A. FE. Verrill—The Bermuda Islands; Geology. 1 
[ep) 
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Variety discrepans (Pfr.). 
This variety is separated only on account of its nearly flat spire. 
This is a variable character, as in P. Nelsoni, and intermediate forms 
are not uncommon. Mr. Gulick records it from the older hard lime- 
stones and red clay pockets at Knapton Hill and near Castle Harbor; 
also from ancient unconsolidated sands at Tucker’s Town (his sta. 
818). We took it from the sand inside a shell of P. Nelsoni, founc 
in a road-cut at Bailey Bay, and also in strata immediately above the 
Devonshire beach-limestones at Hungry Bay. It is found living, 
but is not common. 
Peecilozonites cupula Gulick. 
, Op. cit., p. 417, pl. xxxvi, fig. 2, 1904. 
Figure 49, TYPE. 
Easily distinguished by its dome-shaped spire. It has about 8 
whorls; diameter 16 to 20™™; height, 13 to 15™™. Some specimens 
show traces of subsutural and peripheral color bands. 
IS 
Figure 49.—P. cupula; 50, Pecilozonites Dulli ; 51, Zonitoides Bristoli. Types. 
All copied from Gulick. 
Several specimens were found by Mr. Gulick at a quarry of hard 
limestone near Paynter’s Vale, southwest shore of Castle Harbor (his 
locality 806), associated with other extinct species. 
Peecilozonites Dalli Gulick. 
Op. cit., p. 417, pl. xxxvi, fig. 1, 1904. 
FIGURE 50, TYPE. 
This small species is higher than broad, with an elevated spire, 
rounded apex, and convex base. Diameter, 7 to 7.3"; height 8.5 to 
10™™, Whorls about 9, polished, whitish, with two brownish per- 
ipheral lines. |Umbilicus small, partly covered by the reflexed 
columellar margin. Exact locality unknown. 
