Boyer diss 2009 1046..

Boyer diss 2009 1046.. Boyer diss 2009 1046..

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specimen from the Bison Basin Saddle locality (AMNH 92011: p. 9, fig. 6), which they identified on the basis of its similarity to craniodentally associated elements from the Berru locality, one of which was also figured (p. 10, fig. 7). The authors did not provide a number for the Berru specimen, but Beard (1989) later recognized it as pertaining to MNHN R 416. Szalay and Dagosto considered the distinctive features of the entocuneiform to be its large plantar-projecting process and a facet for MT I that is mediolaterally broad, relatively flat, and saddle-shaped. They viewed the bone as morphologically similar to that of the extant primitive treeshrew Ptilocercus lowii. Because Ptilocercus is capable of grasping with a divergent hallux that exhibits mobility at the metatarsal-entocuneiform joint, Szalay and Dagosto suggested that the same activities could be inferred for plesiadapids. However, no first metatarsals had yet been described for any plesiadapids. Gunnell (1989: p. 41-48) discussed the astragalus, calcaneum, and cuboid of Plesiadapis. His figures 16 and 17 (p. 45) compare the astragalus and calcaneum to that of Marmota. Gunnell acknowledged that the astragalus and calcaneum indicate a high degree of mobility, as argued by Szalay and Decker (1974). However, he brought up the terrestriality hypothesis of (Gingerich, 1976) and noted that mobility of the ankle does not necessarily argue for an arboreal habitus, as indicated by the mobile foot of terrestrial Marmota and as convincingly argued by Jenkins (1974). However, he stated that an ongoing study by him and Gingerich indicated an arboreal habitus for the skeleton of P. cookei. Beard (1989) brought studies of plesiadapiform postcranial anatomy several steps forward with an excellent dissertation, wherein he described and illustrated previously 266

unstudied material. Specifically, he described and figured a skeleton of Nannodectes intermedius (USNM 442229: p. 20-89, figs. 1-16) including the following bones: left scapula, right humerus, right ulna, left radius, right scaphoid, right lunate, left pisifom, right capitate, both hamates, left MC I, right MC II, right MC III, four proximal manual phalanges, four intermediate manual phalanges, several distal manual phalanges, left tibia, left cuboid, left hallucal metatarsal, four non-hallucal metatarsal fragments and two pedal intermediate and two pedal distal phalanges. All of this material plus additional elements associated with this specimen (but not described by Beard) were observed, measured, and in some cases HRxCT-scanned in the course of this study. Furthermore, Beard described isolated elements from Cedar Point Quarry attributed to P. rex (p. 89- 101, figs. 17, 18) including YPM-PU 23976, a proximal humeral fragment (not figured); YPM-PU 23975, a distal tibial fragment; YPM-PU 23977 and UM 94816, right and left astragali, respectively. Of these bones, I was only able to directly study UM 94816. Beard (1989) additionally described a number of previously unstudied bones of P. tricuspidens, relying on Russell’s (1964) documentation of their association to a partial skeleton mentioned above (p. 101-132, figs. 19-21). The bones newly described by Beard included the following: MNHN R 415, a right cuboid; MNHN R 416, a left entocuneiform; MNHN R 5295, a right MT III; MNHN R 5296, a pedal intemediate phalanx; MNHN R 5297, a manual proximal phalanx; MNHN R 5298, a left MT IV; MNHN R 5300, a right MT III; MNHN 5301 and 5303, manual proximal phalanges; MNHN R 5305, a left MC II; MNHN R 5306, a distal epiphysis of a right MT I; MNHN R 5309, a pedal distal phalanx; MNHN R 5310, a fragment of a pedal distal phalanx; MNHN R 5312, a manual intermediate phalanx; MNHN R 5313, a pedal distal phalanx; 267

specimen from the Bison Basin Saddle locality (AMNH 92011: p. 9, fig. 6), which they<br />

identified on the basis of its similarity to craniodentally associated elements from the<br />

Berru locality, one of which was also figured (p. 10, fig. 7). The authors did not provide<br />

a number for the Berru specimen, but Beard (1989) later recognized it as pertaining to<br />

MNHN R 416. Szalay and Dagosto considered the distinctive features of the<br />

entocuneiform to be its large plantar-projecting process and a facet for MT I that is<br />

mediolaterally broad, relatively flat, and saddle-shaped. They viewed the bone as<br />

morphologically similar to that of the extant primitive treeshrew Ptilocercus lowii.<br />

Because Ptilocercus is capable of grasping with a divergent hallux that exhibits mobility<br />

at the metatarsal-entocuneiform joint, Szalay and Dagosto suggested that the same<br />

activities could be inferred for plesiadapids. However, no first metatarsals had yet been<br />

described for any plesiadapids.<br />

Gunnell (1989: p. 41-48) discussed the astragalus, calcaneum, and cuboid of<br />

Plesiadapis. His figures 16 and 17 (p. 45) compare the astragalus and calcaneum to that<br />

of Marmota. Gunnell acknowledged that the astragalus and calcaneum indicate a high<br />

degree of mobility, as argued by Szalay and Decker (1974). However, he brought up the<br />

terrestriality hypothesis of (Gingerich, 1976) and noted that mobility of the ankle does<br />

not necessarily argue for an arboreal habitus, as indicated by the mobile foot of terrestrial<br />

Marmota and as convincingly argued by Jenkins (1974). However, he stated that an ongoing<br />

study by him and Gingerich indicated an arboreal habitus for the skeleton of P.<br />

cookei.<br />

Beard (1989) brought studies of plesiadapiform postcranial anatomy several steps<br />

forward with an excellent <strong>diss</strong>ertation, wherein he described and illustrated previously<br />

266

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