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Windows on the evolution of Picrodus (Plesiadapiformes: Primates): Morphology and relationships of a species complex from the Paleocene of Alberta

Published online by Cambridge University Press:  11 August 2017

Craig S. Scott  and
Richard C. Fox
Craig S. Scott
Affiliation:
Laboratory for Vertebrate Paleontology, Department of Biological Sciences, University of Alberta, Edmonton T6G 2E9, Canada,
Richard C. Fox
Affiliation:
Laboratory for Vertebrate Paleontology, Department of Biological Sciences, University of Alberta, Edmonton T6G 2E9, Canada,
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Abstract

Since 1908, the peculiar North American primate Picrodus Douglass, 1908 (Picrodontidae; Plesiadapiformes) has been thought to contain only a single species, P. silberlingi Douglass, 1908, of late Paleocene age. However, new collections from the Paskapoo Formation, Alberta, Canada, reveal that instead a rich complex of Picrodus species lived during the Paleocene. Three of these, Picrodus calgariensis, P. canpacius, and P. lepidus, are described herein as new. Others, represented by more fragmentary specimens from Canada and the United States, are included in this paper, but are not named. P. calgariensis, from Who Nose? (late Torrejonian), Calgary, is the most primitive known species of Picrodus, having molars with little crenulation of the enamel. P. canpacius, from Cochrane 2 (earliest Tiffanian), northwest of Calgary, most resembles P. silberlingi sensu stricto, but differs in P4 structure, denser enamel crenulation, and weaker molar cusps. P. lepidus, from DW-2 (middle Tiffanian), near Red Deer, is the most advanced, having, for example, a two-rooted P4, tiny p3, and single-rooted p4. At least two of these species also occur in the United States, documented by fossils referred to P. silberlingi by previous workers. Dental evolution within Picrodus seems marked by several trends, including increase in size of i1, simplification of P4, reduction of molar cusps and crests, enlargement of the horizontal occlusal surfaces of the molars, and greater crenulation of enamel. From present knowledge, Zanycteris paleocenus Matthew, 1917 is dentally more primitive than Picrodus, Draconodus Tomida, 1982 is a valid genus, and picrodontids probably originated from “purgatoriid-grade” plesiadapiforms in earliest Paleocene time.

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Type
Research Article
Information
Journal of Paleontology , Volume 79 , Issue 4 , July 2005 , pp. 635 - 657
Copyright
Copyright © The Paleontological Society 

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