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'Alert' 1881-2

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ECHINODERMATA, 125<br />

7. LincMa marmorata.<br />

Ophidiaster marmoratus, Michelin,Mag. Zuol. 1845, Zooph. p. 21, pi. 10.<br />

Liuckia marmorata, Perrier, p. 13o.<br />

If I am correct in referring to this species a series of specimens<br />

from Port Molle and Fitzroy Island, it will be easy to understand<br />

how it is that M. Michelin's species was never again recognized till<br />

the Paris Museum came into the possession of his type ;<br />

that would<br />

appear to be the only example that they possess, and, as M. Perrier<br />

points out, the " typo " is obviously young. The specimens before<br />

me are clearly enough all representatives of the same species ; but<br />

were any one of them described it is quite possible that from the<br />

description alone of that single specimen it would be easy to regard<br />

some others of the series as belonging to another form.<br />

In the first place, though all the specimens are provided with the<br />

intermediate plate that connects into a pentagon the terminal one of<br />

the " ranges de plaques qui occupe la ligne mediane dorsale de<br />

chaque bras," the extent to which this is evident varies a good deal,<br />

and one would hardly think it worthy of especial note in the largest<br />

example were not attention directed to it by the better-marked<br />

characters of some of the smaller. Secondly, the smallest specimen<br />

has the dorsal plates covered with coarse granulations ; of some of<br />

these, at any rate, it would be appropriate to say (again quoting<br />

Perrier) " les granules voisins de leur centre sent un peu plus gros<br />

que les autres;" on the other hand, one, two, or more granules<br />

near the centre acquire, in the larger specimens, a much greater<br />

predominance, and give a somewhat different appearance to the<br />

creature ; in the largest specimen these again have disappeared, and<br />

the whole surface of the plates is more uniformly granular. Thirdly,<br />

the dorsal plates may lose the regularity of outline which is so well<br />

marked (if not exaggerated ?) in Michelin's figure, and which is<br />

expressed by M. Perrier in the words " sensiblement carree," and<br />

become narrower at the angles at which the pores are placed ; this<br />

is perhaps due to the greater development in the number of pores,<br />

of which as many as seven may in some cases be found within the<br />

limits of one area. Lastly, it is only in the smallest specimens that<br />

we find a double row of tubercles fringing the adambulacral spines ;<br />

in aU the larger specimens the row is single, or, in other words, one<br />

row of tubercles ceases to grow proportionately, and becomes obscured<br />

in the general granulation of the actinal surface.<br />

The only considerable point of difference between these specimens<br />

and that figured by Michelin lies in the remarkable coloration of<br />

his specimen ; if, however, M. Desjardin's example from the island<br />

of Mauritius was immediately dried, it might have retained its colour :<br />

while Dr. Coppinger's specimens, which were placed in spirit, might<br />

very possibly have had part of their colouring-matter dissolved out.<br />

The largest example has E equal to 50 miUim.<br />

Prince of Wales Channel, 7 fms.

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