Alticonodon is a genus of extinct mammal from the Late Cretaceous of North America. It is one of the geologically youngest known eutriconodonts, and is a fairly more specialised animal than earlier representatives of this clade.^[1]

Quick Facts Scientific classification, Binomial name ...

Alticonodon Temporal range: Santonian-Campanian, 84.5–83.5 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Chordata
Class:	Mammalia
Order:	†Eutriconodonta
Family:	†Triconodontidae
Subfamily:	†Alticonodontinae
Genus:	†Alticonodon Fox, 1969
Species:	†A. lindoei
Binomial name
†Alticonodon lindoei Fox, 1969

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Alticonodon is currently a monotypic genus, represented exclusively by A. lindoei. It is known from the Milk River Formation deposits of the early Campanian of Alberta, Canada. It is known from two specimens: a dentary fragment bearing two molars, and an isolated lower last molar.

Alticonodon has been consistently recovered as a triconodontid, and more specifically as an alticonodontine,^[2] though the latter term may be redundant in relation to the rest of Triconodontidae.^[3]

Compared to earlier eutriconodonts, Alticonodon has molars better specialised for shearing.^[1] As eutriconodonts as a group had shearing molars due to their carnivorous habits,^[4] it can be inferred that Alticonodon was hypercarnivorous.

This ecological specialisation might have come due to competition with other mammals in the region, such as the various metatherians.^[1]

The Milk River Formation is a rich fossil environment that covered near-shore and terrestrial deposits. It included a few dinosaur species like Saurornitholestes and Acrotholus, as well as a variety of other vertebrate such as the crocodilian Gilchristosuchus, various turtles and fish.

The mammalian fauna was primarily dominated by metatherians and multituberculates, as usual for Late Cretaceous mammaliafaunas, but a variety of older taxa remained; besides Alticonodon, there was also the symmetrodont Symmetrodontoides, and Potamotelses and picopsids. These were the last non-therian mammals (other than the highly successful multituberculates) in North America, suggesting a relictual element to the region's fauna.