4.7 Article

Parthenogenesis through the ice ages: A biogeographic analysis of Caucasian rock lizards (genus Darevskia)

期刊

MOLECULAR PHYLOGENETICS AND EVOLUTION
卷 102, 期 -, 页码 117-127

出版社

ACADEMIC PRESS INC ELSEVIER SCIENCE
DOI: 10.1016/j.ympev.2016.05.035

关键词

Darevskia; Parthenogenesis; mtDNA; Phylogeny; Ecological niche models; Glaciations

资金

  1. project Biodiversity, Ecology and Global Change
  2. North Portugal Regional Operational Program (O Novo Norte) under the National Strategic Reference Framework (NSRF) through the European Regional Development Fund (ERDF) [ON.2]
  3. project Preserving Armenian biodiversity: Joint Portuguese - Armenian program for training in modern conservation biology. of Gulbenkian Foundation (Portugal)
  4. Dokuz Eylul University, Turkey [2009.KB.FEN.003]
  5. FCT [IF2013]
  6. [FCOMP-01-0124-FEDER-007062FCT - Portugal]
  7. [PTDC/BIA-BEC/101256/2008]
  8. Fundação para a Ciência e a Tecnologia [PTDC/BIA-BEC/101256/2008] Funding Source: FCT

向作者/读者索取更多资源

Darevskia rock lizards include both sexual and parthenogenetic species, mostly distributed in the heterogeneous and ecologically diverse Caucasus. The parthenogenetic species originated via directional hybridogenesis, with only some of the sexual species known to serve as parentals. However, it remains unclear when and where these events happened and how many parental lineages were involved. A multilocus phylogeographic analysis was performed on the parthenogens D. unisexualis, D. bendimahiensis and D. uzzeli, and their putative maternal species D. raddei. Results show the parthenogenetic species all have relatively recent origins, approximately 200-70 kyr ago, and at least three hybridization events were involved in their formation. Ecological niche models identify the region where hybridization events leading to the formation of D. unisexualis took place, namely in the northeast of the current distribution. Models also suggest that the sexual D. raddei might have undergone a habitat shift between the Last Interglacial and the Last Glacial Maximum. (C) 2016 Elsevier Inc. All rights reserved.

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