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

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SPONGIIDA. 379and n<strong>on</strong>-rectangular arrangement with those of Eusp<strong>on</strong>gia,, and, asstated already, foreign bodies are <strong>the</strong> excepti<strong>on</strong> even <strong>in</strong> <strong>the</strong> surfacetufts; <strong>the</strong> diameter of <strong>the</strong> fibres is "4 to -7 millim. (Ehlcrs gives -5to '8), except <strong>in</strong> <strong>the</strong> delicate Ditela-netw ork of <strong>the</strong> surface and <strong>in</strong>terstices,where it is •0085 to '022 millim. Ehlers says that <strong>the</strong>fibres c<strong>on</strong>ta<strong>in</strong> " <strong>in</strong> der Axe vere<strong>in</strong>zelte sehr di<strong>in</strong>ne spitz-spitzeNadcln (0-1 mm. lang, -006 mm. breit) welche nur <strong>in</strong> den kegelformigenZuspitzungen an der Oberfiiiche des Schwammes etwasdichter gehiiuft s<strong>in</strong>d." Their occurrence s<strong>in</strong>gly (" vere<strong>in</strong>zelte ") andnot <strong>in</strong> l<strong>on</strong>gitud<strong>in</strong>al series, if that is what is implied, is not <strong>the</strong> usualmode of occurrence of spicules <strong>in</strong> <strong>the</strong> fibres of Chal<strong>in</strong>idas (though itoccurs occasi<strong>on</strong>ally <strong>in</strong> some fibres of Cl(idochal<strong>in</strong>a'), nor is <strong>the</strong>irgreater abundance <strong>in</strong> <strong>the</strong> surface-tufts, so far as I know, usual <strong>in</strong>this family. These statements appear to me to po<strong>in</strong>t towards <strong>the</strong>true explanati<strong>on</strong> of <strong>the</strong> nature of <strong>the</strong>se spicules, viz. that <strong>the</strong>y areforeign, and taken <strong>in</strong> (as is usually <strong>the</strong> case <strong>in</strong> Easjy<strong>on</strong>gki) as foreignbodies <strong>in</strong> small quantities <strong>in</strong>to <strong>the</strong> surface-tufts. A re-exam<strong>in</strong>ati<strong>on</strong>of <strong>the</strong> orig<strong>in</strong>al specimen is desirable. If Esper's species is a Chal<strong>in</strong>id,<strong>the</strong>n <strong>the</strong> present species is a Easp<strong>on</strong>gia-\sovLioY])\\ oi a Chal<strong>in</strong>id form,like <strong>the</strong> Chal<strong>in</strong>opsid representatives of Siphoiwchal<strong>in</strong>a and Pachi/cha-T-<strong>in</strong>a which Schmidt (Sp<strong>on</strong>g. Meerbusen Mexico, p. 80) has describedas Siph<strong>on</strong>oGlial<strong>in</strong>opsis and Puchijchaliiiopsis.I have satisfied myself that ano<strong>the</strong>r explanati<strong>on</strong> which might besuggested, viz. <strong>the</strong> dissoluti<strong>on</strong> of <strong>the</strong> spicules from <strong>the</strong> fibre of <strong>the</strong>Sp<strong>on</strong>ge (as <strong>in</strong> Carter's Aplij^<strong>in</strong>a chal<strong>in</strong>oides, afterwards found tobe a true Chal<strong>in</strong>id), cannot apply to this case. I have studied<strong>the</strong> fibre very carefully, with and without <strong>the</strong> aid of potash, and canassert that it never possessed "proper" spicules.The respective localities (Cape and Torres Straits) perhaps c<strong>on</strong>stituterelative objecti<strong>on</strong>s to <strong>the</strong> specific identity of <strong>the</strong> present withEsper's species.Bab. West Island, Torres Straits.Distributi<strong>on</strong>. Esper's species is from <strong>the</strong> Cape of Good Hope.3. Eusp<strong>on</strong>gia offic<strong>in</strong>alis, L<strong>in</strong>ne, var. cavernosa. (Plate XLI. fig. g.)From a depth of 10 fathoms <strong>in</strong> Torres Straits we have a smallturnip-like sp<strong>on</strong>ge, unfortunately preserved <strong>on</strong>ly <strong>in</strong> <strong>the</strong> dry state,which to <strong>the</strong> unaided eye presents <strong>the</strong> general appearance of a RhizocJmlijia JistuJosa, with several tubular processes, 10 to 35 millim.l<strong>on</strong>g and 8 to 10 millim. <strong>in</strong> greatest median diameter, <strong>on</strong> its uppersurface ; <strong>the</strong>se processes are, however, ragged <strong>in</strong> outl<strong>in</strong>e at <strong>the</strong>irdistal ends, and evidently <strong>in</strong> life opened through <strong>the</strong> fr<strong>in</strong>ged aperture,now obscured by <strong>the</strong> fall<strong>in</strong>g toge<strong>the</strong>r of <strong>the</strong> sides ; <strong>the</strong>ir sides are<strong>in</strong> some cases fenesti'ate. The body of <strong>the</strong> sp<strong>on</strong>ge is rudely globular,and is drawn iip above <strong>in</strong>to m<strong>on</strong>ticular elevati<strong>on</strong>s, which are term<strong>in</strong>atedby <strong>the</strong> tubes just described ; <strong>the</strong> base is somewhat flattened,and has apparently been attached at three po<strong>in</strong>ts to rock or gravel at<strong>the</strong> sea-bottom, porti<strong>on</strong>s of which are still left imbedded <strong>in</strong> <strong>the</strong> sp<strong>on</strong>ge.The chief horiz<strong>on</strong>tal diameters of <strong>the</strong> sp<strong>on</strong>ge-body are 45 and 55

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