This paper addresses the use of fossil species of the horse Equus as strati
graphic markers in the Pliocene and Pleistocene. Current research shows tha
t the species recently so used do not succeed one another in orderly fashio
n, but occur and co-occur at ages other than presupposed by the stratigraph
ic schemes (usually earlier). Horse species should be identified on their m
orphology, not on their stratigraphic age. 'Subspecies' of fossil horses do
not conform to subspecies in zoology, as they lack a geographic range. The
y thus lack taxonomic status and stratigraphic significance and should be a
voided. (C) 1998 Elsevier Science Ltd. All right reserved.