2021
DOI: 10.1016/j.gecco.2021.e01839
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Mid-Pleistocene Transition as a trigger for diversification in the Irano-Anatolian region: Evidence revealed by phylogeography and distribution pattern of the eastern three-lined lizard

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Cited by 12 publications
(9 citation statements)
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“…Thus, given the weak support for the role of several climatic niche variables in diversification (i.e. T max , PREC max , ELEV avg ) and the results of recent studies in subsets of the group (Ghane‐Ameleh et al, 2021), we cannot completely exclude the possibility that climatic niche evolution may have contributed to speciation dynamics of this group during climatic oscillations.…”
Section: Discussionmentioning
confidence: 74%
“…Thus, given the weak support for the role of several climatic niche variables in diversification (i.e. T max , PREC max , ELEV avg ) and the results of recent studies in subsets of the group (Ghane‐Ameleh et al, 2021), we cannot completely exclude the possibility that climatic niche evolution may have contributed to speciation dynamics of this group during climatic oscillations.…”
Section: Discussionmentioning
confidence: 74%
“…Irano-Anatolian and Caucasus biodiversity hotspots are known for their highly endemic alpine and subalpine flora which correlates with a high degree of topological isolation caused by the recent uplift in the various mountain systems in these regions, such as the Turkish-Iranian plateau plateau and its major mountainous components, i.e., Zagros, Alborz, Caucasus, and Kopet-Dag mountains. Although some studies attempted to assess the huge diversity within some endemic taxa in these regions in terms of molecular clock, biogeography, and dispersal patterns (Ghane-Ameleh et al 2021; Noroozi et al 2018), our study is the first to address the issue of mega-diversity in the endemic taxa of Irano-Anatolian and Caucasus biodiversity hotspots through phylogeny, molecular clock, and statistical analyses of diversification.…”
Section: Discussionmentioning
confidence: 99%
“…Pleistocene warming–cooling cycles become more similar in intensity and duration at about 0.9–0.8 Mya, which is in the middle Pleistocene transition [ 65 , 66 ]. Intraspecific diversification of many ectothermic taxa in the Mediterranean Basin and surrounding regions have been found to be related to this later period, e.g., [ 58 , 67 , 68 ]. Although the periods of divergence and diversification found for H. viridiflavus mostly predate the past-climatic scenarios used to infer the range dynamics of the species (i.e., the oldest period is the last interglacial, LIG, which occurred about 0.12–0.14 Mya), they are representative of the warming–cooling cycles that occurred in the late Pleistocene and are representative of the posterior warming tendency.…”
Section: Discussionmentioning
confidence: 99%