ECHINODERMATA - KU ScholarWorks - University of Kansas
ECHINODERMATA - KU ScholarWorks - University of Kansas
ECHINODERMATA - KU ScholarWorks - University of Kansas
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106 THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS<br />
Ambulacra five, short, slightly rounded at aboral end,<br />
with lancet covered by side plates, and 28 side plates in<br />
a space <strong>of</strong> 10 mm. along an ambulacrum. One pore occurs<br />
between side plates along the ambulacral margins, and<br />
side plates are normally disposed. Surfaces <strong>of</strong> calyx plates<br />
ornamented by fi ne growth lines subparallel to plate margins.<br />
Occurrence.—Silurian, Niagara Group, Decatur County,<br />
Tennessee.<br />
Types.—Holotype, 139,105, one specimen with green<br />
label, with three other specimens; paratypes, 139,106, two<br />
sections and two specimens, Troost collection, old number<br />
33,071 and another 1,468 which included 16 specimens<br />
in all, U. S. National Museum, Washington.<br />
219<br />
FIGURES 218-221. Troosticrinus reinwardti (TaoosT), Silurian,<br />
Decatur County, Tennessee (U. S. Natl. Mus., no.<br />
33,071). 218. Anal area <strong>of</strong> metatype, X22.5.<br />
219. Summit and oblique anal tangential section (polished)<br />
<strong>of</strong> metatype, X20. 220. Cross section <strong>of</strong> "E"<br />
ambulacrum, oral view, <strong>of</strong> paratype, X17.5. 221.<br />
Cross section <strong>of</strong> an ambulacrum, oral view, <strong>of</strong> paratype,<br />
X17.5. [Explanation.—An, anal opening; C, canal (radial);<br />
CR, cryptodeltoid; Db, deltoid body; D1, deltoid<br />
lip; H, hydrospire; HD, hypodeltoid; L, lancet; R, radial;<br />
RI, radial limb; S, spiracle; Sp, main side plate; Su,<br />
superdeltoid.]<br />
PHYLOGENETIC TRENDS OF FISSICULATA<br />
Primitive fissiculate blastoids are Polydeltoideus<br />
and Deltoschisma, which have a steeply conical form,<br />
four to six anal deltoids, hydrospire slits exposed in ten<br />
sinus areas, and linear ambulacra with lancet covered<br />
by side plates. Blastoids <strong>of</strong> this group may form a<br />
natural family from which all others could have been<br />
derived.<br />
One trend is in the direction <strong>of</strong> reducing hydrospire<br />
fields on the anal side and closure <strong>of</strong> the sinus<br />
areas to form eight spiracular slits, as seen in Pentremitidea.<br />
Thus, all forms with eight spiracular slits may<br />
form a natural family (Astrocrinidae AUSTIN t1/4 Aus-<br />
TIN, 1843). Within this assemblage one may find<br />
forms in which (1) the lancet has migrated outward<br />
(Cryptoschisma) or (2) has remained the same except<br />
that one ambulacrum is shortened and the hypodeltoid<br />
has become small or atrophied (Astrocrinus, Pentephyllum),<br />
or (3) the pelvis is elongated, the ambulacra<br />
becoming small, with superdeltoid and subdeltoid<br />
fusing to form an epideltoid, and hypodeltoid becoming<br />
atrophied or small (Ceratoblastus), or (4) the<br />
ambulacra shortened, with an epideltoid and hypodeltoid<br />
remaining or (5) the hypodeltoid atrophied,<br />
with concurrent formation <strong>of</strong> radial wings (Nannoblastus).<br />
Pentremitidea probably gave rise to this<br />
group <strong>of</strong> blastoids, and this genus very likely came<br />
from Deltoschisma, which shows a reduction <strong>of</strong> the<br />
hydrospire slits on the anal side. Thus, Deltoschisma<br />
probably gave rise to Pentremitidea by fusion <strong>of</strong> the<br />
cryptodeltoids to form a subdeltoid, complete reduction<br />
<strong>of</strong> the hydrospires on the anal side, and closure<br />
<strong>of</strong> the sinus walls to form eight spiracular slits.<br />
Certain trends seem to have taken place within<br />
the primitive family <strong>of</strong> blastoids characterized by the<br />
possession <strong>of</strong> ten exposed hydrospire fields (Phaeno-