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, THE
| ALMONTOGRAPHICAL SOCLETY.
INSTITUTED MDCCCXLVIT.
LONDON:
MDCCCLII Ii
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PALAONTOGRAPHICAL SOCIETY.
INSTETUTED MDCCCXLVIL.
VOLUME FOR 1909.
LONDON:
MDCCCCIX.
ad Te
ve
DESCRIPTION OF THE FOSSIL REMAINS OF MOLLUSCA FOUND IN
THE CHALK OF ENGLAND: CEPHALOPODA.
ORDER OF BINDING AND DATES OF PUBLICATION. ae
=
ISSUED IN VOL.
PAGES PLATES on see PUBLISHED 7
General Title-page and Index — 1909 December, 1909
1-26 I—x 1853 December, 1853 —
27—36 XI—XVI 1854 May, 1855
37—68 XVII—XXVII _ 1855 February, 1857 |
DESCRIPTION
OF THE
FOSSIL REMAINS OF MOLLUSCA
FOUND IN THE
CHALK OF HNGLAND.
CEPHALOPODA.
BY
DANIEL SHARPE, pres. cEot. soc. F.R. & GS.
LONDON:
PRINTED FOR THE PALZONTOGRAPHICAL SOCIETY
1858—1909.
PRINTED BY ADLARD AND SON, LONDON AND DORKING.
—— ee
i ND EX.
6 | Ammonites navicularis
PAGE
camax verus
onites ... “fe 17
alternatus Rs “ot coe
austeni ... ae i, U2,
bravaisianus 52; xxiii, 7-9
brongniartii we ee
bunburianus Ds Ike
carolinus... nee bee
catinus Peas cite |
cenomanensis ov; xvi, lL
cinctus £ 25; ix, 2
complanatus = hOisevat,1=3
consobrinus Be. we «45
coupel . 23; vii, 1-4, ix, 1
— var. inflata 24; viii, 1
— var.tuberculata 24; viii, 2, 4,
at
cunningtoni 35; xv, 2
curvatus... 21, 49; vii, 8, 9, xxiii, 1
deverianus 43; xix, 5
euomphalus 31; xu, 4
faleatus ... 21; vii, 5-9; 49
feraudianus ie) ooh hPa)
fissicostatus 30
gentoni ... ome ety
gollevillensis ... 48; xvii, 2
goupilianus bas vi, 5, 6
eriffithii ... o 28; xi, 3
hippocastanum ... ...003 Xvil, 2-4
icenicus ... ; 43 ; xix, 4
jukesii.., 007 Ex, LL
largilliertianus ... ae AS
laticlavius ol ;-xiv, |
leptonema 32; xiv, 3
leptophyllus 48 ; xxi, 2, xxii, 1
lewesiensis 46, 48; xxi, 1
mantelli .., 39, 40; xviii, 4-7
milletianus
Aptychus
obtectus ..
octo-sulcatus
oldhami ...
peramplus
planulatus
portlocki ...
prosperianus
ramsayanus
renauxianus
renevierl ...
rhotomagensis
rusticus ...
salteri
saxbii
sussexiensis
varians
— var. costata
PAGE
.. 89; xviii, 1-8, 5, 8
20; vu, 4
42; xix, 3
32; xiv, 2
26; x, 1-3
...29; xii, 3, 4
30; xiii, 2,3
- i. 26
nee) Gree ios ee
41; xix, 2
Ee 44; xx, 2
...803; Xvi, 1-4
a» = Sees xx, I
50; xxi, 3, 5
45; xx, 3
33, 04; xv, 1
22, 23; viii, 5-10
23; viii, 9
— var. intermedia 22, 23; viii, 7
— var. subplana 22,23; viii, 10
— var. subtuberculata 22; viii,
5, 6,8
— var. tuberculata ws oo
vectensis... 45; xx, 4
vellede ... 39; xvii, 7, xix, 6
vielbancii in oF
wiestii 47; xxi, 3
wiltonensis ...083 xxi, 10
woollgari ... Dears Sh be
Neg <b, “ee
gollevillensis 56; xxiv, 5
icenicus 57; XXiv, 7
leptophyllus 55; xxiv, 1
peramplus... ~<00; mary, £0
portlocki ... 56; xxiv, 2, 3, 4, 6?
rugosus 57; xxiv, 8, 9
39 | Belemnitella ...
4
70 FOSSIL REMAINS OF MOLLUSCA IN CHALK OF ENGLAND.
Belemnitella lanceolata
mucronata
plena
quadrata
vera
Belemnites
electrinus
granulatus
lanceolatus
listeri
minimus ...
mucronatus
plenus
quadratus
ultimus ...
Belemnon pustulatum
Nautilus
archiacianus
compressus ..
icine
elegans
expansus
fittoni
fleuriausianus
PAGE
ssi
var. fusiforme
;» Ory one
8: 1, 7-11
9
w
met
DON WW OOD
Mg
a A a, 1
12; iii, 3, iv, 1
11; ii, 3-5
17; vi, 4
16; vi, 3 |
ADLARD AND SON, IMPR., LONDON AND DORKING.
Nautilus levigatus
PAGE
. “hs on, Eee
largilliertianus . 16; vi, 1,2
neocomiensis 15; v,3
pseudo-elegans ; 18; iv, 2
radiatus... a .. 14; 452
sowerbyanus ee sh — 2
undulatus ... $a ze 15; v,4
Trigonellites ... ote a oe o_O Sam
Turrilites as Be ‘oo a seat eee
bechii sae ee ... 66; xxvi, 13
bergeri 65; xxvi, 9-1]
bifrons re 67; xxvii, 6, 7
costatus 66; xxvii, 1-5, 15, 16
desnoyersi as Ce se
giganteus ... xed as as OO
gravesianus 62; xxv, 7, xxvi, 14
mantelli 033 2E¥;- Oe
- morrisii 65; xxvi, 4-8
puzosianus 05; Xkvi, we
scheuchzerianus ... 64; xxvi, 1-3
triplicatus... s 66
tuberculatus 61, 62: XXV, es XXvl, 4,15, 16
undulatus... he Se see Om
varicosa ... > a3 Zh.) Sek
wiestii 67; xxvii, 8, 9,17
PA : i
7% 7 “ts
Py
ss: DESCRIPTION
OF THE
FOSSIL REMAINS OF MOLLUSCA
¥
CHALK OF ENGLAND.
BY
DANIEL SHARPE, F.R.G. & L.S.
PART I.
CEPHALOPODA.
LONDON:
PRINTED FOR THE PALZONTOGRAPHICAL SOCIETY.
1853.
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SrernnnnnenenneneenenEnEEEEnEEEREeT EERE EEE
Cc. AND J. ADLARD, PRINTERS, BARTHOLOMEW CLOSE.
.
bol 5S 7
OF THE
00 INCIL, SECRETARIES, AND MEMBERS
OP THE
PALHONTOGRAPHICAL SOCIETY,
1859.
President.
W. J. HAMILTON, Esea., F.R.S., For. Szc., G.S., &.
Council.
PROF. G. BUSK, F.R.S., L.S., G.S., &.
W. B. CARPENTER, M_D., F.R.S., L.S., G.S., &.
THOMAS DAVIDSON, Esa., F.R.S., G.S., &e.
F. E. EDWARDS, Esa.
ROBERT HUDSON, Esa., F.R.S., L.S., G.S., &.
J. G. JEFFREY, Ese., F.R.S., L.S., &.
ROBERT McANDREW, Esa, F.R.S., L.S., &.
PROF. OWEN, M.D., LL.D., F-R.S., L.S., G.S., &e.
Alton
Bath
Birmingham .
Blandford .
Bolton .
Brighton .
Bristol .
Cambridge
Charmouth.
Cheltenham
Cirencester
Colchester .
Deddington
Devizes
Dublin .
Dudley .
Edinburgh. {
Glasgow
Gloucester
JOHN PICKERING, Esa.
MAJOR-GEN. PORTLOCK, F.R.S., V.P. G.S., &e.
JOSEPH PRESTWICH, Esa, F.R.S., Treas.G.S., &e.
J. W. SALTER, Ese., F.G.S., &.
PROF. TENNANT, F.GS., &.
S. L. WARING, Ese.
N. T. WETHERELL, Ese., M.R.C.S.
REV. THOMAS WILTSHIRE, M.A., F.G.S., &.
Creasurer.
SEARLES WOOD, Esq., F.G.S., &., Twickenham, Surrey, 8.W.
Bonorary Secretary.
J. 8. BOWERBANK, LL.D., F.R.S., L.S., G.S., &e., 3, Highbury Grove, Islington, N.
Local Secretaries.
Wii11aM Curtis, Jun., Esq.
Wa. Watton, Esq.,17, Grosvenor Place.
Wma. Martuews, Esq. Jun, F.GS.,
Edgbaston.
W. Suter, Esq.
Marttuew Dawes, Esq., F.G.S., &.,
Westbrook.
Heyry Cart, Esq.
Wittam Sanpers, Esq., F.G.S., &e.
James Carter, Esq.
Henry Norris, Esq., F.R.C.S.
Tuomas Wricut, M.D., F.G:S., &.
Pror. James Buckman, F.G.S., &e.
Joun Brown, Esq., F.G.S., &c., Stanway.
CHARLES FauLKNER, Esq., F.G.S., &.
Witii1am Cunninetoyn, Esq., F.G:S., &e.
GILBERT SanDERs, Esq., 2, Foster Place.
Joun Gray, Esq., Hagley.
Pror. Batrour, F.R.S., L.S., &., 2,
Bellevue Crescent.
James P. Fraser, Esq.,F.G.S., City Bank.
Joun W. Witton, Esq.
Guildford . R.GopwIn AvstTEy, Esq.,F..R.S.,G.8.,&e.
Huddersfield . Ropexr Wetsu, Esq.
Leeds . Tomas NunNELgY, Esq., F.R.C.S.E.
Leicester . . James Puant, Esq.
Market Rasen Rev. W. W. Cooper.
rae on | Wrnxram Ket, Esq., Gateshead.
Norwich Rosert Fitcn, Esq., F.G.S., &e.
Oxford . Pror. Jn. Puituirs, M.A., F.R.S.,G.8., &.
Paris. . Pror. M. Epwarps, Jardin des Plantes.
Plymouth . J. H. Fue, Esq., F.R.C.S.E., &.
Portsmouth W. A. Raver, M.D.
Richmond, Yorks. Epwarp Woop, Esq., F.G.S., F.R.S.L.&c.
Scarborough . Joun Lecxensy, Esq., F.GS., &e.
Southampton . R. Tovey, Esq., 9, Waterlvo Place.
Stamford . Joun F. Bentiey, Esq.
Stowmarket . C. R. Bree, Esq.
Torquay WitiiaM PENGELLY, Esq., F.G.S., &e.
Wolverhampton Henry Beckett, Esq., Church Street.
Yarmouth . C. B. Rosz, Esq., F.G.S., &e.
York Epw. CuaRLEswortH, Esq., F.G.S., &.
oe <s
That the Society formed be called the Palzontegraphical Society, and that it shall have
for its objects the illustration and description of British Fossil Organic Remains.
if.
Each Subscriber of One Guinea, or more, annually, shall be considered a Member of the
Society. Such subscription to be paid in advance, and shall be due on the 1st day of January,
1847, and each succeeding year.
Lit.
- A Member shall, for each Guinea subscribed annually, be entitled to one copy of every
publication issued by the Society, for the year to which his subscription relates. But no
Member shall be entitled to receive his copy, or copies, until his subscription has been paid.
IV.
The number of copies of the Society’s publications shall be limited to the number of
Members, unless otherwise directed by the Council.
WF
The business of the Society shall be conducted by a President, Treasurer, Hon. Secretary,
and a Council of sixteen Members, who shall be elected at a General Meeting of the Members,
to be held annually in London.
WE.
The accounts of the receipt and expenditure of the Society shall be examined annually by
two Auditors appointed by the Council; the Auditors to be Members of the Society, who are
not Members of the Council, and their statement shall be circulated among the subscribers.
VII.
That the Editors of works published by the Society be entitled to a number of copies of
their works, not exceeding twenty-five, as may be decided by the Council.
ee
REGULATIONS FOR THE DELIVERY OF BOOKS.
They are delivered, free of expense, within three miles of the General Post Office, London.
They are sent to any place in England, beyond the distance of three miles from the
General Post Office, by any conveyance a Member may point out. In this case the parcels are
booked at the expense of the Society, but the carriage must be paid by the Member to whom
they are sent. ‘
They are delivered, free of expense, at any place in London which a Member, resident in
the country, may name.
They are sent to any of the Hon. Local Secretaries of the Society, each Member being
expected to pay the Local Secretary a due share of the carriage of the parcel in which the
books are sent.
Any number of Country Members may unite to have their books sent in one parcel to
any address they may name. In this case they are requested to depute one of their number to
transmit to the Secretary for London a list of the names of those whose books are to be
included in the same parcel.
Those Members who wish their books to be included in any of the parcels to Local
Secretaries are requested to send in their names (with their Christian name in full) and
particular address to the various Local Secretaries, who are respectfully requested to forward
to the Secretary for London an accurate list of all such names, with as little delay as possible.
Unless intimation to the contrary be given to the Secretary for London, the future
deliveries will be made in accordance with the delivery of the first volume.
The Council, desirous of imposing as little trouble as possible upon the Local Secretaries,
particularly request that all subscriptions be paid by Members directly to the Treasurer,
Szartes Woon, Esq., Twickenham, Surrey, by Post Office Order on the Twickenham Office,
or by Cheque on a London Banker. And as there is no other capital for conducting the
affairs of the Society than the Subscriptions paid in advance, the Country Members are
respectfully reminded that an early remittance is absolutely necessary.
As the quantity of plates and letterpress to be delivered to the Subscribers annually will
be increased in proportion to the extension of the Society, the Members are respectfully urged
to obtain as many new Subscribers, and at as early a period, as possible.
Gentlemen desirous of forwarding the objects of the Society, may be provided with
eirculars for distribution by application to the Hon. Secretary.
LIST OF MEMBERS.
HIS ROYAL HIGHNESS THE PRINCE CONSORT.
Abich, Dr. H. Conseiller d’Etat et Membre
de l’Académie Imperial des Sciences de
St. Petersburg, For. M.G.S.
Adam, Thomas, Esq. Halifax.
Addison, Rev. John, Weymouth.
Adlard, J. E. Esq. Bartholomew-close.
Agnew, Lady, Moray-place, Edinburgh.
Allingham, William, Esq. Reigate.
Ansted, Prof.,.M.A., F.R.S., G.S., &c.,
Bon Air, St. Martin’s, Guernsey.
Aplin, C. d’Oyley, H. Esq. Port Phillip,
Australia.
Archeological and Natural History Society,
Taunton.
Arlidge, John T., A.B., &c. Shirley Park,
Croydon.
Asher, A. Esq. Berlin.
Ashley, J. M. sq.
Ashmolean Society, Oxford (per Rev. E.
Hill, Christchurch).
Atheneum Library, Liverpool.
Aveline, W. T., I’sq., F.G.S., Museum of
Practical Geology, Jermyn-street.
Austen, R. A. Godwin, Esq., B.A., F.R.S.,
G.S. &c., Chilworth Manor, Guildford,
Surrey.
Austin, Miss Helena E., at Rev. H. E.
Howes, Frenchay, near Hambrook,
Bristol.
Austen, Rev. J. H., M.A., F.G.S., &c.
Ensbury House, Wimborne.
Babington, C. C. Esq. M.A., L.S., F.G.S. &c.
St. John’s College, Cambridge.
Backhouse, Wm. Esq. Conset Iron Works,
Shotley Bridge, near Gateshead, Tyne.
'» Baines,
Bagshaw, Miss, Stanley Villa, Lansdown,
Cheltenham.
Baily, Wm. H., Esq., F.G.S. Geological
Survey, Dublin.
Samuel, Esq. Brighouse, near
Huddersfield.
Balfour, Prof., F.R.S., L.S. &c. Edinburgh.
Balliere, H. Esq. 219, Regent-street.
Balme, E. B. Wheatley, Esq. Cotewall,
Mirfield, Yorkshire.
Barclay, Joseph G. Esq. 54, Lombard-street.
Barrett, Rev. A. North Cheam House, Surrey.
Barr, W. R. Esq. Park Mills, Stockport.
Barthes, Lowell, and Co. Gt. Marlborough-st.
. Bartlett, M. Esq. Boston, U.S.
Bathurst, Rev. W. H., Darley Dale, Matlock.
Bass, Isaac Gray, Esq. Brighton.
Battersby, Robert, M.D. Torquay.
Beaufoy, George, Esq. South Lambeth.
Beckett, Henry, Esq. Church-street, Wol-
verhampton.
Belfast Library.
Bell, Prof., F.R.S., Pres. L.S., F.G.S. &c.
17, New Broad-street, City.
Bell, Rev. Charles, Hampstead.
Bennett, William, Esq. 5,
Without.
Benson, Starling, Esq. Swansea.
Bentley, J. F. Esq. Stamford, Lincolnshire.
Bernard, Ralph M. Esq. Victoria Square,
Clifton.
Bewley, John, Esq. 16, Brunswick Buildings,
Liverpool.
Bidwell, Henry, M.D. Albrighton, Wolver-
hampton.
Bilke, Edward, Esq. F.G.S., &c., 12, Stam-
ford-street.
Bishopsgate
vi LIST OF MEMBERS.
Binney, E.W.,Esq., F.R.S.,G.S., Manchester.
Binyon, T. Esq. St. Ann’s-square, Man-
chester.
Birmingham Old Library, Union-street.
Blackburne, John George, Esq., F.G.S.,
Mining Engineer, Oldham.
Blackie, W. G. Esq. Ph. D., F.R.G.S., &c.,
36, Frederick-street, Glasgow.
Blackwell, S. H. Esq., F.G.S., &c. Dudley.
Blackwell, ‘Thos. E., F.GS., &c., 65, Pul-
teney-street, Bath.
Bladon, James, Esq. Pontypool.
Blake, W. Esq. Bishop’s Hall, Taunton.
Blount, J. H. Esq. M.B. 53, Clifton-road
East, St. John’s Wood.
Boase, H. S., M.D., F.RS., G.S., &c.
Claverhouse, near Dundee.
Bohn, Henry, Esq. 4, York-street, Covent-
garden.
