254 Meyer—Lower Greensand Brachiopods. 
Terebratula oblonga, Sow.*—Occurring sparingly in the pebble- 
bed, but more frequently in the Bargate-stone near Guildford, in 
the form represented Pl. XI. figs. 12-14. 
T. Tornacensis, var. Roemeri, D’Archiac.—A few single valves 
from the pebble-bed near Guildford. 
T. Robertoni (?) D’ Archiae.—Several imperfect specimens, answer- 
ing most nearly to the description of 7. Robertoni, have been met 
with in the pebble-bed at Hurtmore near Godalming, and also near 
Guildford. See Pl. XII. figs. 10, 11. 
T. depressa (?), Lam.—Fragments of a large Terebratula, which 
may possibly represent 7. depressa, have been obtained from the 
pebble-bed near Godalming. The specimen represented on 
Pl. XII. figs. 15a, 6. is from the Lower Greensand of Shanklin. 
Waldheimia ‘tamarindus, Sow.—Occurring sparingly at Tewsley. 
At Hurtmore, SW. of Godalming, it occurs in the sand imme- 
diately beneath the pebble-bed. 
Rhynchonella latissima, Sow.—Single valves only, from the pebble- 
bed near Guildford ; rare. 
Rh. depressa (?), Sow.—Single valves only, Godalming and Guild- 
ford ; rare. 
Rh. Gibbsiana, Sow., var.—Single valves, Tewsley and Hurtmore, 
&c. 3 rare. 
Figures of several of the above-mentioned species are given in 
the accompanying Plates XI. and XII., in consequence of the 
infrequency of their occurrence in beds of undoubted Lower Green- 
sand. 
In the May Number of the ‘ Geologist’ (vol. vii. No. 77, p. 166), 
there was given a description of a new species of Tepebrceoue from 
the Bargate-stone, under the name of T. trifida, drawings of which 
were to have appeared in the following Number ; but, in conse- 
quence of the somewhat sudden discontinuance of that periodical, 
they were inadvertently omitted : these figures are therefore intro- 
duced on the present occasion. See Pl. XI. figs. 17-23. 
In the foregoing remarks mention has been made more 
especially of the pebble-bed of Godalming as a local deposit ; 
yet, though in one sense local, it should not properly be so 
considered; the same band of pebbly strata being more or less 
traceable in the Greensand along the whole of the North 
Downs,—as at Guildford, Dorking, Nutfield, and Sevenoaks ; 
it may also be observed at Folkestone and Shanklin ; in all 
these places holding exactly the same position in the series. 
So that, although perhaps in part a local, as well as a littoral, 
* Tregret that I am unable, partly for want of space, to enter into a minute 
comparison of the varieties of T. oblonga, some of which, as is shown by Mr. 
Davidson (Mon. Cret. Brach., pt. 2, pl. 2. figs, 29-32), and still more by M. 
D’Orbigny, differ widely from the typical form ; yet all, if I mistake not, within 
such limits as completely to separate them from Tercbratella Fitton described 
aboye, 
