264 HISTORICAL PALEONTOLOGY. 



Glabigerina, Rotalia (fig. 187), and Textularia — groups which 

 are likewise characteristic of the " 



Fig. 187. — Rotalia Boueana, 



Pacific Oceans at great depths. The flints of the Chalk also 

 commonly contain the shells of Foraminifera. The Upper 

 Greensand has yielded in considerable numbers the huge 

 Foraminife)-a described by Dr Carpenter under the name of 

 Faj'keria^ the spherical shells of which are composed of sand- 

 grains agglutinated together, and sometimes attain a diameter 

 of two and a quarter inches. The Cretaceous Sponges are 

 extremely numerous, and occur under a great number of varie- 

 ties of shape and structure ; but the two most characteristic 

 genera are Siphonia and Vetitriculites , both of which are ex- 

 clusively confined to strata of this age. The Siphonice. (fig. 

 188) consist of a pear-shaped, sometimes lobed head, supported 

 by a longer or shorter stem, which breaks up at its base into a 

 number of root-like processes of attachment. The water gained 

 access to the interior of the Sponge by a number of minute 

 openings covering the surface, and ultimately escaped by a 

 single, large, chimney-shaped aperture at the summit. In some 

 respects these sponges present a singular resemblance to the 

 beautiful '' Vitreous Sponges " {Holtenia or Fheronema) of the 

 deep Atlantic ; and, like these, they were probably denizens 

 of a deep sea. The Ventriculites of the Chalk (fig. 189) is, 

 however, a genus still more closely aUied to the wonderful 

 flinty Sponges, which have been shown, by the researches of 

 the Porcupine, Lightning, and Challenger expeditions, to live 

 half buried in the calcareous ooze of the abysses of our great 

 oceans. Many forms of this genus are .known, having " usu- 

 ally the form of graceful vases, tubes, or funnels, variously 

 ridged or grooved, or otherwise ornamented on the surface, 

 frequently expanded above into a cup-like lip, and continued 

 below into a bundle of fibrous roots. The minute structure of 

 these bodies shows an extremely delicate tracery of fine tubes, 

 sometimes empt}-, sometimes filled with loose calcareous mat- 



