514 GASTEROPODA OF THE INFERIOR OOLITE. 



Page 161, line 10, for Minchinhamptom read -ton. 

 „ 180, „ 11,/or Normanniana ?'ea<? Normaniana. 

 „ ,, „ 12, ybr Normannianum rearf Normanianutn. 



,, 181, „ 7, for Peristone read Peristome. 

 „ „ „ 27,for 4:18 read 4<19. 



„ 202, „ 3, for fig. 6 read figs. 6 c and 7. 



„ 203, „ 32, /or posterior rearf anterior. 



„ 205, „ 7, for pi. viii read pi. vii. 



,, 226, „ 24, for subtruntrutana read subbruntrutana. 



„ 231, „ ll,/o?- fig. 13 rea^ fig. 15. 



„ 236, „ 4, /or p. 812 rea.'/ p. 810. 

 „ ,, „ 16, /or Pietet read Pictet. 



„ 238, „ 22,/or Buckholdt reac^Buckholt. 



„ 240, „ 9, /or Deslongchanip's rearf Deslongchamps'. 



„ 241, lines 30 and 34, for Normanniana read Normaniana. 



„ 247, line 25, /;r note p. 152, 1829, 1st edit., read p. 123, 1835, 2nd edit. 



„ 261, „ 24, /or Gasteropoden read Gastropoden : and /or Brannen read Braunen. 



„ 266, „ 6, for subcaniculata read subcanalicvlata. 



„ 272, ,, 5,/or EissoiNA rearf RissOA. 

 ,, ,, ,, 6, /or — reac? EiSSOlNA. 



„ 275, heading, /or Eissoina read Ambebleya. 



„ 336, line 4i,for Pea-grit of Crickley read Oolite-marl, Swifts' Hill. 



„ 369, „ 2, /or "Base-bed rearf "Base-bed." 



„ 389, „ 15, /or columela rea<Z columella. 



,, 390, beginning of line 26, delete the. 



,, 394, line 12, /or inner reffc? outer. 



EXPLANATION OF PLATES. 



Plate II, figs. 6 a, 6 6, ^or fusiforme Tea.dfusiformis. 



Plate IV, fig. 12, for Whidborne collection read Woodwardian Museum. 



Plate XI, fig. 9, for Norn.anniana read Normaniana. 



Plate XIII, line 12, /or fig. 6 read fig. 6 c. 



Plate XVI, fig. 7. This should be represented as x li. 



Plate XXVIII, figs. 11a — c,for Pea-grit, Cricklej, read Oolite-marl, Swifts' Hill. 



Plate XXX, fig. 14, for pu/chior re&d pule krior. 



POSTSCRIPT. 



In addition to the species described and figured in the foregoing Monograph, 

 there are several others in my own collection which I have not ventured to bring 

 forward, in most cases because of their imperfect condition. This is notably tbe 

 case with regard to some specimens obtained in 1887 from the Yeovil sands on 

 the coast, most probably from the Dmnortieria-heds and other horizons of the 

 Jurensis-zone. 



