THE
MINERAL CONCHOLOGY
OF
GREAT BRITAIN;
OR
COLOURED FIGURES AND DESCRIPTIONS
OF THOSE
REMAINS OF TESTACEOUS ANIMALS
OR
WHICH HAYE BEEN PEESERVEB AT VARIOUS TIMES AND DEPTHS
IN
THE EARTH.
By JAMES SOWERBY, F.L.S.
G.S. W.S.
HONORARY MEMBER OF THE PHYSICAL SOCIETY OF GOTTINGEN, OF
THE SOCIETY OF JENA, &C.
AUTHOR OF BRITISH MINERALOGY, EXOTIC MINERALOGY,
TISH MISCELLANY, ENGLISH FUNGI, A BOTANICAL
DRAWING BOOK, AND A NEW ELUCIDATION
OF COLOURS
BRI-
;
DESIGNER OF ENGUSH BOTANY,
^e.
Many, O Lord my God, are thy wonderful works which thou hast done;
they cannot be reckoned up in order to thee: if I would declare and speak
of them, they are more than can be numbered.
Psalm
VOL.
xl. 5.
III.
LONDON:
Printed by
And
W. ARDING,
21,
Old Boswell Court, Carey
Street.
by the Author, J. Sowerby, No. 2, Mead Place, Lambeth;
Longman and Co. and Sherwood and Co. Paternoster Row, &c.
sold
MDCCCXXL
1
PECTEN
cornea.
TAB. CCIY.
Spec. Char.
Orbicular,
much
nearly equal
ears small,
depressed, smooth
•
*
two obtuse teeth
near the ears within each valve.
-A.
THIN fragile
shell
whose Talves are very nearly
being both of them very
acute
;
flat
and shining
the ears prominent and well defined
of each within the valves
is
:
;
alike^
the beak
is
at the base
an obloug blunt tooth
slight difference observable in the relative position
these teeth points out the two valves most readily.
:
a
of
Well
preserved individuals retain some traces of the original
markings
like
such are of a deep brown colour with a horn-
;
transparency on the sides, and of an opaque pale
brown from
the front to the beak, near which the colours
are very distinct
:
other specimens are altogether of a
pale brown colour, these are the most tender.
Found
Blue 3Iarle stratum below high water
in Hampshire.
It has much affinity with Pecten Pleurouectes, but is more slender, and
in the
mark, at Stubbington,
otherways distinct.
difficult to
preserve
Mr. Holloways
such as
Perfect specimens are very rare, and
;
I
am
therefore
much
oblisred to
for the pains he has taken to procure
exliibit clearly all the characters.
me
s
PECTEN
obscura.
TAB. CCV.— F/g-.
Spec.
Sub-orbicular, depressed, with oblongitudinal rugse upon the
Char.
arched
scure
surface
Somewhat
1.
;
ears large.
longer than wide
:
the surface
is
dull,
almost
furrows.
has some indications of diverging
smooth but it
The edge is thick.
of Stonesfield,
Occurs upon the sandy Limestone slate
to me long
forwarded
near Oxford. My specimen was
;
since by Dr. Williams.
PECTEN
Tx\B.
lens.
CCV.— Figs.
2
and
3.
Orbicular, convex; surface marked
diverging arched striae; strise deeply
Spec. Char.
wilh
punctured.
Nearly
shell
near the beaks; t!ie
remains are much broken
lenticular, but thickest
seems to be tender, as
its
my specimens.
the ears are not perfect in either of
produce of t'ue forest marble near Oxford.
A
PECTEN
laminata.
TAB. CCY.-^Fig,
Char.
Spec.
arched, diverging
striee
equal
A HE
Suborbicular^
striae
;
4.
depressed^
striated;
ears triangular^ un-
:
the largest plaited.
are slij^htly undulated; to the naked eye they
appear smooth, but when carefully examined with a
lense,
plaits
minute lines may be traced across them. The
upon the ear form a strong character, whence the
name.
In shelly Limestone (Cornbrash)
Chatley Lodge,
at
in Somersetshire.
PECTEN
TAB.
Spec. Char.
arcuata.
CCV— Figs.
Orbicular,
:
ears large
;
7.
with arched
upon the
stride
sur-
the side beneath the largest
arched.
is
A. SMALL
shell, prettily
marked with arched,
sometimes forked farrows.
largest
and
depressed,
punctured and diverging
face
5
is
quadrangular
;
The
;
the
they are both punctured.
