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Hyaenodonta

Extinct order of mammals

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Species from order Hyaenodonta.
derivative work: user:The Explaner · CC BY 4.0

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Through Extinction, Europe and North America

The order currently consists of three superfamilies, Hyaenodontoidae, Hyainailouroidea, and Limnocyonoidea, in addition to smaller groups such as the Galecyon clade. The hyaenodontoids consisted of Hyaenodontidae and Proviverrinae, the hyainailouroids consisted of Hyainailouridae, Prionogalidae, and Teratodontidae, and with the limnocyonoids consisted of Limocyoninae, Sinopinae, and Arfiinae. Hyaenodonts saw their diversification peak during the Middle-Late Eocene, before seeing a significant decline in diversity following the Eocene-Oligocene extinction event. In Afro-Arabia and Europe, they saw a recovery in diversity following the extinction event before seeing a terminal decline something during the Late Oligocene and Early Miocene respectively. The last hyaenodont would go extinct 7.5 Ma.

The extinction of the order has been debated by experts, many experts argued that their extinction was the result of competition with carnivorans. But over the recent years, many experts have questioned that hypothesis and argued their decline and extinction in most of their range was due to climatic changes.

Taxonomy

Classification

Hyaenodonts were considerably more widespread and successful than the oxyaenids, the other clade of mammals originally classified along with the hyaenodonts as part of Creodonta. In 2015 phylogenetic analysis of Paleogene mammals, by Halliday et al., monophyly of Creodonta was supported and was placed in the clade Ferae, closer to Pholidota than to Carnivora. However, most experts consider Creodonta to be considered to be a polyphyletic order as it contains two unrelated clades. Most experts have now recovered Hyaenodonta and Oxyaenodonta as distinct orders within Pan-Carnivora.

Recent phylogenetic modeling suggests hyaenodonts were sister group to the Oxyaenodonta-Carnivoraformes clade.

Phylogeny

Cladogram of Hyainailourinae recovered by Al-Ashqar et al. (2025):

Evolution

When the order arose exactly has changed over the years, Solé and Smith (2013) suggested hyaenodonts arose in the Late Paleocene roughly 58 Ma. Solé et al. (2009), as well as Borths and Stevens (2019), suggested an Early Paleocene origin for the order. However, majority of phylogenetic modeling over the recent years had support a Late Cretaceous origin for the order.

The biogeographic origin of the group has also been hotly debated by experts. Solé et al. (2009) suggested an African origin for the order as the known oldest hyaenodonts were recovered there, in additional to the diversity of hyaenodonts within the Ouarzazate basin. Bayesian analysis by various studies had found strong evidence of hyaenodonts originating from Europe. Borths et al. (2016) noted while European and North America origins were problematic due to hyaneodonts not being recorded before the Paleocene-Eocene boundary, European Paleocene records were poor unlike North America. They also noted Afro-Arabian origins for the order have never been tested using phylogenetic analysis and was based on the assumption that Lahimia was a basal hyaenodont although more recent analysis suggest it wasn't a basal hyaenodont. On the other hand, Bayesian analysis by Al-Ashqar et al. (2025) found stronger evidence of a North American origin than a European origin.

From Europe, hyaenodonts would have dispersed into Africa and from there dispersed into India. The oldest known hyaenodonts were Lahimia and Tinerhodon from the middle Paleocene of Morocco. Afterwards, hyaenodonts dispersed into Asia from either Europe or India, and dispersed into North America from either Europe or Asia. Proviverrines experience a radiation in diversity during the Early Eocene, due to the lack of competition and the Early Eocene Climatic Optimum. In Africa, hyaenodonts saw an increase in subfamilial richness after the end of the Early Eocene Climatic Optimum. During the middle to late Eocene, hyaenodonts, along with carnivorans, replaced oxyaenids, mesonychians, and miacoids in North America and Europe. With the former, the extinction of European mesonychids and oxyaenids resulted in the diversification of hyaenodonts, as well as an increase in body size. For most of the Paleogene, hyaenodonts were the dominant group of mammalian carnivores in Africa and Europe.

The order saw a massive decline globally during the Eocene-Oligocene extinction event due to the decline of favorable prey and the expansion of open environments. Following the boundary event, hyaenodonts experienced a rebound in diversity in Europe and Afro-Arabia. During the Early Miocene, the formation of the Gomphotherium land bridge saw the dispersal of hyaenodonts into Eurasia.

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