Bonney, Rev. George, St. Peter’s College,
Westminster.
Booth, Prof., United States.
Borradaile, Charles, Esq. Upper Tooting.
Bosquet, M., Pharmacien, Maaestricht.
Botfield, Beriah, Esq. M.P., F.R.S., L.S.,
G.S., &c., 5, Grosvenor Square.
Bouchard - Chantereaux, Mons. President
de l’Administration du Museum, Bou-
logne.
Bower, Rev. E., Closworth, near Yeovil.
Bowerbank, J.S., LL.D., F.R.S., L.S., G.S.
&e., 3, Highbury-grove, N., Hon. Sec.
Bradley, Lonsdale, Esq., F.G.S., &c., Prior
House, Richmond, Yorkshire.
Brady, Right Hon. M., Dublin.
Brady, Antonio, Esq. Stratford, Essex, and
Admiralty Office, Somerset House.
Braikenridge, Rev. G. W., F.L.S., G.S. &e.
Clevedon, near Bristol.
Bramley, Lawrence, Esq. Halifax.
Brassey, Thos. Esq. jun. 56, Lowndes-sq.
Bravender, J.C. Esq.,F.S.G.,&c.,Cirencester.
Bree, C. R. Esq., 130, Princes Street, Edin-
burgh.
Briggs, Major-General, F.R.S., G.S., &c.
Oriental Club, Hanover-square.
Briggs, Miss Ellen, 3, Arlington-street.
Brighton and Sussex Natural History
Society, T. B. Horne, Esq. 7, Pavilion
Parade.
Bristow, Henry W. Esq. F.G.S. &. Museum
of Practical Geology.
British Museum, Departmental Minera-
logical and Geological Library.
Broome, C. E. Esq. M.A., &c., Elmhurst,
Batheaston, Bath.
Brown, John, Esq. F.G.S., &c., Barnsly.
Brown, Isaac, Esq. Ackworth.
Brown, John, Esq. F.G.S., &c., Stanway,
near Colchester.
Brown, T. C. Esq. Cirencester.
Browne, Charles J. P. Esq. Bridgewater.
Browne, Wm. Meredith, Esq. Westminster
Fire Office, King-street, Covent-garden.
Bruce, Rev. J. C., Newcastle-on-Tyne.
Brunel, I. K. Esq. F.R.S., G.S., &c., 18,
Duke-street, Westminster.
Bryson, Alexander, Esq. Edinburgh.
Buckman, Prof. James, F.G.S., &c. Royal
Agricultural College, Cirencester.
Bullock, Henry, Esq. 15, Cumberland-street,
Bryanstone-square.
Bunbury, E. H. Esq. F.G.S. &c. 15, Jermyn-
street, Piccadilly.
Busk, Professor G., F.R.S., L.S., G.S., 15,
Harley-street, Cavendish-square.
Butcher, Henry J. Esq. Devizes.
Byerley, Isaac, Esq. Upton, Birkenhead.
Caird, H. W. Esq. Albury Park, Guildford.
Calvert, John, Esq. 189, Strand.
Cambridge University Library (per Rev.
James Power).
Cann, James M. Esq. 5, Church-street,
Edge-hill, Liverpool.
Carpenter, W. B. M.D. F.R.S., LS.,
G.S., &c., University Hall, Gordon-
square.
Cardiff Literary and Scientific Institution.
Carter, James, Esq. 30, Petty Cury, Cam-
bridge.
Carter, R. Esq. Halifax.
Carter, Rev. W. A. Eton College.
Carus, Dr. Victor, Leipzig, per Williams
and Norgate, 14, Henrietta-st., Covent-
garden.
Catt, Henry, Esq. West-street, Brighton.
Cautley, Colonel Sir Proby T., F.R.S., G.S.,
&e., 31, Sackville-street, Piccadilly.
LIST OF MEMBERS. vii
Cavill, Edmund, Esq. F.G.S. Saxmundham.
Cawdor, The Earl of, Trustee, British Museum,
F.R.S., G.S., &c., 74, South Audley-
street.
Chambers, Robert, Esq. F.R.S.E., G.S., &c.
Edinburgh.
Chapman, Thomas, Esq. F.G.S., 23, New-
street, Spring-gardens.
‘Charlesworth, Edward, Esq. F.G.S., &c.
York.
Chariton, E., M.D. 7, Eldon-square, New-
castle-on-Tyne,
Chippenham Literary and Scientific Insti-
tution.
Chisholme, W. Esq.
Cholmeley, Mrs. Octavia, The Priory, Stroud,
Gloucester.
Christy, Henry, Esq., F.G.S., &c., 103,
Victoria-street, Westminster.
Clabon, J. M. Esq., F.G.S., &c., 21, Great
George-street.
Clapham, Thos. Richard, Esq. Austwick
Hall, near Settle.
Clark, Edward, Esq. F.G.S., &c., Sandgate,
Kent.
Clark, Henry, M.D. Midland House, South-
ampton. .
Clark, Rev. Samuel, Training Institution,
Battersea.
Clark, Rev. Francis F., B.A. Malpas, near
Newport, Monmouthshire.
Clark, Prof. W., F.R.S., G.S., &c., Cam-
bridge.
Clarke, Robert, Esq. Cincinnati, Ohio, U.S.
Clarke, Rev. W. B., F.G.S., &c., St. Leo-
nard’s, near Sydney, New South Wales.
Clayton, Rev. J. H. Farnboro’ Rectory,
Bagshot.
Clennell, Jno. E. Esq. Hackney.
Cochrane, Charles, Esq. Ormsby Iron Works,
Middlebro’-on-Tees.
Colchester, W. Esq., F.G.S., &c., Harwich.
Cole, Jno. W. Esq. 18, Randolph-road,
Maid Hill West.
Coles, Henry, Esq. F.G.S. &c.24, Cambridge-
road, Hammersmith.
Colvin, Lieut.-Col. C. B. Leintwardine, near
Ludlow.
Collings, Rev. W. T., F.L.S., G.S. Seigneur
de Sark, Channel Islands.
Collingwood, F. S. W. Esq. Glanton Pyke,
Glanton, Northumberland.
Cooke, Major A., R.E. Ord.
Perth.
Cooke, W. R. Esq. Burford, Oxon.
Cooke, Rev. R. B., F.G.S., &c. Wheldrake
Rectory, York.
Cooke, Major A., R.E. Perth.
Cooper, Rev. W. H., M.A. &c. Sussex-
square, Brighton.
Cooper, Rev. W. W. West Rasen, near
Market Rasen, Lincolnshire.
Corder, Mrs. Ipswich.
Cormack, Dr., New York (U.S.)
Cornthwaite, Rev. T.M.,M.A.Walthamstow
Cornwall Library, Truro.
Cotsworth, Mrs.
Cotton, R. P., M.D. &c. 47, Clarges-street,
Piccadilly.
Crewdson, W.D. Esq. Helme Lodge, Kendal.
Crowley, Alfred, Esq. Croydon, Surrey.
Crum, Walter, Esq. F.R.S. Thornliebank,
Glasgow.
Cubitt, W. Esq. F.G.S. &c. Bedford Hill,
Streatham, Surrey.
Cubitt, Geo. Esq. 65, Warwick-square,
S.W.
Cull, R. Esq. 18, Tavistock-street, Bedford-
square.
Cunningham, James, Esq. 50, Queen-street,
Edinburgh.
Cunnington, W. Esq., F.G.S., &c., Devizes,
Wilts.
Curtis, W. jun. Esq. Alton, Hants.
Cust, Lady Elizabeth, 13, Eccleston-square.
Survey,
Darwin, Charles, Esq. M.A., F.R.S., L.S.
G.S., &c., Down, Farnborough, Kent.
Davidson, Thomas, Esq., F.R.S.,G.S., Mem.
Geo. Soc., France, &c., 44, Lorn Road
Terrace, Brixton.
Davis, John Ford, M.D. 13, Royal Crescent,
Bath.
Daw, Robert, Esq. Customs, 3, Leigham
Terrace, Plymouth.
Dawes, J. S. Iisq. F.G.S., &c. Smithwick,
Birmingham.
Dawes, M. Esq. F.G.S. Westbrook, Bolton.
Dawson, Dr. J. W., F.G.S., &c., MacGill’s
College, Montreal.
ie
vill LIST OF MEMBERS.
Day, Alfred, D.C.L. Westbury, near Bristol.
Day, Hen. Geo. Esq. B.A. St. John’s Coll.
Cambridge.
Deane, H. Esq. Clapham, Surrey.
De Castro, James, Esq. 5, Park Villas,
Richmond.
Deshayes, Mons., For. M.G.S., Paris.
Deslongchamps, M., Eudes, For. M.G.S.,
Caen.
Devon and Exeter Institution, Exeter.
Devonshire, Duke of, Chancellor of the
University of London, F.R.S., G.S. &c.
10, Belgrave-square.
Dickenson, Joseph, M.D., F.R.S., L.S. &c.
5, Nelson-street, Great George-square,
Liverpool.
Dickinson, W.
Worthington.
Dickinson, Joseph, Esq. F.G.S. Inspector of
Coal Mines, Pendleton.
Dickinson, W. H. Esq. St. George’s Hospital.
Dickinson, Henry, Esq. Coalbrook Dale.
Digby, Lady T., Mintern, near Dorchester.
Dilke, C. Wentworth, Esq., F.G.S., 76,
Sloane-street.
Dillwyn, L. L. Esq. M.P., F.R.S., L.S. G.S.,
&c., Hendrefoilan, Swansea.
Dixon, George, Esq. Great Eyton, near
Stokesley, Yorkshire.
Donkin, Henry, Esq. 5, Paragon, New Kent-
road.
Dorset County Museum Library, Dorchester.
Douglas, Rev. Robert, Stoke Lacy Rectory,
Bromyard.
Dover Proprietary Library.
Esq. Shannon House,
Dowell, Geo. M. Esq. Trinity College,
Dublin.
Dratleford, Rev. D. J. Chewton, Mendip,
Somersetshire.
Drewitt, R. D. Esq. Peppering, near Arundel.
Ducie, the Earl of, F.R.S., G.S., &c., 30,
Prince’s Gate.
Duckworth, — Esq. Smith and Co., Book-
sellers, Liverpool.
Duff, Patrick, Esq. Elgin.
Dumortier, Mons. I. Lyons.
D’Urban, John, ‘Esq. 32, Gordon-street,
Gordon-square.
Durham, the Dean and Chapter of, Durham.
Dymock, Rev. T. F. Ventnor, Isle of Wight
Eardley, Lady, Frognell, Torquay.
Kassie, Wm. Esq. jun. Railway Saw-mills,
Gloucester.
East Sussex Medical and Chirurgical Society,
Hastings (Dr. Greenhill).
Edwards, William, Esq. 9, London-street,
Norfolk-square, Paddington.
Edwards, F. E. Esq. 2, John-street, Down-
shire-hill, Hampstead. :
Edwards, Prof. Henry Milne, For. M.R.S.,
&c., Jardin des Plantes, Paris.
Egerton, Sir Philip de Malpas Grey, Bart.
M.P., Trustee Brit. Museum, F.RS.,
G.S., &c. Oulton Park, Cheshire, and
6, Albermarle-street.
Elliot, John, Esq. Kingsbridge, Devon.
Enniskillen, William Willoughby, Earl of,
D.C.L., F.R.S., G.S., &c. Florence-
court, Enniskillen, and Athenzum.
Escher von der Linth, Arn., For. M.G.S.,
Zurich.
Etheridge, R. Esq., F.G.S., &c., Museum
Pract. Geology, Jermyn-street.
Evans, Thomas, M.D. Gloucester.
Eyton, Thos. C. Esq. F.L.S., G.S., &c.
Vineyard, near Wellington, Salop.
Falconer, Hugh, M.D., F.R.S5 L.S., G.S. &e.
31, Sackville-street.
Falconer, Thomas, Esq. F.G.S., &c., Usk,
Monmouthshire.
Falkner, Frederick, Esq. Bath.
Falkner, Thomas Alexander, Esq. M.A.
Weymouth.
Farnham, Lord, Carlton Club, 94, Pall Mall.
Farrer, J. W. Esq. F.G.S. &c. Ingleborough,
Yorkshire.
Faulkner, Charles, Esq. F.S.A., GS.
Museum, Deddington, Oxon.
Favre, M. Alph., Prof. Geology, Academy,
Geneva.
Fenton, James, Esq. M.A., Grappenhall,
Lodge, near Warrington.
Ferguson, Daniel, Esq. Coatham Redcar,
Yorkshire.
Ferguson, W. Esq. 26, Lloyd-square, Pen-
tonville.
Ferguson, Wm. Esq. F.G.S. 31, Torrington-
square.
LIST OF MEMBERS. * ix
Fisher, Rev. J. H., F.G.S. &c. Kirby Lons-
dale.
Fisher, Rev.Osmond, M.A. F.G.S.Colchester.
Fitch, Robert, Esq. F.G.S. &c. Norwich.
Fitton, W. H., M.D., F.R.S., L.S., G.S., &c.
4, Sussex Gardens, Hyde Park.
Fletcher, T. W. Esq. F.R.S., G.S., S.A., &c.
Dudley, Worcestershire.
Flower, J. W. Esq. Park Hill, Croydon.
Forchhammer, George, Pu. D., For. M.G.S.
Copenhagen.
Fox, Rev. W. D. Delamere Forest, near
Chester.
Fraser, James P. Esq. F.G.S. City Bank,
Glasgow.
Fraser, John, M.D. Wolverhampton.
French, Richd. Esq. Trin. Coll., Cambridge.
Froggat, John, Esq., Church-gate, Stock-
port.
Fryer, A. Esq. Chatteris, Cambridgeshire.
Fuge, J. H. Esq. F.R.C.S.E. Plymouth.
Fuller, Henry J., M.D. 13, Manchester-
square.
Gatty, Charles, Esq. Felbridge Park, East
Grinstead.
Galton, Douglas, Esq. R.E., F.G.S., &c. 12,
Chester-street, Grosvenor-place.
Gandy, Gerard, Esq. Kendal.
Gassiot, I. P. Esq. F.R.S. &c. Clapham.
Gavey, George E. Esq. F.G.S., &c.
Geological Society of Dublin.
Geological Society of Manchester.
Geological and Polytechnic Society of the
West Riding of Yorkshire, Leeds.
Geslin, M. Berthaud, Paris.
Gibson, G. S. Esq. Saffron Walden.
Gibson, Thos. F. Esq. F.G.S. &c. 124,
Westbourne-terrace, Hyde-park.
Gilchrist, Dr. Royal Institution, Dumfries.
Glossop, F. H. N. Esq. Isleworth.
Godlee, Rickman, Esq. Lillies, Upton, Essex.
Gomonde, W. H. Esq. F.G.S. &c.
Gordon, P. L. Esq. Craigmyle.
Gough, Thomas, Esq. Preston Hall, Kendal.
Gough, Capt. the Hon. G. S., F.L.S., &c.
Rathnonan, House, Clonmel, Ireland.
Gould, John, Esq. F.R.S., L.S., Z.S., &c.
Broad-street, Golden-square.
Graham, Cyril, Esq.
Gratton, Joseph, Esq. 32, Gower-street.
Gray, C. Esq. Bliston.
Gray, John, Esq. Lyttleton-terrace, Hagley,
near Stourbridge.
Gray, Thos. Esq. 37, Montieth-row, Glasgow.
Greene, Prof. J. B., Cork.
Griesbach, Rev. A. W. Wollaston, Welling-
borough, Northampton.
Griffith, Edw. Esq. F.R.S., &c. Common
Pleas Office, Serjeant’s Inn, Chancery-
lane.
Griffith, N. Esq. F.G.S., &c. Dublin.
Griffith, Sir Richard, Bart., LL.D., F.G.S.,
&c. Dublin.
Grosvenor, Horace, Esq. Cincinnati, Ohio;
USS.
Grundy, Thomas, Esq. Northampton.
Gruner, M. Louis, Directeur de lEcole
Imperiale des Mines, &c. St. Etienne,
Loire, France.
Guise, W. V. Esq. F.G.S. &c. Elmore-court,
near Gloucester.
Hagenow, Chevalier Frederic de, Pu. D. &c.
Griefswald, Pomerania.
Hall, Robert, Esq. 8, Dean’s-yard, West-
minster.
Hall, William, Esq., Feversham, Kent.
Hall, Robert W. Esq. F.G.S. Raglan House,
Wheath, Glamorganshire.
Hall, James, Esq. For. M.G.S. Geological
Survey, States Library, Albany, New
York, U.S.
Halle, University, Library of.
Hambrough, B. J. Esq. F.G.S. Niton, I.W.
Hamilton, E. M.D., F.L.S., 22, Grafton-
street, Bond-street.
Hamilton, W. J. Esq. F.R.S., For. Sec. G.S.,
23, Chesham-place, Pimlico.
Hansfield, J. Esq.
Hanson, Samuel, Esq. Botolph-lane.
Harkness, Prof. Robert, F.R.S., G.S.,Queen’s
College, Cork.
Harmar, Richard, Esq. 9, Brock-street, Bath.
Harris, W. Esq. F.G.S. Charing, Kent.
Harrison, Wm. Esq. Galligreaves House,
Blackburn.
Hastie, Alexander, Esq. M.P. &c. Glasgow.
Haughton, Prof. S., M.A., F.R.S., G.S. Trin.
Coll., Dublin.
2
‘LIST OF MEMBERS.
Hawes, Rev. Henry, B.A., F.LS. &c..
Southsea, Portsmouth.
Hawkins, M. R. Esq. 4, Stanhope-street,
Hyde Park Gardens.
Hawkins, B. Waterhouse, Esq. F.L.S.,G.S.
Belvidere-road, Norwood.
Heales, Alfred, Esq. Doctors’ Commons.
Hector, James, M.D.Edinburgh (Maclachlan
and Stewart).
Henslow, Rev. John S., M.A., F.L.S., G.S.
and C.P.S. Prof. Bot. Camb., Hitcham,
Bildeston, Suffolk.
Heywood, James, Esq. F.R.S., G.S. &c.
Atheneum.
Higgins, E. T. Esq. 10, Brook-terrace, Birk-
enhead.
Highley, Samuel, Esq. jun. F.G.S. Box Hill,
Surrey.
Hill, Miss, Rock House, Bath.
