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NUMBER 557 43<br />
formula: S1_2>S3>S4>S5. Last (fifth) cycle rarely present and<br />
never complete, the largest number of septa reported being 68,<br />
corallites with only 48 septa being most common. S^_2 only<br />
slightly exsert, their inner edges attaining the columella, their<br />
upper edges bearing 5-7 coarse teeth. S3 shortest septa, bearing<br />
3 or 4 small, blunt teeth. Each S3 flanked by a pair of long S4,<br />
each bearing 7 or 8 blunt teeth and meeting in a V-shaped<br />
junction near inner edge of common S3 and continuing to<br />
columella to meet the inner edge of the S2. Fossa of variable<br />
depth, but usually quite shallow. Columella papillose, consisting<br />
of papillae indistinguishable from teeth on inner edges of<br />
S.,_2, and S4.<br />
DISCUSSION.—Oulangia stokesiana miltoni is distinguished<br />
from the nominate subspecies and two other Recent species (O.<br />
bradleyi Verrill, 1866, and O. cyathiformis Chevalier, 1971) by<br />
having a relatively small corallum with correspondingly fewer<br />
septa: 48-66 instead of 96. Previously known only from off<br />
northeastern Honshu, and South Korea, this subspecies is<br />
herein reported from the Sea of Japan in the Oki Channel, off<br />
southwestern Honshu at 100-135 m, the greatest recorded<br />
depth for this subspecies. Like Letepsammia formosissima,<br />
specimens from the northern range (off Japan) of this<br />
widespread Indo-West Pacific species have a smaller corallum,<br />
and thus has been distinguished as a subspecies.<br />
MATERIAL EXAMINED.—New Records: TM (KT9015,<br />
CB-6), 3 corallites, USNM 92646. Previous Records: 75<br />
syntypes, TIUS.<br />
TYPES.—Approximately 150 syntypes (Plate 41 a,b) are<br />
deposited at the TIUS (41051). Type Locality: Shiogamamachi<br />
(east of Teizan Canal), Matsushima Bay, near Sendai,<br />
Honshu, depth unknown.<br />
DISTRIBUTION.—Pleistocene of Sagami Bay region. Recent:<br />
Northeastern coast of Honshu from Shiogama to<br />
Sagami Bay; ?Miyake-jima; Oki Channel, off southwestern<br />
Honshu; coast of South Korea from Pusan to Tokchokto,<br />
Yellow Sea; 0-135 m.<br />
DIAGNOSIS.—See Part 1.<br />
Family OCULINIDAE<br />
Madrepora Linnaeus, 1758<br />
Madrepora oculata Linnaeus, 1758<br />
ACCOUNT.—See Part 1.<br />
Cyathelia Milne Edwards and Haime, 1849<br />
DIAGNOSIS.—Colonies arborescent, formed by regular,<br />
alternate, extratentacular budding. Coenosteum dense and<br />
faintly costate. Well-developed pali occur before first three<br />
septal cycles; columella papillose.<br />
TYPE SPECIES.—Madrepora axillaris Ellis and Solander,<br />
1786, by monotypy.<br />
Cyathelia axillaris (Ellis and Solander, 1786)<br />
PLATE \%a-c<br />
Madrepora axillaris Ellis and Solander. 1786:153, pi. 13: fig. 5.<br />
Cyathelia axillaris.—Milne Edwards and Haime. 185Ob:72-73.<br />
Cyathohetia axillaris.—Milne Edwards and Haime, 1857:110-111.—Duncan,<br />
1876:438.—Alcock, 1898:28.—Bedot, 1907:145, pi. 15: fig. 103.<br />
Cyathelia cf. axillaris.—Eguchi, 1942:138 (142), pi. 6: figs. 2, 3 [synonymy].<br />
Cyathelia axillaris.—Eguchi, 1968:C28, pi. C20: figs. 5-7; pi. C24: figs. 4. 5<br />
[synonymy].—Kikuchi, 1968:8, pi. 5: fig. 1.<br />
DESCRIPTION.—Coralla sparsely branched, resulting in<br />
small, robust, bushy colonies, the largest known about 7.5 cm<br />
in height, supporting approximately 100 corallites (Eguchi,<br />
1968, pi. C24: fig. 4). Branching is essentially sympodial, but<br />
two buds often originate on opposite sides of a terminal<br />
corallite, the parent corallite ultimately becoming immersed in<br />
thick coenosteum within the branch axil. Corallites circular<br />
when small, often becoming elliptical or even medially<br />
constricted if located at a branch axil. Corallites relatively<br />
large, up to 11 mm in GCD. Branch coenosteum dense,<br />
granular, light brown to tan in color, and usually faintly costate.<br />
Corallites often pigmented a darker shade of brown.<br />
Septa usually hexamerally arranged in 4 cycles; however,<br />
small corallites (i.e., 10 mm GCD) sometimes have an extra (13th) half-system for<br />
a total of 52 septa. Septal formula: S1_2>S3>S4. Su2 up to 1.5<br />
mm exsert, quite thick, and have straight inner edges reaching<br />
about one-fourth distance into fossa. S3 equally exsert but only<br />
about two-thirds as wide as S:_2- S4 less exsert and about 80%<br />
width of the S3. Twelve thick pali, each about 1.5 mm wide,<br />
form a palar crown encircling columella. Another crown of 12<br />
P3, each palus of equal width but slightly thicker than P1-2,<br />
occurs slightly recessed from the columella and slightly higher<br />
in fossa. Pali and septal faces highly granular. Columella<br />
papillose.<br />
DISCUSSION.—Cyathelia is a montypic genus distinguished<br />
from other oculinid genera by having two crowns of pali before<br />
its first three septal cycles. It has a distinctive colony shape,<br />
easily recognized by its sparse branching and large corallites in<br />
relation to its branch diameter.<br />
MATERIAL EXAMINED.—New Records: Alb-4944, 1 colony,<br />
USNM 92660; TM (KT9015, CB2-2), 1 colony, ORI; TM<br />
(KT9015, CB1-2), 2 colonies, USNM 92661; TM (KT9202,<br />
YS1), 1, USNM 92662; TM (KT9202, YT2), 1, USNM 92663;<br />
off Yenoshima, Honshu, 4 colonies, USNM 92664; Monoiso,<br />
Misaki, Sagami Bay, 1 colony, USNM 92665; Ashima, Sagami<br />
Bay, 1 colony, USNM 92666. Previous Records:<br />
Challenger-\96, 1 colony, BM 1880.11.25.88 (reported by<br />
Moseley, 1881).<br />
TYPES.— The types of M. axillaris have not been traced,<br />
although Ellis and Solander's (1786) original illustration of the<br />
species is diagnostic for this distinctive species. Type Locality:<br />
Eastern Indian Ocean, depth unknown.