Plesiadapis


Plesiadapis is one of the oldest known primate-like mammal genera which existed about 58-55 million years ago in North America and Europe. Plesiadapis means "near-Adapis", which is a reference to the adapiform primate of the Eocene period, Adapis. Plesiadapis tricuspidens, the type species, is named after the three cusps present on its upper incisors.

Taxonomy

The first discovery of Plesiadapis was made by François Louis Paul Gervaise in 1877, who first discovered Plesiadapis tricuspidens in France. The type specimen is MNHN Crl-16, and is a left mandibular fragment dated to the early Eocene epoch.
This genus probably arose in North America and colonized Europe on a land bridge via Greenland. Thanks to the abundance of the genus and to its rapid evolution, species of Plesiadapis play an important role in the zonation of Late Paleocene continental sediments and in the correlation of faunas on both sides of the Atlantic. Two remarkable skeletons of Plesiadapis, one of them nearly complete, have been found in lake deposits at Menat, France. Although the preservation of the hard parts is poor, these skeletons still show remains of skin and hair as a carbonaceous film—something unique among Paleocene mammals. Details of the bones are better preserved in fossils from Cernay, also in France, where Plesiadapis is one of the most common mammals.

Classification

The following are possible shared derived features of Plesiadapiformes: maxillary-frontal contact in orbit, the presence of a suboptic foramen, an ossified external auditory meatus, the absence of a promontory artery, the absence of a stapedial artery, and a strong mastoid tubercle.
Although the placement of the Plesiadapis lineage is still up for debate, the consensus in the 1970s was that they were closest to early tarsier-like primates. Plesiadapiformes have also been proposed as a nonprimate sister group to Eocene-Recent primates. A study done in 1987 linked Plesiadapiformes with adapids and omomyids through nine shared-derived features, six of which are cranial or dental: auditory bulla inflated and formed by the petrosal bone, ectotympanic expanded laterally and fused medially to the wall of the bulla, promontorium centrally positioned in the bulla, and large hypotympanic sinus widely separating promontorium from the basisphenoid, internal carotid entering the bulla posteriolaterally and enclosed in a bony tube, nannopithex fold on the upper molars, and loss of one pair of incisors.
In 2013, a phylogenetic analysis that includes also the basal primate Archicebus positions Plesiadapis firmly outside of the Primates, as a sister group to both Primates and Dermoptera.
SpeciesSynonymsLocalities
P. tricuspidens
Gervais, 1877

  • P. gervaisi
Lemoin, 1887
  • P. rhemensis
Rütmeyer, 1891
  • P. remensis
Stehlin, 1916
  • P. trouessarti
Schlosser, 1921

  • Cernay, France
  • Lentille, France
  • Berru, France
  • Rilly, France
P. intermediusGazin, 1971
Gazin, 1956
  • Pr. simpsoni
Gazin, 1956
Gingerich, 1974
  • Na. gazini
Gingerich, 1974

  • Douglas Quarry, Montana
  • Little Muddy Creek, Montana
  • Keefer Hill, Wyoming
  • Saddle, Wyoming
P. simpsoniGazin, 1956
  • Pr. simpsoni
Gazin, 1956
  • P. jepseni
Gazin, 1956
  • Na. simpsoni
Gingerich, 1974

  • Ledge, Wyoming
  • West End, Wyoming
P. gidleyiMatthew, 1917
Matthew, 1917
  • P. tricuspidens
Teilhard, 1922
  • Na. gidleyi
Gingerich, 1974

  • Mason Pocket, Colorado
  • Joe's Bone Bed, Texas
  • Black Peaks, Texas
P. fodinatusJepsen, 1930
  • P. rubeyi
Gazin, 1942
  • P. farisi
Dorr, 1952
  • P. jepseni
Gazin, 1956

  • Princeton Quarry, Wyoming
  • Schaff Quarry, Wyoming
  • Ravenscrag, Saskatchewan
  • Titanoides, Wyoming
  • Fossil Hollow, Wyoming
  • Chappo, Wyoming
  • Dell Creek Quarry, Wyoming
P. dubiusMatthew, 1915
  • No. dubius
Matthew, 1915
  • P. pearcei
Gazin, 1956