Hills, William Henry, Esq. Sunderland.
Hitchman, Dr. John, County Asylum, Derby.
Holmes, George B. Esq. Horsham.
Hony, Rev. W. E., F.G.S. &c. Archdeacon of
Sarum, Baverstock, near Salisbury.
Hopgood, James, Esq. Clapham Common.
Hopkins, W. Esq. M.A., F.R.S., G.S.
Cambridge.
Horner, Leonard, Esq. F.R.S., G.S. 17,
Queen’s Road West, Regent’s Park.
Horner, Rev.JohnS. Mello Park,near Frome.
Howard, Mrs. Greystoke Castle, Penrith.
Howitt, Thomas, Esq. Lancaster.
Hoyland, Chas. Esq. 16, Old Broad-street.
Hudson, Robert, Esq. F.R.S., G.S. Clapham.
Huguenin, O. F. U. T. Esq. Java.
Hull, Edward, Esq. F.G.S. &c. Museum
Pract. Geology, Jermyn-street.
Hull, Edwd. Esq., Manor House, Little
Hampton, Bengworth, Eversham.
Hull, W. D. Esq. F.G.S. &c. 49, Milner-
square, Islington.
Hunt, Z. D. Esq. F.G.S. Aylesbury.
Hunter, Rev. S. Wolverhampton.
Hunter, Rev. Robert.
Hutchins, Miss, Alton, Hants.
Hutton, R. Esq. F.G.S., M.R.LA. &c.
Putney Park.
Huxley, T. H. Esq. F.R.S., L.S., Sec. G.S.,
Museum Practical Geology, Jermyn
Street.
Illingworth, Rev. E. A. 8, Mecklenburgh
street, Mecklenburgh-square.
Illingworth, R. S. Esq. 9, Norfolk-crescent.
llott, James, Esq. Bromley, Kent.
Ipswich Museum, Ipswich.
Jackson, W. Esq. Newton, near Penrith.
Jackson, Edward S. Esq. M.A., F.G.S. &c.
Totteridge House, Enfield Highway,
Middlesex.
James, Lieut.-Col. H., R.E., F.R.S., G.S.
&c. Ordnance Survey, Southampton.
Jardine, Sir Wm. Bart. F.R.S.E., F.L.S. &c.
Jardine Hall, Lockerby, N.B.
Jarvis, Richard H. Esq. F.G.S. 24, Dorset-
square.
Jeffreys, J. G. Esq. F.R.S., L.S. 1, Mon-
tague-square.
Jennings, F. M. Esq. M.R.I.A. &c. Cork.
Johnes, J. Esq. F.G.S. Dolan Cothi, Llandilo,
North Wales.
Johnson, William, Esq. Eton College.
Jones, Rear-Admiral T., M.P., F.L.S., G.S.
&c. 30, Charles-street, St. James’s.
Jones, John, Esq. Gloucester.
Jourdain, Dr. Director, Museum, Lyons.
Jukes, J. B. Esq. M.A., F.R.S., G.S. &e.
Geological Survey of Ireland, Stephen’s-
green, Dublin.
Keal, John, Esq. Bellevue-house, Bristol.
Kell, William, Esq. Gateshead, near New-
castle-on-Tyne.
Kenyon, the Hon. Mrs., Parade, Shrewsbury.
Kenyon, J. R. Esq. British Museum.
King, Prof. W. F.G.S. Prospect-hill, Galway.
King, W. P..Esq. Rodney-place, Clifton, -
Bristol.
Konigliches Ober Berg. Amt. Bonn.
Kingston, G. S. Esq. Grote-street, Adelaide,
S. Austrailia.
Knapp, Charles, Esq. 2, Harcourt-buildings,
Temple.
Krantz, M. Bonn.
Kuprainoff, Lieut.-Col., St. Petersburg.
Laidlay, John W. Esq. Calcutta, and
Hindon, near Arundel.
Landseer, George, Esq. Cunningham-place,
St. John’s Wood.
LIST OF MEMBERS. xi
Lankester, Edwin, M.D., LL.D., F.RS.
L.S. 8, Savile-row, Bond-street.
Lashmar, Dr. C. Croydon.
Law, Rev. Julius, Conran, Durham.
Lawrance, John, Esq. F.G.S. Elton, Oundle.
Leckenby, Jno. Esq. F.G.S. Scarborough.
Lee, John, LL.D., F.R.S., R.A.S., GS. &c.
5, College, Doctors’ Commons.
Lee, Jno. Edward, Esq. F.G.S. The Priory,
Caerleon, Monmouthshire.
Leeds Library, Leeds, Yorkshire.
Leigh, Dr. J. S., 7, St. Stephen’s-terrace,
Westbourne Park.
Lesson, E., M.D., Bonchurch, Isle of Wight.
Lemon, Sir C. Bart. F.R.S., G.S. &c. 40,
Charles-street.
Library of the University, King’s College,
Aberdeen.
Lidstone, Roger, Esq. Plymouth.
Lindsay, Chas. Esq. 10, Addle-street, Doctors’
Commons.
Lingard, Jno. R. Esq. Alderley, near Wilms-
_ low, Cheshire.
Lister, J. J. Esq. F.R.S. &c. Upton, Essex.
Lister, Jno., M.D., F.G.S. &c. Shibden Hall,
near Halifax.
Lister, Rev. W. Bushbury, Staffordshire.
Literary and Philosophical Society of Shef-
field.
Literary and Philosophical Society of New-
castle.
Literary and Philosophical
Cheltenham.
Liveing, G. E. Esq. St. John’s College,
Cambridge.
Liverpool Free Public Library (J. S. Dalton,
Esq.)
Llewelyn, J. D. Esq. F.R.S., L.S. &c. Pentle-
gare, Swansea.
Llewellen, W. jun. Esq. F.R.S. &c. Pontypool.
Lloyd, John, Esq. 77, Snow-hill.
Lloyd, Frederick, Esq. 50, Dorset-square.
Long, H. W. Esq. Rood Ashton, Trowbridge.
London Institution, Finsbury Circus.
Longman, Messrs. and Co. Paternoster-row.
Lonsdale, W. Esq. F.G.S. Burnham, Bridge-
water.
Loriére, Mons., Jardin des Plantes, Paris.
Lovén, Prof. S., Stockholm.
Low and Son, Ludgate-hill. |
Institution,
Lowry, J. W. Esq. F.R.G.S. 45, Robert-
street, Hampstead-road.
Lubbock, Sir John W. Bart. M.A., F.R.S.,
L.S., G.S. Mansion-house-street.
Ludlow Natural History Society.
Lury, S. H. Esq. 16, Old Board-street.
Lyell, Sir C., M.A., F R.S., L.S., G.S. &e.
53, Harley-street, Cavendish-square.
Mackeson, Henry B. Esq. F.G.S. &c. Hythe,
Kent.
Mackey, Lieut.-Col., Fairhill, near Exeter.
Maclaren, Charles, Esq. F.R.S.E., G.S. &c.
Moreland Cottage, Grange, Edinburgh.
Maclean, William C. Esq. St. Ann’s Thicket,
Portsea.
Macleod, John, M.D., H.M.S. Hermes.
McAndrew, R. Esq. F.R.S. Allhallows
Chambers, Lombard-street.
McDowell, Geo. Esq., Dublin.
McDowell, G. M. Esq. F.T.C.D., Trinity
College, Dublin.
McIntosh, John, Esq. Taunton.
Macredie, P.B.M. Esq. Perceton Irvine, N.B.
Majendie, A. Esq. F.R.S., G.S. &c. Heding-
ham Castle, Castle Hedingham, Essex.
Major, Charles, Esq. Red Lion Wharf, Upper
Thames-street.
Malta Library, Malta.
Mansell, John, Esq. Cossington, Bridge-
water.
Marcou, Professor of Geology, Zurich.
Marier, Mons. Paul, 10, Rue Blanche, Paris.
Marsh, John, Esq. Burnt Tree, near Dudley.
Marshall, James G. Esq. M.P. Leeds.
Marshall, Matthew, Esq. Bank of England.
Martin, P. J. Esq. F.G.S. &c. Pulborough.
Martineau, F. Edgar, Esq. 42, George-street,
Edgbaston, Birmingham.
Matthieson, James, Esq. 19, Belitha-terrace,
Barnsbury Park.
Matthews, W. jun. Esq. F.G.S. Edgbaston,
Birmingham.
Maw, G. Esq. Barratt’s-hill House, Broseley,
Salop.
Meade, Rev. R. J. Castle Cary.
Mechanics’ Institution, Lewes.
Mechanics’ Institution, Llandilo.
Mechanics’ Institution, Leicester.
xl LIST OF MEMBERS.
Medlock, Henry, Esq. Great Marlborough-
street.
Melbourne University Library, Australia.
Melville, Prof. M.D. &c., Queen’s College,
Galway.
Merian, Prof. Directeur de Museum, Basle.
Meryon, Edward, M.D. F.G.S. 14, Clarges-
street.
Middleton, John, Esq. 63, St. Stephen-
street, Norwich.
Mitchell, Dr. J. F.R.S. King-street, Kil-
marnock, Ayrshire. _
Mitchenson, John, Esq. 56, South-street,
Durham.
Mohr, Ernest, Herr, Heidelberg.
Mold, W. H. Esq. Aldersley, Derbyshire.
Molini, Charles Frederick, Esq. 17, King
William-street, West Strand.
Monk, Jas. Esq. Aden Cottage, Durham.
Moore, J. C. Esq. F.R.S., G.S. &c. 4, Hyde
Park Gate, Kensington.
Moore, Charles, Esq. F.G.S. Cambridge-
place, Widcome-hill, Bath.
Moore, Joseph, Esq. 25, Park Terrace,
Brixton-road.
Morant, A. W. Esq. F.G.S. 2, Britannia-
terrace, Great Yarmouth.
Morgan, Rev. William Leigh, Cardiff.
Morgan, William, Esq. Swansea.
Morris, John, Professor, F.G.S. Kensington.
Morson, T. N. Esq. Southampton-row,
Russell-square.
Morton, George Highfield, Esq. 5, London-
road, Liverpool.
Mosley, Sir Oswald, Bart. D.C.L., F.LS.,
G.S. &e. Rolleston Hall, Burton-on-
Trent.
Murchison, Sir R. I., G.C.St.S., M.A.,
D.C.L,° ) Bot! GSS TLS. ee dF
Belgrave-square.
Murdock, William, M.D. 320, Rotherhithe.
Museum of Practical Geology, Jermyn-street.
Neale, Edward V. Esq. West Wickham, Kent.
Neale, T. C. Esq. Chelmsford.
Neale, Henry, Esq. Foxhangers, Devizes.
Neison, Francis, G. P. Esq. F.L.S. &c.
3a, St. James’s-square.
Nelson, Lieut.-Col. R. I., R.E. 9, Moles-
worth-terrace, Stoke, Devonport.
New York State Library, Albany, U.S.
Newman, Edward, Esq. F.L.S. &c. 9, Devon-
shire-street, Bishopsgate-street.
Norfolk and Norwich Literary Institution.
Norris, Henry, Esq. F.R.C.S. &c. Char-
mouth, Dorset.
Norton, J. H., M.D., F.G.S. &c. Amroath
Castle, near Tenby.
Nunneley, Thomas, Esq. Leeds.
Nutt, David, Esq. 270, Strand.
Oldham, Prof. 18, Pembroke-road, Dublin.
Olivier, Lieut.-Col. H. S. Pottern Manor,
Devizes.
Ormerod, G. W. Esq. M.A., F.G.S. &c.
Chagford, Exeter.
Owen, R., Professor, M.D., LL.D., F.R.S.,
L.S., G.S., &c. British Museum.
Paine, Mrs. Farnham.
Papillon, Rev. J. Lexden.
Parry, Thomas G. Esq. F.G.S. Highnam
Court, near Gloucester.
Pattisson, Mrs. Jacob, Witham, Essex.
Payne, Rev. Wm. Reading.
Paynter, Rev. Samuel, Stoke Hill, Guildford,
Surrey.
Peace, William, Esq. Haigh, near Wigan.
Pearson, Sir Edwin, K.H., M.A., F.R.S. &c.
7, Chester-terrace, Regent’s Park.
Pease, Thomas, Esq. Henbury, near Bristol.
Peckover, Algernon, Esq. F.L.S. Wisbeach.
Pengelly, William, Esq. F.G.S. Torquay.
Penny, Rev. James, M.A. &c. Blandford.
Penruddocke, Charles, Esq. Compton Park,
near Salisbury, and 12, Hereford-street,
Oxford-street.
Perkins, Rev. R. B. Wotton-Underedge,
Gloucestershire.
Perry, George, Esq. Croydon, and Charter
House.
Pertz, Dr. Berlin.
Phillips, Prof. John, M.A., F.R.S., G.S. &e.
Magdalen Bridge, Oxford. +
Philosophical Society of Glasgow.
Philosophical Society, Leicester.
Philosophical Society, York.
Phear, Rev. Sam. Geo., Emmanuel College,
Cambridge.
LIST OF MEMBERS. xu
Pickering, John, Esq. Tufnell-park-road,
Upper Holloway.
Pictet, Prof. Geneva.
Pidgeon, Jonathan S. Esq. Pembridge Villa,
Bayswater.
Pierson, Charles, Esq. Blenheim Parade,
Cheltenham.
Plant, James, Esq. Princess-street, Leicester.
Plomley, F., M.D., F.L.S. &c. Maidstone.
Pollock, Lady, Clapham-common.
Portal, Wyndham S. Esq. Malshanger
House, Basingstoke.
Portlock, Major-General, LL.D.,F.R.S.,G.S.
&c. 58, Queen’s Gardens, Hyde Park, W.
Portman, Hon. Miss, 5, Prince’s Gate, Hyde
Park.
Powles, T. W. Esq. 46, Wimpole-street.
Pratt, S. P. Esq. F.R.S., L.S., G.S. &c. 25,
Thurlow-square, Brompton, S.W.
Preston Literary and Philosophical Insti-
tution.
Prestwich, Joseph, Esq. F.R.S., G.S. 10,
Kent-terrace, Regent’s Park Road.
Pritchard, Rev.C., M.A., F.R.S.&c. Clapham.
Prout, Rev. E., F.G.S. &c. Mission House,
Blomfield-street, Finsbury.
Provis, William A. Esq. The Grange, Elles-
mere, Salop.
Queen’s College, Galway.
Raban, Major, Junior United Service Club,
Regent-street.
Radcliffe Library, Oxford.
Ramsay, Prof. A. C., F.R.S., G.S. &c.
Museum of Practical Geology, Jermyn-
street.
Ramsay, William, Prof. of Humanity, Uni-
versity of Glasgow.
Rankin, R. M.D. Carluke, Glasgow.
Ranlin, Professor, Bordeaux.
Ransome, Mrs. Robert, Ipswich.
Raper, W. A., M.D. Parade, Portsmouth.
_ Rashleigh, J. Esq. 3, Cumberland-terrace,
Regent’s Park.
Rich, Messrs. 12, Tavistock-row, Covent-
garden.
Richardson, W. S., Esq. F.G.S. &c. 26,
Dorset-place, Dorset-square.
Richardson, William, Esq. Southeram, near
Halifax.
Risley, Rev. William Cotton, M.A. Ded-
dington, Oxfordshire.
Robbins, George S. Esq. F.G.S. Midford
Castle, near Bath.
Roddam, Jonathan, Esq. Newhouse, Wear-
dale, Durham.
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Roots, William, M.D., F.S.A. &c. Surbiton,
Kingston, Surrey.
Roper, F. C. S. Esg. F.G.S., L.S. Pembury-
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xvl
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House, near Tenby, S. Wales.
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field.
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LIST OF MEMBERS.
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Kennington-lane.
Young, James, Esq. Tower-hill, East Smith-
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INTRODUCTION.
Tue best general account of the Chalk Formation of England will be found in the
‘Geology of England and Wales,’ by Conybeare and Phillips, 1822, in which is em-
bodied a detailed description of the Chalk Cliffs in the neighbourhood of Dover by
Mr. W. Phillips, published in the fifth volume of the ‘Transactions of the Geological
Society.’ The divisions of the Formation which Mr. Phillips has pointed out, are more
minute than can be followed in the present Monograph, since few collectors attend to the
precise part of the series from which their specimens are derived. I have, therefore,
usually contented myself with referrimg specimens to one or other of the following great
divisions of the Chalk, which are easily recognised, although they are not separated by any
well-defined lines.
1. Upper Chalk; my specimens of which are principally from Norfolk, or from
Gravesend and Northfleet : this division is rich in Organic Remains.
2. Middle Chalk, which contains but few Fossils: those examined are mostly from
Kent, Surrey, Sussex, and the Isle of Wight.
3. Lower or Grey Chalk, containing numerous Fossils, especially Ammonites and
Turrilites: the neighbourhood of Dover, and of Lewes, and the Isle of Wight furnish
large supplies ; many specimens have also been procured from the numerous Chalk-pits
along the foot of the North Downs, and others have been obligingly sent from Devizes,
by Mr. W. Cunnington.
4, The “ Chloritic Marl” of the Isle of Wight, a bed of some six or eight feet thick at
the base of the Chalk, is very rich in Organic Remains, with which I have been most
liberally supplied from the rich Collection of Mr. S. Saxby, Jun., of Bonchurch. The
“Chalk with Siliceous Grains,” of Somersetshire, is probably on the same parallel as the
“Chloritic Marl,” and also contains abundance of Shells, of which a large collection
formed at Chardstock has been most obligingly lent me by Mr. J. Wiest: these have the
advantage of being far better preserved than is usual with the Chalk Fossils. I have also
had the use of Collections from this bed, belonging to Mr. E. H. Bunbury and
Mr. Morris.
1
2 INTRODUCTION.
Besides the gentlemen already mentioned, I am indebted for the loan of specimens to
Mr. Baber, Mr. Bowerbank, Mr. Henry Catt, Mr. Faulkner, Mr. Flower, Mr. Hudson,
Mr. J. G. Low, Mr. S. J. Mackie, Dr. Mantell, Mr. H. Taylor, and Mr. Wetherell, whose
names will be frequently mentioned in the course of the work, together with those of
others, who may be kind enough to lend me similar assistance. I have also to thank
Mr. Morris most especially for his valuable assistance in determining many obscure
species, and Mr. S. P. Woodward, for notes relating to specimens in the British Museum,
and for many drawings of parts requiring particular accuracy.