I have a single valve of this
along with Ostrea gregarea
(tab.
(fig.
7.)
111.
Devizes, and another upon Coral rag
perfect.
and
dotted,
ears are dissimilar
f.
in sandstone,
1
(fig. 5.)
&
3.)
from
but not so
PECTEN similis.
TAB. CCV.— Fig. 6.
Char.
Spec.
Suborbicular^ depressed^
striated
;
archedj diverging; ears unequal; sides
striaB
straight.
1
HIS differs from the last in having a straight side be-
neath the larger ear, in being long^er, and having no dots
first sight it much resembles it.
Limestone, probably belonging to the
Forest Marble, from Shotover Hill, Oxford.
in the striae
Upon
;
but at
shelly
PECTEN
rigida.
TAB. CCV.—Fig.
Char.
Spec.
striated;
Orbicular,
stride
8.
depressed
;
strongly
arched, diverging; ears large,
unequal, decussated.
A LARGER
shorter,
From
the Rev.
shell than the last, which it resembles, but
and has fewer and deeper striae.
is
Castle Combe, in Forest Marble, by favour of
H. Steiuhauer.
CUCULL^A
oblonga.
TAB. CCYL—Figs.
Syn.
CucullEea oblonga.
Spec. Char.
Miller,
and
2.
MSS.
Transversely oblongs gibbose^ lon-
gitudinally
shaped
1 HE width
i
striated
lines
;
anterior
;
wedge-
side
beneath the cartilage numerous.
of this Cucullaeais above twice
its
length
the front inclines slightly to the posterior side, which
:
is
upon the surface are numerous, irreguThe beaks are
the edge is entire.
lar, and elevated
the flat rhomboidal space between
elegantly incurved
small
the
:
striae
:
;
them
marked with from 9
is
The
specimen of
finest
pair figured
it
:
much
labour and perseverance by Mr.
J. S. Miller, of Bristol.
me
parallel lozenges.
belongs to a valuable collection that has
been made with
also sent
12
to
this shell as yet obtained is the
G.
W.
Braikenridge, Esq. has
a good example.
at Dundry in the
The single
ore.
They were both found
inferior Oolite, holding grains of iron
valve represented was sent
me by
the
it is in the
Rev. Mr. Steinhauer, from Cross Hands
same kind of stone. I regret that a single valve exhibiting the teeth more perfectly, which I have just received
from Mr. Miller, did not arrive time enough for me to
:
alter the figure.
It
shews the
lateral plates bent at right
angles near their bases where they approach the middle
Mr. Steinhauer has
of the hinge.
from
little
also sent
me fragments
Sodbury.
The name
is
that
Mr. Miller has given
and
in a catalogue of
lent
me
some valuable
for publication.
it
in his letters,
shells
he has kindly
CUCULL^A
decussata,
TAB, CCVL--Figs.
Cucullaea decussata.
Syn.
Char.
Spec.
Transversely ovate
longitudinal ridges
gular
lines
wA-BOUT
one-fiftli
4.
Parkinson III. 171.
flattish
;
and
3
;
g-ibbose^ with
anterior side an-
;
beneath the cartilage
wider than long
:
few^.
the ridges are but
and are decussated by fine and close lines
the interior margin in old shells is crenu-
elevated,
little
of growth
lated
:
:
the teeth of the hinge,
when they
are not worn,
are striated or crenulated upon their Sides, as I have ob-
served when speaking of C. glabra, (Vol.
I. p.
T received this from the same gentleman
152, t.67.)
who
sent Mr.
Parkinson the specimens he describes, Mr. Francis Crow,
who
collected
them
all
near Faversham, in Kent
:
they
are silicious casts, with a small portion of the shell re-
maining.
CUCULL^A
carinata.
TAB. CCYIL— Fig.
Spec.
Char.
Obliquely cuneiform, smooth
ridg-e running"
up
to the beak.
i^ENGTH and breadth nearly equal
bounds the anterior
side bein^
but the rid^e that
one
is
acuteness of the angle
the anterior side, with the remaining surface,
from C. glabra
sufficient to distinguish this
smoothness of the surface
A
;
very oblique,
The
sixth longer than the width.
made by
an-
;
and distinguished by a
pointed,
side
terior
i.
silicious cast
may
arise
(tab. 67.)
is
the
from wear.
from Black Down.
