Evolution of the Family Equidae, Subfamily Equinae, in North, Central and South America, Eurasia and Africa during the Plio-Pleistocene

Biology (Basel). 2022 Aug 24;11(9):1258. doi: 10.3390/biology11091258.

Abstract

Studies of horse evolution arose during the middle of the 19th century, and several hypotheses have been proposed for their taxonomy, paleobiogeography, paleoecology and evolution. The present contribution represents a collaboration of 19 multinational experts with the goal of providing an updated summary of Pliocene and Pleistocene North, Central and South American, Eurasian and African horses. At the present time, we recognize 114 valid species across these continents, plus 4 North African species in need of further investigation. Our biochronology and biogeography sections integrate Equinae taxonomic records with their chronologic and geographic ranges recognizing regional biochronologic frameworks. The paleoecology section provides insights into paleobotany and diet utilizing both the mesowear and light microscopic methods, along with calculation of body masses. We provide a temporal sequence of maps that render paleoclimatic conditions across these continents integrated with Equinae occurrences. These records reveal a succession of extinctions of primitive lineages and the rise and diversification of more modern taxa. Two recent morphological-based cladistic analyses are presented here as competing hypotheses, with reference to molecular-based phylogenies. Our contribution represents a state-of-the art understanding of Plio-Pleistocene Equus evolution, their biochronologic and biogeographic background and paleoecological and paleoclimatic contexts.

Keywords: Equidae; Equinae; biochronology; equini; evolution; hipparionini; paleoclimatology; paleoecology; phylogeny; protohippini.

Grants and funding

This research was funded by the National Science Foundation (DBI:ABI 1759882 and 1759821) to R.L. Bernor and E. Davis, respectively, under the aegis of the FuTRES Equid working group for which they, O. Cirilli and H. Machado have been funded. F.K. has been funded by Finnish Cultural Foundation (project nr. 00220063). Z.L. acknowledge the Admission Scholarship from University of Ottawa, and a Canadian Graduate Scholarship-Doctoral Program from Natural Sciences and Engineering Research Council of Canada. A.M.J. thanks the Yale Institute for Biospheric Studies for funding. L.P. thanks the European Commission’s Research Infrastructure Action, EU-SYNTHESYS projects AT-TAF-2550, DE-TAF-3049, GB-TAF-2825, HU-TAF-3593, HU-TAF-5477, ES-TAF-2997, the SYNTHESYS Project http://www.synthesys.info/ (access on 5 August 2022) which is financed by European Community Research Infrastructure Action under the FP7 “Capacities” Program, and the research project “Ecomorphology of fossil and extant Hippopotamids and Rhinocerotids” granted to L.P. by the University of Florence (“Progetto Giovani Ricercatori Protagonisti” initiative). J.S. wishes to acknowledge the Academy of Finland (AoF. project nr. 340775/346292, “NEPA-Non-analogue ecosystems in the past”). F.S. is supported by Sapienza “5 per mille” funds (ref. SPC: 2021-0070-1350-175998).