In giving the generic characters of Fossil Shells, it seems unnecessary to add
descriptions of the Animals supposed to have inhabited and formed them; since such
descriptions must be more or less conjectural, and information on this head is amply
and more fitly provided by writers on the recent branches of Natural History. The
Paleontologist must be contented with descriptions of the shell only, such as were
furnished by the earlier school of Conchologists. The student who desires information
about the Molluscous inhabitants of recent Shells, should consult the ‘ History of British
Mollusca and their Shells,’ by Forbes and Hanley, and the ‘ Figures of Molluscous Animals’
by Mrs. Gray, or he will find in the ‘ Rudimentary Treatise of Recent and Fossil Shells’
by S. P. Woodward a large amount of information condensed into a small and most
economical form.
i a
FOSSIL REMAINS OF MOLLUSCA
FOUND IN THE CHALK.
CEPHALOPODA.
BELEMNITES, Auctorum.
_ Animal unknown, enclosing a straight elongated conical, or fusiform calcareous shell
or guard more or less pointed below, and pierced above with a conical cavity or alveolus,
in which is lodged the phragmacone, a hollow horny cone divided into chambers by nearly
horizontal septa, which are traversed on the anterior or ventral margin by a siphuncle.
Wall of the alveolus entire. Exterior of the shell marked, in many species, by a furrow
down the front, and one down the middle of each side, but without any branching
vascular impressions.
The above description includes all the parts of the Belemnites which have been found
in the Chalk; but in some of the beds of the Oolitic series more perfect specimens are
found, in which the phragmacone is produced far above the walls of the calcareous shell,
and is provided with two elongated, slender, testaceous processes, proceeding from the
dorso-lateral margins of its upper edge; and the whole body is invested with a thin
testaceous or corneo-calcareous integument. For full descriptions of these interesting
remains the reader is referred to the Memoirs of Professor Owen in the ‘ Philosophical
Transactions of 1844,’ and of Dr. Mantell in the volumes of the same work for 1848 and
1850, and to the ‘ Paléontologie Francaise, Terrains Jurassiques’ of M. D’Orbigny.
M. D’Orbigny separated from the Belemnites those species which have a fissure down
the anterior or ventral side of the alveolar cavity, and which are provided with two longitudinal
depressions down the dorso-lateral portions of the shell, from which, in some species,
proceed branching vascular impressions ; to these he has given the name of Belemnitella.
1. Betemnirzs vitimus, D’Ord. Plate I, fig. 17.
BELEMNITES MINIMUS, in part? Lister. Hist. Anim. Anglie, tab. vii, fig. 32 ?
— Lister!, Phillips. Geology of Yorkshire, vol. i, tab. i, fig. 18 ?
— uLtimus, D’Orbigny. Paléont. France. Terr. Cret., Supp., p. 24.
4 FOSSIL MOLLUSCA OF THE CHALK.
B. Testd sub-cylindricd, inferné rotundatd, acuminata ; superné rotundato-quadraté ;
antice, lateraliterque lined impressd leviter notatd.
Shell sub-cylindrical, slightly flattened both on the front and sides of the upper part,
rounded below, and tapering gradually to a blunt point; with a slight furrow down the
upper part in front, and a slight furrow down the upper part of the middle of each side ;
opening oval.
Length, 2 inches ; a5
Found by Mr. Saxby, in the Chloritic Marl of Bamana: in the Isle of Wight ; found
also in the Red Chalk of Yorkshire, and in the Gault of Folkstone.
This species is usually confounded with Belemnites minimus of the Gault, from which
it is to be distinguished by a more cylindrical form, the slightly squared oval opening, and
shortness of its lateral furrows. 2. minimus on the contrary is spindle-shaped, with a round
opening, and a double line impressed on each side, which reaches nearly to the point.
Professor Phillips first pomted out the necessity of separating the two species (‘ Geol.
Yorksh.,’ vol. i, p. 46), and called this one B. Lsterz, although that name had previously
been applied by Dr. Mantell to the other species. Lister undoubtedly had the two species
before him when he wrote; but his name having been since restricted by all authors to
the common Gault species, which has been called indiscriminately B. minimus and B.
Listeri, it would increase the confusion to apply either of those names to this species,
which may therefore pass under M. D’Orbigny’s name of B. ultimus.
Plate I, fig. 17, a, 6, c. Three views of Mr. Saxby’s specimen, from the Chloritic
Marl of Bonchurch: the point having been worn away, its
outline is restored from another specimen.
BELEMNITELLA, D’ Orbigny.
Animal unknown, enclosing a straight, elongated, conical, or fusiform calcareous
shell or guard, more or less pointed below, and pierced above with a conical cavity or
alveolus, in which is lodged the phragmacone, a hollow horny cone, divided into chambers
by nearly horizontal septa, which are perforated on the anterior or ventral margin by a
siphuncle. Wall of the alveolus divided on the anterior side by a perpendicular slit, which
remains open above, but is gradually closed below, where its place is marked by a groove
on the outside of the shell, and a corresponding groove on the inside of the alveolus.
Back of the exterior of the shell marked by two longitudinal depressions, which in some
species are connected with complicated vascular impressions.
The remains of Belemnitella hitherto found in the Chalk, in this country, are limited
to the calcareous shell; in addition to which portions of the phragmacone are preserved
in the specimens of 4. mucronata found in the Cretaceous Sandstone of Maestricht and
Ciply.
BELEMNITELLA. 5
The genus Belemnitella was separated from Belemnites by M. D’Orbigny, on account
of the slit down the front of the alveolus, and the vascular impressions on the back and
sides of the shell, which are wanting in Belemnites; the latter character is most strongly
developed in B. mucronata and B. quadrata, and but faintly seen in B. lanceolata and
B. plena. These characters seem a slight foundation for a separate genus; but the
division has been generally adopted. All the Belemnitellee, yet known, belong to the Chalk.
The Belemnitellze may be divided into two sections, depending on the form and lining
of the alveolar cavity: in B. mucronata and B. lanceolata the alveolus is a regular cone,
with a rounded base, of which the apex forms an angle of about 20 degrees ; the cavity is
lined by a smooth continuous shelly layer, which in the fossils is denser, and less
crystalline than the rest of the shell; this cavity is filled by the phragmacone, and is
slightly marked by the edges of the septa.
In B. guadrata the lower part of the cavity for about one third of an inch is in the
form of a cone, with a round base, of which the apex has an angle of about 20°; this is
lined with a smooth shelly layer, and was evidently destined to receive the phragmacone.
The cavity then widens out suddenly, and becomes nearly square; this upper angular part
has no special lining, but is rough, with irregular rings marking the growth of the shell ;
the anterior slit reaches a little way into the lower part of the cavity. It has been
suggested, that the upper angular part of the cavity may be due to decay; but its form is
too constant and regular to be so explained.
The Swedish species B. sudventricosa of Wahlenberg (B. mamiillatus, Nills., B. scania,
Blainv.) has a cavity of analogous form to B. quadrata, with an irregularly triangular
aperture above. M. Konig figured this species under the name of Pazzllus belemnoideus
(Icones, No. 218), apparently regarding its peculiar form of cavity as a sufficient generic
character. But, as at present, we do not know the form of the phragmacone of either of
these species, we cannot estimate the importance of the difference in the form of the cavity.
The vascular impressions are very differently developed in the different species of
Belemnitella; they all have two depressions which extend down the sides of the posterior
part ; at the edge of the cavity these depressions are nearly as broad as the space between
them, they diverge slightly and become narrower in their course downwards, and termi-
nate near the apex of the shell, almost as near to the anterior as to the posterior side.
These two depressions are usually all that we see of the vascular markings on B. lanceolata
and B. plena, and on worn specimens of the other species; but on well-preserved
specimens of B. mucronata and B. quadrata they are bounded on each side by an
impressed line, from which spread off a number of branches, dividing and subdividing
with great complication, which cover the sides and front of the shell.
Casts of the alveolar cavity of Belemnitelle are frequently found in the flint of the Upper
Chalk, which sometimes show more clearly the form of the cavity than can be seen in the
shells themselves; the two woodcuts a and B are copied with Dr. Mantell’s permission,
from the second edition of his ‘ Geological Excursions round the Isle of Wight,’ p. 440 ;
6 FOSSIL MOLLUSCA OF THE CHALK.
the specimen they represent was found in the Chalk near Ventnor, and is in the Cabinet of
Mr. 8. H. Beckles. Fig. shows the upper part of one side of the phragmacone apparently
complete; the upper transverse lines are too sinuous to represent the edges of the septa,
which, as far as we know them, are nearly horizontal. Perhaps, the lower parallel and
nearly horizontal lines may mark the edges of the septa, and the upper waving lines may
indicate the growth of the margin of the phragmacone, which seems to have been
furnished with two lateral processes.
In fig. a, the cast displays very clearly the complicated groove running down the back
of the alveolar cavity.
Fig. A Fig. B
1. BELEMNITELLA MucRONATA, Schlotheim, Sp. Plate I, figs. 1, 2, and 3.
BELEMNITES, 1* species: Breyn, DE BELEMNITIS, figs. 1—6.
BELEMNITES MUCRONATUS, Schlotheim. Petref., p. 47, No. 4.
— _ Mantell. Sussex, t. xvi, fig. 1.
— _— Nilsson. Petrif. Suec., t. ii, fig. 1.
_— — Sowerby. Min. Conch., t. 600, figs. 2 and 4.
BELEMNITES ELECTRINUS, Miller. Geol. Tr., 2d series, vol. ii, t. viii, figs. 18—21.
ACTINOCAMAX VERUS? Miller. Loe. cit., t. ix, figs. 17 and 18.
BELEMNITELLA MUCRONATA, D’Orbigny. Paleont. Franc. Terr. Crét., t. vii.
— — Geol. of Russia and the Ural Mountains, vol. ii, t. xliii,
figs. 1 and 4, not figs. 2 and 3.
B. Testé subcylindricd, impressionibus duabus vascularibus ramosis notatd, antice
jissurata, posticé obtusd mucronata ; apertura subrotundd ; alveolo conico excentrico.
Shell elongated, subcylindrical, widening very slightly above, obtuse below, with a
distinct rounded point. Opening circular. Alveolus forming a regular hollow cone, with
a round base, and an apex of 18° to 20°, which is considerably nearer to the anterior than
to the posterior side of the shell; the position of the septa may be faintly traced on the
linmg of the alveolus. The fissure extends to within half an inch of the apex of the
cavity, but may be traced to the bottom, on the inside, by a continued depression ; another
BELEMNITELLA. 7
impressed line runs down the dorsal side of the cavity. The vascular impressions are
usually well-marked, and cover a large part of the surface, they branch off from a pair of
double lines, which commence near together on the two sides of the back, and separate
gradually as they extend downwards to near the point.
B. mucronata is nearly allied to B. lanceolata; it may be recognised by a more
cylindrical form with a distinct mucro, by its well-marked vascular impressions, and by
the eccentricity of the alveolar cavity.
In a fine specimen from Norwich, measuring 33 inches in length, the greatest diameter
is 3ths of an inch, and the fissure extends externally ?ths of an inch. But all the
specimens found in this country are broken off at the top, where the walls of the alveolus
are very thin. They are found in the Maestrict Sandstone with the upper part much
better preserved, the whole being 6 inches long, the alveolus spreading out at top toa
width of above an inch, and with an external fissure 23 inches long.
Found everywhere in the Upper Chalk of the South of England, and particularly
abundant in Norfolk. It is also found in the Upper Chalk of France, Germany, Belgium,
Sweden, and Russia. Also in the Cretaceous Sands of Maestrict and Ciply near Mons,
and at Faxoe in Denmark.
2. BELEMNITELLA LANCEOLATA, Schlotheim, Sp. Plate I, figs. 4—6.
BELEMNITES, 2* species: Breyn, DE BELEMNITIS, figs. 7—10.
— LANCEOLATUS, Schlotheim. Petrefactenkunde, p. 49, No. 8.
— MucRoNATUS, Brong. and Cuvier, t. iii, fig. 1?
— — Blainville. Belemnites, t. i, fig. 12.
— — Sowerby. Min. Conch., t. 600, fig. 1, excluding all the
other figures.
— a Woodward. Geol. Norfolk, p. 49.
BELEMNITELLA MUCRONATA, Var. FUSIFORME, D’Orbigny. Geol. of Russia and the
Ural Mountains, vol. ii, t. xliii, figs. 2
and 3.
B. Testa elongata, fusiformi; anticé subdilatatd, fissuraté ; postice acuminate ;
apertura subrotundd ; alveolo conico, centrali.
Shell elongated, fusiform, widening at the opening, then somewhat contracted, and
again enlarging to about two thirds its length, whence it gradually tapers off to a
point. Alveolus slightly oval above, circular below, forming a regular hollow cone, of
which the apex with an angle of 20° is nearly on the central axis of the shell; the
alveolar cavity is lined by a distinct shelly layer, faintly marked by numerous horizontal
rings, very near each other in the lower part, and becoming gradually more distant
upwards, and is slit down its anterior side by a fissure which extends within nearly to the
apex of the cavity; but is partially closed on the outside by the new layers of shell, which
in old specimens cover about half an inch of the lower part of the original fissure. Another
8 FOSSIL MOLLUSCA OF THE CHALK.
impressed line runs down the back of the alveolar cavity. Vascular impressions apparently
resembling those of B. mucronata are faintly marked and frequently obliterated.
This Belemnite, which was well distinguished by the earlier writers on the subject, has
been confounded by all later authors with B. mucronata, from which it is distinguished
externally, by its less cylindrical form, and fainter vascular impressions ; and internally,
by the central position, and more circular section of the alveolus.
Breyn, one of the earliest writers who made an approach towards the true nature of
Belemnites, distinguished the present species from B. mucronata without naming either,
and has given good figures of both, as Species 1 and 2. He was followed by Schlotheim,
who, referring to Breyn’s figures, names his lst species B. mucronatus, and his 2d species
B. lanceolatus, which names we must adopt, on the principle of priority ; an unlucky re-
mark of Schlotheim that, perhaps, Montfort’s Hidolithus hastatus might prove a variety of
his B. lanceolatus, has led both D’Orbigny and Bronn to throw aside Schlotheim’s name
b. lanceolatus, as a synonym of B. hastatus ; the slightest reference to Breyn would have
saved them from this error, as that author’s 2d species belongs clearly to the Genus
Belemnitella, the shit down the front of the alveolar cavity being well shown in the
figures, and clearly described in the text.
Miller was probably aware of the difference between the two species, since finding this
one figured by Blainville as B. mucronatus, he gave to the original B. mucronatus the new
name of B. electrinus. Woodward living in Norfolk, where the two species are abundant,
was well acquainted with both, and distinguishes them clearly in his Catalogue, as
B. mucronatus tapering off to a point, and B. electrinus obtuse, with a mammillated
point.
Sowerby, Min. Con., t. 600, threw the two species together, figuring them both under
the name of B. mucronatus, and the same is done by M. D’Orbigny, in the second volume
of the ‘Geol. of Russia, where they are well figured as Belemnitella mucronata, variété
fusiforme and variété renflée ; but m the ‘ Paléontologie Frangaise’ we have only the true
B. mucronata, well figured and described, without any allusion to the other form.
3. BELEMNITELLA QuaDRATA, Defrance, Sp. Plate I, figs. 7—11. :
BELEMNITES QUADRATUS, Blainville. Belemnites, t. i, fig. 9.
_— GRANULATUS, Sowerby. Min. Conch., t. 600, figs. 3 and 5.
BELEMNON PUSTULATUM, Kenig. Icones Foss. Sect., No. 216.
BELEMNITELLA QUADRATA, D’Orbigny. Paléont. Frang. Terr. Crét., t. vi, figs. 5—10- :
B. testd subcylindricd, granulatd ; apice obtusiusculo mucronato ; apertura subquadrata :
alveolo inferné rotundato conico, superné expanso subquadrato.
Shell nearly cylindrical, rounded towards the apex, which ends in a distinct point ;
alveolus wide, and four-sided above; round and conical below, with a short slit on the
anterior side, which reaches into the rounded part of the cavity; surface almost entirely
BELEMNITELLA. 9
covered with small granulations ; vascular impressions strongly marked in the young shell,
but somewhat concealed by the granulations in the full-grown shell.
The external form of B. guadrata is nearly the same as that of some varieties of
B. mucronata ; so that worn specimens which have lost both their outer surface and the
upper part of the alveolus may easily be confounded; and there has been confusion in
consequence in the synonyms. But it is well distinguished both by the granulations
of the surface and the square opening.
The lower part of the alveolar cavity, lined with a distinct, smooth, shelly layer, is of
the form of a rounded cone, about a quarter of an inch deep; above this, the cavity
suddenly widens out, and changes its character; it is irregularly four-sided, and the
surface has no special lining, but is roughened by the rings of growth of the shell.
The fissure is shallow, and reaches to the top of the lower division of the cavity.
Unfortunately, the Phragmacone of this species is not known; it would probably corre-
spond in form with the lower part of the cavity only.
Length, 25 inches; greatest breadth, =4,ths of an inch; cavity, 2ths of an inch, of
which the broader part occupies 4th, and the narrow rounded cone, 4th of an inch.
B. quadrata is found in the middle beds of the chalk of the counties of Kent, Surrey,
and Sussex, but is no where a common species. It has also been found in the upper
chalk of Northfleet.
It occurs, according to M. D’Orbigny, in the white chalk of Rheims in France, and
of Visé in Belgium.
4, BELEMNITELLA PLENA, Blainv., Sp. Plate I, figs. 12—16.
Breyn. De Belemnitis, fig. 15?
BELEMNITES PLENUS, Bainville. Belemnites, t. i, fig. 6.
—_— LANCEOLATUS, Sowerby. Min. Conch., t. 600, figs. 8 and 9.
— — Geinitz. Quadersansteingebirge, t. vi, figs. 3—5.
BELEMNITELLA VERA, D’Orbigny. Paléont. Franc. Terr. Crét., Suppt., t. ii.
B. testé elongaté fusiformi, sublevi, superné rotundato-trigond canaliculatd, medio
rotundata dilatatd; apice acuminato.
