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LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

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DESCRIPTION OF 8PEC1EB 187<br />

Dt-tmocerat haffmanni STANTON, Geol. 9OC. Am., Bull., vol. 5, 1894—AHTEHSON,<br />

Calif. Acad. Sci., Pr., 3d aer., vol. 2, 1002, p. 94 (inpart), pi. 10, fig, 203; Cottonwood<br />

district, Shasta County (not pi. 5, figs. 120-123); upper beds of the<br />

Horsetown group, Horsetown, Shasta County.<br />

The holotype of this species seems to have been lost, andit is therefore permissible<br />

to choose a lectotype. Gabb's original figures of the species seem to be composite,<br />

and to be based upon more than one species, and therefore are defective. The<br />

lectotype (Calif. Acad. Sci. type Coll.) has the following dimensions: greatest<br />

diameter, 80 mm.; width of umbilicus, 31.5 mm.; height of whorl, 35 mm.; thickness<br />

of whorl, 30 nun.; umbilical ratio, 0.339:1. This specimen was obtained at the<br />

old mining camp of Horsetown and is the only form of Ptuosia found theTc that can<br />

properly represent Gabb's spcciea. In thia lectotype the section of the whorl is<br />

more inflated than in Gabb's figures; the constrictions are brood and are bordered<br />

behind by a rounded ridge; there are usually six or seven constrictions on a single<br />

whorl; they are Sexiradiate, curving at first forward near the umbilical border, then<br />

gently backward to above the middle of the side, then forward again, crossing ths<br />

ventral zone with a forward sinus; between the constrictions the surface is marked<br />

by 18 to 22 rounded costae, all of which eroBS the ventral zone. The walls of the<br />

umbilicus are abrupt below, rounded above, the curvature merging into that of tbe<br />

slightly inflated sides. The examples of this specics obtained by the writer from the<br />

type locality may be regarded as topotypes; moat of them have only six constrictions,<br />

and all have fewer than are shown in Gabb'a drawings, but the measurements given<br />

above do not differ materially from those obtained from his figures.<br />

This apecies appears to belong to the group of Putosict mayoriajut (d'Orbigny), as<br />

seen in its external form, ornamentation, and autural characters. Other examples of<br />

the apecies have been obtained from Locality 1650 (Calif. Acad. Sci.) in the Neptune<br />

zone on Hulen Creek, and on Bee Creek, and on the North, fork of tbe Cottonwood<br />

Creek.<br />

Puzasta rtetidei Anderson, n. sp.<br />

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