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LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

LOWER CRETACEOUS DEPOSITS CALIFORNIA AND OREGON

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99 LOWEB CBETACEODB <strong>DEPOSITS</strong> IN <strong>CALIFORNIA</strong>. <strong>AND</strong> <strong>OREGON</strong><br />

It may be that ia some cases errors have resulted, aud in fact they could<br />

scarcely be avoided, but if this work were delayed until these and other<br />

difficulties were removed, it would not soon be done. However, the remoteness<br />

of this province from that of Europe and other regions from<br />

which Lower Cretaceous faunas have been described affords some measure<br />

of relief from the exactions imposed upon students working under the<br />

shadow of older institutions. Whatever shortcomings may result from<br />

these and other circumstances, it is believed that there are many students<br />

of Meso&oic paleontology in this and other countries who will welcome<br />

the new and significant matter contained in this contribution, even though<br />

in the view of some it may seem defective. For such students this work<br />

has been done.<br />

ECHINODERMATA<br />

Echinoderm remains are not abundant in the Pacific Coast Cretaceous,<br />

aJthough in both California and Oregon they have been found sparingly<br />

in the lowest stratigraphic group of the Shasta series, and also in the lower<br />

part of the Chico series and in its later beds. Stanton (1895, p, 31} has<br />

mentioned the discovery of spines and fragments of the test of Cidarts,<br />

and joints of the column of Pentacritvus, on the Shelton ranch, north of<br />

Paskenta, Tehama County, and the latter genus also at Stephenson's<br />

on the Cold fork of Cottonwood Creek, Tehama County.<br />

Clark later described these forms as far as their fragmentary condition<br />

permitted; accounts of them are here given. At both localities these<br />

fossils occur in the Paskenta group of the Shasta series, not far from its<br />

local base, and incidentally indicate near-shore conditions of the strata<br />

from which they came. Evidences connected with their occurrence and<br />

their associates confirm this view. Stanton (1835, p. 22) also mentions<br />

the finding of remains of PerUacrinus in beds of nearly the same age new-<br />

Riddle, Oregon.<br />

CIDA&IDAE Gray<br />

Cidaris Leake<br />

Cidarit tchamaensw Clark<br />

Ctttori* tehamaemrie CXtA&K, XT. B, Geo!. 8nrv„ Mon. 51, 1916, p. 44, pi, 9, fie. 1;<br />

Shelton'a ranch, 5 mi lea north of Fasten ta, Tehama County .—KEW, Univ.<br />

Calif, Publ, Geo)., vol. 12, 1920, p. 54, pi. 3, 1; locality as above.<br />

This species is described from a single apine, BS follows: "Test unknown. Spines<br />

large and. dub-ahaped, witk rows ot granule* intending from neck to point of spine."<br />

Length 30 nun.; width in thickest port, 12 mm.

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