Shell elongated; when young cylindrical, with a tapering point; when full-grown
fusiform, swelling out below the middle, and tapering below to a point; front marked
with a slight furrow; a broad longitudinal depression on each side of the back, giving
somewhat of a three-sided form to the upper part of the shell. All the specimens have the
walls of the alveolar cavity broken off, leaving usually a projecting conical end, in the
centre of which the point of the alveolus may be distinguished.
The specimen, fig. 12, belonging to Mr. Morris, has fortunately the lower part of the
cavity preserved, but not enough to show any trace of a fissure; therefore the supposed
fissure figured by M. D’Orbigny, pl. ii, figs. 2, 4, and 7, in a more truncated specimen,
9
~
10 FOSSIL MOLLUSCA OF THE CHALK.
must be due to decay. Geinitz has figured the lower portion of the Phragmacone, but his
figure is hardly intelligible.
Although the specimens of this Belemnite are found truncated at different attitudes,
and the fracture is either nearly flat or more or less conical, there are common characters
in the broken ends of all, which are without doubt connected with the manner of growth
of the shell. There are usually two more prominent ridges on each side, and three slighter
ridges on the back. The sides of the angular cone thus formed, appear to have some
analogy with the angular opening of B. guadrata, and render it probable that B. lanceolata
will be found to belong to the same division of the genus as that species.
M. D’Orbigny has named this species B. vera, on the supposition that it is the
Actinocamax verus of Miller; but the description given by that author proves that, as
Mr. Sowerby correctly observed in the ‘ Mineral Conchology,’ 4. verus is a worn specimen
of B. mucronata. Miller describes his species as having “ two longitudinal, towards the
apex branching, impressions of blood-vessels.” He also states that it is often found in
flints. Both the description and the placing in it in the chalk with flints are decisive
against regarding it as B. lanceolatu. Every species of Belemnite, when rolled and worn
at the top, may present a form similar to that of Miller’s figure 17; and the B. mucronata
especially, in decaymg peels off in concentric layers, as in his figures 11, 12, and 13,
‘Geological Transactions,’ 2d series, vol. u, pl. 9. It is probable that when describing
Articonamax verus, Miller may have had before him worn specimens of several species of
Belemnite. Such names founded on misconception had better be allowed to drop.
But in this instance, as Miller’s description applies to B. mucronata, there is no room for
his name of 4. verus. The name first in point of priority is B. plenus of Blainville, which
has consequently been adopted. Sowerby’s name, 2. Janceolatus, is not only posterior to
Blainville, but had been previously applied by Schlotheim to another species.
Length, 33 inches ; greatest breadth, 3ths of an inch.
Common throughout the grey chalk of the South of England, and found in the lower
beds of the chalk in Belgium, Germany, and the North of France.
Navtitus, Zinn.
Shell discoidal, spiral, chambered, compressed or ventricose, with contiguous whorls
regularly convoluted on the same plane, the last partially or entirely concealing the previous
whorl; chambers separated by transverse, concave septa, with simple sinuous margins,
and traversed near their centre by a continuous siphuncle ; the last chamber large, and
capable of containing the animal.
rue,
NAUTILUS. 1]
1. Navtitus tzvieatus, D’Orb. Plate II, figs. 1 and 2.
NavTILus L&vieatus, D’Orbigny. Paléont. Franc. Terr. Crét., pl. xvii.
NV. testé globosd, levi, umbilico minimo aut nullo ; apertura semi-circulari ; septis parum
arcuatis ; siphunculo subcentral.
Shell globose, smooth, with the back and sides uniformly rounded, and a very faint
line running along the middle of the back ; umbilicus very small and entirely concealed
in the inner whorls; septa slightly arched, with nearly straight margins; siphuncle a little
in front of the centre; mouth nearly semi-circular, but rather wider than high, deeply
indented by the preceding whorl, with a broad shallow mesial sinus.
This shell attains a large size. A specimen from Brighton measures 43 inches in
diameter and 33 inches in breadth.
NV. levigatus is one of the commonest of the cretaceous species, and is found throughout
the whole range of the Chalk, viz., in the Upper Chalk near Brighton ; in the Middle Chalk
near Maidstone, Hemel Hempstead, and Tring; in the Grey Chalk at Dover and Lewes ;
in the Chloritic Marl of Bonchurch in the Isle of Wight; and in the Chalk with siliceous
grains at Chardstock and on the coast of Dorsetshire. It is found in France in the Upper
Green Sand, the Lower and Middle Chalk.
The only cretaceous species of WVautilus for which this could be mistaken, are J.
Bouchardianus, D’Orb. and NV. simplex, Sow. (NV. Clementinus ? D’Orb.) both of which have
a more marked umbilicus, and a depression on the ventral margin of the septa; the latter
is also a less globose shell, and has the siphuncle nearer the ventral than the dorsal margin.
2. Navuriius expansus, Sow. Plate II, figs. 3—5.
NAUTILUS EXPANSUS, Sowerby. Min. Conch., t. 458, fig. 1.
— Arcutracianus, D’Orbigny. Paléont. Franc. Terr. Crét., t. xxi.
NV. testé inflata, lateraliter compressiusculd, umbilicatd, subtiliter striata ; umbilico
sub-carinato; apertura laté sub-pentagond; septis undulatis; siphunculo sub-centralt.
Shell globose, with sloping slightly flattened sides and a sharply defined umbilicus ;
surface elegantly marked by fine sharp lines of growth, which are deeply incurved in front ;
whorls increasing rapidly in size and nearly concealing the preceding whorls; septa very
flexuous; siphuncle within the centre of the septum; mouth about as broad as high,
somewhat pentangular, rounded in front, with nearly straight sloping sides deeply
indented by the inner whorl, and with a deep, broad, rounded sinus.
Diameter 24 inches, breadth 12 inch.
LV. expansus is confined to the lowest bed of the Chalk; it is rare in the Chalk Marl of
Hamsey near Lewes, and in the Chloritic Marl of Bonchurch in the Isle of Wight; and
12 FOSSIL MOLLUSCA OF THE CHALK.
abundant in the Chalk with siliceous grains at Chaldon and Man-of-War Cove in Dorset-
shire, and Chardstock in Somersetshire. M. D’Orbigny cites it from the Craie Chloritée
of Mount Ste. Catherine, near Rouen.
The figure in the ‘ Mineral Conchology ’ is taken from a specimen somewhat expanded
at the mouth by pressure ; but the form of the umbilicus and the fine sharp striz leave no
doubt of its identity with WV. Archiacianus, D’Orb. |
3. Nautitus Destonecuampsianus, D’Orb. Plate III, figs. 1 and 2.
NAUTILUS ELEGANS, part. Mantell. Fossils of the South Downs, t. xxi, fig. 8.
— DESLONGCHAMPSIANUS, D’Orbigny. Paleont. Franc. Terr. Crét., t. xx.
NV. testé sub-globosd, umbilicatd, transversim costata et longitudinaliter striatd; umbilico
carinato ; costis elatis fexuosis ; striis tenuibus decussatis ; apertura semi-ovali.
Shell sub-globose, umbilicated, elegantly ornamented with sharp elevated transverse
flexuous ribs, which are usually crossed by thin longitudinal lines; the latter are often
obliterated in ill-preserved casts; the ribs rise within the umbilicus and are bent at a
sharp angle over its carinated margin ; they then sweep forward in a bold curve, and form
a deep sinus on the back, where they occasionally divide into two; the ribs are steep on
their front side and sloping behind, thus forming a series of steps on the surface ; the edge
of the umbilicus is angular or raised into a slight keel.
The longitudinal lines are very prominent in some specimens, but can hardly be
discerned in others; but the species can always be distinguished by the form of the ribs,
the deep and angular umbilicus. It is common in the Grey Chalk of Lewes, Dover, the
Isle of Wight, &c., and in the Chalk with siliceous grains of Chardstock, Somersetshire.
In France it abounds in the Craie Chloritée of Mount Ste. Catherine, near Rouen.
Diameter 25 inches, breadth 1? inch.
4. Navtitus ELEGANS, Sowerby. Plate ITI, fig. 3; and Plate IV, fig. 1.
NAUTILUS ELEGANS. Sowerby. Min. Con., t. 116.
— — Mantell. Fossils of the South Downs, t. xx, fig. 1.
— — DOrbigny. Paléont. Franc. Terr. Crét., t. xix.
NV. testa globosd, costata ; costis equalibus, rotundatis, sub-lexuosis ; apertura semi-
circulari ; siphunculo inter dorsum et septi centrum posito ; umbilico minimo.
Shell globose, uniformly rounded, ribbed; umbilicus slightly marked on the outer but
entirely concealed in the inner whorls ; ribs equal, rounded, and regular, bending in a
simple curve from the umbilicus to the back, where they form a broad shallow sinus ;
aperture semi-oval, a little higher than broad, deeply indented by the preceding whorl.
Siphuncle placed about half way between the centre of the septum and the back.
NAUTILUS. 13
Diameter 63 inches, breadth 5 inches. A gigantic specimen, sent me by Mr. Tyler
from Hamsey near Lewes, reaches 11} inches in its greatest diameter, and the ribbing
continues of about the same breadth throughout. ‘This species is common in the Grey
Chalk of the South of England and in the lower beds of the Chalk of France.
For many years all the ribbed Nautili found in the Chalk were confounded together
under the name of JV. elegans. Sowerby separated JV. radiatus. But we owe to M.
D’Orbigny the clear distinction of the different species, which may be known as follows :
JV. elegans is the most globose shell of the group, and has the smallest umbilicus ; it is
also to be known by the position of the siphuncle between the back and the centre of
the septum.
lV. pseudo-elegans is rather less globose than the preceding, has a more distinct
umbilicus, broader and fewer ribs, and the siphuncle between the ventral margin and the
centre of the septum; the two species are so much alike that the only character to be
relied on for distinguishing them is the position of the siphuncle.
NV. radiatus is easily recognised by a flatter form, with sloping sides, large umbilicus
and deep septa with a sinuous margin; the siphuncle occupies nearly the same position
as in the last; but there is also a marked depression of the septum close to the ventral
margin, which is not found in either JV. elegans or pseudo-elegans.
NV. Neocomiensis has flat and nearly parallel sides, a very large umbilicus, the ribs
much bent on the back, the siphuncle between the centre and the ventral margin, but
without the ventral depression of the septum.
LV. Deslongchampsianus is easily distinguished by the cross longitudinal ribs, and even
if these are lost, by the elevated edge of the umbilicus.
In all these species the ribbing is only seen in the exposed portion of the outer whorl,
being concealed withm by a layer of shell formed by the ventral fold of the mantle.
Thus specimens which have lost the outer whorl may appear partially or entirely smooth.
5. NAUTILUS PSEUDO-ELEGANS, D’Orb. Plate IV, fig. 2.
NAUTILUS PSEUDO-ELEGANS, D’Orbigny. Paléont. Franc. Terr. Crét., t. viii and ix.
NV. Testé ovata, subcompressd, costaté, umbilicatd; costis aqualibus, rotundatis,
flexuosis ; umbilico parvo ; apertura semi-ovali ; septis arcuatis ; siphunculo inter ventrem
et septi centrum posito.
Shell ovate, ribbed, with a small well-marked umbilicus; ribs broad, rounded, and
flexuous, with a deep sinus on the back; aperture semi-oval, higher than broad, deeply
indented by the preceding whorl; septa arched, with the siphuncle between the centre
and the ventral margin.
Diameter 7 inches, breadth 4 inches.
Common in the Grey Chalk of Lewes and elsewhere. Professor E. Forbes appears to
14 FOSSIL MOLLUSCA OF THE CHALK.
have seen specimens from the Lower Green Sand,* to which Formation M. D’Orbigny
states that it is confined in France.
M. D’Orbigny separated this species from JV. elegans, which it closely resembles ; it is
less globose, has broader and more flexuous ribs, deeper septa, and a more distinct
umbilicus; but it is best distinguished by the position of the siphuncle, which in this
species is situated between the inner margin and the centre of the septum, and in
LV. elegans is nearer to the back. Notwithstanding this character, most writers seem
disposed to throw them together.
6. Navuritus rapiatus, Sow. Plate V, figs. 1 and 2.
NaUTILUS RADIATUS, Sowerby. Min. Conch., t. 356.
_ —— D Orbigny. Paleont. Franc. Terr. Cret., t. xiv.
N. Testé ovatd, subcompressd, costatd, late umbilicatd; costis latis, caqualibus,
flexuosis; septis arcuatis, margine flexuosis, ad ventrem depressis; siphunculo inter
ventrem et septorum centrum posito.
Shell gibbose, with sloping flattish sides and rounded back, ornamented with broad
flexuous equal ribs; septa, with a flexuous margin low at the sides and produced at the
back, marked with a deep depression close to the edge of the preceding whorl; siphuncle
between the centre and the ventral margin ; aperture semi-oval, cousiderably higher than
broad, slightly indented by the preceding whorl; umbilicus large, exposing all the inner
whorls.t
Diameter 7 inches, breadth 4 inches.
Common in the Chalk with siliceous grams at Chardstock in Somersetshire, and
also found in the Grey Chalk near Dover, Guildford, &c. In Professor Forbes’s ‘ List of
Lower Green Sand Fossils’ it is mentioned as found at Atherfield and Sandgate, and
M. D’Orbigny quotes it in France from the Lower Chalk, the Upper and Lower Green
Sands.
NV. radiatus is easily distinguished from JV. pseudo-elegans by its large umbilicus, the
flexuous margin, and the ventral depression of the septa; the latter character separates it
also from /V. Neocomiensis.
* Journal of Geol. Society, vol. i, p. 353.
+ The ribs begin to show themselves when the shell is about one inch in diameter ; previously, it is
ornamented with fine sharp elevated lines marking the growth of the shell, crossed by finer longitudinal
lines, as seen in fig. 2; a similar ornament is found in many species of Nautilus when young.
NAUTILUS. 15
7. Navutitus Neocomiensis, D’Orb. Plate V, fig. 3.
Navutitus Neocomiensis, D’Orbigny. Paléont. Frang. Terr. Crét., t. xi.
NV. Testé inflata, lateraliter compressa, late umbilicatd, costatd; costis latis flecuosis,
dorso sub-angulatis ; septis margine paulum flecuosis ; siphunculo inter ventrem et septorum
centrum posito.
Shell gibbous, with flattened sides and a broad umbilicus, ornamented with rounded
flexuous ribs, which are less marked at the sides but broad and large on the back, where
they bend so rapidly as to form an almost angular sinus; the sides of the whorls being
nearly parallel, and the whorls increasing but slowly in breadth, the whole shell has a
flattened form by which it is easily recognised; margins of the septa slightly curved ;
siphuncle half-way between the centre and the inner margin of the septa.
We have only seen one small specimen from the Grey Chalk, which we can refer to
this species ; it is from Urchfont near Devizes, in the Collection of Mr. Cunnington, and is
2 inches in its greatest diameter and 12 inch in breadth; although a good deal broken,
it shows all the peculiar characters of the species. This species is more common in the
Lower Green Sand of Dorking, Atherfield, Sandgate, &c., where it sometimes reaches
above 7 inches in diameter. M. D’Orbigny quotes it as common in the lower beds of the
Middle Division of the Neocomian Formation in France.
The only species with which this can be confounded is WV. radiatus, from which it may
be known by its flatter form, larger umbilicus, septa less flexuous and without any de-
pression at the ventral margin, and the more angular sinus of the ribs on the back.
8. NauTitus unpuLatus, Sow. Plate V, fig. 4.
NAUTILUS UNDULATUS, Sowerby. Mineral Conchology, t. xl.
NV. Testaé gibbosd ; juniore levi, lateribus sub-compressis, dorso lato-rotundato ; adultd
lateraliter expansd, transversim undulato-costaté ; septorum margine flexuoso ; siphunculo
sub-ventrali ; apertura semi-ovali ; umbilico clauso.
Shell when young, smooth and regular, with flattish sides, a broad rounded back, and
semi-oval aperture ; when about two inches in diameter, it enlarges rapidly, expands at the
sides, and begins to undulate over the back; when adult, the whole shell is ribbed in
broad, coarse undulations, which are deepest on the back, but ill-defined on the sides ;
back marked by a line at first slightly raised, which in the old shell forms a ridge
between the undulations; umbilicus covered; septa flexuous ; siphuncle near the ventral
margin.
We have only seen one specimen of this species from the Chalk, which was found by
Mr. Wiest in the Chalk with siliceous grains of Chardstock; it is a young shell,
16 FOSSIL MOLLUSCA OF THE CHALK.
23 inches in diameter and 13 inch broad at the mouth; it is imteresting, as it shows
the change from the neatness of the young shell to the coarse irregular wavy form of the
adult.
This shell is found more plentifully in the upper*part of the Lower Green Sand, where
it reaches a diameter of 4 or 5 inches. M. D’Orbigny has not met with it in France.
When young, JV. wadulatus has considerable resemblance to JV. dargilliertianus, from
which it is distinguished by its closed umbilicus; in its undulated stage it cannot be
confounded with any other species.
9. NAUTILUS LaRGILLIERTIANUS, D’Orb. Plate VI, figs. 1 and 2.
NAUTILUS LARGILLIERTIANUS, D’Orbigny. Paléont. France. Terr. Crét., t. xviii.
NV. Testaé discoided, compressd, umbilicatd, delicatim striata ; lateribus complanatis ;
dorso planiusculo, in medio lineato ; umbilico magno, margine declivi ; aperturd ovato-
rhomboided ; septorum marginibus flecuosissimus ; siphunculo sub-ventralt.
Shell discoidal, with fine lines of growth which are not seen in the cast; with flat
sides and a somewhat flattened back, marked with a slightly raised mesial line; umbilicus
large, with perpendicular sides, exposing all the inner whorls; aperture rhomboidal
with rounded corners, deeply indented by the preceding whorl; margin of the septa very
flexuous ; siphuncle very near to the inner margin. In old shells the back is slightly
undulated.
Diameter 2 inches, breadth Zths of an inch.
This elegant shell is easily distinguished from the other Cretaceous species by the
rhomboidal form of the whorls, well-defined umbilicus, and flexuous septa; the stric are
only seen in very well-preserved specimens.
Found occasionally in the Grey Chalk at Lewes, and in the Chloritic Marl of the
Isle of Wight; more common in the Chalk with siliceous grains of Chardstock and
Chaldon.
