514 
GASTEROPODA OF THE INFERIOR OOLITE. 
Page 161, line 10, for Minchinhamptom read -ton. 
180, ,, 11, for Normanniana vead Normaniana. 
12, for Normannianum read Normanianum. 
181, ,, 7, for Peristone read Peristome. 
» 9 24, for 418 read 419. 
202, ,, 3, for fig. 6 read figs. 6c and 7. 
203, ,, 32, for posterior read anterior. 
205, ,, 7, for pl. viii read pl. vii. 
226, ,, 24, for subtruntrutana read subbruntrutana. 
231, ,, ,11, for fig. 13 read fig. 15. 
236, ,, 4, for p. 812 read p. 810. 
» » 16, for Pietet read Pictet. 
238, ,, 22, for Buckholdt read Buckholt. 
240, ,, 9, for Deslongchamp’s read Deslongchamps’. 
241, lines 30 and 34, for Normanniana read Normaniana. 
247, line 25, fur note p. 152, 1829, 1st edit., read p. 123, 1835, 2nd edit. 
261, ,, 24, for Gasteropoden read Gastropoden: and for Brannen read Braunen. 
266, ,, 6,for subcaniculata read subcanaliculata. 
272, ,, 5, for Rissotna read Rissoa. 
» 5 6, for — read Rissorna. 
275, heading, for Rissorna read AMBERLEYA, 
336, line 4, for Pea-grit of Crickley read Oolite-marl, Swifts’ Hill. 
369, ,, 2, for “ Base-bed read “ Base-bed.” 
389, ,, 15, for columela read columella. 
390, beginning of line 26, delete the. 
394, line 12, for inner read outer. 
EXPLANATION OF PLATES. 
Plate II, figs. 6 a, 6b, for fusiforme read fusiformis. 
Plate IV, fig. 12, for Whidborne collection read Woodwardian Museum. 
Plate XI, fig. 9, for Nornanniana read Normaniana. 
Plate XIII, line 12, for fig. 6 read fig. 6c. 
Plate XVI, fig. 7. This should be represented as x 13. 
Plate XXVIII, figs. 11 a—e, for Pea-grit, Crickley, read Oolite-marl, Swifts’ Hill. 
Plate XXX, fig. 14, for pulchior read pulchrior. 
the 
POSTSCRIPT. 
Ty 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. 
case with regard to some specimens obtained in 1887 from the Yeovil sands on 
coast, most probably from the Dumortieria-beds and other horizons of the 
Jurensis-zone. 
This is notably the 
