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Boyer diss 2009 1046..

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MATERIALS AND METHODS<br />

Material examined<br />

All known specimens referable to the Plesiadapidae and representing a major<br />

portion of the cranium were examined in this study except for one specimen of P.<br />

tricuspidens that could not be located, MNHN CR 7377.<br />

Previously unpublished or largely undescribed material studied includes three<br />

specimens referable to Pronothodectes gaoi: UALVP 46685, a crushed skull from DW-2,<br />

a “middle” late Paleocene (Ti3) locality in the Paskapoo Formation in central Alberta<br />

(Fox, 1990b); and UALVP 46687 and 49105, isolated basicranial fragments from the<br />

DW-2 and Joffre Bridge localities, respectively. Joffre Bridge is near DW-2 from the<br />

same strata and represents the same faunal zone.<br />

Previously described specimens for which aspects of morphology are redescribed<br />

due to original errors or lack of detail in verbal or illustrative documentation include<br />

those referred to Plesiadapis tricuspidens, Nannodectes intermedius and N. gidleyi.<br />

Specimens of P. tricuspidens from the Berru locality of the Paris Basin assessed here<br />

include MNHN CR 125, 126, and 965, as well as the Pellouin skull. Additional<br />

specimens include isolated petrosals that represent P. tricuspidens (M. Godinot,<br />

pers.com.): MNHN BR 17414-19, 1371. The skull of Nannodectes intermedius, USNM<br />

309902, from the Ti1-aged Bangtail locality in south-central Montana (Gingerich et al.,<br />

1983), is figured and discussed. Finally, I include images, description and analysis of N.<br />

gidleyi (AMNH 17388), the specimen originally described by Simpson (1935) and later<br />

considered by MacPhee et al. (1983).<br />

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