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ECHINODERMATA - KU ScholarWorks - University of Kansas

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BLASTOID STUDIES 23<br />

lapping deltoids, with broad sinuses. Lower Carboniferous,<br />

England.<br />

CODASTER ACUTUS M'Coy, 1849<br />

Plate 12, figures 1-7, 9; text-figs. 8, 9<br />

Codaster acutris M'Coir, 1849, pp. 250-251.<br />

Description.—Calyx calcitic, cup-shaped in side view,<br />

pentagonal in oral view, 14 mm. long by 11 mm. wide,<br />

slightly compressed, with flat summit and rounded base.<br />

Stem round, crenellar, with small round lumen. Basal<br />

circlet cup-shaped in side view, rounded pentagonal in<br />

basal view, large, 6.5 mm. long by 9 mm. wide, with a<br />

prominent bluntly rounded median ridge on each basal<br />

plate. Radials five, pentagonal in side view, wide, each<br />

9 mm. long by 8 mm. wide, with flat truncated top bearing<br />

sinuses so that the ambulacra are almost invisible in<br />

side view. Each radial sinus is 2 mm. long by 5.5 mm.<br />

wide, with deltoids overlapped by thickened radial limbs.<br />

Deltoids four, short, lancet-shaped, each 6 mm. long<br />

by 3 mm. wide, confined to summit, with low crests, and<br />

with approximately eight hydrospire slits exposed on each<br />

side <strong>of</strong> an ambulacrum except in anal area where they<br />

are lacking. The slits extend to the adjacent radial limbs.<br />

Approximately 16 cover plate sockets occur on each side<br />

<strong>of</strong> each deltoid lip. On the anal side, the thick horseshoeshaped<br />

epideltoid, adjacent to the oral opening, surrounds<br />

the adorai portion <strong>of</strong> the anal opening on three sides and<br />

is overlapped by the radial limbs. The aboral part <strong>of</strong> the<br />

anal opening was presumably covered by a pentagonal<br />

hypodeltoid which is missing, probably as a result <strong>of</strong><br />

disturbance <strong>of</strong> sediment in which it was buried, judging<br />

from the worn nature <strong>of</strong> the theca. Hydrospire slits are<br />

lacking on anal side and therefore only eight hydrospire<br />

fields are developed.<br />

Ambulacra five, short, petaloid, confined to summit,<br />

each 3.75 mm. long by 1.75 mm. wide, with the adorai<br />

end <strong>of</strong> lancet 2 mm. from oral opening and exposed between<br />

side plates for a short distance aborally, but generally<br />

covered by side plates. Primary side plates subquadrangular,<br />

30 in a length <strong>of</strong> 10 mm., with a subtriangular<br />

secondary side plate on the adoral-abmedial corner<br />

<strong>of</strong> each primary side plate. The brachiolar area <strong>of</strong><br />

attachment is shared equally between a primary side<br />

plate and its associated secondary side plate. Approximately<br />

four main cover-plate sockets correspond to each<br />

side plate along the main food groove and three side<br />

cover-plate sockets along either side <strong>of</strong> each side food<br />

groove. Surfaces <strong>of</strong> calyx plates are ornamented with<br />

fine growth striae parallel to plate margins.<br />

Remarks.—The genus Codaster is a specialized form<br />

that, as now understood, should be restricted to fossils<br />

known from the Lower Carboniferous <strong>of</strong> England. It was<br />

probably derived from a form like Trionoblastus <strong>of</strong> the<br />

Devonian, in which the superdeltoid and subdeltoid plates<br />

are fused to form the epidcltoid.<br />

Occurrence.—The labels on the specimens are generalized<br />

and merely indicate unspecified Lower Carboniferous<br />

strata <strong>of</strong> Yorkshire, Lancashire, and Derbyshire,<br />

England.<br />

Types.—Plesiotypes 367, six specimens, Harvard Museum<br />

<strong>of</strong> Comparative Zoology, Cambridge, Mass. The<br />

description was based mainly on characters <strong>of</strong> one <strong>of</strong><br />

these specimens, with an old name "Pentremite asteria"<br />

and number 2319, Malham, Yorkshire, England, on the<br />

label. Plesiotypes 96,267, three specimens, Carboniferous<br />

limestone, Yorkshire, England, labelled Codaster acutus;<br />

S3,200, three specimens, Carboniferous limestone, Lischowney,<br />

Derbyshire, England, labelled Codaster acutus,<br />

Springer collection; S3,218, two specimens, Carboniferous<br />

limestone, Lancashire, England, labelled Codaster<br />

trilobatus, Springer collection; S3,219, three specimens<br />

<strong>of</strong> the Hambach collection, Carboniferous limestone,<br />

Lischowney, Derbyshire, England, labelled Codaster trilobatus<br />

in the Springer collection; and S3,220, two specimens,<br />

Carboniferous limestone, Settle, Yorkshire, England,<br />

labelled Codaster trilobatus var. acutus, Springer<br />

collection, U. S. National Museum, Washington.<br />

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

FIGURES 8, 9. Codaster acutus M'CoY, Lower Carboniferous,<br />

England; part <strong>of</strong> "A" ambulacrum showing main<br />

and outer side plates seen in two specimens (Harvard<br />

Mus. Comp. Zoology, no. 367, fig. 8, X45; U. S. Natl.<br />

Mus., no. S3,218, fig. 9, X37.5). [Explanation.—Bf,<br />

brachiolar facet; Bp, firachiolar pit; OSp, outer side plate;<br />

Sp, main side plate.]<br />

Type-species, by original designation (herein).—Codarter (Cryptoschisma?)<br />

iaeviusculus ROWLEY, 1900.<br />

Generic diagnosis.—Fissiculate blastoids with ten<br />

exposed hydrospire fields, an epideltoid and hypodeltoid,<br />

broad radial sinuses, lancet covered by side plates,<br />

ambulacra extending down sides <strong>of</strong> theca; form <strong>of</strong><br />

calyx conical in side view. Mississippian, Missouri.

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