The Cambridge natural history, Vol. 01 (of 10)Hickson, Sydney J. (Sydney John)
Science
The Cambridge natural history, Vol. 01 (of 10)
Hickson, Sydney J. (Sydney John)
Animals
_Lelapia australis_, a recent species, should probably be placed here as
the sole living representative. Dendy has shown[223] that this remarkable
species has a skeleton of the same fibrous character as is found in typical
Dialytinae, and that the triradiate spicules in the fibres undergo a
modification into the "tuning-fork" type (Fig. 86, C), to enable them to be
compacted into smooth fibres. {193}"Tuning-forks," though not exclusively
confined to Pharetronids, are yet very characteristic of them.
[Illustration: FIG. 86.—Portions of the skeleton of _Petrostroma schulzei._
A, Framework with ensheathing pellicle; B, quadriradiate spicules with
laterally fused rays; C, a "tuning-fork." (After Doederlein.)]
II. LITHONINAE.—The main skeletal framework is formed of spicules fused
together, and is covered by a cortex containing free spicules.
[Illustration: FIG. 87.—A spicule from the skeleton framework of
_Plectroninia_, showing the terminally expanded rays. (After Hinde.)]
The sub-family contains only one living genus and a few recently described
fossil forms. _Petrostroma schulzei_[224] lives in shallow water near
Japan; _Plectroninia halli_[225] and _Bactronella_ were found in Eocene
beds of Victoria; _Porosphaera_[226] long known from the Chalk of England
and of the Continent, has recently been shown by Hinde[226] to be nearly
allied to _Plectroninia_; finally, _Plectinia_[227] is a genus erected by
Počta for a sponge from Cenomanian beds of Bohemia. Doederlein, in 1896,
expressed his opinion that fossil representatives of Lithoninae would most
surely be discovered. The fused spicules are equiangular quadriradiates;
they are united in _Petrostroma_ by lateral fusion of the rays, in
_Plectroninia_ (Fig. 87) and _Porosphaera_ by {194}fusion of apposed
terminal flat expansions of the rays, and in some, possibly all, genera a
continuous deposit of calcium carbonate ensheaths the spicular reticulum.
Thus they recall the formation of the skeleton on the one hand of the
Lithistida and on the other of the Dictyonine Hexactinellida (see pp. 202,
211). "Tuning-forks" may occur in the dermal membrane.
[Illustration: FIG. 88.—_Astrosclera willeyana_, Lister. A, the Sponge, ×
about 3. _p_, The ostia on its distal surface. B, a portion of the skeleton
showing four polyhedra with radiating crystalline fibres. C, an ostium; the
surrounding tissue contains young stages of polyhedra. (After Lister.)]
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