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y exaggerated incrementals. Aperture subquadrate.<br />
Outer lip straight, thin, sharp, simple within, crenulated<br />
in harmony with the external ribbing, abruptly<br />
constricted at the mouth of the anterior canal. Inner<br />
lip strongly concave, nonplicate. Canal open, very<br />
short, sharply recurved, truncate anteriorly.<br />
Dimensions of incomplete holotype: Height, 12.4<br />
mm.; diameter 3.2 mm.<br />
Holotype: U.S.N.M. 325445.<br />
Type locality: Bolten Phosphate Company's pits,<br />
Stono River, Charleston County, S. C. Pleistocene.<br />
0 erithiopsis (Laskey a) emersonii persubulata differs<br />
from L. emersonii s.s. in the more slender, attenuated<br />
outline. Among the Recent forms commonly referred<br />
to the species s.l., the New England representatives<br />
seem consistently less slender than those in the South<br />
Atlantic waters. The fossil representatives, even those<br />
from the Yorktown formation, are all referable to the<br />
more slender race.<br />
Distribution: Virginia: Yorktown formation, Yorktown, York<br />
County; half a mile below Suffolk waterworks dam, Nansemond<br />
County.<br />
North Carolina: Duplin marl, Natural Well, and Magnolia,<br />
Duplin County. Waccamaw formation, Cronly, half a mile east<br />
of the factories, Columbus County.<br />
Outside distribution: Pliocene: Caloosahatchee marl, Caloosahatchee<br />
River, Fla. Pleistocene, Simmons Bluff and Bolten<br />
Phosphate Company's pits, Stono River, S. C. Recent, The<br />
Carolinas to the Antilles in shallow water?<br />
Family TRIPHORIDAE<br />
Genus TRIPHORA Blainville<br />
1828. Triphora Blainville, Dictionnaire sci. nat., vol. 55; p. 344.<br />
Type by monotypy: Triphora gemma tum Blainville=Cerithium<br />
tristoma Blainville. Recent, off Mauritius.<br />
The sinistral coiling characterizes the genus and the<br />
family.<br />
Triphora dupliniana (Olsson)<br />
Plate 27, figure 3<br />
1916. Triphoris dupliniana Olsson, Bull. Am. Paleontology, vol.<br />
5, No. 27, p. 18 pl. 3, fig. 8.<br />
Shell sinistral, elongate-conic, with nearly straight sides;<br />
nuclear whorls 1 +, the last turn with transverse ribbing and<br />
2 peripheral carinae; post-nuclear whorls 11, suture indistinct;<br />
the 1st 5 whorls, with 2 subequal spirals, on the 6th whorl, an<br />
intermediate spiral makes its appearance and increases gradually<br />
in strength; on the body-whorl, the uppermost spiral is the<br />
strongest; spirals tuberculated by 22 riblets which moreover<br />
extend somewhat diminished across the interspiral spaces; base<br />
sloping with 3 smooth spirals; columella smooth; anterior canal<br />
moderately long, closed or nearly so and bent both to the right<br />
and backwards ; mouth small, rounded ; outer lip oblique, with<br />
a deep anal notch bordering the suture.<br />
Length 5.75 breadth 1.75 mm.<br />
This species belongs to the group of Triphoris, such as T.<br />
melanum, which have only 2 spirals on the earlier post-nuclear<br />
whorls, later 3, with the last spiral coming in between the other<br />
2. The open, anal sinus and bent, tubular anterior canal are<br />
the main diagnostic characters of this species.<br />
Duplin formation; Natural Well, N. C.<br />
PART 2. SCAPHOPODA AND GASTROPODA 205<br />
Yorktown formation; James river, north of Smithfield, Va.<br />
Olsson.<br />
Dimensions of topotype : Height, 5.8 mm. ; maximum<br />
diameter, 1.7 mm.<br />
Topotype: U.S.N.M. 114256.<br />
Triphora apania Woodring (Carnegie Inst. Washington<br />
Pub. 385, p. 329, pl. 25, fig. 2, 1928) from Jamaica,<br />
and Triforis calypsonis Maury (Bull. Am. Paleontology,<br />
vol. 5, no. 29, p. 122, pl. 21, fig. 13, 1917) from<br />
the Dominican Republic, are closely related forms.<br />
In Triphoris bartschi Olsson (pl. 27, fig. 5), the<br />
posterior of the 3 spirals is the least elevated and the<br />
last to appear. The type, like that of T. dupliniana,<br />
comes from the Duplin marl at the Natural Well, and<br />
like T. dupliniana, the species occurs also in the Yorktown<br />
formation on the James River above Smithfield.<br />
Distribution: Virginia: Yorktown formation, "James River<br />
north of Smithfield" (Olsson). ·<br />
North Carolina: Duplin marl. Natural Well and llh miles<br />
northwest of Magnolia, Duplin County.<br />
Superfamily PTENOGLOSSA<br />
Family EPITONIIDAE<br />
Genus EPITONIUM "Bolton" Roeding<br />
1798. Epitonium "Bolten" Roeding, Museum Boltenianum, pt.<br />
2, p. 9'1.<br />
Type by subsequent designation (Suter, Manual New Zealand<br />
Mollusca, p. 319, 1913) : Turbo scalaris Linnaeus=Scalaria pretiosa<br />
Lamarck. Recent, in the western Pacific.<br />
The genus has been gradually increasing in prominence<br />
since the Triassic and is represented in the Recent<br />
seas by some 150 to 200 species of "wentle traps" distributed<br />
from the polar regions to the tropics and from<br />
between tides to abysmal depths.<br />
Subgenus HYALOSCALA De Boury<br />
1890. Hyaloscala De Boury, Soc. malacol. italiana Boll., vol.<br />
14, p. 90 of separate.<br />
Type by original designation : Seal-aria clathratula Adams.<br />
Recent, in the western Atlantic from Marthas Vineyard to<br />
Key West.<br />
Hyaloscala includes small, thin shells, usually of<br />
slender outline, made up of convex whorls separated<br />
by moderately impressed sutures, sculptured by laminar<br />
axials not fused at the sutures into a continuous series.<br />
The aperture is oval, broadening anteriorly, and the<br />
reflected inner lip completely closes the umbilical<br />
chink.<br />
A number of species from the European Tertiary<br />
have been referred to this subgenus, and the Recent<br />
forms, though not very numerous, have a wide distribution<br />
both in longitude and latitude.<br />
Epitonium (Hyaloscala) carolinae Gardner, n. sp.<br />
Plate 28, :figure 50<br />
Shell small, delicate, slender. Imperforate. Whorls<br />
probably 8, contiguous, convex, tapering to an acute