LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON
LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON
LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON
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description of species 231<br />
Belemnopsit (Hibolittt) dimntrmdei Anderson, n- sp.<br />
(Plau SB, 6|um 3, 3», lb)<br />
Only fragmentary examples of this specks have yet been found. Two such fragments<br />
found near together seem to have been parts of a single individual and have<br />
been figured as auch. Both show the characteristic diventroid section and rounded<br />
dorsal side of the guard. Nevertheless, the larger of these fragments is taken as<br />
the holotype, to which the other may be regarded as supplementary. In the holotype<br />
(Calif. Acad. Sci. type Coll.), the dorsal side iB semicircular in section, whereas the<br />
ventral aide is traversed by two parallel grooves, between which there is a low,<br />
rounded ventral ridge, of which the curvature has a shorter radius. The guard is<br />
slightly fusiform, tapering from near the middle toward both ends, but more rapidly<br />
toward the apex. The holotype has the following dimensions: length (incomplete),<br />
64 mm.; maximum diameter, 9.S mm. It was found in the lower part of the Horsetown<br />
group on Fiddler Creek, half a mile north of the big bend of the crcek at which<br />
the Mitchell zone is exposed, and not less than 600 feet beneath it. The nearest<br />
know a analogue appears to he "Betemnitea" bicanalteuiala de Blainvi lie, as figured by<br />
d'Orbigny (1842, pi. 3, figs. 13-16), which Stolley places in the genus Hiboliles de<br />
Montfort. According to d'Orbigny (1850, p. 62), this spcciea ia of Neocomian or<br />
lower Xeocornian ago.<br />
jVeohibolitet Stolley 1911<br />
Ncchiboliles fontinalif Anderson, n. sp.<br />
(Piste SI, 6gun» J, 8)<br />
Bdemnitet&p. <strong>AND</strong>ERSON, Calif. Acad. Set., Pr, 3d ser., vol. 2, 1902, p. 146, pi. 8, figs.<br />
109, 170; Texas Springs, Shasta County.<br />
The guard of this species is long and slender, slightly fusiform in ita lower twothirds,<br />
expanded in its alveolar portion; section of guard nearly circular, axia central;<br />
phragmacone only slightly inserted, with an apical angle of about 26 degrees;<br />
ventral groove rather faint, not showing on the bolotypa; apex acuminate. The<br />
holotype (Calif. Acad. Sci. typo Coll.) measures: length, 68 mm.; greatest diameter,<br />
7 mm.; diameter below alveolus, 6 mm. Thia example, with varioua others leas complete,<br />
was found at Texas Springs, 3 miles east of Horsetown, associated with Sonneralia<br />
stantoni, Beudantreeras haydeni, and TetebraUlla dtnsleonia Anderson. The<br />
species has some resemblance to Ifeohibolites vliimve (d'Orbigny) from the Cenomanian<br />
of England, but its relation is perhaps only generic. It is longer, more slcndar,<br />
and has a more acuminate point. Ita horizon, as shown by its assoc iates, ia near that<br />
at Horsetown which is believed to be near the upper limit of the group. It has been<br />
thought by earlier writers to represent the lowest beds of the Cbico series; in cither<br />
case the horizon is in the upper part of the Albian.<br />
BELKWNQTEUTIIIDAE Zittel<br />
Belcmnnteuthis Pierce (Conoleulhis d'Orbigny)<br />
Behmnoteulhis (CWoteuiAw) pacifiea Anderson, n. sp.<br />
(Flats 77, figures 2,3}<br />
Phragmacone large, circular in section, apparently straight, tapering slowly;<br />
septa tlun, numerous, "nested"; holotype (Calif. Acad. Sci. type Coll.) is an incomplete<br />
example, showing only eight septa; diameter of largest septum, 76 mm.; diameter<br />
of smallest septum, 65 mm.; deeply and uniformly concave; average interval at<br />
center, 5 mm.; total length of holotype (est.), 300 mm.; phragmacone without guard