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70<br />
vermiformis is easily distinguished from all other North Pacific<br />
corals by its small, slender, cylindrical corallum and aligned<br />
mural spots. Its small size and inconspicuous habit have<br />
undoubtedly caused this relatively widespread species to have<br />
been overlooked in the past. The specimen reported herein from<br />
Soyo Maru-425 is 2.3 mm in calicular diameter and 3.2 mm in<br />
length with large P2 and a fascicular columella. It can be<br />
identified based on the generic diagnosis; illustrations of this<br />
species may be found in the references listed in the synonymy.<br />
MATERIAL EXAMINED.—New Records: Soyo Maru-425,1<br />
specimen attached to a dead Crispatotrochus rubescens, TIUS<br />
53695, Plate 22g. Previous Records: Syntypes of C. vermiformis,<br />
MCZ; specimens reported by Cairns (1979, 1982) and<br />
Cairns and Parker (1992).<br />
TYPES.—Thirty-eight syntypes of Coenocyathus vermiformis<br />
are deposited at the MCZ (Cairns, 1979). Type<br />
Locality: Off Florida Keys, 274-329 m.<br />
DISTRIBUTION.—The single Japanese record from off Koshiki<br />
Retto, southwestern Kyushu (300 m) is the first report of<br />
this genus from the North Pacific. It was apparently overlooked<br />
by Yabe and Eguchi (1942b) in their report of Cyathoceras<br />
rubescens. Elsewhere: It is known to be common on both<br />
sides of the Atlantic; off St. Paul and Amsterdam Islands,<br />
southern Indian Ocean; the New Zealand region, including the<br />
Antipodes and Campbell Plateaus; off Tasmania; and off<br />
southeastern Australia; 80-1229 m.<br />
Truncatoguynia Cairns, 1989a<br />
DIAGNOSIS.—Solitary, elongate compressed-cylindrical, and<br />
free. Budding by transverse division. Epitheca smooth; rows of<br />
thecal pores occur in every intercostal space, alignment of rows<br />
appearing to flank the secondary costae. Septa only slightly<br />
exsert and variable in symmetry, arranged in 2 or 3 size classes.<br />
Pali and columella absent.<br />
TYPE SPECIES.—Truncatoguynia irregularis Cairns, 1989a,<br />
by monotypy.<br />
Truncatoguynia irregularis Cairns, 1989<br />
PLATE 30r/<br />
Truncatoguynia irregularis Cairns. 1989a:43. pi. 22: figs. f,g; pi. 23: figs. c,f.<br />
DESCRIPTION.—Corallum an elongate, laterally compressed<br />
cylinder with rounded thecal edges. Largest Japanese specimen<br />
examined 44.4 mm in length, with calicular diameters up to 5.8<br />
x 4.3 mm. Base of specimens (anthocauli) terminate in an<br />
elliptical scar about 3.9 x 3.1 mm in diameter, revealing 12-24<br />
primary septa. Theca thin, smooth, and in ail Japanese<br />
specimens, somewhat wom, the coralla obviously dead when<br />
collected. Thecal pores irregular in appearance, more common<br />
toward the base of a corallum and often absent from theca near<br />
calice. In several weathered coralla and the older (basal)<br />
portions of others, the secondary septa and associated overlying<br />
theca are absent, resulting in a characteristic diagenetic form<br />
SMITHSONIAN CONTRIBUTIONS TO ZOOLOGY<br />
consisting of 12-18 lamella (septa) radiating from a central<br />
columella. Corallum white.<br />
Most coralla hexamerally arranged in three cycles of septa<br />
and an additional pair of S4 in each of the four end half-systems<br />
according to the formula: S1_2>S3>S4 and a total of 32 septa;<br />
however, one specimen had 14 primary septa and another had<br />
18. Su2 slightly exsert (1.1 mm) with slightly sinuous inner<br />
edges that are strongly fused to the columella. S3 only one-third<br />
to one-half width of an S1 and also have slightly sinuous inner<br />
edges, but they do not attain the columella. S4 rudimentary,<br />
consisting of a short row of spines. Fossa deep. Columella an<br />
elongate fusion of lower, inner edges of S^.<br />
DISCUSSION.—This species was previously known only<br />
from its type locality in the South China Sea. Although all the<br />
Japanese specimens were dead when collected, they do allow a<br />
refinement of the original description and reinforce the<br />
observation that the septal symmetry of this species is indeed<br />
irregular.<br />
MATERIAL EXAMINED.—-New Records: TM (KT9202,<br />
YT1), 1, USNM 92753, 2, ORI. Previous Records: Types of<br />
T. irregularis, USNM.<br />
TYPES.—The holotype (81890) and 10 paratypes (81891) of<br />
T. irregularis are deposited at the USNM. Another paratype is<br />
deposited at the Australian Museum (G15252). Type Locality:<br />
Alb-5311: 21°33'N, 1 ^tf'E (South China Sea north of<br />
Pratas Island), 161 m.<br />
DISTRIBUTION.—Osumi Shoto, northern Ryukyu Islands;<br />
north of Pratas Island, South China Sea; 80-161 m.<br />
DIAGNOSIS.—See Part 1.<br />
Family FLABELLIDAE<br />
Flabellum Lesson, 1831<br />
Subgenus Flabellum (Flabellum) Lesson, 1831<br />
DIAGNOSIS.—See Part 1.<br />
Flabellum (F.) pavoninum Lesson, 1831<br />
PLATES 30g-i, 3la-e<br />
Flabeilum pavoninum Lesson, 1831:2.—Gray, 1849:75-76.—Marenzeller,<br />
1888a:41-42.—Cairns, 1989a:46-50, pi. 23: figs, g-1; pi. 24: figs. a-d,g,h<br />
[synonymy].<br />
Flabellum distinctum Milne Edwards and Haime, 1848a:262.—Marenzeller,<br />
I888a:42.—Yabe and Eguchi, 1932a:387, 389; 1932b:443; 1941b:101;<br />
l942a:93-95, pi. 5: figs. 3-6; pi. 6: figs. 3,4,9, 10; pi. 7: fig. 7; 1942b:l 12,<br />
130-131, pi. 11: figs. 10-12.—Eguchi, 1938, table 2; 1944:132-134, 5 figs;<br />
I968:C44 [in part: pi. C28: figs. 5, 6].—Utinomi, 1965:255.—Eguchi and<br />
Miyawaki, 1975:58.—Mori and Minoura, 1980:321-326, figs. 1-5.—Zou<br />
et al., 1981. pi. 1: figs. 2, 3.—Song, 1982:136-137, pi. 3: figs. 1-4;<br />
1991:135.<br />
Flabellum coalitum Marenzeller, 1888a:48-49.—Cairns, 1989a:46, 50, pi. 24:<br />
figs, e.f.i-1.<br />
Flabellum sp. cf. distinctum.—Okutani, 1969:12.—?Hamada, 1969:254.<br />
DESCRIPTION.—Corallum compressed, the planar faces<br />
meeting at acute edges and projecting 2.5-3.8 mm beyond the