02.11.2013 Views

PDF - Eprints@CMFRI

PDF - Eprints@CMFRI

PDF - Eprints@CMFRI

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

169<br />

We ha ve found no other coral which agrees better to our specimen than BOURNE's B. cumingii and<br />

SEMPER 's Rbodopsammia ovalis. After SEMPER the polyps are provided " mit gelben Tentakeln und<br />

brillant orangefarbenem Mund ". FRICKE described the colour of the polyps as yellow with red oral discs.<br />

Mater ial :<br />

Northern R. S. : HLM Fri 78-3 (Ras Umm Sidd, 138 mi·<br />

Dis t r ib uti 0 n : Red Sea ; Ceylon ; Philippines.<br />

Rem ark s : If our identification proves correct, this is the first record of the species from the<br />

Red Sea .<br />

The taxonomic position of Balanopbyllia is in a poor state. Many of the so-called species are described<br />

on the strength of a single or a limited number of specimens, and many are certainly only ecomorphs or<br />

geographical variants. A revision of the genus is most desirable .<br />

Genus Rbizopsa mmia VERRILL, 1869<br />

T Y pes p e c i e s : Rbizopsammia pulcbra VERRI LL, 1869.<br />

G e n e ric c h a r act e r s : Small colonies, formed by extra tentacular budding and by stolon-like<br />

expansions, from which new corallites develop. Septa according to POURTALES plan, no paliform lobes,<br />

columella spongy, wall porous.<br />

Rbizopsammia wettsteini new spec.<br />

(Plate 39. Figs. 1-4)<br />

We have two specimens before us , which we adjoin with some hesitation to the ge nus Rbizopsammia.<br />

Both are small colonies formed by extratentacular budding and with stolo ns bearing young corallites.<br />

The corallites are about 10 mm high, the calices are almost round, 7 to 10 mm in diameter, the<br />

largest calyx measuring 11.5 by 10 .5 mm . The corallites have a smaller diameter at their base.<br />

Columella loosely packed and spongy. Septa in four complete cycles, fifth and sixth cycle incomplete.<br />

Septa of the first two cycles almost identical, sloping downwards from the edge to the columella, which<br />

makes the calices appear wide and open. Edges of first two cycle septa irregularly dentate or fra yed, only<br />

in very few cases are the edges intact. Septa perforated. Sides covered with granules and striations vertically<br />

to edge. Septa of higher orders are even more irregularly frayed and perforated . The quarternaries<br />

unite beneath the short tertiaries and join the columella. Moreover, they are joined to the first and second<br />

septa at the upper margin of the calxy by a spongy network of septa fringes , which makes these twelve<br />

points appear thicker. This is particularly evident on the first cycle septa.<br />

Costae, especially in the upper part of the coraUite, not clearly visible with numerous granules, often<br />

forming reticular ridges, interspersed with numero us perforations.<br />

PW 73 614- 1 consists of a principal calyx with two secondary calices o n one side. Two ribbed stolons<br />

branch out from this colony, one of which has developed a daughter corallite at the end, the upper<br />

portion of which is missing. Some specimens of Polycyatbus [uscomarginatus settle on the substrate<br />

supporting the colony.<br />

PW 73 614- 2 is also a small colony comprising three corallites with two stolons, each with a small<br />

daughter coraHite.<br />

The most strik ing features of R. wettsteini are the porosity and sponginess of the coral and its wide<br />

open calices.<br />

Materia l:<br />

Gulf of Aqaba: Basel PW 73614-1,2 (Eilat).<br />

Rem a rk s : Rbizopsammia wettsteini is named after the late Peter WETTSTEIN, who collected<br />

corals in the Gulf of Aqaba as part of Prof. HOTTINGER 's work on Foraminifera in 1971 and 1973 . His<br />

accidental death occurred in December 1975 before he could complete t he identification of his corals.

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!