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LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

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description of species 153<br />

this ratio increases; the sides slope from below the median line to the periphery, the<br />

section of the whorl becoming subovate; the costal ridges form at ahout 40 mm.<br />

diameter, and are at first rounded, separated by interspaces of about the same width;<br />

at a diameter of 100 mm. these ridges become relatively narrow and cross the ventral<br />

zone; the suture line is known only from Gabb's figure (ISflB, pi. 22, fig. 14b), The<br />

holotype has the following dimensions: greatest diameter, 108 mm.; width of umbilicus,<br />

40.6 mm.; height of whorl, 45 mm.; width of whorl, 36 mm.; umbilical ratio,<br />

0,37&:1.<br />

Lytoeeroa (&MsmaJe/Ja) gaineai Anderson, n, sp,<br />

(Pitta 3D, fi|v« 3, 4, 5)<br />

Lytoceras rel. dttvaJtanum (d'Orbigny) <strong>AND</strong>ERSON {in part), Calif. Acad. Sci., Pr.,<br />

3d ser., vol. 2, 1902, p. 81, pi 6 figs, 140-143; upper part of Horsetown group,<br />

Hulen Creek and Horsetown, Shasta County.<br />

Shell small, discoidal, moderately inflated, "gradurabilieate," section of whorl<br />

quadrate, higher than broad; surface marked by regularly spaced periodic constrictions,<br />

about 18 to the whorl, inclined forward; between these the surface is marked<br />

by numerous fine growth lines; both constrictions and growth lines becoming weaker,<br />

or quite disappearing upon the abdominal surface; sides and ventral zone somewhat<br />

flattened in older stages. In this species the umbilical ratio is smaller than in<br />

LyCocerae duvalianttm (d'Orbigny), which belongs to a distinct subgenus.<br />

Tbe holotype of this species (Calif. Acad. Sci. type Coll.) has the following dimensions:<br />

greatest diameter, 58 nun.; width of umbilicus, 16.5 mm.; height of whorl,<br />

24 mm.; width of whorl, 22 mm.; umbilical ratio, 0.384:1.<br />

Twelve or more good examples were obtained at Locality 1656 (Calif. Acad. Sci.),<br />

in the Neptune zone, associated with Ptttosia koffmatmi (Gabb) and other middle<br />

Albian forms. It has also been collected at the old mining camp of Horsetown,<br />

Shasta County, and nt Texas Springs, 3 miles to the east.<br />

STEPILANQCEJUTUMB Neumayr<br />

In the broader family Stepbaaoceratidae Neumayr, of the Mesosoie, later authors<br />

have rccogni-xcd various subfamilies, among which Morphoceratinac Hyatt has found<br />

acceptance among many. In such relationship Pavlow and Lamplugh (1661, p. 470)<br />

groupedQlcottephanueNeumayr, Polyptychita, Simbirekiles, Astieria and Virgatilee.<br />

Since then Spath (1624, p. 87) has proposed as family groups Simbirskitidoc and<br />

Polyptychitidae, the latter of which Seems to cover satisfactorily many western<br />

forms, including Polyptychitea, Simbirakitts Pavlow, and £ui)

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