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LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

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description of species 133<br />

Maude Island (Queen Charlotte Islands), from beds that have been thought to<br />

belong in the Haida group, which apparently is much younger than those at Ono.<br />

Nerinea sp. undet.<br />

(PUL* 9, FI«UN» 3,1)<br />

Shell small, spire short, relatively thick, turreted as in the preceding species,<br />

although sloping more rapidly to tbe apex; basal part not known. This species<br />

occurs with the preceding at Locality 1353 (Calif. Acad. Sci.) in the Ono zone, near<br />

tho baae of the Horsetown group on the Cottonwood Creek, Shasta County. Because<br />

of the rarity of the genus in tbe Cretaceous of California, this form is here<br />

recorded with the preceding.<br />

"Nerinea" dispar Gabb<br />

jVerinfo dupar GABB, Paleont. Calif., vol. 1, 1864, p. 113, pi. 19, figs. 63, Gfla; North<br />

fork of Cottonwood Creek, Shasta County; vol. 2,1869, p. 231, "Shasta Group."<br />

Cottonwood Creek—STEWAM, Phila. Acad. Nat.ScL, Pr,, vol. 78,1926, p. 322,<br />

This species seems not to bave been recognized by later writers, and there is no<br />

record of its occurrence in the Shasta series other than that given by Gabb, The<br />

holotype is in the Museum of Paleontology, University of California. Stewart<br />

gives its dimensions as follows: length (incomplete), 55 mm.; width, 13.5 mm.<br />

According to Stewart (1926, p. 322) it is "related to 'Cltmtcala' dtmenlina<br />

(d'Orbigny) from the Cretaceous (Albian) of Europe."<br />

A similar form, although much smaller than Gabb's species, has been found in<br />

the lower Chico beds of Middle fork of Cottonwood Creek.<br />

CEIUTUIIDAE Menke<br />

CEN'FHTUM tlrigotum Stanton<br />

Ctrithium ttriaoaum STANTON, U. S, Geol. Surv., Bull. 133, 1895, p. 71, pi. 13, fig. 7;<br />

Shelton a ranch, 5 miles north of Paskenta, Tehama County.<br />

"Shell small, slender, consisting of nine or ten rounded whorls, surface ornamented<br />

by narrow, elevated, transverse eeatae and by revolving line*., There are<br />

eight coetae on each whorl, so arranged that they form continuous varices the full<br />

length of the shell. Pour of the revolving lines are visible on the spire.<br />

"Height, G mm.; greatest breadth, 2 mm."<br />

The list of species (Stanton, 1SG5, p. 18) containing this form contains also Apatite<br />

cratiicallis, "Olcotltphanua" mulabilis Stanton, "HoplUe*" angulatut, and other<br />

species characteristic of the Paskenta group.<br />

Potamide* diadema Gabb<br />

Potamuto diadema GABB, Paleont. Calif., vol. 1, 1864, p. 130, 227, pi. 20, fig. 85;<br />

North fork of Cottonwood Creek, Shasta County; vol. 2, 1869, p. 227; "Shasta<br />

Group," Cottonwood Creek—STANTON, U, S. Geol. Surv,, Bull. 133, 1895, p.<br />

13; lower Horsetown, North fork of Cottonwood Creek—STEWART, Phila.<br />

Acad. Nat. Sci., Pr., vol. 78,1926, p. 356; Locality and horizon as above.<br />

This specieB tB abundant in the lower beds of the Horsetown group of the Shasta<br />

series.<br />

It has been found abundantly in the beds exposed near tbe bridge at Ono (Locality<br />

1353, Calif. Acad. Sci.), where it ia associated with Neocrasprdilee aguila nov.,<br />

Acroleuikii kerrunsii nov., and Inaceramus colonicus nov.

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