CUCULLtEA fibrosa.
TAB. CCVIL— Fig. 2.
Spec. Char.
Obovate,
gibbose,
logitudinal elevated striae
margin
terior
straight,
with
upon the
numerous
surface
;
an-
prominent near the
hinge.
liENGTH
less than the
C
the lines
width
but
;
in its
general aspect
much
oblique, and the
more gradually rounded unto the middle
upon the surface are sharp, and frequently
resembling
anterior side
glabra,
it is
less
is
crossed by the lines of growth.
Cast
in
Calcedony, in a sandstone holding mica and
green sand; found at Black
me by Miss E.
Hill.
Down, and
transmitted to
ti
TRIGONIA eccentiica.
TAB. CCVIIL— F/g'5. and 2.
1
Trigonia eccentrica.
Syn.
p. 175. tab. 12. /.
Parkinson,
rior side produced,
iii.
5.
Transversely ovate,
Spec. Citar.
vol.
convex; ante-
posterior side round,
vi^ith
oblique undulating ridges on the surface.
The length is
only half the width
;
the edge
is
very re-
comes to the produced part of the
anterior side, where it bends a little forward, and then
The ridges are straight and transturns suddenly back.
gularly curved
till it
verse near the beaks where they almost cross the shell
those placed nearer the front are confined to the posterior
the lines of
side, are undulated, and are crossed by
growth,
two views of one valve, which was found
on Black Down by the Rev. J. H. Steinhauer it is
I have the
silex, stained perhaps by vegetable matter.
opposite valve imperfect from Hembury Fort, Devonalso silicious.
shire, through the hands of Mr. Goodhall:
I have o-iven
;
TRIGONA
affinis.
TAB. CCYin.—Fig.
Trigona
Syn.
affinis.
Miller,
3.
MSS.
gibbose,
half
thick, regularly elliptical, about one-third
wider
Spec. Char.
Transverse,
oval,
covered by transverse ridges.
Very
than long, and
remarkable for the slight protuberance of
the beak, behind which there
in Corbula,
is
and many other
not that cavity observable
shells.
The
transverse
12
ridges are very uniform, and somewhat inversely imbricated.
The
anterior half
The handsome mass
this rare
species rests,
Mr. Miller
collection,
;
it is
from
smooth.
upon which
public use by
of silicized shells,
was sent
named
its
is
me
affinis in
for
the catalogue of his
resemblance, although distant, to
Triffonia sinuata of Parkinson.
13
CORBULA.
sided
valves
dissimilar unequal-
two
Shell with
Gen. Char.
La March,
Bruguiere.
Hinge
sub-transverse.
;
two, one in each valve
;
teeth
ligament internal.
of the most easily defined genera, being well disone
tini^uished by the dissimilarity of the valves, of which
One
and
generally so small as to be included in the other,
valve,
larger
the
by the single recurved conical tooth in
the
and a corresponding pit with an irregular tooth
with inother both valves are more or less gibbose,
ancurved beaks, a projecting and sometimes recurved
are
recent,
and
fossil
Several species, both
side.
is
m
:
terior
described
;
some are
slender, others very stout shells.
CORBULA
gigantea.
TAB. CClX,—Figs.
Spec. Char.
when
Gibbose,
when young
old transversely oblong
produced,
and
5, 0,
surface
recurved;
furrowed near the beaks
;
7.
suborbicular,
anterior side
concentrically
posterior side beset
;
with short spines.
have the furrows and ribs between, which
are equal and very regular, extended over the whole
Young
shells
surface of both valves
;
they are broadest over the middle,
and gradually diminish to the sides
in size,
the
the ribs are closer,
front,
and
at length
and
:
as the shell increases
prominent towards
less
disappear
:
when
full
grown,
short obtuse spines placed in longitudinal rows occupy
14
The
the posterior side and part of the front.
side
The
substance
which
is
This
is
very thin, except that of the hing-e,
strong.
shell is
abundant
Devonshire, Whetstone
his
3d
posterior
very concave, and separated by an obtute ridge.
is
Vol. p. 226.
I
:
in
it is
sandstone, called in
have received
of growth from ray kind
Miss E.
the
mentioned by Parkinson
it
in
in various stages
and amiable correspondent,
Hill.
