Carpodaptes

The fossil record of Carpodaptes is relatively sparse excluding jaw and teeth fragments. However, much can be concluded off of these few fragments. Their upper jaw had a dental formula of 2:1:3:3 and 2:1:2:3 on their lower jaw. Carpodaptes are characterized by their plagiaulacoid dentition seen on their first lower premolar. Their p4 had 5-7 apical cusps depending on the specimen.[2] This enlarged p4 would have potentially allowed the mammal to have crack open nuts and seeds as well as act as a slicing function on invertebrates. Their p3 is characterized by lingual apical cusps that are flattened and sometimes even concave.[4] In some species of Carpodaptes, their upper M1 indicates a specialized wedging function that acts in accordance with their p4. The varying development of dentition between Carpodaptes species indicates they were adapting their teeth to conform with a high fiber diet. However, their teeth are still rather primitive in comparison to other early-diverging primatomorphans of this era. Carpodaptes are also recognized by the loss of their p2, and some species even show to have a shortening of their mandible to potentially exert a greater biting force. Finally, their upper molars are studded and file-like which would have assisted with breaking open nuts and seeds.[2]

Carpodaptes is part of an early diverging group of primates that lived approximately 60 million years ago. This genus was first identified in 1921 by Matthew and Granger.[3] They are sister taxa to Carpolestes and Carpocristes. Carpocristes, unlike Carpolestes and Carpodaptes, dominated Asia whereas the other two thrived in North America.[1] Within the genus, 7 species have been identified: Carpodaptes aulacodon, Carpodaptes cygneus, Carpodaptes hazelae, Carpodaptes hobackensis, Carpodaptes jepseni, Carpodaptes rosei, and Carpodaptes stonleyi.[5]

It was originally thought that Carpodaptes was a subset of the genus Carpocristes until recent discoveries found the progression of ridges, serrations, and apical cusps more well defined in Carpodaptes than Carpocristes. This suggests that Carpocristes diverges from an earlier common ancestor with Carpodaptes rather than Carpodaptes being a direct descendant of Carpocristes.[4]

The brief connection of North America with Europe could help explain how Carpodaptes expanded to Asian localities, however it is perplexing that no fossil evidence has been recovered from European regions. This may suggest Carpodaptes survived more efficiently in a warm and dry climate than a warm and moist one.[2]

Carpodaptes prospered during the late Paleocene and some species made it through the early Eocene. Fragments of Carpodaptes have been notably found in the Swan Hills of Canada, Big Horn Basin, and Clark Forks Basin in Wyoming. This suggests that Carpodaptes lived in a subtropical, humid climate in which there would have been plenty of flora to seek refuge from larger animals.[2] This coincides with the hypothesis that Carpodaptes mainly consumed fruits and nuts as there is a corresponding diversification of plant species in the late Paleocene.[4] At the same time, insects began to recover from the Paleocene–Eocene Thermal Maximum which allowed Carpodaptes to expand into broader niches with a broader dietary requirement. The radiation of insect herbivores in the late Paleocene is a possible explanation of a rise in CO2 levels at the end of the Paleocene.[1] This would have been in part of Carpodaptes radiation into scansorial insectivores. It could also explain why many species of Carpodaptes did not survive through the Paleocene-Eocene boundary.