SUB-CLASS I 



SELACHII 



17 



of the Leptocarclii {Amphioxits) and Cydostomi (lampreys and hag-fishes) as 



independent classes equivalent to that of the fishes, ^^ 



and in the closer union of the ganoids and bony fishes, 



which are frequently grouped under the common 



denomination of Teleostomi. The class of fishes in its 



restricted sense thus comprises the four still-existing 



sub-classes of Selachii, Dipnoi, Ganoidei, and Teleostei ; 



while to these must be added the extinct sub-classes 



of Ostracodermi (or Ostracophori) and Arthrodira, which 



are restricted to the Palaeozoic. 



No fossil remains of Leptocardii are known. It 

 must also be remarked that there is no satisfactory 

 evidence of extinct representatives of the Cydostomi 

 or Marsipohrandiii. Certain annelid jaws from the 

 Palaeozoic formations, known as Conodonts, were once 

 erroneously supposed to be teeth of this class (see vol. i. 

 p. 255). The problematical organism from the Old 

 Eed Sandstone of Achanarras, Caithness, named Palaeo- 

 spondylus gunni'^ by Traquair (Fig. 30), is likewise very 

 doubtfully placed here. The largest specimens of this 

 form do not exceed 0*05 m. in length. The skull 

 terminates in front in a ring of calcified cirri [dx, l.c, 

 v.c), which surround a large bilaterally symmetrical 

 orifice (h). Behind the skull there extends backwards 

 a pair of elongated cartilages (x), usually lying in the paiaeospold'yiS' gunm, Tm- 

 fossil parallel with the vertebral column. There are quair. Lower oici Red Sand- 



,-^, .,, p, ,. ., stone ; Caitlmess. a, Separate 



vertebral centra m the form of broad rmgs ■ m the small lobe ; 6, Anterior depres- 

 abdominal region these bear short and stout neural p °els1on'^or fenekm ;°clc™orM 

 spines, but no ribs; in the caudal region the neural cirri ; lc, Lateral cirri ; «,Sup- 



i ' . ^ o . posed narial opening; p. a, Para- 



and haemal spines are very slender, while the former chordai portion of skuii; t.ji, 



T .1 ji 1 ,, 1 T J- ,1 T 1 , • Trabeculo - palatine portion of 



are longer than the latter and distinctly dichotomise skuii; t'.c.ventrai cirri ; x,Pro- 

 at the distal end. 



paired limbs. 



There is no undoubted evidence of v3'|a?tw1'rTc?T"a°rf ^'^""^ ^^^^^ 



Sub-Class 1. SELACHII. Cuvier. 



(Elasmohrandiii, Bonap. ; Chondropterygii, Giinther ; Placoidei, Ag.) 



Eiidoskeleton cartilaginous; exoskeleton, when present, strudurally identical 

 with the teeth (placoid scales). Usually five (rarely six or seven) pairs of branchicd 

 arches, the clefts exposed or covered only by a flap of skin, withoid opercidum. In 

 the living forms — op)tic nerves not decussating but forming a chiasma ; bidbus 

 arteriosus of the heart with two, -three or more series of valves ; air-bladder absent ; 

 intestine with a spiral valve ; ovaries with few large ova. 



The unsegmented cartilaginous cranium of the Selachii is more or less 

 imperfectly hardened with polygonal granules of phosphate of lime ; but the 

 vertebrae are very variously calcified, can thus be readily preserved in a fossil 

 state, and, according to Hasse, display features of special importance for the 



^ Jjean, B., The Devonian "Lamprey" Palaeospondylus gunni, Traqnair (Mem. N.Y. Acad. Sci. 

 vol. II. pt. 1), 1900. Bibliography. — Traquair, R. H., A still further contribution to our knowledge 

 of Palaeospondylus (Proc. Roy. Phys. Soc. Ediub. vol. XII.), 1894. 



VOL. II C 