CORBULA
lavigata.
TAB. CClX.--Figs.
1
find 2.
Spec. Char.
Orbicular, gibbose, smooth,
thin ; beaks prominent, incurved.
and
VERY smooth regularly convex thin shell, scarcely
I have only seen one, that is the
smaller valve, and only an imperfect specimen of that
but it shews the hinge, in which it exactly agrees with
i\.
wider than long.
C. gigantea.
cies is situated
The
tooth in this valve in both these spe-
upon the posterior edge of the
pit that
receives the tooth of the other valve, in which they differ
from other Corbulae, although
traces of such a disposition.
From Black Down, by
in
some of them there are
favour of Miss E. Hill.
CORBULA
globosa.
TAB. CClX.—Fig,
3.
Spec. Char.
Globose, smooth ; anterior side of
the larger valve produced into a lip ; truncated ; beaks equal.
A VERY
small shell, equal in thickness to
the posterior side
is
its length
round, the anterior obscurely trun;
15
cated,
and the front obtuse
protruded in the form of a
is
of the other valve
I say in
:
is
always a
little
the
bent,
beyond the anterior side
lip
many
have a considerable number that
than the want of this
many specimens
in
:
margin of the larger valve, which
specimens, because I
differ in
no other respect
they can hardly be younger, as
they are mostly of the same, or even of a larger size.
Very abundant
lip
;
Highgate Hill, frehave never met with a divided
in the blue clay of
quently in clusters
;
and
I
pair.
CORBULA
Pisum.
TAB. CCIX.— jPzV
Spec. Char.
Subglobose^ irregular, concentrically
furrowed
anterior side
;
sliohtly
margin of one valve produced
A
RUGGED looking
v*»ry
4.
;
truncated
;
beaks unequal.
shell
the beak of the larger valve is
prominent, even ventricose, especially in oldsubjects
;
;
the expanded margin extends beyond the anterior side of
the smaller valve, and a considerable part of
The
furrows are commonly worn away
stance, together with
it
some
;
tlie front.
which circum-
irregularity in the shape, give
the aspect of a shell that inhabits holes in stone.
Several of
this
my
correspondents have favoured
from Barton and Hordle
Cliffs
:
among
me
with
others Miss
Bennett, the Rev. Mr. Iremonger, and the Rev. Mr.
Bingley, wherefore I suppose it is a very common species
there, although not noticed by Brander.
16
CORBULA
revoluta.
TAB. CClX.—Figs.
Syn. Tellina revoluta.
Spec. Char.
8 to 13.
Bi^occhi b\6.
tab. 12./. 6.
Transversely oblong', tumidj trans-
versely furrowed
;
anterior side produced, trun-
cated, with a carina
running
beak
to the
;
mar-
gin of the larger valve prominent, inflected;
beaks unequal.
Var.
deep
transverse furrows few,
(costata)
/3
anterior side
rather
pointed^
(fi»s.
11,
12^
and 13.)
J.
HE width
is
frequently twice the length
the lesser valve
is
the edge of
;
almost wholly enclosed in the larger,
the margin of which at the front i» expanded, and rather
bent inwards, whence the
name given by
anterior side of the larger valve
is
Brocehi.
extended
in the
The
form of
a truncated beak, but liable, as well as the general form,
to such irregularities as are
bit holes
and cracks
and sharp, except
common
in rocks
in var.
/3,
;
S^alve is
which inha-
which has them rounded, and
the ridges between them sharp.
'
to shells
the furrows are numerous
The beak
of the larger
very gibbose in old shells.
From Barton
Cliff
by favour of the Rev. Mr. Bingley,
some have the furrows so irregular that it is
difficult to say to which variety they belong, otherwise I
should have been led by the general form to consider the
in plenty
var.
/3
;
a distinct species.
17
MODIOLA
subcarinata?
TAB. CCX.—Fig.
M.
Syn.
subcarinata
ris 191
?
1.
La March, Foss. de PaMuseum a' His-
Annates du
toire Xaturelle,
VL
Vol.
p. 122.
V.
IX. tab. 17./ 10.
Oblong, smooth, gibbose
Spec. Char.
side keel formed, rather obtuse
convex ; front concave.