M. D’Orbigny cites it as common in the Lower Chalk of the North of France.
10. Navtitus FLEuRiIAusIANUS, D’Ord. Plate VI, fig. 3.
NAUTILUS FLEURIAUsIANUS, D’Orbigny. Paléont. Frang. Terr. Cret., t. xv.
Navutitus Sowrrsyanus? D’Orbigny. Ibid., t. xvi.
N. Testé lateribus compressa, dorso rotundatd, sub-umbilicatd, levi; aperturd semi-
ovata ; septorum marginibus flexuosis ; umbilico minimo ; siphunculo sub-centralt. .
Shell with slopmg and somewhat flattened sides and rounded back, smooth, with a
very small umbilicus; mouth semi-oval, higher than wide, deeply indented by the pre-
NAUTILUS. 17
ceding whorl; margin of the septa flexuous ; siphuncle sub-central, but rather nearer to
the ventral than to the dorsal margin.
Diameter 33 inches, breadth 2 inches.
Found occasionally in the Chalk with siliceous grains, at Chardstock. M. D’Orbigny
quotes it as common in beds of the same age in the North and West of France.
Our specimens have a rounder back and more flexuous septa than M. D’Orbigny’s
figure of WV. flewriausianus, in which characters they approach his figure of JV. Sowerbyanus,
from which they are distinguished by a smaller umbilicus. I am inclined to regard them
both as one species, and have adopted the name of WV. fleuriausianus, as the other would
be liable to confusion with the WV. Sowerbii of the ‘Mineral Conchology.’ I have only
seen casts of the WV. flewriausianus, which do not show the siphunculus, and have
described its position upon the authority of M. D’Orbigny’s figure and description.
11. Navtitus Firtron1, Sharpe. Plate VI, fig. 4.
NavTILUs comMPREssUs, Fitton. Trans. Geol. Soc., 2d series, vol. iv, pp. 203 and
367, Note.
NV. testd levi, compressé, complanatd, umbilicata ; lateribus planis, obliquis ; dorso
angusto, rotundato, in medio lineato ; umbilico magno ; apertura truncato-sagittatd, apice
rotundata ; siphunculo sub-ventrali ; septorum marginibus flexuosissimis.
Shell discoidal, smooth; sides flat, sloping; back narrow and rounded, marked with a
faint lme along the middle; umbilicus large, allowing the inner whorls to be seen, its
walls nearly perpendicular; aperture sagittate with the angles rounded off; septa with a
very flexuous margin ; siphuncle very near the lower margin of the whorls.
Diameter about 3 inches, breadth 1 inch.
This shell has a good deal of resemblance to JV. Saxbii of Morris, in general form,
proportions, and flexure of the septa; but differs from that species in its rounded back.
This species was first noticed by Dr. Fitton in the Upper Green Sand, Western Lines
Isle of Wight, and placed in the Museum of the Geological Society ; it is called in his lists
NV. compressus, which name had unfortunately been previously applied to another species.
It has since been found by Mr. Wiest in the Chalk with siliceous grains of Chardstock ;_
both of the specimens are imperfect. It is named after the original discoverer.
Ammonites, Bruguiére.
Animal unknown: shell chambered, discoidal, compressed or ventricose, spiral, with
contiguous whorls regularly convoluted on the same plane, the last partially or entirely
concealing the previous whorl: chambers separated by transverse flexuous septa, deeply
sinuated towards the edges, divided into branching lobes, and traversed by a continuous
tube situated at the outer or dorsal edge of the shell; the last chamber large.
3
18 FOSSIL MOLLUSCA OF THE CHALK.
Ammonites are distinguished from other genera of discoidal chambered Cephalopods
by the branching lobes of their mantle, causing the edges of the septa to form a very
complicated pattern against the side of the whorl, which is seen when the surface is removed
or worn away. ‘The forms of these lobes have been used, as distinguishing specific
characters, by Von Buch and many subsequent writers. Although I am not disposed to
attach so much importance to them as is sometimes done, I have, as far as possible, given
au outline of the lobes of the septa of each species.
To facilitate description, Von Buch proposed to restrict the term /obe to the more sub-
divided and branching portions of the edges of the chamber which extend downward from
the mouth of the shell, and to call saddles the more rounded and less intersected divisions
which project upward towards the mouth; thus the outline of a septum is made up of /odes
alternating with saddles. The middle of the back of the whorl is occupied by the dorsal
lobe, opposite to which is the ventral lobe, which, abutting against the previous whorl, is
always concealed: between these are the /ateral lobes and saddles. References to these
names will be found in the explanation of Plate VII.
In using these characters, the observer must bear in mind that they vary at different
ages of the animal, and are therefore practically of less use to the conchologist than might
be expected. Not only do all the ramifications of the lobes mcrease in complexity during
the whole life of the Ammonite, a mere notch in the young stage growing into a branch
of its lobe, but the number of lobes may also increase with age. According to M.
D’Orbigny, all Ammonites have only six lobes at the earliest period of their existence ;
namely, the dorsal and ventral lobes, and the superior and inferior lateral lobes on each side
of the whorl. In some species this number continues the same through life; but more
commonly the lobes increase in number with the growth of the shell, small auvazlary lobes
being added on each side near the junction with the inner whorl. The number of auxiliary
lobes varies in different species ; but as this depends on the age of the shell, they form a
character of little service. Moreover, as the lobes are most branched near the edge of the
whorl, many of the minor ramifications are obliterated on the worn cast of an Ammonite.
The two sides of the shell being usually symmetrical, it is only necessary to figure the
outline of the septa of the back and one side. But there are some species of Ammonites
in which the siphuncle, instead of being placed at the middle of the back, is often found
“more or less on one side; and when this is the case, the lobes of the septa are also dis-
placed to the same extent, so that the tube remains in the middle of the dorsal lobe.
Most of those species are symmetrical when young, and the change takes place at very
different periods of growth in different individuals. ‘This curious irregularity is most often
seen in A. denarius, Fittoni, splendens, and Lyelli of the Gault, 4. Duncani and Callo-
viensis of the Kelloway’s Rock. ‘I'he displacement usually consists in shifting the tube to
one of the angles of the back; but specimens of 4. Calloviensis are found with the tube
placed near the middle of one of the sides. M. D’Orbigny has illustrated this deformity
in describing, in the Paléontologie Francaise, the species liable to it.
AMMONITES. 19
Many species of Ammonites are distinguished by a large lateral process formed on each
side of the mouth, either when the animal is full-grown or at intervals during its growth.
Such forms are mostly found in the Oolitic Formations, but 4. rostratus, which is common
jn the Upper Green Sand, affords a good example of such a mode of growth.
In many of the secondary strata are found pairs of shelly plates of very peculiar struc-
ture, which have received various names, and still more discordant explanations, from
different authors. Parkinson called them 7zgonellites,Von Meyer Aptychus, Deslongchamps
Minsteria. They have been thought by many writers to be external bivalve shells of the
Lamellibranchiate order; or internal shells of Cephalalopods; Riippell thought some of
them scales of Reptiles; some have been regarded as palatal teeth of Fishes; and M.
D’Orbigny has lately considered them the side plates of pedunculated Cirrhipedes. But
the opinion which seems to have most probability in its favour is that the Z'rgonellites were
the opercula of Ammonites, which view has been ably supported by Voltz;' the principal
reasons for this opinion are derived from the structure of the plates being analogous to
that of many opercula, and their having been often found within the open chamber of
Ammonites, to the mouths of which their form and size nearly correspond. Each plate is
triangular, with one straight edge, which laps over or under the corresponding edge of its
fellow plate. ‘The lines of growth are always seen on the concave side of the plates, show-
ing that to have been the external surface. Voltz divides the Aptychi (or Trigonellites)
into three sections: Ist, the cornez, consisting of a single (?) horny plate, with a flexible
fold down the middle; 2d, the zméricati, which have a pair of plates with an external
horny epidermis, covered internally, that is on the convex side, with calcareous layers laid
over one another like tiles; 3d, the ced/ulosi, which have a pair of plates with a thick,
cellular, calcareous layer on the inner or convex surface. he Zrigonellites are rare in the
Chalk ; those which have been found will be described in connection with the Ammonites
to which they are supposed to belong.
In the first volume of the ‘Journal of the Geological Society,’ p. 232, Mr. Strickland
has described some supposed opercula of Ammonites, consisting of one semi-oval calcareous
plate, without any suture, which have been found in the Lias: no similar form has yet
been found in the Chalk.
=~ b es)
1. AmMonives compLanatus, Mantell. Plate VII, figs. 1—3.
AMMONITES COMPLANATUS, Mantell. Fossils of the South Downs, p. 118.
— — Sowerby. Min. Conch., t. 569, fig. 1.
— LARGILLIERTIANUS, D’Orbigny. Paléont. Frang. Terr. Crét., pl. xcv.
A. testé discoided, compressissimd, leviusculd, tenuiter striatd ; striis numerosissimis
fleauosis, umbilicum versus obsoletis, deinde distinctis et ad margines dorsi sub-tuberculatis ;
1 Neues Jahrbuch, 1837, pp. 304 and 432.
20 FOSSIL MOLLUSCA OF THE CHALK.
dorso truncato, lateribus subcarinato, medio planiusculo ; apertura sagittata ; anfractibus
taterioribus occultis ; umbilico clauso.
Shell discoidal, much compressed, partially smooth, but marked with very numerous
striz, which are only faintly visible on the middle of the whorl, where they curve away
from the mouth, and more distinct towards the margin, where they are nearly straight;
each of the striz is produced into a point projecting beyond the edge of the truncated
back, thus forming a slight keel on each side of the back; whorls increasing very rapidly
in height, and entirely covering the umbilicus; mouth sagittate; lobes of the septa
numerous, and much subdivided.
Diameter 8 inches, height of the outer whorl 5 inches, thickness 1,8,ths of an inch.
Found in the Grey Chalk of Hamsey, near Lewes. The species is very rare; and I
have only seen the two specimens figured, which were collected by Dr. Mantell, and are
now in the British Museum ; M. D’Orbigny states that it is very rare in France, and has
been found at Rouen and Cassis, in the beds of the same age as in England.
This species and the next described, 4. odtectus, are nearly related, and are remarkable
for the rapid increase of the height of their whorls, which entirely close the umbilicus ; and
also for the great flexure of the upper edges of the lobes of the septa, which project
forward in the middle of the whorls, in a very unusual degree.
2. AMMONITES oBTECTUS, Sharpe. Plate VII, fig. 4.
A. testé discoided, compressissimd ; lateribus delicatim costatis: dorso truncato, tri-
carinato ; costis numerosissimis, complanatis, medio angulatis et tuberculatis; carinis
dorsalibus nodulosis; aperturé truncato-sagittatéd ; anfractibus «nterioribus occultis ;
umbilico clauso.
Shell discoidal, much compressed, with slightly convex sides, and a narrow truncated
back ; ornamented on the sides with numerous flat ribs, which rising at the umbilicus
slope forward in a straight line to the middle of the whorl, whence they bend back at a
sudden angle, and continue in a slight curve to the dorsal margin, where they terminate ;
every second or third rib bears a rounded tubercle at the angle, on the middle of the
whorl; and here and there a rib is inserted between the others reaching only from the row
of tubercles to the dorsal margin; the angle of flexure of the ribs varies with age, being
at first very obtuse, and changing gradually till it becomes about a right angle; back
narrow and truncated, with three keels, which are ornamented with small knobs equal in
number to the ribs; each lateral keel is marked off from the side of the whorl by an im-
pressed line running very near the edge ; whorls increasing very rapidly in height, and
entirely covering the umbilicus; section of the whorls sagittate with the point cut off;
septa with long, very narrow, and ramified lobes, which are only partially seen in the
specimen figured.
AMMONITES. 21
Diameter of our only specimen 22 inches, breadth of the aperture ?ths of an inch,
height of the last whorl 1#ths of an inch; but the specimen must have been much
larger, as it originally had, at least, one more whorl.
Found by Mr. Wiest at Chardstock, in the Chalk with siliceous grains.
This elegant shell has some characters which are so rare among the Ammonites, that
we only know one other species to which to compare it, 4. complanatus, Sow. (A. largil-
liertianus, D’Orb.); it agrees with that species in general form, in the embracing
~ character of the whorls, covering the umbilicus, and in the curve of the septa, which
advance towards the middle of the whorl, and fall back towards the ventral and dorsal
margins ; from this last character combined with the flexure of the ribs we conjecture that
the mouth had a sinus in the middle resembling that in the genera Wawtilus and
Bellerophon. The lobes of the septa have been imperfectly seen; they bear a strong
analogy to those of 4. complanatus, without altogether agreeing with them. The de-
scription being taken from a single imperfect specimen is necessarily incomplete: this
specimen appears to be unique.
ror
3. Ammonites Fatcatus, Mantell. Plate VII, figs. 59.
AMMONITES FALCATUS, Mantell. Fossils of the South Downs, t. xxi, figs. 6 and 12.
= -—— Sowerby. Min. Conch., t. 579, fig. 1.
== — D’Orbigny. Paleont. Franc. Terr. Crét., t. xcix.
— curvaTus, Mantell. Loc. cit., t. xxi, fig. 18.
ek = Sowerby. Min. Conch., t. 579, fig. 2.
A. testa discoided, compressd, bicurvato-costatd, tuberculatd ; tuberculis, costisque
numero variantibus ; dorso canaliculato, utrinque tuberculato ; umbilico mediocri ; apertura
oblonga.
Shell discoidal, and flattened, with numerous ribs extending from the umbilicus to the
edge of the back, in double curves, meeting in advancing angles on the middle of the
side, and variously tuberculated; back with tubercles on each side, and a hollow canal
in the middle; umbilicus of middling size, bounded by steep sides; whorls half con-
cealed ; aperture oblong ; septa with two lateral lobes, slightly subdivided.
The above are the most constant characters in this very variable species, in which the
ribs are either very broad or minutely sub-divided, or replaced by tubercles. The best
marked varieties are those which were described by Mantell and Sowerby as distinct
species, although specimens may be found with all the characters of both varieties com-
bined, as fig. 5. 4. falcatus originally included the forms without lateral tubercles, as our
fig. 7, and A. curvatus the more tuberculated forms, like fig. 6, which have two rows of
tubercles on each side of the back. We are indebted to M. D’Orbigny for uniting them.
The tubercles usually diminish in number and prominence, as the shell increases in
22 FOSSIL MOLLUSCA OF THE CHALK.
growth; but fig. 8 is a very remarkable variety, in which the tubercles have almost taken
the place of the ribs, of which only a few are to be seen in a very young stage.
Diameter 2 inches ; thickness ;*;ths of an inch.
Found sparingly in the Grey Chalk, the Chloritic Marl, and the Chalk with siliceous
grains, throughout the Southern Counties; and also in the Green Sand of Blackdown. It
occurs in beds of the same age in France.
A. falcatus is related to 4. lautus and A. tuberculatus, which have a similar canal down
the back; but the peculiarly curved ribs readily distinguish it from those species, while
its dorsal canal distinguishes it from several species which have ribs with a similar
double curve.
4, Ammonires varians, Sow. Plate VIII, figs. 5—10.
AMMONITES VARIANS, Sowerby. Min. Conch., t. 176, lower figures only.
— — Brongniart. Envir. de Paris, t. vi, fig. 5.
— — Bronn. Lethzea Geogn., t. xxxiii, fig. 2.
= — D Orbigny. Paléont. Franc. Terr. Crét., t. xcii, figs. 3, 4, & 5.
— — var. INTERMEDIA and var. SUB-PLANA, Mantell. Fossils of the
South Downs, t. xxi, figs. 2, 5, and 7.
— Bronenrtartil, Haan... Amm. et Goniat., No. 43.
A. testaé discoided, radiatd, tuberculatd, carinatd ; radiis numerosis flecuosis, plerum-
que furcatis, bi-vel tri-tuberculatis ; tuberculis parvis ; dorso carinato, lateribus angulatis,
tuberculatis, carind levi; umbilico medioert ; apertura truncato-sagittatd.
Shell discoidal, ornamented on the sides with numerous flexuous, simple, or forked
ribs, each of which bears a small tubercle at its rise on the edge of the umbilicus, and a
larger tubercle at its termination on the side of the back, and in some varieties an
additional tubercle at the point of bifurcation; umbilicus rather small and well defined ;
whorls half concealed ; back narrow with a prominent keel, and a row of tubercles at each
side; section of the whorls considerably higher than broad, sagittate with a truncated
top ; aperture with the upper part of the whorl projecting forward, and produced into a
blunt point. Septa with 5 or 6 trifid, subdivided lateral lobes.
Ammonites varians, as its name implies, assumes many forms, which may be arranged
under the four followimg varieties :—
Ist Var. sub-tuberculata, Pl. VIII, figs. 5, 6, and 8. The young shel] has about
fifteen slight tubercles round the umbilicus, connected by very faint ribs, with about
thirty well-marked tubercles at the edge of the back: the adult shell has the ribs more
prominent and less numerous, about twelve rising from the umbilicus, and increasing to
about twenty at the edge of the back, an additional distinct tubercle occurs at the
bifurcation of each rib, and a row of fainter tubercles usually occurs on the branches of the
divided ribs, half-way between the fork of the ribs and the back; making four rows of
AMMONITES. 23
tubercles on each side of the whorl; the margin of the umbilicus is rounded off; and thie
width of the aperture varies from seven to eight tenths of its height. This is the com-
monest form of the species.
2d Var. costata, Pl. VIII, fig. 9, of the same form and proportions as the preceding,
but with mere undulations of the surface in place of ribs ; the tubercles round the edges
of the umbilicus and of the back small, but distinct ; the other tubercles obsolete. ‘This
variety is rare.
3d Var. intermedia of Mantell, Pl. VIII, fig. 7; a much flatter shell than the lst and
2d varieties, the width of the aperture being only half the height of the whorl; the ribs
are prominent and more numerous, twenty in number at the umbilicus, increasing to
thirty at the dorsal margin; the dorsal tubercles are distinct, the others inconspicuous.
Not very abundant.
Ath Var. swb-plana of Mantell, Pl. VIII, fig. 10 ; proportions the same as the last, ribs
more numerous, but very slight; dorsal tubercles about fifty, small but distinct; no
tubercles on the side of the whorl ; umbilicus small, well-defined, with the side steep, and
bounded by an angular edge with very faint tubercles. Abundant at Ventnor in the Isle
of Wight.
