Arcto-Tertiary relict, with centres of species diversity in Asia and Central America. We evaluated the potential causes of this disjunct distribution in Trichadenotecnum using a molecular phylogeny, divergence dating and ancestral area reconstruction. Phylogenetic analysis identified three separate clades of New World Trichadenotecnum, whereas all other groups were distributed in the Old World. Ancestral area and dating analyses recovered three independent events of trans-Beringian dispersal in the Oligocene to Miocene (27–15 Mya). The formation of two disjunct centres of diversity can be explained by the restriction of distributional areas to temperate refugia during the Quaternary glaciations (2.5–0.02 Mya). The South American Trichadenotecnum appeared to have arisen from two independent dispersal events in the Miocene (19–9 Mya). These estimated dispersal dates are much older than the generally assumed date (Pleistocene: c. 3 Mya) for the formation of the Isthmus of Panama.
Publisher en Oxford University Press
Date
    Issued2017-06
Language
  • eng
Resource Type journal article
Version Type AM
Identifier HDL http://hdl.handle.net/2115/75535
Relation
  • isVersionOf DOI https://doi.org/10.1093/biolinnean/blx006
Journal
    • PISSN 0024-4066
    • EISSN 1095-8312
    • NCID AA00565321
      • en Biological Journal of the Linnean Society
      • Volume Number121 Issue Number3 Page Start501 Page End513
File
    • fulltext 2017BJLS.pdf
    • 984.14 KB (application/pdf)
      • Issued2017-06
Oaidate 2023-07-26