ECHINODERMATA - KU ScholarWorks - University of Kansas
ECHINODERMATA - KU ScholarWorks - University of Kansas
ECHINODERMATA - KU ScholarWorks - University of Kansas
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BLASTOID STUDIES 31<br />
mm. long by 5.5 mm. wide, pentagonal in basal view,<br />
composed <strong>of</strong> three normally disposed basais. Radials five,<br />
each 11.5 mm. long by 4.5 mm. wide, with deep, narrow,<br />
tapering sinus 10.5 mm. long by 2.5 mm. wide; radials<br />
overlapping deltoids.<br />
Deltoids four, short, not visible in side view, triangular,<br />
covered by radial limbs, with deep median<br />
septum between adjacent hydrospire canals. On the anal<br />
side, the quadrangular hypodeltoid (missing) abuts<br />
against the radial limbs and rests on two internal cryptodeltoids.<br />
The cryptodeltoids are on either side <strong>of</strong> the<br />
anal opening, are overlapped by the radial limbs, and<br />
overlap the superdeltoid internally on the adorai side <strong>of</strong><br />
the anal opening. They appear to be continuous with<br />
the two anal septa <strong>of</strong> the superdeltoid and separate the<br />
anal opening from the adjacent hydrospire canals internally.<br />
The superdeltoid, adjacent to the oral opening,<br />
is homologous with the deltoid lips <strong>of</strong> the other four deltoids<br />
and together with them helps to surround the oral<br />
opening. Spiracles five, with four piercing the adorai<br />
ends <strong>of</strong> the four deltoids and the anispiracle formed between<br />
the superdeltoid and hypodeltoid. Five hydrospire<br />
folds occur on each side <strong>of</strong> an ambulacrum, making ten<br />
fields in all, with aboral ends <strong>of</strong> the outermost slits exposed.<br />
Ambulacra five, linear, each 13 mm. long by 2 mm.<br />
wide, slightly recurved onto aboral side, lancet covered<br />
by side plates, with 22 side plates in 10 mm. The side<br />
plates are normally disposed, with a subtriangular secondary<br />
side plate on the adoral-abmedial bevelled corner<br />
<strong>of</strong> each primary side plate, and a large bifasiculate<br />
brachiolar muscle scar split between the primary and<br />
secondary side plates. The pores are formed as gaps between<br />
side plates and margins <strong>of</strong> the radial sinuses. The<br />
brachiolar pit is admedial from the brachiolar facet, leading<br />
adorally to a side food groove. Two side cover-plate<br />
sockets occur on each side food groove and four main<br />
cover-plate sockets on each side plate along the main food<br />
groove. A curved pore furrow occurs on each primary<br />
side plate, curved aborally and abmedially around the<br />
brachiolar facet, ending in a pore. Near the radiodeltoid<br />
suture the side plates are firmly fixed against the radial<br />
sinus and pores are absent. The surfaces <strong>of</strong> the calyx<br />
plates are ornamented with fine growth lines parallel<br />
to plate margins.<br />
Remarks.—This species was selected as the type-species<br />
because it clearly shows the internal and external features<br />
that characterize the genus.<br />
Occurrence.—Middle Devonian, coral zone <strong>of</strong> the<br />
Widder beds, Hungry Hollow Formation, Joseph Bell<br />
Quarry, Thedford area, Ontario, Canada.<br />
Type.—Holotype, E15,934, one specimen, collected<br />
by CHARLES SOUTHWORTH (1943), purchased by Buffalo<br />
Society <strong>of</strong> Natural Sciences, Buffalo, New York.<br />
HYPEROBLASTUS BASSLERI (Reimann)<br />
Plate 52, figures 3-5<br />
Pentremitidea bass/eni REIMANN, 1945, p. 33, pl. 7, figs. 3-5.<br />
Description.—The figured specimen is 27 mm. long<br />
by 13 mm. wide, vault 17 mm. long, pelvis 10 mm. long,<br />
and pelvic angle 55 degrees.<br />
Occurrence.—Middle Devonian, Traverse Group,<br />
Thunder Bay Formation (now Partridge Point Formation),<br />
Partridge Point, near Alpena, Michigan.<br />
Type.—Paratype, E15,337, one specimen, Buffalo<br />
Society <strong>of</strong> Natural Sciences, Buffalo, New York.<br />
HYPEROBLASTUS CUMMINGSI (Reimann)<br />
Plate 9, figures 1-3<br />
Pentremitidea cummingsi REIMANN, 1935, p. 28, pl. 2, fig. 19, pl.<br />
4, fig. 8.<br />
Description.—The figured specimen is 14 mm. long<br />
by 9.5 mm. wide, vault 11.5 mm. long, pelvis 2.5 mm.<br />
long, and pelvic angle on basal circlet 75 degrees and on<br />
radial bodies 160 degrees. Approximately five hydrospire<br />
folds occur on each side <strong>of</strong> an ambulacrum.<br />
Occurrence.—Middle Devonian, coral zone <strong>of</strong> Widder<br />
beds, Hungry Hollow Formation, Arkona, Ontario,<br />
Canada.<br />
Type.—Hypotype, E15,935, one specimen, Buffalo<br />
Society <strong>of</strong> Natural Sciences, Buffalo, New York.<br />
HYPEROBLASTUS DOTIS (Reimann)<br />
Plate 9, figures 7, 9-11; text-fig. 28<br />
Pentretnitaea dotis REIMANN, 1945, p. 37, pl. 6, fig. 13.<br />
Description.—The figured specimen is 9 mm. long<br />
by 5.5 mm. wide, vault 5.5 mm. long, pelvis 3.5 mm.<br />
long, and pelvic angle 60 degrees on basal circlet and 130<br />
degrees on radial bodies. Five hydrospire folds occur on<br />
each side <strong>of</strong> an ambulacrum.<br />
Occurrence.—Middle Devonian, coral zone <strong>of</strong> Widder<br />
beds, Hungry Hollow Formation, Thedford, Ontario.<br />
Types.—Holotype, E15,401, one specimen; paratypes,<br />
E13,052, four specimens, Buffalo Society <strong>of</strong> Natural Sciences,<br />
collected by CHARLES SOUTHWORTH (1941), identified<br />
by REIMANN ( 1944); an ambulacrum <strong>of</strong> one <strong>of</strong> these<br />
specimens is shown in text-figure 23.<br />
HYPEROBLASTUS ERIENSIS (Reimann)<br />
Plate 11, figures 4-6<br />
Pentremitidea eriensis REIMANN, 1945, pp. 37-38, pl. 7, fig. 11.<br />
Description.—The figured specimen is 7.5 mm. long<br />
by 5.5 mm. wide, vault 6 mm. long, pelvis 1.5 mm. long,<br />
and pelvic angle 75 degrees on basal circlet and 160<br />
degrees on radial bodies. Base fiat, triangular.<br />
Occurrence.—Middle Devonian, Tichenor Limestone,<br />
Springbrook Station, New York.