The first three varieties usually reach a diameter of two inches to two inches and a
half; the fourth variety rarely attains an inch and a half in diameter.
Ammonites varians is found abundantly in the Grey Chalk, the Chloritic Marl, the
Chalk with siliceous grains, and the Upper Green Sand, wherever those Formations occur
in the southern parts of England. It is common in France in beds of the same age.
The 4. varians of Sowerby included 4. Coupe, which is here separated from it, in
accordance with the views of Brongniart and many other authors. ‘The reasons for this
separation will be found under 4. Cowper.
The variations in form of the shells still remaiming under 4. varians are so con-
siderable, as almost to justify our regarding the 1st and 2d varieties as one species, the 3d
and 4th as another; or, if we admitted M. D’Orbigny’s opinion, that the broader shells
were females and the flatter ones males, we might take the first two varieties to be the
former, aad the last two the males: but our present imperfect knowledge of the sexes of
hving Cephalopods does not justify such a division.
5. Ammonites Courzi, Brong. Plate VIII, figs. 1—4. Plate IX, fig. 1.
AMMONITES CoupPEI, Brongniart. Envir. de Paris, t. vi, fig. 3.
— — Haan. Amm. et Goniat., No. 42.
— — Bronn. Lethea Geogn., t. xxxiii, fig. 4.
_ VARIANS, Sow. Min. Conch., t. 176, middle and upper figures.
= — var. TUBERCULATA, Mantell. Foss. S. Downs, p. 116.
— — Haan. Amm. et Goniat., No. 45.
- — DOrbigny. Paléont. Franc. Terr. Cret., t. xcii, figs. 1, 2, and 6.
24 FOSSIL MOLLUSCA OF THE CHALK.
A. testd discoided, aliquando sub-inflatd, costatd, tuberculatd, carinatd ; costis inter-
ruptis, simplicibus vel furcatis, tri-vel quatuor-tuberculatis ; tuberculis prominentibus ; dorso
latiusculo, utrinque tuberculato, medio carinato; umbilico profundo; apertura truncato-
ovata.
Shell discoidal, with the whorls inflated when young, but somewhat flattened when
adult, ribbed, and tuberculated ; back broad and keeled, with a row of prominent tubercles
on each side; aperture ovate, with the upper part of the whorl projecting forward, and
produced into a blunt poimt ; umbilicus deep and rounded off at its upper edge. ‘The ribs
and tubercles vary much both in size and number at different stages of growth and in
different varieties of the species. Septa with four trifid, sub-divided lateral lobes.
This species admits of a division into two strongly-marked varieties, which Haan
regarded as distinct species :—
_ 1st Var. tuberculata of Mantell, whorls of the young shell (Pl. VIII, fig. 4,) inflated,
their width being equal to their height, with three rows of very prominent tubercles con-
nected by thick, ill-defined ribs; the tubercles of the inner row round the edge of the
umbilicus are the smallest, ten in number in a very young shell, twelve in a shell of 13 inch
in diameter; the tubercles of the next row, situated on the middle of the whorl, are very
large and prominent, and equal in number to the preceding; the tubercles of the outer
row on the edge of the back are of an intermediate size, and about half as many again as
the others; in the adult shell (Pl. VIII, fig. 2; Pl. IX, fig. 1,) the whorls are a little
flattened, the ribs better marked, the tubercles rather less prominent, and a fourth row of
small tubercles is inserted between the middle and the dorsal rows; the width of the
aperture is equal to =°,ths of the height of the whorl. The usual diameter of this variety is
about 23 inches, but specimens are occasionally found in the Grey Chalk of 6 inches
diameter: this enlargement is not due to an increased number of whorls, but to a larger
size at every stage of growth.
2d Var. inflata, P). VIII, fig. 1, whorls inflated, their width being one fourth more
than their height, with two rows of very large and prominent tubercles; those of the
inner row which are seated on the middle of the whorl being the largest, and ten or
eleven in number; the outer row on the edge of the back somewhat smaller, and sixteen
or seventeen in number; back broad, with a very prominent keel. This variety reached
25 inches in diameter, and 13 of an inch in thickness.
Ammonites Coupei is common in the Chloritic Marl of the Isle of Wight, and in the
Chalk with siliceous grains of Dorsetshire; and is found sparingly in the Grey Chalk of
the Southern Counties.
The original description of 4. varians in the ‘Mineral Conchology’ included our
A. Coupei, which was first separated by Brongniart: most subsequent authors have re-
garded them as distinct species, until they were reunited by M. D’Orbigny, who con-
siders that all the varieties of the two species pass into one another, and may in part be
accounted differences of sex, the more inflated forms being regarded as females. We
AMMONITES. 25
know nothing certain respecting the sexual differences of form in Ammonites ; but even
if it were admitted that such. differences existed, they would not suffice to bring
A. varians and A. Coupei together, as in each species there are two well-marked differences
of form, so that there are varieties enough to supply distinct sexes in each species. The
young shells of both varieties of 4. Coupei nearly resemble each other; the differences
between them begin in their middle stage, and increase as they grow older, the 1st variety
gradually approaching 4. varians in form, while the 2d variety recedes farther from that
species. The young 4. varians always present a strong contrast, in its flat, faintly-ribbed
form, to the rounded and tuberculated young shell of 4. Cowpei: it is only in the adult
form of one variety of each species that any confusion can arise between them.
6. Ammonitxs cinctus, Mantell. Plate IX, fig. 2.
AMMONITES cINCTUS, Mantell. Fossils of the South Downs, p. 116.
—_: — Sowerby. Min. Conch., t. 564, fig. 1.
A. testaé discoided ; ambulacris rotundatis, transversim costatis ; costis tenuibus, alter-
natim majoribus furcatis ambulacrum totum amplectentibus, minoribus intermediis dorsalibus ;
dorso rotundato ; umbilico parvo ; apertura ovali.
Shell discoidal, with rounded whorls crossed by numerous slight, irregularly flexuous
ribs; these are twelve in number at the umbilicus, divide into two before reaching the
middle of the side, and are continued over the rounded back; between each of the
branches of the larger ribs there are one or more short ribs, which only extend across the
back; umbilicus small; whorls about two thirds concealed; aperture oval. The septa
have not been seen.
Diameter, 3°8 inches; width, 1°1 inch.
From the Grey Chalk of Middleham, Sussex. The figure is taken from Dr. Mantell’s
original specimen, now in the British Museum. No other specimen of the species is
known.
A. cinctus is well characterisd by its very peculiar ribbing, and cannot be confounded
with any other species. The specimen shows the form of the mouth very nearly complete.
Hoplites
7. Ammonites BunBURIANUS, Sharpe. -Plate IX, fig. 3.
A. testé discoided, compressé, lateribus transversim multi-sulcata, dorso tri-seriatim
tuberculata : umbilico parvo ; apertura ovato-rhomboided.
Shell discoidal with flattened sides; crossed by twenty-five unequal furrows, continued
over the back, which is marked by three rows of tubercles; the furrows are very small
near the umbilicus, and gradually grow wider and deeper towards the back where they
are most important: on the back the spaces between the furrows form broad ribs, each of
which has three longitudinally flattened tubercles, one on the middle and one on each side
4
26 FOSSIL MOLLUSCA OF THE CHALK.
of the back; umbilicus small, with steep sides; whorls more than half concealed ; aper-
ture oval; septa with three slightly indented lateral lobes.
Diameter, 14 inch; width, 3ths of an inch.
Only one specimen has been seen, which was presented by Mr. E. H. Bunbury to the
Museum of Practical Geology; it is from the Chalk with siliceous grains of Chardstock,
Somersetshire. The species is named after its discoverer.
8. AMMONITES PERAMPLUS, Mantell. Plate X, figs. 1—3.
AMMONITES PERAMPLUS, Mantell. Fossils of the South Downs, p. 200.
—_ — Sowerby. Min. Conch., t. 357.
= —_ D’Orbigny. Paléont. Frang. Terr. Crét., t. 100, figs. 1, 2.
— Prosperianus, D’Orbigny. Loc. cit., t. 100, figs. 3 and 4.
A. testé subinflati: anfractibus rotundatis ; junioribus costatis, costis flexuosis,
amplectentibus, quarum sex majoribus intus tuberculatis ; adolescentibus utrinque undato-
costatis, dorso plano ; adultis rotundatis, intus sub-undatis ; senioribus rotundatis, simplici-
bus : apertura imprimis semt-circulari, deinde ovata.
Shell gibbose, with rounded whorls, of which nearly two thirds are concealed, varying
in proportions and ornament at different periods of growth; side of the umbilicus very
steep ; septa with four or five unequally trifid, branching lateral lobes.
The young shell, up to a diameter of two inches, has the whorls broader than they are
high, ornamented by about twenty-five rounded ribs, which bend forward as they cross the
back ; of these six are stronger than the others, and rise from six large pointed tubercles
on the edge of the umbilicus, fig. 3, 4. prosperianus, D’Orb. At a diameter of four to
six inches, the intermediate minor ribs disappear, the tubercles become obsolete, and the
back smooth, and there remain about twelve broad, rounded, straight ribs on each side of
the whorl, which do not meet on the back, fig. 2.
When the shells reaches a diameter of a foot, the whorl is higher than broad, and
nearly smooth, with no trace of its previous ornament, except a series of blunt ill-defined
tubercles round the umbilicus, connected with faint undulations on the inner half of the
whorl (fig. 1).
Very old specimens, which may be found exceeding two feet in diameter, have the
whorls smooth and entirely devoid of ornament, and the aperture laterally compressed.
A. peramplus is found in the middle part of the Chalk throughout the counties of
Kent, Sussex, Surrey, Hertfordshire, and Wiltshire, and the Isle of Wight; but is most
abundant in the South Downs. It reaches from the white chalk without flints high up into
the chalk with flints, but large individuals are only found in the lower parts of its range,
the uppermost beds in which it occurs only containing very small specimens. M. d’Orbigny
quotes it only from the Upper Green Sand of the South of France.
M. dOrbigny conjectured, p. 335, that his 4. prosperianus might, perhaps, prove the
young of A. peramplus, which farther observation has shown to be the case.
AMMONITES. 27
Frio not yer ‘3
9. Ammonites Wootueari, Mantell. Plate XI, fig. i and 2.
Ammonites WooLtiGari, Mantell. Fossils of the South Downs, t. xxi, fig. 16; t- xxii,
fig. 7.
— — Sowerby. Min. Con., t. 587, fig. 1.
— — D' Orbigny. Prodrome de Paléontologie, p. 189.
— — (not), D’Orbigny. Pal. Franc., t. 108, fig. 1-3.
c — Carotinus? D’Orbigny. Loc. cit., t. xci, fig. 5, 6.
A. testd subcompressd, costatd, tuberculatd, interrupté carinatd : juniore, costis 16-18
elevatis, tri-tuberculatis, dorso interruptis, carind dorsali profundé serrata ; adolescentz,
costis rarioribus ad dorsum uni-tuberculatis, carind dorsali obsoleté ; adultd, costis bi-
tuberculatis, tuberculis mazimis, dorso concavo: umbilico lato: apertura oblonga.
Shell compressed, ribbed, tuberculated, and keeled; changing its form and ornaments
as it enlarges; when two to three inches in diameter it has sixteen to eighteen sharp,
elevated ribs on the side of each whorl, each rib bearimg three tubercles, one near the
umbilicus and two near the back; the back has a sharp and deeply serrated keel, the
serrations corresponding in number to the ribs: when about four inches in diameter, the
keel is less prominent, the ribs are fewer and nearly obsolete, and bear one enormous
tubercle at their dorsal end: as the shell continues to enlarge, the whorl grows broader,
and has two rows of ten very large tubercles on each side, one close to the umbilicus, the
other at the dorsal edge, the back has entirely lost its keel, and is smooth and hollow
between the dorsal tubercles: umbilicus large and shallow, with two thirds of the whorls
exposed: aperture at first oblong and narrow, ultimately nearly of equal height and
breadth. The septa have not been clearly seen, they appear to have four or five trifid
lateral lobes.
Diameter of old shell, 1 foot; width, 3 inches.
A rare shell in the Middle and Lower Chalk of Sussex.
There is hardly any species of Ammonite which undergoes so great a metamorphosis as
A. Woollgari ; the young and middle stages of growth were well figured by Dr. Mantell ;
the older stage is not often met with, the only specimen which I have seen is in Mr.
Baber’s collection, but is too imperfect to figure. The shell described as 4. Woollgari
in the ‘ Paléontologie Frangaise,’ has no resemblance whatever to Dr. Mantell’s species ;
this error is pointed out by M. d’Archiac, in the ‘ Histoire des Progrés de la Géologie,’
vol. iv, p. 347, note, and has been corrected by M. d’Orbigny in the ‘Prodrome de
Paléontologie,’ vol. i, p. 188. In the latter work M. d’Orbigny quotes his 4. Carolinus,
Pal. Frang., t. 91, fig. 5 and 6, as the young of 4. Woollgari ; which identification is very
doubtful, as the French shell has twice as many ribs, is less compressed, and has the keel
more completely separated from the ribs by two regular channels, than our species.
or
28 FOSSIL MOLLUSCA OF THE CHALK.
10. Ammonires Grirritau, Sharpe. Plate XI, fig. 3.
A. testé discoided levi, sulcis 4 vel 5 flecuosis ornatd: dorso rotundato (impresso ?),
umbilico parvo : apertura semiovali: semptorum marginibus ramosissimis, lobis trifidis.
Shell discoidal, smooth; each whorl crossed by four or five slightly waved, transverse
furrows, bounded on each side by a slight elevation; back rounded and marked in the
cast by a small medial groove; umbilicus small and well defined; whorls four fifths
concealed ; aperture semi-oval; margins of the septa very complex, with four trifid
lateral lobes.
Diameter, 5 inches; width 23 inches.
Found in the hard Chalk of Aughanloe and Benbraddagh, in the County of Derry, by
the Ordnance Geological Surveyors.
The specimens examined being all internal casts, the above description is necessarily
unperfect, and may require modification when better materials are found. ‘The species is
nearly allied to 4. Lewesiensis, Sow., and A. Mayorianus, d’Orb.; it is distinguished from
the former by its transverse furrows, from the latter by less breadth at the back, and from
both by the want of transverse ribs, and a smaller umbilicus: the lobes of the septa of the
three species are much alike. The shell is named after Richard Griffith, Esq., to whose
labours we are indebted for the Geological Map of Ireland.
11. Ammonites AusTENI, Sharpe. Plate XII, fig. 1 and 2.
A. testé discoided, compressd, transversim costatd; costis flecuosis inequalibus,
majortbus paucis ambulacrum amplectentibus, minoribus numerosis dorsalibus: dorso
rotundato : umbilico parvo : apertura rotundato sagittata.
Shell discoidal, transversely ribbed: whorls flattened at the sides, rounded over the
back, ornamented with numerous unequal flexuous ribs, all passing over the back, of which
a few, larger than the rest, embrace the whole whorl, the others only reaching to the
middle of the side; the number of larger ribs varies, being eight or ten on the whorl of a
young, and about twenty on that of an old shell: back narrow and rounded: umbilicus
small, and bounded by steep sides exposing half the inner whorl: aperture bluntly
sagittate. j
Diameter of the specimen fig. 1, 16 inches; height of outer whorl, 6 inches; width of
the aperture, 35 inches: it often reaches much larger dimensions.
Found in the Grey Chalk of Surrey, Kent, and Sussex, and in the Upper Green Sand
near Dorking.
It is singular that a species to be found in abundance near London should never have
been published; it has probably been mistaken by collectors for 4. planulatus, Sow., to
which it has some resemblance; but that species has transverse furrows where this has
AMMONITES. 29
projecting ribs. I have named it after Robert A. C. Austen, Esq., F.R. and G.S., in whose
neighbourhood at Chilworth, this Ammonite is very abundant.
Des oc ere lo ©
12. AmmoniTis pLaANuLATUS, Sowerby. Plate XII, fig. 3 and 4.
AMMONITES PLANULATUS, Sowerby. Mineral Conchology, t. 570, fig. 5.
A. testa discoided : anfractibus complanatis, externé costatis, interné levibus ; sulcis 5
transversis subflexuosis, impressis ; costis numerosis, brevibus: dorso rotundato transversim
costato: umbilico magno: aperturd semi-ovatd: lobis septorum lateralibus inequaliter
bifidis.
Shell discoidal, with four or five whorls flattened on the sides, and rounded on the
back, crossed by five deep, slightly flexuous furrows, between which are many short slight
ribs, which cross over the back and only reach the middle of the side of the whorl:
umbilicus large and well-defined, leaving three fifths of the inner whorls visible: aperture
semi-oval : lateral lobes of the septa unequally bifid.
Diameter, 23 inches.
Rare in the Grey Chalk near Lewes and Bonchurch; common in the Upper Green
Sand near Cambridge.
I have seen but few specimens of this species from the Chalk, and as that originally
figured by Sowerby is badly preserved and somewhat crushed, and does not show the
margins of the septa, a figure is added of a well preserved internal cast from the Upper
Green Sand. M.d’Orbigny unites to Sowerby’s species, under the name of 4. Mayorianus,
an Ammonite found in the Lower Green Sand and Gault of France, which differs from
our species in having only four transverse furrows instead of five, the furrows more
flexuous, and bounded by stronger swellings, and the cast entirely smooth; it has,
moreover, the lateral lobes of the septa trifid, which distinguishes it from Sowerby’s
species. I cannot, therefore, regard his species as identical with ours. M. d’Orbigny’s
reason for dropping Sowerby’s specific name, that it had been previously used by
Schlotheim for another species, is also insufficient: since Schlotheim’s species being
abandoned by every one, including M. d’Orbigny himself, ‘Terr. Jurass.,’ vol. i, p. 509,
the name remains open for the next species to which it has been applied, which is the one
here described.
13. Ammonites catinus, Mantell. Plate XIII, fig. 1.
AMMONITEs caTINUs, Mantell. Fossils of the South Downs, t. xxii, fig. 10. (Not t. xxii,
fig. 5.)
A. testa inflata : anfractibus paucis, latis, rotundatis, lateribus 10-12 tuberculatis, dorso
levibus : umbilico lato, profundo: apertura transversd, semi-circulari.
