Hyracotherium leporinum
Hyracotherium leporinum
Summary
Hyracotherium leporinum was a small, very early odd-toed ungulate. It was once presented as the archetypal ‘dawn horse’, but current phylogenetic work places it close to the base of Perissodactyla, before the major split between the horse lineage and the tapir–rhinoceros lineage. It is therefore more useful to picture it as a primitive perissodactyl in its own right than as a miniature modern horse.
Its low-crowned cheek teeth combine rounded cusps with developing transverse crests. That dentition is suited to cropping and processing relatively soft vegetation, so browsing on leaves, shoots and fruit is a reasonable dietary interpretation rather than evidence for grazing. A small, terrestrial and fairly active animal is plausible by comparison with other early perissodactyls, but the London Clay species itself is known much better from its skull and teeth than from its limbs.
The type is a fragmentary but uncrushed skull with a substantial upper tooth row, making cranial and dental anatomy unusually informative for such an early mammal. The cheek teeth are also notably variable, which is why the species is best understood from combinations of characters across the tooth row rather than from a single worn molar.
Quick Identification
Look for: a small perissodactyl upper jaw with a gap immediately behind P1, a simple P2 lacking a protocone, P3–P4 with strong outer cingula and distinct paraconules, and low-crowned molars with strong intermediate cusps and crests. A single isolated molar can overlap other early perissodactyls, so the tooth-row combination is much more reliable.
Diagnostic Features
- A distinct diastema separates P1 from P2, with P1 positioned closer to P2 than to the canine.
- P2 lacks a protocone, leaving it markedly simpler than the following upper premolars.
- P3 and P4 have strong labial cingula, and their protocones lie directly lingual to the paracones rather than being strongly offset.
- P3 has no metaconule whereas P4 has a strong metaconule, producing a conspicuous change in premolar complexity along the row.
- M1–M3 have strong para- and metaconules with constricted protolophs and metalophs, and a centrocrista that is only weakly flexed towards the cheek side.
Fossil Details
Recorded Fossil Sites
London Clay Formation
References
- Bronnert, C.; Métais, G. (2023). Early Eocene hippomorph perissodactyls (Mammalia) from the Paris Basin. Geodiversitas, 45(9), 277–326 View reference
- Owen, R. (1841). Description of the fossil remains of a Mammal (Hyracotherium leporinum) and of a bird (Lithornis vulturinus) from the London Clay. Transactions of the Geological Society of London, 6(1), 203–208 View reference
- Simpson, G. G. (1952). Notes on British hyracotheres. Zoological Journal of the Linnean Society, 42(284), 195–206 View reference
- Smith, T.; Smith, R. (2003). Terrestrial mammals as biostratigraphic indicators in upper Paleocene–lower Eocene marine deposits of the southern North Sea Basin. Causes and Consequences of Globally Warm Climates in the Early Paleogene, 513–520. Geological Society of America, Boulder, Colorado View reference
- Tissier, J.; Smith, T. (2026). Earliest perissodactyls reveal large-scale dispersals during the PETM. Proceedings of the National Academy of Sciences of the United States of America, 123(4), e2519690122 View reference