;
anterior
;
posterior lobe
arched inwards in this shell;
edge is straight.
whereas in M. modiolus of Linn, that
is above twice
obliquely,
taking the measure
The margin of the front is
The
length,
modiolus of Linn. It
the width, and greater than in M.
the lines of growth, and is
is often strongly marked by
very pearly beneath a thin brown epidermis.
subcarinata of La
This is probably not the Modiola
description ; but I
Marck, although it agrees with the
must consider
it
as such until I obtain the
tinguishing them.
ties of
It
may
means of
dis-
probably be one of the varie-
MytiUus modiolus of Brocchi
;
but as that author,
varieties of rewho is apt to treat fossil species as only
instance, it is not easy
cent shells, does so in the present
The specimens figured are the
to determine this point.
much
Highgate Hill. The large one has been
produce of
appears to retain
broken by pressure, but the small one
its
original form undisguised.
MODIOLA bipartita.
TAB. CCX.— F/g-s. 3 and 4.
Elongated, smooth, rather gibbose ;
above the
anterior side obtuse, suddenly raised
irregular.
lobe
posterior ; posterior
Spec Ckar.
but readily
related in general form to the last,
lobe
posterior
the
of
separation
distinguished, by the
Nearly
1.8
from the remainder of the
shell
by a kind of step parti-
cularly prominent near the beak
also
;
the length
is
greater
the carinated form of the beak not so evident
;
and the front edge has two or three waves
The
regular curve.
shell
in place of
a
seems to be very thin and not
pearly.
Casts of this in ferruginous indui'ated marl, with
all the shelly remains worn off, have been forwarded to me by Miss jE. Hill, who obtained them
from Lantrissent near Cardiff. Similar casts occur at
Osraington ; he plate contains two views of one &f
these that was given rae by Miss Benett. Fig. 3 is from
nearly
an imperfect cast
Park, in Sussex
in
I
:
ferruginous sand, from
received
it
MODIOLA
^qualis.
TAB. CCX.— jP/g-.
Spec. Char.
lobe
Oblong-,
largC;,
is
2.
convex, smooth, anterior
obscurely defined.
The regular curvature
angle,
Parkham
from G. A. Mantell, Esq
of the margin which presents no
a striking feature in this Modiola
:
the two ends
are nearly equal in width, and the posterior lobe almost
as large as the remainder of the valve, and very gradually united with
it.
A cast in loose
Park,
in
The length
is
about twice the width,
ferruginous sandstone, from
Sussex, by G. A. Mantell, Esq.
Parkham
19
MODIOLA minima.
TAB. CCX.— Figs. 5, 0, and
7.
Ovato-subtriangular, smooth
Spec. Char.
;
front
nearly straight^ ends rounded^ posterior lobe
small, distinct.
Only
half as long again as wide:
is
it
vary broad
the margin forms a
anteriorly, and has small beaks
prominent angle with the hinge line at their junction.
;
This occurs in a grey argillacious Limestone the
largest was sent me from Taunton, by my friend R.
Hare, Esq. One of the small ones was found near Bel;
fast,
by Dr. M'Donnel, along with Gryphites.
MODIOLA
cuneata.
TAB. CCXl.-'Fig,
Elongated, convex, smooth
Spec. Chau.
rior part
cuneated
concave
ly
1.
;
;
back arched
;
;
ante-
front slight-
posterior side distinct, convex.
twice as long as wide; most gibbose near the
forward end
heaks, and gradually depressed towards the
in the form of a wedge.
AnouT
From
the inferior Oolite of Somersetshire.
MODIOLA gibbosa.
TAB. CCXl.— Fig.
Syn.
Modiola anatina.
Elongated,
Spec Char.
smooth
;
Smith Strat. Si/stem 89.
reniform, very gibbose,
back broad, arched.
ISTearly three times as long as wide
valve
is
2.
equal to
its
width.
;
the depth of each
The end
is
obtuse, not
29
wedge-shaped as
guishes
it
in the last,
in all ages.
The
a character that
posterior lobe
and gibbosc.
I have several specimens of
this shell
is
from Bradford,
Wilts, and from Claverton Hill, near Bath.
it
distin-
well defined
I believe
belongs to Smith's FuUers'-earth Rock.
MODIOLA
TAB.
Spec.
Char.
anterior
CCXL— F/g-.
Oblong,
lobe
reniformis.
3e
sub-reniform,
slightly
expanded
;
smooth
;
posterior
lobe small.
