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97<br />

1918. VAUGHAN. 191: pI. 84/ 3.3 • .<br />

1941 , CROSSLAND, 21 ; pis. 1- 3, 4 (upper and lower fig.; pI. 4, lower fig .. is not P. lutea, it is<br />

the same picture as pI. 3, lower fig., and repr~nts P. so/ida No. 21).<br />

1948. CROSSLAND. 202 : pI. 14 (upp« fig.).<br />

1952. CROSSLAND. 242.<br />

1954. ROSSI . 55 .<br />

1967. SCHEER. 428.<br />

1974. MERGNER & SCHUHMACHER. 265.<br />

1974. SCHEER & PILLAI. 42.<br />

1976. PILLAI & SC HEER. 50.<br />

1980. HEAD. 150. 454.<br />

a/v,o/ala 1860. MI LNE EDWA RDS (& HAI~IE) . 178.<br />

1879. KLUNZINGER 2. 43: pI. 5/20.<br />

1971 . LOVA & SL08DDKIN. 124.<br />

ar~"o$ll 1797. ESPER, 80; pI. 65.<br />

1860. MILN E EDWARDS (& HAIME). 180.<br />

1879. KLUNZINGER 2. 43.<br />

1948, CROSSLAND, 202; pis. 11 (lower fig.); 14 (lower fig.) ,<br />

cong/ort/vala 1834 . EliRENBERG, 341 (No. 937 in Berlin Musr:um) .<br />

(non co nglomerata 1846 . DANA).<br />

1860. MILNE EDWARDS (& HAIME). 179.<br />

1888. FAUROT. 119.<br />

f,ago$4 1 1846. DANA. 536: pI. 55 /9. 9 •.<br />

1954. WELLS. 454; pI. 171 (synonymy),<br />

mu"ayens;s 1918. VAUGHAN. 192; pI. 84/4, 4a, b. S.<br />

R,dS.a J 1905 . BERNARD. 236:pI.1l17.<br />

Red Sea 8 1905. BERNARD, 242.<br />

CROSSLAND (1941) has discussed FORSKAL 'S types, and VAUGHAN (1918) has given a good description<br />

of this species. We mention here only the skeletal variation displayed in the present material.<br />

The corallum is always massive. The surface is smooth or with gibbosities or may develop lobulations.<br />

The calices are polygonal, deep or very shallow. In polygonal calices the wall is thin. But in many cases<br />

the wall is thickened and the calices are rounded as seen in P. mUrTayensis.<br />

When the septal and mural elements are thickened they display gTanulations.<br />

Pali 4 to 5, moderately developed or not visible. But in some rounded shallow calices five pali are<br />

very conspicuous along with the septal denticles between them and the wall.<br />

Columella mostly a single style, but in some cases it is represented by a compact mass incorporating<br />

the septal ends.<br />

M a terial :<br />

Gulf of Aqaba :<br />

I orthern R. S.:<br />

Central R. S.:<br />

Jerus. SLR 650- 2 (Marsa Abu Zabad).<br />

T. Aviv NS 247 , 6108 (Eilat).<br />

Basel PW 73 SOl (Eilat); 73 659, 660, 693 , 706 (EI Kura).<br />

HLM EC 455 , 456, 457 (Eilat).<br />

USNM Wa 52 (Ghardaqa).<br />

HLM X2 : 2-7 (Guballsl.).<br />

479 (Ras Abu Suma); 64, 65 (Koseir, duplicates from KLUNZINGER).<br />

EC<br />

P. Sud. Sa 4 (Sanganeb R. ).<br />

HLM RM 18 , 11 7 (Wingate R.).<br />

Southern R. S.: HLM EC 368, 369 , 370,371 , 374 (Massawa).<br />

Di s t rib uti 0 n : Red Sea ; Zanzibar; Natal; Madagascar; Seychelles; Reunion; Mauritius; Maldives;<br />

Lakshadweep; South India; Sri Lanka ; Andaman and Nicobar Isis.; Mergui Archipelago; COCOS-Keeling<br />

IsIs. , Philippines; Great Barrier Reef; MarshaIllsls.<br />

Rem a rk s : BER ARD (1905) has already pointed out the similarity of P. alveolata by KLUNZING ER<br />

to P. solida. We have not examined MILNE EDWARDS & HAIME 's type of P. alveolata. However, the<br />

specimens described by KLUNZINGER (1879) are not separable from P. solido.<br />

P. mUrTayensis VAUGHA is only a skeletal variation of the present species. Some of our specimens<br />

certainly show gradation towards P. mUrTayensis.<br />

P. fragosa DANA may also belong to a variant of P. solido , though we have no convincing proof for<br />

such a conclusion.

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