498
Journal of Paleontology 92(3):488–505
Holotype.—CMCIP 76789, holotype; CMCIP 76790, paratype; UMMP 74681.2, paratype.
Diagnosis.—Cleiocrinus with medium conical to bowl-shaped calyx; sutural pores few, positioned along plate sutures to either side of each plate corner; plates ornamented withfine pitting; median ray ridges narrow, rounded; 20 free arms; abundant fixed pinnules.
Occurrence.—The occurrences documented here are from the middle–upper Bobcaygeon Formation, Kirkfield Quarry, Upper Ordovician (lower Katian) and from the Bobcaygeon–Verulam contact zone, LaFarge Quarry, UpperOrdovician (lowerKatian).
Description.—Calyx medium cone with bowl-shaped base, as high as wide; plates ornamented with fine pitting; median ray ridges narrow, rounded. Upper and lower margins of fixed brachial plates undulatory, medial portion of distal margin deflected downward; distal plate margins slightly elevated from the calyx surface and appearing to overlap the plates above, giving the appearance of weak imbrication. Sutural pores positioned along plate sutures, relatively
large in size compared to other species, typically eight per plate, positioned to either side of each plate corner; pores more closely spaced in more distal plates. Infrabasals not observed; infrabasal circlet probably
confined to basal concavity and overlapped by higher circlet as is typical in other Cleiocrinus species. Basals and radials arranged in a single circlet of 10 plates.
Basals small, pentagonal, higher than wide, with angled surface directed upwards. Radials slightly smaller than basals, rectangular as known, wider than high. Rays comprised of numerous fixed brachials that are fused
laterally; interray plates absent. Posterior interray imperfectly preserved, articulation with CD basal not observed; middle to higher portion of posterior interray forming an anal series comprised of a single column of wide, low plates; anal series plates four to five times wider than high, upper and lower margins strongly undulatory and similar in shape to the patelloid process of flexible crinoids. Anal series ornamented by a broad, protruding anitaxial ridge. Primibrachials two; first primibrachial roughly hexagonal,
largest plate in calyx, more than twice as wide as high, resting on underlying radial and sloping upper margins of adjacent basals; second primibrachial axillary, wider than high. Secundibra- chials three in preserved rays, third axillary, all secundibrachials approximately twice as wide as high. Tertibrachials four to six, bifurcating at different positions within rays, dimensions becoming more equant distally, but still wider than high throughout. Quartibrachials variable in number, giving rise to one arm and two large fixed pinnules per quarter ray; 20 free arms and 40 large fixed pinnules in total; higher quartibrachials giving rise to additional, smaller fixed pinnules that grade into
free pinnules. Undulatory pattern of plate margins becoming increasingly exaggerated in higher fixed brachials. Arm openings 20; two large fixed pinnules positioned
between each arm, 40 large fixed pinnules in total. Brachials weakly cuneate uniserial, pinnulate. Stem obtusely pentagonal with rounded margins; lumen
large, diameter ~60% stem diameter. Proximal to medial stem heteromorphic, N212; nudinodals moderately thick with smooth, rounded latera, priminternodals slightly thinner and with smaller diameter than the first; internodals very thin, not visible in side view, entirely overlapped by nudinodals, comprised of five narrow petal-like arcuate segments that are only marginally in lateral contact. Distal column, holdfast, distal arms, and tegmen unknown.
Etymology.—The specific name lepidotus is derived from the Greek lepidotós, meaning scaly, in reference to the scale-like appearance of the calyx plates.
Materials.—CMCIP 76789, holotype (middle–upper Bobcay- geon Formation, Kirkfield Quarry); CMCIP 76790, paratype (middle–upper Bobcaygeon Formation, Kirkfield Quarry); UMMP 74681.2, paratype (Bobcaygeon-Verulam contact zone, LaFarge Quarry).
Remarks.—Cleiocrinus lepidotus n. sp. is most similar to C. perforatus but differs from this and all other species of Cleiocrinus on the basis of its plate ornamentation, the number and arrangement of sutural pores, and the condition of the posterior interray. Whereas C. lepidotus n. sp. is ornamented with fine pitting, other Cleiocrinus species are unornamented (C. perforatus) or have a variety of ridges arranged in radiating, concentric, and/or rhombic patterns (all other species). Among species of Cleiocrinus, sutural pore number and arrangement ranges from several large pores along each plate margin (C. perforatus) to small elongated slits (C. laevis) to many small, closely spaced circular pores (all other species). In con- trast, C. lepidotus n. sp. has few, relatively large sutural pores (typically two per plate margin) that are positioned to either side of each plate corner. In addition, in many species of Cleiocrinus, the external plate sutures converge into larger pores before reaching the inner surface of the plate (e.g., C. regius, C. bromidensis). The large pores of C. lepidotus n. sp. appear to penetrate the calyx directly and do not converge, a character apparently shared with C. perforatus. Finally, all species of Cleiocrinus for which the posterior is known have a posterior interray that is not in contact with the tegmen, whereas the posterior of C. lepidotus n. sp. is in contact with the tegmen.
Cleiocrinus sp. Figure 4.6
Figure 6. Cleiocrinus lepidotus n. sp. from southern Ontario. (1, 5–8) CMCIP 76789, holotype (middle–upper Bobcaygeon Fm., Kirkfield Quarry); (1) lateral view of partial crown and stem, posterior interray indicated by arrow; (5) lateral view of partial crown, opposite side; (6) radial/basal circlet showing radial plate (center), wide fixed primibrachials, and adjacent basals; (7) proximal (upper) stem articular facet, photographed under alcohol; (8) distal (lower) stem articular facet, photographed under alcohol; (2, 3, 9–11) CMCIP 76790, paratype (middle–upper Bobcaygeon Fm., Kirkfield Quarry); (2) lateral view of distal calyx and arm bases; (3) posterior view of partial calyx; (9) close-up of fixed brachial plates showing pitted ornamentation; (10) closeup of fixed brachial plates showing sutural pores adjacent to plate corners, photographed under alcohol; (11) close-up of posterior interray; (4) UMMP 74681.2, paratype (Bobcaygeon-Verulam contact zone, LaFarge Quarry), lateral view of small partial calyx. All scale bars 5mm unless otherwise indicated.
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