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LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

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218 lower cretaceotffi deposits in california and oRegon<br />

Hamilea imilalor Anderson, n. sp.<br />

(Plaus «, fipim 4, &}<br />

A single fragmentary example of a hamitid species was found in the Perrin zone<br />

at Locality 1688 (Calif, Acad. Sci.) in the upper part of the Horsetown group. It<br />

Bcems to be closely related to Hamitea ormolus Sowerby, although it ia from a lower<br />

stratigraphic horizon, here regarded as middle Albian. Aa far aa the species can be<br />

described from this example, it has the following characters:<br />

Shell large, tapering slowly, section of costate limb elliptical, rounded on both<br />

dorsal and ventral borders; surface marked by numerous oblique, rounded ribs,<br />

separated by wider interspaces, the interval being about 3 mm, broad; ventral zone<br />

bordered on both sides by single rows of broad, low, rounded tubercules, which<br />

appear upon each third rib, although their exact relation to the rib is not clearly<br />

acen; septum aa seen in the figure, the lobes and their principal branches being bipartite,<br />

in the manner of Xjftowai. The holotype (Calif. Acad. Sei. type Coll.)<br />

has the following dimensions: length, 67 mm.; dorse-ventral diameter, at larger end,<br />

43 mm.; transverse diameter, larger end, 31 mm,; same diameter at smaller end,<br />

30 mm.<br />

This spcciea has the general characters of Hamiita armatut Sowerby, as figured by<br />

Boule and Thevenin (IGCKM.907, p. 5ft) especially with respec t to the suture line. The<br />

holotype of the present apeciea was associated with AcantAopIiles ptrrini, Cleoniccras<br />

{eewitei, Phylloeerat ihtresat, and iHplyckoccras lam Gabb, all of which are found<br />

100 to 200 feet beneath the Xeptune zone in the upper part of the Horsetown group.<br />

Ptychaceraa d'Orbigny<br />

Ptychoctraa natriee Anderson, n. sp.<br />

(Plata Bl, figure<br />

Shell small or of moderate site having the two limbs folded closely together;<br />

section of the two limbs subepiadr&te; smaller limb subcircular in section, nearly<br />

smooth, tapering gradually; larger limb quadrate in section, slightly concave on its<br />

dorsal contact with the smaller limb; costate, with gently inclined, simple costae<br />

crossing the ventral tone as smooth rounded ridges; ventral zone rounded; septa not<br />

exposed on holotype. The species belongs to the group represented by Piychoceras<br />

puioirianum d'Orbigny, found in the Neocomian (Barremian) of Franco, which is its<br />

nearest known analogue. The holotype (Calif. Sci. type Coll.) was found in<br />

the Mitchell zone at Locality 1657 (Calif. Acad. Sci.) on the west branch of Mitchell<br />

Creek, a mile above the mouth of this stream. It has the following dimensions:<br />

total length, AS mm.; transverse measure (both limbs), 24 mm.; height of aperture,<br />

13 mm.; width of aperture, 13 mm.; top of crosier roundly curved. This example<br />

was found associated with SkaaticrioccTaz ponienie, Paeudocrioecras ap., and tnoceramus<br />

ovatoidea nov., in strata regarded as upper Barremian in age.<br />

Diptychoceras Gabb<br />

Diplychoccroe laepc Gabb<br />

Diplychoeeraa JAM'S GABB, Paleont. Calif., vol. 2, 1869, p. 144, pi. 25, figs. 21, 21a,<br />

21b; "Shasta Group," Cottonwood Creek, Shasta County.<br />

Gabb's account reads in part aB follows:<br />

"Shell moderate in site, limbs long and slender, section of the smaller limb subelliptical,<br />

slightly flattened on the ventral (dorsal) side; second limb subcircular,<br />

very slightly emarginate by the encroachment of the preceding branch; last limb<br />

suddenly incurved, and extending to (or beyond ?) the middle of the shell. Surface

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