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Regardless, Major [3] did denote the central cusp in lagomorphs as '6,' and similarly denotes a cusp that would now be considered the protocone as '6' in both the Plesiadapis and Pelycodus figures.
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The p4 resembles a canine, having a single cusp that is about as high as the highest cusp on m1 and lacking accessory shelves or cusps.
In a bicuspid valve, the two conjoined cusps form a larger cusp that operates with the remaining, normal cusp to perform the valve function [2].
The metacone is a robust cusp that is separated from the paracone by a shallow and narrow notch.
In some individuals, there is an accessory cusp that is positioned mesiolabial to the hypolophid.
Much of the discussion has revolved around a prominent central cusp that appears in the upper cheek teeth of fossil taxa, and for an ontogenetically brief period, in extant lagomorphs.
This is in contrast to the P3 of Dawsonolagus, which shows a single buccal cusp that is positioned on the distal margin of the tooth, generally similar to the 'J' shaped tooth of ochotonids and many stem lagomorphs.
A survey of the AMNH collections has revealed several specimens that show a minor second buccal cusp that is mesial to the primary cusp (Fig. 5).
The mesostylid is situated midway between the metaconid and the entoconid and is a relatively well-developed cusp that is more isolated than that of G. aslius.
The protocone is a large and crestiform cusp that is mesiolabially oriented, forming most of the mesiolingual border of the tooth.
The flow affects the stability of the underlying helmet, which can be subject to a leakage out of the cusp that is similar to the small mass releases observed with the SOHO/LASCO coronagraph.
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