Articles | Volume 22, issue 9
https://doi.org/10.5194/cp-22-1585-2026
https://doi.org/10.5194/cp-22-1585-2026
Research article
 | 
31 Aug 2026
Research article |  | 31 Aug 2026

Anatolia (Türkiye) during the late Eocene and the Eocene–Oligocene Transition: successive warming and cooling, aridification, and implications for the westward dispersal of Asian terrestrial mammals

Paul Botté, Alexis Licht, Anne-Lise Jourdan, Leny Montheil, François Demory, Mustafa Kaya, Faruk Ocakoğlu, Mehmet Serkan Akkiraz, Deniz İbilioğlu, Pauline Coster, Grégoire Métais, Benjamin Raynaud, and K. Christopher Beard

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Cited articles

Abels, H. A., Dupont-Nivet, G., Xiao, G., Bosboom, R., and Krijgsman, W.: Step-wise change of Asian interior climate preceding the Eocene–Oligocene Transition (EOT), Palaeogeogr. Palaeocl., 299, 399–412, https://doi.org/10.1016/j.palaeo.2010.11.028, 2011. 
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Anderson, N. T., Kelson, J. R., Kele, S., Daëron, M., Bonifacie, M., Horita, J., Mackey, T. J., John, C. M., Kluge, T., Petschnig, P., Jost, A. B., Huntington, K. W., Bernasconi, S. M., and Bergmann, K. D.: A unified clumped isotope thermometer calibration (0.5–1,100 °C) using carbonate-based standardization, Geophys. Res. Lett., 48, e2020GL092069, https://doi.org/10.1029/2020GL092069, 2021. 
Arason, Þ. and Levi, S.: Maximum likelihood solution for inclination-only data in paleomagnetism, Geophys. J. Int., 182, 753–771, https://doi.org/10.1111/j.1365-246X.2010.04671.x, 2010. 
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Short summary
The Eocene–Oligocene Transition (EOT; ~34 Ma) marks a major global cooling that transformed terrestrial ecosystems and influenced mammalian dispersals. A continental record from Anatolia reveals a Late Eocene warming followed by abrupt cooling at the EOT, documented by geochemistry and sedimentology. This interval is also characterized by increasing aridity, which likely contributed to the decline of endemic taxa and facilitated the westward expansion of Asian mammals into western Europe.
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