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Boyer diss 2009 1046..

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CHAPTER 6:<br />

SUMMARY AND CONCLUSIONS<br />

This section serves to summarize and emphasize major contributions and<br />

conclusions of the foregoing chapters.<br />

New crania of plesiadapids and reassessment of cranial stucture<br />

Chapter 2 provides the first description of crania referred to a member of the<br />

genus Pronothodectes (Fox, 1990). Furthermore, it provides the most extensive and<br />

detailed documentation and description of plesiadapid cranial morphology heretofore<br />

available. Finally, it examines a larger sample of better preserved cranial material, with<br />

more advanced visualization techniques than any other study on plesiadapid crania. The<br />

fossil and analytical resources of this work allowed me to describe distinctive features of<br />

taxa traditionally thought to represent basal plesiadapids (such as Pronothodectes and<br />

Nannodectes) and more derived plesiadapids (such as Plesiadapis tricuspidens), as well<br />

as similarities shared by them. These new observations revealed the morphology of basal<br />

plesiadapids to be different from previous perceptions in some ways (e.g., Russell, 1964;<br />

Bloch et al., 2007). Major findings include the following: (1) the bony composition of<br />

the plesiadapid tympanic bulla is uncertain, but best interpreted as petrosal in origin given<br />

available evidence (including that presented here); (2) all known plesiadapids other than<br />

P. tricuspidens appear to have nasals that exhibit a slight lateral flaring at their caudal<br />

extent (as compared to the mediolateral width of either the rostrocaudal midpoint or the<br />

547

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