THE UPPER SILURIAN PERIOD. 



I2 9 



species of Platyostoma (fig. 72, K) also belong to the same 

 family ; and the entire group is continued throughout the 

 Devonian into the Carboniferous. Amongst other well-known 

 Upper Silurian Gasteropods are species of the genera Holopea 



Fig. 72. Upper Silurian Gasteropods. a, Platyceras ventricosum, Lower He'der- 

 berg, America ; b, Euomphalus discors, Wenlock, Britain ; c, Holopella. obsoleta, Lud- 

 low, Britain ; d, Platyschisma helicites. Upper Ludlow, Britain ; e, Holopella gracilior, 

 Wenlock, Britain;/, Platyceras mnltisinttatum, Lower Helderberg, America; g, Holo- 

 pea. subconica, Lower Helderberg, America; h, h', Platyostoma. Niagarense, Niagara 

 Group, America. (After Hall, M'Coy, and Salter.) 



(fig. 72, g), Holopella (fig. 72, c), Platyschisna (fig. 72, d\ 

 Cydonema, Pleurotomaria, Murchisonia, Trochoncma, &c. The 

 oceanic Univalves (Heteropods) are rep- 

 resented mainly by species of Bellero- 

 phon ; and the Winged Snails, or Ptcro- 

 pods, can still boast of the gigantic Thecce 

 and Comtlarice, which characterise yet 

 older deposits. The commonest genus 

 of Ptcropoda, however, is Te?itaailites (fig. 

 73), which clearly belongs here, though 

 it has commonly been regarded as the 

 tube of an Annelide. The shell in this 

 group is a conical tube, usually adorned 

 with prominent transverse rings, and 

 often with finer transverse or longitudi- 

 nal striae as well ; and many beds of the 

 Upper Silurian exhibit myriads of such tubes scattered promis- 

 cuously over their surfaces. 



