102 PALEONTOLOGY OF NEW JERSEY. 
appear somewhat uncommon in the deposits of this period within the State, 
as only some two or three fragments of it have been found beyond this one 
specimen, and its name does not appear in many of the lists of Miocene 
shells of New Jersey. 
Locality: The specimen is from Heislerville, Cumberland County, N. J., 
and belongs to the collections sent from Rutgers College, New Brunswick, 
Nod. 
BUSYCON SCALARISPIRA. 
Plate xvii, figs. 11 and 12. 
Busycon scalarispira Conrad: Proc. Acad. Nat. Sci. Phila., 1862, p. 584; Catalogue, 
ibid., p. 561; Meek, Smith. Check List Miocene Foss., p. 22. 
Fulgur scalarispira Heilprin: Proc. Acad. Nat. Sci. Phila., 1887, p. 403. 
Fulgur scalariformis Heilprin: ibid., pp. 397 and 398; Tert. Foss. U.S., p. 8. 
‘“‘Subfusiform; spire moderate, turreted, sides above the angle oblique; 
angle subcarinated, with numerous approximate subcompressed tubercles; 
whorls striated transversely. * * * Allied to B. rugosum, but differs in 
wanting the channel round the base of the whorls.” (Conrad, Phil. Acad. 
Nat. Sci., 1862, p. 584.) 
I have seen only small and imperfect examples of this shell. It seems 
to have been somewhat rare over the region of these deposits. The largest 
fragment which I have seen is but little more than one inch in diameter, and 
retains three and a half volutions outside of the mamillated nucleus; but it 
shows the broken ridge of another full volution beyond these, which would 
have given it a width of probably fully two inches across the spire. The 
spire is decidedly scalariform, the elevation of the inner above the outer 
volutions rapidly increasing in the outer whorls, with the sides of the whorl 
nearly vertical above those outside of it, and the surface marked by very 
fine distinct spiral lines throughout, which are wavy on the outer surface 
below the compressed nodes that line the outer angle of the spire. These 
nodes are at first very small near the nuclear apex of the spire, and increase 
both in size and distance as the shell increases in size, becoming large and 
conspicuous on the outer volutions. 
This shell is near B. coronatum Con., but differs in that the volutions of 
the spire are flat on the top instead of rapidly sloping, and the nodes are 
