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A well-preserved fossil talus [National Museum of Myanmar Primates (NMMP) 82] of a large-bodied primate is described from the late middle Eocene Pondaung Formation of central Myanmar. The specimen was collected at Thandaung Kyitchaung, a well-known amphipithecid primate-bearing locality near the village of Mogaung. NMMP 82 adds to a meager but growing sample of postcranial remains documenting the large-bodied primates of the Pondaung Formation. This new talus exhibits a suite of features that resemble conditions found in living and fossil haplorhine primates, notably anthropoids. As such, the phylogenetic signal deriving from the morphology of NMMP 82 conflicts with that provided by NMMP 20, a partial skeleton (including a fragmentary calcaneus) of a second large-bodied Pondaung primate showing undoubted adapiform affinities. Analysis subtalar joint compatibility in a hypothetical NMMP 82/NMMP 20 combination (talus/calcaneus) reveals a substantial degree of functional mismatch between these two tarsal bones. The functional incongruence in subtalar joint morphology between NMMP 20 and NMMP 82 is consistent with the seemingly divergent phylogenetic affinities of these specimens, indicating that two higher level taxa of relatively large-bodied primates are documented in the Pondaung Formation. On the basis of its size and morphology, we refer the NMMP 82 talus to the large-bodied amphipithecid Pondaungia. The occurrence of anthropoid-like tali in the Pondaung Formation obviates the need to invoke homoplasy to explain the shared, derived dental characters that are common to amphipithecids and undoubted anthropoids. Functionally, the NMMP 82 talus appears to have pertained to a primate that is engaged in active quadrupedalism in an arboreal environment along broad and subhorizontal branches. The primate taxon represented by NMMP 82 was capable of climbing and leaping, although it was not particularly specialized for either of these activities. [ABSTRACT FROM AUTHOR]

The phylogenetic affinities of the primates of the late middle Eocene Pondaung Formation of Myanmar have long been disputed. The discovery of the NMMP 39 talus (Marivaux et al.: Proc Natl Acad Sci USA 100 (2003) 13173-13178) provided the first clear evidence from the postcranium that a relatively large-bodied haplorhine primate is represented in the Pondaung fauna. Another talus (NMMP 82; Marivaux et al., 2010). Talar morphology, phylogenetic affinities and locomotor adaptation of a large-bodied amphipithecid primate from the late middle Eocene of Myanmar, Am J Phys Anthropol DOI: 10.1002/ajpa.21307) has been recently recovered which also pertains to Haplorhini. The metric and nonmetric features supporting the hypothesis of anthropoid affinities for NMMP 39 have been criticized by Gunnell and Ciochon (Gunnell GF, Ciochon RL. 2008. Revisiting primate postcrania from the Pondaung Formation of Myanmar. In: Fleagle JG, Gilbert CC, editors. Elwyn Simons: a search for origins. New York: Springer. p 211-228). Their analysis, however, was based on a very limited choice of variables, taxa, and individuals. Based on an extended sample, we are able to produce both principal components and discriminant functions that yield a rather clear separation of extant haplorhine and strepsirhine tali. Both principal components and discriminant function scores of the Pondaung tali fall with those of haplorhine primates. In addition, the Pondaung tali lack all the derived nonmetric features characteristic of strepsirhine primates, but exhibit all the features characteristic of haplorhine primates. We dispute the features Gunnell and Ciochon (2008) claim are uniquely shared by the Pondaung tali and adapiforms. Their rejection of the phylogenetic significance of the features shared by these tali and haplorhines is unwarranted by the evidence. Based on both metric and nonmetric features, the Pondaung tali are structurally most similar to the tali of haplorhines, particularly anthropoids., (© 2010 Wiley-Liss, Inc.)