ECHINODERMATA - KU ScholarWorks - University of Kansas
ECHINODERMATA - KU ScholarWorks - University of Kansas
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.