P. ancepsSimpson, 1936
  • P. jepseni
Gazin, 1956
  • P. praecursor
Gingerich, 1974

  • Tongue River, North Dakota
  • Douglas Quarry, Montana
  • Keefer Hill, Wyoming
  • Scarritt Quarry, Montana
  • Saddle, Wyoming
  • Highway blowout, Montana
P. rexGidley, 1923
Gidley, 1923
  • No. gidleyi
Simpson, 1927
  • P. paskapooensis
Russel, 1964

P. churchilliGingerich, 1974
  • P. farisi
Krishtalka, 1975

  • Croc Tooth Quarry, Wyoming
  • Airport, Wyoming
  • Long Draw Quarry, Montana
  • Badwater, California
  • Sand Draw, Wyoming
P. simonsiGingerich, 1974
  • Sand Draw, Wyoming
P. cookeiJepsen, 1930
P. insignisPiton, 1940
Launay, 1908
Piton, 1940

P. walbeckensisRussel, 1964
P. remensisLemoine, 1887
P. russelliGingerich, 1974
  • P. daubrei
Teilhard, 1922
Russell, 1967

Anatomy and remains

Plesiadapis is one of the most completely known early primatomorphs, with a significant amount of the skeleton known. Though, the skeleton is mostly known from P. gidleyi and the relatively late P. tricuspidens. The skull is overall reminiscent of a lemur, though it lacks the postorbital bars. The brain was probably relatively large compared to similarly sized contemporary mammals, namely the arctocyonids. The dental formula is usually, with two incisors, one canine, three premolars, and three molars in either half of the upper jaw; and one incisor, one canine, three premolars, and one molar in either half of the lower jaw. The incisors are quite long. Already, Plesiadapis had lost the first premolar from the mammalian common ancestor, but later primatomorphs would lose the second premolar as well. P. dubius consistently lacks the lower second premolar, and about half of P. rex specimens lack it too. P. gidleyi and European Plesiadapis lack the lower canines.
The skeletal adaptations are consistent with a largely arboreal lifestyle in the trees. The sacrum of P. gidleyi is similar to that of the eastern gray squirrel, though lacking the strong spines. The humerus is robust and features a strong S-curve.
Nearly all of what is known about the anatomy of plesiadapiforms comes from fragmentary jaws and teeth, so most definitions of plesiadapiform genera and species are based on dentition. Plesiadapis' dentition shows a functional shift toward grinding and crushing in the cheek teeth as an adaptation towards increasing omnivory and herbivory.
The skull of Plesiadapis is relatively broad and flat, with a long snout with rodent-like jaws and teeth and long, gnawing incisors separated by a gap from its molars. Orbits are still directed to the side, unlike the forward-facing eyeballs of modern primates that enable three-dimensional vision. Plesiadapis had mobile limbs that terminated in strongly curved claws, and it sported a long bushy tail which is preserved in the Menat skeletons. The way of life of Plesiadapis has been much debated in the past. Climbing habits could be expected in a relative of the primates, but tree-dwelling animals are rarely found in such high numbers. Based on this and other evidence, some paleontologists have concluded that these animals were mainly living on the ground, like today's marmots and ground squirrels. However, more recent investigations have confirmed that the skeleton of Plesiadapis is that of an adept climber, which can be best compared to tree squirrels or to tree-dwelling marsupials such as possums. The short, robust limbs, the long, laterally compressed claws, and the long, bushy tail indicate that it was an arboreal quadruped. Remains found showed that it had a body mass of around.

Palaeoecology

The teeth of P. russelli and P. cookei indicate these species were adapted to eat leaves. Large Plesiadapis species in Europe evolved to become increasingly adapted for folivory across the Palaeocene-Eocene boundary, although they were not as adapted for a folivorous diet as Platychoerops daubrei.