Diversification in the steppe rat snake <i>Elaphe dione</i> (Pallas, 1773) coincides with the Mid-Pleistocene climatic transition of Eurasia
Our study is the most comprehensive phylogeographic analysis of <i>E. dione</i> to date. The territory of central China most probably served as an ancestral area of this species, where <i>E. dione</i> diverged from its most recent common ancestor with <i>E. bimaculata</i> during the Late Miocene. The most active period of diversification in <i>E. dione</i> was estimated to have occurred later (∼1.3 Mya) than other widespread Palearctic species. Furthermore, this period is correlated across the species' range and coincides with the beginning of the Mid-Pleistocene climatic transition. Climatic and environmental transitions during this period may have triggered the allopatric divergence of <i>E. dione</i> in multiple glacial refugia. Notably, diversification in the Western Palearctic resulted in a greater number of phylogeographic lineages, which could be linked to a greater number of suitable refugia. However, further evidence is needed to confirm these scenarios.
Authors
- Polina I. Chernigova
- Roman A. Nazarov (ORCID: https://orcid.org/0000-0002-7827-6387)
- K Akhmedenov
- Simonov Evgeniy
- Artem Lisachov (ORCID: https://orcid.org/0000-0003-3270-2894)
- Sayagul G. Akhmedenova (ORCID: https://orcid.org/0000-0002-2024-6281)
- Daniel Jablonski
- Oleg Ermakov
- Anastasia Klenina
- Andrey Bakiev
Institutions
- Penza State University (RU)
- Kasetsart University (TH)
- Lomonosov Moscow State University (RU)
- Mahambet Otemiusly West Kazakhstan University (KZ)
- Samara Federal Research Scientific Center (RU)
- Institute of Cytology and Genetics (RU)
- Severtsov Institute of Ecology and Evolution (RU)
- Tyumen State Medical University (RU)
- Comenius University Bratislava (SK)
Publication Details
- Journal
- PeerJ
- Published
- 2026-02-02
- DOI
- https://doi.org/10.7717/peerj.20351
- Primary Topic
- Amphibian and Reptile Biology
- Type
- article
- Field-Weighted Citation Impact
- 0.00