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

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448 COLLECTIONS FROM MELANESIA.apparently partly formed by upgrowths from short stems placedbeside it, which, though now s<strong>in</strong>gle, appears to have been orig<strong>in</strong>allycompound also ; <strong>on</strong>e surface of this expansi<strong>on</strong> is almost level, buth<strong>on</strong>eycombed densely with open<strong>in</strong>gs with rounded edges, vary<strong>in</strong>gfrom 1 to 4 millira. iu diameter ; <strong>the</strong> o<strong>the</strong>r surface is broken up <strong>in</strong>toseven more or less pr<strong>on</strong>ounced vertical ridges, irregular and frequently<strong>in</strong>terrupted, 3 to 10 millim. <strong>in</strong> height ; this surface and itsridges are also str<strong>on</strong>gly h<strong>on</strong>eycombed, and between <strong>the</strong> open<strong>in</strong>gsusually project po<strong>in</strong>ts and ridges of sp<strong>on</strong>ge-tissue. It measures130 millim. (5g <strong>in</strong>ches) <strong>in</strong> breath, 120 millim. (4^ <strong>in</strong>ches) <strong>in</strong> height.The sec<strong>on</strong>d specimen is strap-shaped, 24 to 30 millim. across, somewhatabruptly bent at <strong>on</strong>e po<strong>in</strong>t, and term<strong>in</strong>ated by two smaU lobes ;like <strong>the</strong> o<strong>the</strong>r specimen, <strong>on</strong>e surface is comparatively level and ish<strong>on</strong>eycombed ra<strong>the</strong>r m<strong>in</strong>utely (open<strong>in</strong>gs "3 to -5 millim. <strong>in</strong> diameter),while <strong>the</strong> o<strong>the</strong>r is rugose, from <strong>the</strong> presence of several demi-canals,about 2 to 4 millim. across, which run from <strong>the</strong> middle to <strong>the</strong> marg<strong>in</strong>of <strong>the</strong> fr<strong>on</strong>d ; <strong>the</strong> surface between <strong>the</strong>m is m<strong>in</strong>utely h<strong>on</strong>eycombed anddrawn up <strong>in</strong>to a few sharp po<strong>in</strong>ts and ridges. The colour is darkishgrey, vary<strong>in</strong>g to greenish iu both specimens. The spiculati<strong>on</strong> isessentially that of <strong>the</strong> above-menti<strong>on</strong>ed form of C. re<strong>in</strong>ivardti, but<strong>the</strong> skelet<strong>on</strong> smooth acuate is <strong>on</strong>ly '0003 to '0079 millim. <strong>in</strong> diameter,and <strong>the</strong> short, stouter, smooth acuate is want<strong>in</strong>g ; this slightdifference <strong>in</strong> spiculati<strong>on</strong> appears to justify <strong>the</strong> separati<strong>on</strong> of thisform under a dist<strong>in</strong>ct varietal name. It is perhaps as nearly relatedto <strong>the</strong> orig<strong>in</strong>al form as <strong>the</strong> first-menti<strong>on</strong>ed specimens. The remarkablefan-shaped specimen appears (hav<strong>in</strong>g regard to <strong>the</strong> multiplecharacter of its base) to be <strong>made</strong> up of several " pers<strong>on</strong>s " whichhave united to form a s<strong>in</strong>gle symmetrical-fr<strong>on</strong>d.Ilab. Bird Island, N.E. Australia, coral-reef.78. Clathria fr<strong>on</strong>difera.(Plate XLII. fig. i ; and Part II. of this Ileport, Plate LIII. fig. J.)Halich<strong>on</strong>dria fr<strong>on</strong>difera, Boiverbcuik, Proc. Zool. Soc. 1875, p. 2S8.Amphilectus froudifer, Vosmaer, Notes Roy. Mus. Ne<strong>the</strong>rl. ii. p. 115.A very comm<strong>on</strong> species, especially <strong>in</strong> Torres Straits. At firstI was <strong>in</strong>cl<strong>in</strong>ed to separate <strong>the</strong> specimens from Bowerbank'sspecies <strong>on</strong> account of <strong>the</strong> greater development of cerat<strong>in</strong>ous substance<strong>in</strong>vest<strong>in</strong>g <strong>the</strong> l<strong>in</strong>es of skelet<strong>on</strong>-spicules. In <strong>the</strong> Australianspecimens this occupies from half to two thirds of <strong>the</strong> diameter of<strong>the</strong> fibres, while <strong>in</strong> <strong>the</strong> type specimen from <strong>the</strong> Straits of Malaccaits place is often almost entirely taken by spicules, and extends tohalf <strong>the</strong> diameter of <strong>the</strong> fibre <strong>on</strong>ly <strong>in</strong> some cases. The c<strong>on</strong>sistencyof <strong>the</strong> sp<strong>on</strong>ge is hence much tougher and more elastic <strong>in</strong> <strong>the</strong>Australian specimens. The ma<strong>in</strong> skelet<strong>on</strong>-spicules are much stouter<strong>in</strong> <strong>the</strong> Malacca specimens.Dr. Bowerbank has omitted to describe a very f<strong>in</strong>e tricurvate fleshspiculowhich occurs both <strong>in</strong> his specimens and <strong>in</strong> <strong>the</strong> present <strong>on</strong>es.His descripti<strong>on</strong> is also mislead<strong>in</strong>g <strong>in</strong> not stat<strong>in</strong>g, what his own typespecimen satisfactorily exhibits, and what <strong>the</strong> Australian examples

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