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72<br />
38-41 mm; seventh cycle gradually added up to a GCD of<br />
about 65 mm at which size all 384 septa are usually present.<br />
S1_4 equal in size only in large coralla, the S4 being slightly<br />
less wide than S1-3 in smaller coralla; regardless of size, inner<br />
edges of all S^ attain the columella. Upper, inner edges of<br />
S1-4 moderately sinuous, becoming thicker and more sinuous<br />
deeper in fossa. S5 half to three-quarters width of S1_4, have<br />
moderately sinuous inner edges, and do not attain the<br />
columella. S6 about one-third width of S5, and S7, if present,<br />
rudimentary: only about 0.5 mm wide and 2-3 mm long. Fossa<br />
deep and narrow, formed by vertical inner edges of S1_4.<br />
Columella elongate, composed of a trabecular to solid fusion of<br />
the lower, inner edges of the S1_4, as much as 30 mm long and<br />
about 2 mm wide.<br />
DISCUSSION.—Several of the Indo-West Pacific species of<br />
Flabellum (Flabellum) were compared by Cairns (1989a, table<br />
5) and further distinguished by discriminant analysis (Cairns,<br />
1989b). Flabellum patens was found to be most similar to F.<br />
pavoninum, differing primarily in corallum shape. To quantify<br />
the difference in shape, F. patens has a lower face angle<br />
(20°-32° vs 32°-42° for F. pavoninum), a higher GCD:LCD<br />
(2.05-2.50 vs 1.98-2.41), a lower GCD:H (1.04 vs 1.34),<br />
higher edge crests (4.8-6.1 vs 2.5-3.8 mm), and a tendency to<br />
have S7.<br />
Yabe and Eguchi's (1942a) report of F. pavoninum<br />
lamellulosum from off Seto was not illustrated and their two<br />
specimens cannot be located, but based on their description,<br />
these specimens would appear to be F. patens.<br />
MATERIAL EXAMINED.—New Records: Alb-5313, 8,<br />
USNM 40757,2, ORI; Alb-5314,1, USNM 92813; YO70-770,<br />
1, USNM 92314; off Pengue, Taiwan, 3, CAS 74993. Previous<br />
Records: 4 syntypes of F. patens, BM; F. pavoninum<br />
paripavoninum of Yabe and Eguchi (1942a,e): Soyo Maru-4\9,<br />
1, TIUS 43441; 5oyo Maru-343, 1, TIUS 43445.<br />
TYPES.—The lectotype and 5 paralectotypes of F. patens are<br />
deposited at the BM, the lectotype designated by Cairns<br />
(1989a:52). Type Locality: Challenger-192: 5°49'S,<br />
132°14'E (Kei Islands, Banda Sea), 256 m.<br />
DISTRIBUTION.—Japan: Kii Strait, Honshu; off northeastern<br />
Shikoku; off southwestern Kyushu; Formosa Strait; South<br />
China Sea north of Pratas Island; 223-402 m. Elsewhere:<br />
Philippines, Banda Sea; 256-439 m.<br />
Flabellum (F.) magnificum Marenzeller, 1904<br />
PLATE 31./-/<br />
Flabellum magnificum Marenzeller. 19O4a:276-277.pl. 17: fig. 13.—Utinomi,<br />
1965:255.—Cairns, 1989a:5O-51, pi. 25: figs, a-j [synonymy].<br />
Flabellum pavoninum.—Yabe and Eguchi. I942a:90-91. pi. 5: fig. 2a-c [in<br />
part Soyo Marn-437]; 1942b: 129. pi. 11: fig. 7a-c.<br />
Flabellum pavoninum magnificum.—Yabe and Eguchi, 1942a:89-90, pi. 5:<br />
fig. la-c; 1942b:129, pi. 11: fig. 8a-c.<br />
DIAGNOSIS.—Angle of thecal edges 140°-172°; inclination<br />
SMITHSONIAN CONTRIBUTIONS TO ZOOLOGY<br />
of planar thecal faces quite open, 44°-58°. Discontinuous edge<br />
crests usually not present. Thecal faces bear reddish brown<br />
stripes associated with each costa. Pedicel narrow, only<br />
1.5-2.3 mm in diameter. Ratio of GCD:LCD = 1.65-1.96.<br />
Septa hexamerally arranged in 7 cycles, the last cycle never<br />
complete, the largest known specimen having 376 septa. Septal<br />
formula: S1_4>S5>S6>S7. Columella well developed.<br />
DISCUSSION.—No additional specimens of this large and<br />
elegant species are reported herein. It is known in Japanese<br />
waters from only four specimens reported by Yabe and Eguchi<br />
(1942a,b) and Utinomi (1965). A full description and illustrations<br />
are given by Cairns (1989a). It is distinguished (Cairns,<br />
1989a,b) from other Indo-West Pacific Flabellum by attaining<br />
a very large corallum size with up to 7 cycles of septa, having<br />
the largest face angle (44°-58°), and having very long lateral<br />
edges.<br />
MATERIAL EXAMINED.—New Records: None. Previous<br />
Records: Soyo Maru-437, 1, TIUS 43448 (F. pavoninum of<br />
Yabe and Eguchi, 1942a) (Plate 31»; Soyo Marw-416, 1, TIUS<br />
50094 (F. p. magnificum of Yabe and Eguchi, 1942a).<br />
TYPES.—The holotype appears to be lost from the ZMB (see<br />
Cairns, 1989a). Type Locality: Valdivia-199: 0° 15.57*,<br />
98°04'E (off western Sumatra), 470 m.<br />
DISTRIBUTION.—Japan: Off Seto, Kii Strait, Honshu; off<br />
southeastern Shikoku; East China Sea off southwestern Kyushu<br />
(induing off Danjo Gunto); 307-700 m. Elsewhere: Philippines,<br />
Indonesia, west of Sumatra; 291-616 m.<br />
Flabellum (F.) angustum Yabe and Eguchi, 1942<br />
PLATE 31/<br />
Flabellum disticlum angustum Yabe and Eguchi, 1942a:95, pi. 6: figs. 5-7;<br />
1942b: 131.—Eguchi, 1968:C4.<br />
DISCUSSION.—A new subspecies of F. distinctum was<br />
described by Yabe and Eguchi (1942a,b) based on 60 Pliocene<br />
coralla from Kochi-ken, Shikoku. Although a Recent specimen<br />
from Sagami Bay was also attributed to this taxon, Yabe and<br />
Eguchi (1942a) clearly indicated that the type locality<br />
corresponded to the fossil locality and illustrated only fossil<br />
specimens. Their rationale for the new subspecies was that the<br />
specimens had edge angles less than 70°. In fact, the edge angle<br />
of the fossil specimens is bimodal, ranging from 102°-123°<br />
near the pedicel to 52°-54° in upper corallum. The fossil<br />
specimens from Shikoku do appear to be a separate species, but<br />
the Recent specimen(s) from Sagami Bay were not illustrated<br />
and were not examined by the author.<br />
MATERIAL EXAMINED.—New Records: None. Previous<br />
Records: Syntypes of F. p. angustum, TIUS.<br />
TYPES AND TYPE LOCALITIES.—Sixty syntypes (Plate 31/)<br />
from the Pliocene of Tonohama, Kochi-ken, Shikoku are<br />
deposited at the TIUS (43436). Additional Recent syntypes<br />
from Sagami Bay are also deposited at the TIUS (59333).<br />
DISTRIBUTION.—Known only from the type localities.