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ECHINODERMATA - KU ScholarWorks - University of Kansas

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52 THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS<br />

syntypes). Rundle Limestone, Stoney Squaw Mountain<br />

(P. perelongatus type), and Cascade Mountain (P. grandis<br />

type), Alberta, Canada.<br />

Types.—Syntypes, 111,762, three specimens, U. S. National<br />

Museum, Washington. Plesiotypes, 8,914 (holotype<br />

<strong>of</strong> Pentremites grandis WARREN), one specimen; 8,915<br />

(holotype <strong>of</strong> Pentremites perelongatus WARREN), one<br />

specimen, Geological Survey <strong>of</strong> Canada, Ottawa.<br />

Genus CARPENTEROBLASTUS Rowley, 1901<br />

Type-species, by original designation.—Granatocrinus (Schizoblassus)<br />

magnibasis ROWLEY, 1895.<br />

Generic diagnosis (emend. FAY, herein).—Spiraculate<br />

blastoids with eight spiracles in addition to an<br />

anispiracle, located between epideltoid and hypodeltoid<br />

plates, lancet exposed along food groove proper,<br />

with ?two hydrospire folds on each side <strong>of</strong> an ambulacrum,<br />

one pore between adjacent side plates along<br />

deltoid and radial margins, base convex, radials overlapping<br />

deltoids, and calyx form conico-elliptical.<br />

Mississippian, Missouri, ?Kentucky.<br />

Remarks.—The genus Carpenteroblastus may have<br />

been derived from a form similar to Lophoblastus in<br />

which the three hydrospire folds atrophied to produce<br />

two folds on each side <strong>of</strong> an ambulacrum.<br />

CARPENTEROBLASTUS MAGNIBASIS (Rowley)<br />

Plate 37, figures 11-12; plate 45, figures 10-12; text-figs. 74-76<br />

Granatocrinus (Schizoblastus) magnibasis ROWLEY, 1895, p. 220,<br />

figs. 11-14.<br />

Description.—Calyx calcitic, flattened ellipsoidal, with<br />

convex base in side view, strongly pentagonal in top view,<br />

11 mm. long by 11.5 mm. wide, vault 9 mm. long, pelvis<br />

2 mm. long, pelvic angle 130 degrees, periphery at midheight,<br />

summit flat. The stem is not well preserved, but<br />

is round, crenellar, and about 1 mm. in diameter. Basal<br />

circlet 1.5 mm. long by 6 mm. wide, pentagonal in basal<br />

view, convex outward, with large round ridges on each<br />

side <strong>of</strong> basiradial sutures, and with three normally disposed<br />

basal plates. Radials five, each hexagonal in side<br />

view, 9 mm. long by 5 mm. wide, with narrow, moderately<br />

deep sinus 7 mm. long by 1.5 mm. wide, with<br />

outward-projecting sides and rounded raised rims, giving<br />

a marked stellate appearance to the calyx in top view;<br />

radials overlapping deltoids.<br />

Deltoids four, large, broadly lancet-shaped, each 3.5<br />

mm. long by 4.5 mm. wide, the adorai tips <strong>of</strong> each pierced<br />

by two separate spiracles, thus forming eight spiracles<br />

around the oral opening. On the anal side the anispiracle<br />

is located between a pentagonal epideltoid and pentagonal<br />

hypodeltoid; thus, a total <strong>of</strong> nine spiracles occur around<br />

the oral opening.<br />

Ambulacra five, long, linear, recurved below, each 13<br />

mm. long by 1.5 mm. wide, with lancet exposed along<br />

food groove, the exposure being progressively wider toward<br />

the adorai end. There are 30 side plates in a space<br />

<strong>of</strong> 10 mm. along an ambulacrum, normally disposed,<br />

with one pore between plates, notched slightly in the<br />

sides <strong>of</strong> the deltoids and radials. There are four coverplate<br />

sockets to each side plate along the main food<br />

groove, and ?two hydrospire folds on each side <strong>of</strong> an<br />

ambulacrum. The surfaces <strong>of</strong> the calyx plates are ornamented<br />

by coarse growth ridges parallel to margins.<br />

Occurrence.—Lower Mississippian, upper part <strong>of</strong> Burlington<br />

Limestone, Louisiana, Missouri.<br />

Types.—Holotype, RX-194, one specimen, Rowley<br />

collection; metatypes, RX-22, three specimens, Rowley<br />

collection, Department <strong>of</strong> Geology, <strong>University</strong> <strong>of</strong> Illinois,<br />

Urbana.<br />

Genus CORDYLOBLASTUS Fay, n. gen.<br />

Type-species, by original designation (herein).—Pentremites acutangulus<br />

SCHULTZE, 1867 (adv. publ., 1866).<br />

Generic diagnosis.—Spiraculate blastoids with five<br />

spiracles, one <strong>of</strong> which is an anispiracle located between<br />

a superdeltoid and hypodeltoid, with two internal<br />

cryptodeltoids and large hypodeltoid, seen in<br />

side view, but the other four deltoids are overlapped<br />

by radials and not visible in side view, a single pore<br />

occurring between adjacent side plates along radial<br />

margins, lancet covered by side plates, four to nine<br />

hydrospire folds on each side <strong>of</strong> an ambulacrum; calyx<br />

club-shaped in side view. Devonian, Germany, Spain.<br />

FIGURE<br />

PAGE<br />

1-3. Orophocrinus cam panulatus (I-Luvomcu), syntype, S3,236,<br />

coll. (purchased by SPRINGER), U.S. Natl. Mus.; Lower<br />

Mississippian, Chouteau Limestone, Sedalia, Mo.; oral, "D"<br />

ambulacral, aboral views <strong>of</strong> HAMBACH'S original figured<br />

specimen (all X3.1) 36<br />

4-9. Orophocrinus stelliformis (OwEN & SHUMARD), neotypes,<br />

S4,961 (new holotype figs. 4,7,9, new paratype fig. 8),<br />

Springer coll., old number S3,234, U.S. Natl. Mus.; Lower<br />

EXPLANATION OF PLATE 13<br />

Mississippian, Lower Burlington Limestone, Burlington,<br />

Iowa; 44, oral, "D" ambulacral, aboral views (all X2.5)<br />

(also figured by ETHERIDGE & CARPENTER, 1886, pl. 15,<br />

fig. 11); 7, oral view <strong>of</strong> oral plates <strong>of</strong> holotype, A indicating<br />

anal side ( X30); 8, anal view <strong>of</strong> new paratype<br />

showing anal covering plates in place between epideltoid<br />

and hypodeltoid plates ( X25); 9, detail view <strong>of</strong> "B" ambulacrum,<br />

mouth toward top, one outer side plate outlined<br />

in white ( X44) 36

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