The adaptive radiation of hipparionins after their Old World dispersal was linked with a trend towards smaller body sizes. The appearance of the small-sized forms has usually been associated to open environments and grazing diets. A recent approach, moreover, highlights the role of life history modifications related to habitat conditions as triggers of their size shifts. Here, we test the relationship between hipparionin size and diet analyzing the dental microwear textures of different-sized hipparionins from Vallesian and Turolian circum-Mediterranean localities. Our results show that hippari-onins were mainly mixed-feeders and that there was no general link between body size and diet. However, we identified broader feeding spectra in western Mediterranean smaller forms and more specialized grazing diets in larger ones, a differentiation not found in the eastern Mediterranean hipparionins. At odds with the notion of more open habitats eastward, we detected a larger browsing component in eastern hipparionin diets. The consumption by extant equids of more woody browse during the dry season leads us to propose a greater seasonality as a possible cause. Considering the argu-able role of external abrasives on the microwear, another interpretation might involve the presence of more grit in the eastern opener habitats. Interestingly, we found that sympatric hipparionins tend to have similar feeding habits, which points to the fact that their diets were influenced by the local environment. Our results, then, suggest that the small size of some hipparionins resulted from different selective pressures rather than to a general adaptation to increasing habitat opening., MCIN/AEI [PID2020-117118GBI00]; CERCA Program, Generalitat de Catalunya; Wenner-Gren International Collaborative Research Grant; Ege University [TTM/001/2015, TTM/001/2016]; AGAUR [2017 SGR 960]; FI-DGR 2016 grant - AGAUR (Generalitat de Catalunya) [2016FI_B00202]; Erasmus + fellowship; [SYN-THESIS ES-TAF-1846]; [CGL2015-63777], We would like to thank M. Fernandez and X. Aymerich for the molding of the material from the ICP (Institut Catala de Paleontologia Miquel Crusafont) . G.O-O. acknowledges the help received from F. Martin (PALEVOPRIM) during the obtainment of the DMT parameters and the posterior analyses. We further thank to D. Kostopoulos (Aristotle University of Thessaloniki) for his comments on the earlier versions of this manuscript. The editors (Y. Nakamura, A. Bush, and J.X. Samuels) and four reviewers including J. Saarinen are acknowledged for their helpful comments. Moreover, we would like to thank to the authorities of the following museum collections to give access to the related materials: Museo Nacional de Ciencias Naturales (MNCN), ICP museum, Laboratory of Geology and Palaeon-tology at the University of Thessaloniki, Palaeontological Museum Dimitar Kovachev at Asenovgrad, and the Ege University Natural History Museum. Funding for this study was provided by the Grant PID2020-117118GBI00 funded by MCIN/AEI/10.3039/501100011033 (M.K) , the project CGL2015-63777 (M.K) , and the CERCA Program, Generalitat de Catalunya. R.S.S., T.K., S.M., and G.M. were granted through a Wenner-Gren International Collaborative Research Grant (PIs: R.S. Scott and T. Kaya) to collect most of the Vallesian and Turolian equiddental molds from the eastern Mediterranean, and S.M. and T.K. were supported by the Ege University Research Projects TTM/001/2015 and TTM/001/2016. M.K. and G.O-O. were part of a research group recognized without funding by AGAUR (2017 SGR 960) and G.O-O. was supported by a FI-DGR 2016 grant (2016FI_B00202) awarded by AGAUR (Generalitat de Catalunya) and held an Erasmus + fellowship during his stay in the PALEVOPRIM laboratory (CNRS and University of Poitiers). The grant SYN-THESIS ES-TAF-1846 for the stay of J.C. at the MNCN of Madrid is also acknowledged.