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Omomyidae

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Omomyids
Temporal range: 55–34 Ma Late Paleocene – Oligocene[1]
The skull of Anaptomorphus
Scientific classification
Kingdom:
Animalia
Phylum:
Chordata
Class:
Mammalia
Order:
Primates
Suborder:
Haplorrhini
Family:
Omomyidae
Subfamilies

Omomyids (members of the family Omomyidae) are a diverse group of extinct primates that radiated during the Eocene epoch (34 to 59 mya) between about 55 and 34 million years ago (mya). Fossils of omomyids are found in North America, Europe, Asia, and possibly Africa. Omomyids are one of two groups of Eocene primates with a geographic distribution spanning holarctic continents, the other being the adapids (family Adapidae). Early representatives of the Omomyidae and Adapidae appear suddenly at the beginning of the Eocene (59 mya) in North America, Europe, and Asia, and are the earliest known crown primates.

Features that characterize many omomyids include large orbits (eye sockets), shortened rostra and dental arcades, loss of anterior premolars, cheek teeth adapted for insectivorous or frugivorous diets, and relatively small body mass (i.e., less than 500 g). However, by the late middle Eocene (about 40 mya), some North American omomyids (e.g., Macrotarsius) evolved body masses in excess of 1 kg and frugivorous or folivorous diets. Large orbits in genera such as Tetonius, Shoshonius, Necrolemur, and Microchoerus indicate that these taxa were probably nocturnal. At least one omomyid genus from the late Eocene of Texas (Rooneyia) had small orbits and was probably diurnal.

Like primates alive today, omomyids had grasping hands and feet with digits tipped by nails instead of claws. Features of their skeletons strongly indicate that omomyids lived in trees. In at least one genus (Necrolemur), the lower leg bones, the tibia and fibula, were fused as in modern tarsiers. This feature may indicate that Necrolemur leaped frequently. Most other omomyid genera (e.g., Omomys) lack specializations for leaping, and their skeletons are more like those of living dwarf and mouse lemurs.

Omomyid systematics and evolutionary relationships are controversial. Various authors[citation needed] have suggested that omomyids are:

  1. stem haplorhines [i.e., basal members of the group including living tarsiers and anthropoids].
  2. stem tarsiiformes [i.e., basal offshoots of the tarsier lineage].
  3. stem primates more closely related to adapids than to living primate taxa.

Attempts to link omomyids to living groups have been complicated by their primitive (plesiomorphic) skeletal anatomy. For example, omomyids lack the numerous skeletal specializations of living haplorhines, including:

  1. significant reduction of the canal for the stapedial branch of the internal carotid artery.
  2. a "perbullar" (rather than "transpromontorial") route of the canal for the promontory branch of the internal carotid artery.
  3. contact between the alisphenoid and zygomatic bones.
  4. presence of an anterior accessory cavity confluent with the tympanic cavity.

Omomyids further demonstrate a gap between the upper central incisors, which presumably indicates the presence of a rhinarium and philtrum to channel fluids into the vomeronasal organ. Omomyids as a group also lack most of the derived specializations of living tarsiers, such as extremely enlarged orbits (Shoshonius is a possible exception), a large suprameatal foramen for an anastomosis between the posterior auricular and middle meningeal circulation (again, Shoshonius is a possible exception, but the contents of the foramen in this extinct taxon are unknown), and extreme postcranial adaptations for leaping. In other respects (i.e., presence of an aphaneric, or intrabullar, ectotympanic bone connected to the lateral bullar wall by an unbroken annular bridge), omomyids are uniquely derived among primates.

Classification

References

  1. ^ Savage, RJG, & Long, MR (1986). Mammal Evolution: an illustrated guide. New York: Facts on File. p. 365. ISBN 0-8160-1194-X.{{cite book}}: CS1 maint: multiple names: authors list (link)
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