A
MORE obtuse and
less
comparatively compressed
curved
:
shell than the last,
the length
is
and
about twice the
width.
This
shell, of
which I have seen but one specimen,
said to be from the inferior Oolite, near Bath,
is
MODIGLA imbricata.
TAB. CCKlL'-'Figs.
Spec. Char.
ridges
elongated
Oval,
upon the surface
;
l
;
and
3,
with imbricated
back angular, front
concave.
A HIS
is
as broad
a slightly compressed shell
;
the ridges
;
about twice as long
upon the surface are the edges of
the shell left prominent after each successive addition to
its
margin during
its
growth.
The anterior
lobe forms a
slightly elevated ridge extending to the beak.
The Rev. T. O. Marsh sent me the specimen (fig. 3)
from Felmarsham, near Bedford.
I have had larger
casts brought me from Milton Ernest, also in Bedfordshire,
by Mr. Goodhall, who has kindly favoured me
with several shells obtained by him in the course of a
short tour.
Fig. 3 is from a much compressed and bro-
ken
shell,
taken out of clayey Limestone, found in an
alluvial deposit in the parish of Gisleham, near
toff,
in Suffolk,
Lowes-
by the friendly Mr. Thurtell.
MODIOLA Hillana.
TAB. CCXIL—-Fig. 2.
Spec. Char.
Depressed, elongato-ovate, concen-
trically striated
slightly
An
posterior
,•
concave
;
end narrow
front
;
posterior lobe obscure.
elegantly formed shell, rather more than twice as
long as wide
;
the back forms a kind of keel from the
centre of which the shell tapers towards the beaks
;
these
are not very prominent; and together with the small
22
convexity of the posterior lobe, give that end a narrow
contour.
The
striae
the lines of growth
;
are obtuse ridges coinciding with
they are smooth.
Miss E. Hill, whose kindness I have often had occame this shell from Pickeridge
Hill, near Roundsford Park, Taunton.
It is found in a
grey argillacious Limestone, that is in some parts so soft
sion to acknowledge, sent
and loose that the
shells
may be picked
in other parts the stone
strongly to
is
it,
in
is
firm,
out of it with ease j
and the
shell adheres
which case the surface of the
shell that
exposed by fracture has a glistening velvety lustre,
its crystalline structure.
The specimens
arising from
are frequently narrower than the figure.
MODIOLA aspera.
TAB. CCXlL-^Fig\
4.
Spec. Char. Ovate^ elongated^ posteriorly pointed ;
very g'ibbose,
elevated^
longitudinally striated;
rough,
very numerous
;
stride
posterior
lobe obscure^ wrinkled, small.
1 HE small and nearly flat posterior lobe leaves the beaked
end of this Modiola so small as to give it much of the
contour of a Mytillus.
gether
is
The depth
of the two valves to-
greater than the width, and the length
the depth.
The roughness
of the
strias
is
twice
proceeds from
minute elevated scales, that are most conspicuous near
the margin of the shell, and are nearly obliterated to-
wards the beaks.
For this beautiful shell I am indebted to Mr. Goodhall,
who brought it from a pit in Gregory's Land, at Felmarshara, near Bedford.
23
AMMONITES
Sowerbii.
TAB. CCXIII.
a. Sowerbii.
Syn.
Spec.
Char.
Miller
MSS.
Catalogues.
Discoid, carinated, with about eight
spiniform tubercles upon each whorl
fined, entire
Var.
;
elliptical.
four, the inner ones concealed to the
bases of the tubercles
many
;
the outer part of the volutions
gentle undulations
;
the inner part
except that the base of each tubercle
the centre in an obtuse ridge.
rated from the body of the shell
In var.
/3
;
even,
extended towards
The
keel nearly sepa-
it is
round and
entire.
the ridges from the bases of the tubercles are
have a furrovy on each side of
var. a appear to be
rarest specimens
:
it.
The
far
sunk as
inner whorls of
more gibbose than the outer ones.
Mr. Miller considers the
one of his
shell figured as
his collection has also to boast of seve-
ral smaller specimens, belonging to var.
in the gibbosity of the whorls
Dundry,
is
is
more prominent, and the keel sometimes so
to
keel de-
aperture circular^ keel sometimes impressed.
IS
Volutions about
has
aperture
;
;
in the Inferior OoHte.
they were
(3,
which vary
all
found at