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Functional morphology of the postcranium and locomotor behavior of Neosaimiri fieldsi, a Saimiri ‐like Middle Miocene platyrrhine
Author(s) -
Nakatsukasa M.,
Takai M.,
Setoguchi T.
Publication year - 1997
Publication title -
american journal of physical anthropology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.146
H-Index - 119
eISSN - 1096-8644
pISSN - 0002-9483
DOI - 10.1002/(sici)1096-8644(199704)102:4<515::aid-ajpa7>3.0.co;2-q
Subject(s) - postcrania , quadrupedalism , theria , eutheria , arboreal locomotion , anatomy , biology , extant taxon , forelimb , calcaneus , taxon , paleontology , evolutionary biology , ecology , structural basin , habitat , phanerozoic , cenozoic
A number of postcranial specimens of Neosaimiri fieldsi, a Middle Miocene platyrrhine, were discovered in 1988, 1989, and 1990 at La Venta, Colombia. Until recently only three postcranial specimens of this species had been discovered and the present material adds further information about this taxon's postcranial morphology. In overall skeletal dimensions and in postcranial features, Neosaimiri is most similar to Saimiri among extant medium‐sized platyrrhines, but differs from Saimiri in having more rugose surface markings, a longer olecranon, a smaller anterior process of the distal tibia, an absence of a distal surface extension on the anterior tibial shaft, an absence of an anterior midtrochlear depression of the talus, and a shorter distal calcaneus relative to the calcaneal tuberosity. These differences suggest that Neosaimiri was relatively heavily built, possessed a more dominant forelimb in quadrupedal progression, and utilized a less stabilized upper ankle joint, and a shorter power arm for plantarflexion. Neosaimiri is interpreted as an arboreal quadruped with frequent leaping across arboreal gaps, as in extant Saimiri, with perhaps less frequent running and leaping than in Saimiri. As with the dentition, the postcranial specimens suggest the close relationship between Neosaimiri and extant Saimiri. Am J Phys Anthropol 102:515–544, 1997. © 1997 Wiley‐Liss, Inc.