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Report on the zoological collections made in the Indo-Pacific Ocean ...

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SPONGIIDA. 591bodies are c<strong>on</strong>stantly present, travex's<strong>in</strong>g <strong>the</strong> ma<strong>in</strong> mass of <strong>the</strong>skelet<strong>on</strong> ; <strong>the</strong>se fibres are, however, much less abundant than <strong>in</strong><strong>the</strong> orig<strong>in</strong>al specimen of Lamarck, and <strong>the</strong> wall of <strong>the</strong> sp<strong>on</strong>ge isth<strong>in</strong>ner. Abundant.Hah. Providence and Cerf Islands, Mascarenes, and Amirantogroup ; beach to 24 fms.Distributi<strong>on</strong>. " Mediterranean " (^Lamarck) ; Zanzibar (Hi/att).3. Hipposp<strong>on</strong>gia s<strong>in</strong>uosa.Sp<strong>on</strong>gia s<strong>in</strong>uosa, Pallas, Elench. Zooph. p. 394 ;Lamarck, Ann. Mus.Hist. Nat. XX. p. 371.p Sp<strong>on</strong>gia feuestrata, Lamarck, torn, cit, p. 374.Sp<strong>on</strong>gia lapidescens, subspecies mauritiana, Hyatt, Mem. Bost. Soc.ii. p. 528,Lamarck's and Pallas's S. s<strong>in</strong>uosa seem, by <strong>the</strong>ir descripti<strong>on</strong>s, tobe referable to a Hipposij<strong>on</strong>gia of which I describe two formsbelow. S. fenestrata, Lamarck, is probably a more sessile and <strong>in</strong>crust<strong>in</strong>gform of <strong>the</strong> same species. The questi<strong>on</strong> of identity is besetwith great difficulties, ow<strong>in</strong>g to <strong>the</strong> want of au<strong>the</strong>ntic specimens of<strong>the</strong> different species for reference. A S2)ecimen l<strong>on</strong>g c<strong>on</strong>ta<strong>in</strong>ed <strong>in</strong> <strong>the</strong>Nati<strong>on</strong>al collecti<strong>on</strong>, and labelled S. ma'andriformis or mceandr<strong>in</strong>iformis,differs from <strong>the</strong> form described below as var. mauritianama<strong>in</strong>lj' <strong>in</strong> its somewhat more slender fibre (•016-'045 millim. <strong>in</strong>thickness) ; but its history is unknown.AYith regard to Pallas's descripti<strong>on</strong>, I would remark (1) that <strong>the</strong>dry skelet<strong>on</strong> of our specimens is not tender ("tenera"), but hardand almost <strong>in</strong>compressible ; (2) it atta<strong>in</strong>s a vertical thickness of35 millim. ; (3) <strong>the</strong> cavities meander and anastomose, and are notmerely " obl<strong>on</strong>gte vel cotyloidese "; (4) <strong>the</strong> colour is a f<strong>in</strong>e amberyellow; (5) <strong>in</strong> var. mauritiana <strong>the</strong> fibres are <strong>on</strong>ly approximatelyparallel and perpendicular, except at <strong>the</strong> very surface.The term " surface nivellee " used by Lamarck <strong>in</strong> his descripti<strong>on</strong>of IS. fenestrata well expresses <strong>the</strong> appearance which <strong>the</strong> sp<strong>on</strong>gehas of hav<strong>in</strong>g been 'pared smooth, as <strong>in</strong> <strong>the</strong> sj)ccies i/. dcrasa. (seePart I., p. 382, of this Keport).It is easy to dist<strong>in</strong>guish am<strong>on</strong>g <strong>the</strong> specimens two varieties, ofwhich <strong>on</strong>e apparently corresp<strong>on</strong>ds to <strong>the</strong> more typical form of Hyatt'ssubspecies, and may <strong>the</strong>refore stand under that name, viz.Hipposp<strong>on</strong>gia s<strong>in</strong>uosa, var. mauritiana.The general form of <strong>the</strong> sp<strong>on</strong>ge is that of a low, horiz<strong>on</strong>tally extendedmass, apparently orig<strong>in</strong>ally attached by <strong>on</strong>e or more smallpo<strong>in</strong>ts ; it is about 35 millim. high, and throws out short subcyl<strong>in</strong>drical,term<strong>in</strong>ally-rounded lobes 25-35 millim. <strong>in</strong> diameter. Colour <strong>in</strong>macerated state bright amber-yellow. Diameter of <strong>the</strong> meander<strong>in</strong>gcanals of <strong>the</strong> skelet<strong>on</strong> 2-5 to 5 millim.The skelet<strong>on</strong> c<strong>on</strong>sists of a str<strong>on</strong>g horiz<strong>on</strong>tal system of l<strong>on</strong>g sec<strong>on</strong>daryfibres ly<strong>in</strong>g parallel to <strong>the</strong> surface, and of sliort stout, primary

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