192 



ACANTHODII 



Family DIPLACANTHIDAE. The spines are much developed, may be 

 serrated and grooved ; they usually occur between the pectoral' and 

 pelvic fins. In Diplacantlms there are two pectoral spines on each side 

 (Fig. 163). There are two dorsal fins, and usually clavicular plates. 



Diplacanthus, Ag. (Fig. 156, A); Parents, Ag. ; Mesacanthus (Fig. 

 164, B) ; Ischnacanthus, Eg.; Devonian, Scotland. Climatius, Ag. 

 (Fig. 164, A); Devonian, Scotland and England. 



Family ACANTHODIDAE. The intermediate spines are vestigial or 

 absent ; the remaining spines are more slender ; there is only a single 



FIG. 104. 



A, CUmatius scutiger, Eg., Lower Old Red Sandstone, Forfarshire ; B, Mesacanthus Mitchell!, 

 Eg., ibid. ; C, Acanthodes sulcatus, Ag., Lower Carboniferous, Edinburgh ; D, Acanthodes (tracilis, 

 Roemer, Lower Permian, Bohemia ; restored outlines. (A after A. S. Woodward, B and C 

 after Traquair, D after Fritsch, from A. 8. Woodward, Proc. Geol. Assoc.) a, anal, d, dorsal, 

 p, pectoral, and v, pelvic fins ; i.sp, paired ventral spines. 



dorsal fin ; and the pelvic fin tends to dwindle in size as the pectoral 

 becomes larger. 



Acanthodes (Acanthoessus), Ag. ; Devonian, Europe and N. America 

 (Fig. 164, C and D) ; Carboniferous and Permian, Europe. Cheir acanthus, 

 Ag. (Fig. 158); Devonian, Scotland. Acanthodojisis, H. and A.; Car- 

 boniferous, Great Britain. Protacanthodes, Fr. ; Permian, Europe. 



INCERTAE SEDIS. 



Family GYRACANTHIDAE. Isolated large spines and small tubercles, 

 found in Palaeozoic deposits, and to which the names Gymcanthus and 

 Oracanthus have been given, have long been a puzzle to palaeontologists. 

 Quite recently, A. S. Woodward has shown that they belong to a fish 