‘Shell gibbous, with three or four broad whorls, depressed and smooth on the back,
30 FOSSIL MOLLUSCA OF THE CHALK. —
elevated and tuberculated on the sides near the large and deep umbilicus; tubercles
10 to 12 on each whorl, large and ill-defined; inner whorls half concealed: aperture
transverse, nearly semicircular.
Diameter, 10 inches ; width of aperture, 5 inches.
Very rare in the Grey Chalk of Wiltshire and Sussex.
This rare Ammonite, of which only two specimens have been met with, is the only
species yet known in the Chalk of the Family of the Coronaru, so abundant in the middle
Oolites.
A misprint in the explanation of Dr. Mantell’s Plate xxii, where fig. 5, is called 4. catinus
instead of 4. zavicularis, has led to this species being confounded with 4. Mantellii, both
in the ‘ Paléontologie Francaise,’ and in Bronn’s ‘ Index Paleontologicus.’
14. Ammonites Porriocki, Sharpe. Plate XIII, fig. 2 and 3.
AMMONITES FIssicosTaTus, Portlock. Geology of Londonderry, &c., pp. 408 and 764.
A. testa inflata, costatd, tuberculaté : ambulacris rotundatis : juniore, tuberculis latera-
libus 10, costis 20 transversis, dorso interruptis; adultd, tuberculis binis, dorsalibus,
majoribus ; costis rarioribus: umbilico parvo, profundo: aperturd transversim ovali:
septorum marginibus lateraliter trilobatis, lobis trifidis.
Shell gibbous, with few rounded whorls wider than high, and a small deep, smooth
umbilicus: when one and a half to two inches in diameter the whorl has ten large blunt
tubercles on the middle of each side, and twenty strong rounded ribs, rising either singly
or in pairs from the tubercles, and curving slightly forward to near the middle of the back,
where they become obsolete; when three inches in diameter only one rib rises at each
tubercle, which bears a second larger tubercle near the middle of the back, and the
intervening ribs disappear : in the internal cast the back has a slight medial groove: inner
whorls nearly half concealed: aperture transversely oval: septa with three trifid lateral
lobes.
Diameter, 3 inches; width of aperture 2 inches.
Found in the hard Chalk of Tamlaght, in the county of Derry, by the Ordnance
Geological Surveyors.
The young shell bears some resemblance to A. fissicostatus, to which this species was
first referred, but it is distinguished by more transverse whorls and fewer ribs, and at a
later stage of growth by the large dorsal tubercles. I have named it after Lieutenant
Colonel Portlock, R.E., who conducted the Geological branch of the Ordnance Survey of
Ireland at the time the specimens were found, and first published a notice of them.
AMMONITES. 31
Dovvilleicevas
15. Ammonites EvompHALUS, Sharpe. Plate XIII, fig. 4.
A. testé inflatd, costatd, tuberculatd: anfractibus latis, dorso depressis, lateribus
angulatis, spinosis: costis inequalibus ; majoribus alternantibus latero bi-tuberculatis, ad
dorsum bifidis: dorso depresso, transversim costato, demum tuberculato: umbilico magno,
profundo : apertura transversd, angulata : septorum marginibus lobis 4 trifidis simpliciusculis.
Shell gibbous, with a broad flattened back and angular whorls, crossed by numerous
unequal tuberculated ribs, which bifurcate at the back; the ribs are about twenty in
number on the side of the whorl, alternately larger and smaller; the larger ribs bearing a
small tubercle near the umbilicus, and a strong spine at the edge of the back; the number
of ribs on the back is about double that on the sides of the whorl, two springing from
each spine, curving forwards and meeting again at the opposite spine; about every fourth
dorsal rib is larger than the others, and bears two slight tubercles: umbilicus broad and
funnel-shaped, leaving three fourths of the inner whorls visible: aperture transverse and
angular : septa with four very simple, trifid, lateral lobes, and the lateral saddle very small.
Diameter, three fourths of an inch; width of aperture, half an inch; height of the
last whorl, one third of an inch.
From the base of the Lower Chalk, at Man of War Cove, on the coast of Dorsetshire,
in the collection of E. H. Bunbury, Esq.
Only one imperfect specimen of this pretty Ammonite has been seen; in many
characters it is closely related to 4. Martiniz, D’Orb., having, like that species, the lateral
saddle much smaller than the first auxiliary saddle, but it has a flatter back than
A. Martini, and somewhat different ribbing.
Ace nihoceras
16. Ammonites Laticiavius, Sharpe. Plate XIV, fig. 1.
A. testa discoided : anfractibus paucis, planatis, costatis, tuberculatis ; costis 35 radian-
tibus, 8-tuberculatis, dorso interruptis: umbilico parvo: dorso, marginibus bi-tuberculatis,
medio planiusculo: apertura rhomboidali.
Shell with three or four whorls, flattened on the sides; ornamented on each side with
thirty-five equal, straight ribs, each bearing four tubercles, not continued across the back ;
in the young shell the ribs are either single, or unite in pairs at the umbilicar tubercle,
but after reaching a diameter of three inches, each rib is quite distinct: tubercles in eight,
nearly equidistant rows, three on the flat side of the whorl, and one on each side of the
back: umbilicus small and well defined, leaving four fifths of the inner whorls visible:
back smooth and hollow between the tubercles: aperture rhomboidal.
Diameter, 65 inches ; height of last whorl, 3 inches; width of aperture, 23 inches.
A very rare shell in the Grey Chalk of the Isle of Wight.
This species belongs to the large group of Ammonites with squared whorls and straight
32 FOSSIL MOLLUSCA OF THE CHALK.
tuberculated ribs, of which 4. Rhotomagensis is usually taken as the type; the septa have
not been well seen.
17. Ammonites OupHAmi, Sharpe. Plate XIV, fig. 2.
AMMONITES ALTERNATUS, Portlock. Geology of Londonderry, &c., pp. 408 and 764.
A. testi discoided: anfractibus ellipticis, transversim radiatis; radiis alternatim
majoribus, dorso interruptis: dorso rotundato, impresso: umbilico magno: apertura semi-
ovali : lobis septorum trifidis ramosissimis.
Shell discoidal, with slightly flattened, rounded whorls, ornamented with numerous
transverse ribs, alternately reaching the umbilicus, or stopping on the side of the whorl, but
all interrupted at the back: umbilicus large and shallow, leaving one third of the inner
whorls visible: back marked in the internal cast with a slight medial groove: aperture
semi-elliptical: margins of the septa with three trifid, branching, lateral lobes.
Diameter, 4 inches ; height of last whorl, 1§ inch, width of aperture 1} inch.
Found in the hard Chalk of Dungiven, in the County of Derry, by the Ordnance
Geological Surveyors.
This species is closely allied to 4. Lewesiensis, Sow., having the same general form and
grooved back, and nearly similar septa; the most obvious distinction is in the ribs, which
in A. Lewesiensis are equal, and all die out on the side of the whorl without reaching the
umbilicus. Having only seen one waterworn specimen of 4. Oldhami, I offer the
description of it with some diffidence. It is named after Thomas Oldham, Hsq., of the
Ordnance Geological Survey of Ireland.
A. alternatus, Woodward, should be expunged from our catalogues, resting on an
execrably drawn figure of a broken specimen of 4. interruptus; which I learned from
seeing Woodward’s original drawing, in the possession of Mr. 8. P. Woodward of the
British Museum.
18. AmmonitTEs LEpTonEMA, Sharpe. Plate XIV, fig. 3.
A. testé discoided, compressiusculd, transversim subtilissimé costatd: costis numero-
sissimis, simplicibus, flecuosis, ambulacrum totum amplectentibus : umbilico magno: dorso
angustato, rotundato: apertura sagittato-ovata.
Shell discoidal, with four whorls rounded at the umbilicus, and slightly compressed
towards the back, enlarging rapidly, and ornamented by very numerous, equal, fine, thread-
like, flexuous ribs, which embrace the whole whorl; umbilicus large and shallow; back
narrow, and rounded ; aperture ovate.
Diameter, 1? inch, height of last whorl, seven eighths; width of aperture, five eighths
of an inch.
Very rare in the Grey Chalk of Ventnor, Isle of Wight.
a
AMMONITES. 33
This species resembles 4. Vellede, Mich., in its general form and elegant thread-like
ribs, but-is at once distinguished by its larger umbilicus. The specimen figured is the
only one which has come under my notice.
A * £ ae
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19. cinta RuotromaceEnsis, Defrance. Plate XVI, fig. 1—4.
AMMONITES RHOTOMAGENSIS, Brongniart. Environs de Paris, t. vi, fig. 2.
— a Sowerby. Min. Conch., t. 515.
— — Bronn. Lethza Geogn., t. xxxiii, fig. 1-3.
— a D’Orbigny. Pal. Franc., t. 105 and 106.
— SussEexrEensis, Mantell. Geol. Sussex, t. xxi, fig. 10. (Not t. xx, fig. 2.)
A. testa discoided, costatd, tuberculata : anfractibus tumidis, quadrato-rotundatis : costis
rectis, simplicibus, rotundatis, equalibus ; junioribus septem, adultis sex-tuberculatis: dorso
juniore rotundato, tuberculis triserialibus ; adulto bituberculato, transversim costato, vel
medio plano: umbilico magno : septorum lobis lateralibus inequaliter bifidis ?
Variat anfractibus planiusculis, tuberculatis ; costis subobsoletis ; dorso plano.
Shell discoidal ; whorls tumid, flattened at the back and sides, with nearly a square
section ; about one third concealed ; crossed by about twenty-four simple, straight, rounded
ribs, which when young bear seven tubercles, and when full grown six tubercles each; the
tubercles are thus placed,—one row near the umbilicus, and two rows on each side of the
back, the seventh row on the middle of the back disappears in adult shells, leaving the
back either smooth and flat, or crossed by a continuation of the ribs; umbilicus large and
ill-defined, with sloping sides. The lateral lobes of the septa are unequally bifid ?
Diameter, 8 inches ; width, 35 inches ; height of aperture, 3 inches.
Very abundant in the Grey Chalk of all the southern counties, and in the Chloritic
Marl of the Isle of Wight, and Chalk with silicious grains of the West of England.
The 4. Rhotomagensis, as above defined, presents very constant characters; from its
youngest stage, fig. 3, till it has attained about two thirds of its full size, the only change
is a gradual increase in the number of the ribs, but the form and number of the tubercles
continues the same; this distinguishes it from 4. Sussexiensis and A. Cunningtoni,
in both of which the dorsal are, in young shells, more numerous than the lateral tubercles.
In the adult 4. Rhotomagensis the tubercles on the middle of the back disappear; in
some specimens the ribs are continued prominently across the back, in others the back is
flat and nearly smooth. The size at which the change takes place varies very much.
Specimens are often found which, though less than three inches in diameter, have all the
characters of the adult shell, one of these is represented of the natural size in fig. 2; but
more frequently they reach nearly six inches in diameter before losing the dorsal tubercles,
as in the case of fig. 1. The superior lateral lobe of the septa is always bifid, with more
or less unequal terminal branches; the termination of the next lateral lobe varies, some
34 FOSSIL MOLLUSCA OF THE CHALK.
specimens having it distinctly trifid, as it is figured in the ‘ Pal. Frang.,’ fig. 106, while
others have it unequally bifid.
A marked variety is found in the Chalk with siliceous grains of Somersetshire and
Dorsetshire, in which the ribs are nearly obsolete; but the general form of the shell, the
tubercles, and the outline of the septa identify the species.
M. d’Orbigny unites 4. Aippocastanum, Sow., to A. Rhotomagensis, in which I cannot
coincide ; the unequal ribs of the former contrasting too strongly with the extreme regularity
of the latter to admit of their belonging to one species.
20. Ammonites Sussexiensis, Mantell. Plate XV, fig. 1.
AmMMONITES SussEXIENSIS, Mantell. Geol. Sussex, t. xx, fig. 2. (Not t. xxi, fig. 10.)
A. testi discoided, costatd, tuberculatd : anfractibus tumidis, quadrato-rotundatis : costis
rectis, lateraliter simplicibus, bituberculatis ; gunioribus, dorso bi- vel tri-divisis, tri-tuber-
culatis ; adultis, dorso continuis simplicibus: umbilico magno: septorum lobis lateralibus,
primo bifido, secundo trifido.
Shell discoidal; whorls tumid, flattened at the back and sides, with nearly a square
section, very little concealed ; ornamented with sixteen or eighteen tuberculated ribs; on
the sides of the whorls the ribs are all equal, straight, rounded, and bearing two large
tubercles, one near the umbilicus, the other near the back; but the dorsal portion of the
ribs varies with the age of the shell; at three inches diameter (the youngest examined)
each rib divides on the back into two or three ribs, which reunite at the opposite tubercles
and bear three small tubercles each; a little later it is only the middle tubercle which is
divided into two; after this the rib is continued across the back as in one form of A.
Rhotomagensis: umbilicus very large, concealing hardly one fifth of the inner whorls.
The superior lateral lobe of the septa is bifid, the inferior lateral lobe trifid.
Diameter, 6 inches; width, 2 inches; height of aperture, 24 inches.
Found occasionally in the Grey Chalk near Lewes, Sussex.
The two shells originally figured in the Geology of Sussex by Dr. Mantell, under the
name of 4. Sussexiensis, belonged to two different species, to one of which the name of
A. Rhotomagensis had just before been given in France; the other being the species above
described as 4. Sussexiensis. The distinctions between them having been overlooked, they
were united together by Sowerby in the ‘ Mineral Conchology,’ vol. vi, p. 25, and all
subsequent authors having adopted the same view, 4. Sussexiensis has been viewed as a
synonym of 4. Rhotomagensis: the adult shells, though a good deal alike, may be
distinguished by the number of their ribs, but in their younger stage the differences in the
dorsal ribs and tubercles are too great to allow of any confusion between them.
AMMONITES. 35
21. Ammonites Cunninetont, Sharpe. Plate XV, fig. 2.
A. testé inflata, tuberculato-spinosd: anfractibus tumidis rotundatis ; lateraliter
biseriatim spinosis; dorso planulatis, tuberculatis: tuberculis dorsalibus imprimis tri-
serialibus, medio numerosioribus, deinde obsoletis: umbilico magno: apertura transversim
ovali : septorum lobis lateralibus, superiore bifida, inferiore trifidd.
Shell with few broad rounded whorls, each with two lateral rows of about ten spinose
tubercles, one row of moderate size near the umbilicus, the other of large spines at the edge
of the back: three rows of smaller elongated tubercles on the back; those of the two
outer rows corresponding in number to the lateral spines; im the central row two or three
smaller tubercles to each of the others: as the shell increases in size the tubercles of the
middle row gradually disappear, and the other dorsal tubercles coalesce with the spines,
leaving the back smooth, and only four rows of Jarge spines on the whorl: umbilicus
large, leaving nine tenths of the inner whorls visible: aperture transversely oval: superior
lateral lobe of the septa bifid, inferior lateral lobe trifid.
Diameter, 6 inches; width, 34 inches; height of aperture, 24 inches.
The only specimen seen was found in the Grey Chalk of Upton Scudamore, near
Warminster.
This species is nearly related to 4. Sussexiensis, from which it is distinguished by its
broader whorls, fewer and larger lateral tubercles, and different arrangement of the dorsal
tubercles. The species is named after William Cunnington, Esq., F.G.S., of Devizes,
whose zeal in illustrating the Geology of his neighbourhood entitle him to our gratitude.
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AMMONITES. 37
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22. Ammonites CenomaneEnsis, D’Archiac. Plate XVII, fig. 1.
AMMONITES CENOMANENSIS, D’ Archiac. Mém. de la Soc. Géol. de France, 2me serie,
vol. ii, pp. 62 and 78; Histoire des Prog. de la Géol.,
vol. iv, p. 347, note.
— — D’Orbigny. Prodrome, vol. ii, p. 146.
— WooLuicakl, Id. Pal. Frang. Terr. Crét., vol. i, t. 108, figs. 1—3.
— VIELBANCII ? Td. Prodrome, vol. ii, p. 189.
A. testi inflata, transversim costato-tuberculatd ; anfractibus quadratis ; costis nume-
rosis, rectis, etate juniort ad dorsum quinque-tuberculatis, adulté simplicibus, continuis,
bituberculatis ; dorso latissimo, utroque latere tuberculato.
Shell inflated; whorls nearly square, crossed by about sixteen thick, straight, equal
ribs; each rib starts from a large tubercle on the margin of the umbilicus, and bears
another larger tubercle at the side of the back; the very young shell has not been seen ;
but at 4 inches diameter there are three tubercles on the dorsal part of each rib, between
the two larger ones already mentioned; at the diameter of 8 or 9 inches these three
tubercles are lost in a strong straight rib crossing the back, and forming right angles at
its continuation with the lateral ribs; in the still older shell, of a foot in diameter, the
ribs are less prominent, but the two tubercles at the sides of the back project 13 inch.
Largest diameter, 1 foot; width, 5 inches; height of aperture, 4 inches.
Common in the Grey Chalk of Kent, Surrey, and Sussex.
This Ammonite is so closely related to 4. Rhotomagensis, that it may perhaps be only
a variety of that species. The principal differences are in the ribs of the old shells, which
in 4. Rhotomagensis become less and less distinct, till they finally disappear ; in 4. Ceno-
manensis grow very prominent and square, and finally run into large projecting horns.
It appears to have been distinguished by M. D’Archiac and M. D’Orbigny indepen-
dently. The latter author first confounded it with 4. Woollgari, of Mantell, with which
it has little m common; but M. D’Archiac gave it the name which it must retain.
23. AMMONITES HIPPOCASTANUM, Sowerby. Plate XVII, figs. 2, 3, and 4.
AMMONITES HIPPOCASTANUM, Sowerby. Mineral Conchology, t. 114, fig. 2.
A. testd inflata, costatd, spinoso-tuberculatd ; anfractibus paucis, celeriter crescentibus,
angulatis ; costis 12—20 valde inequalibus, tuberculatis ; tuberculis 7 seriatis, inequalibus ;
lateralibus interdum spinosis: dorso lato, 5 tuberculato : umbilico parvo, profundo : aper-
turd transversim rhomboided.
Shell gibbose, with few broad and angular whorls, which increase rapidly in size,
ornamented with transverse, unequal ribs, and seven rows of large unequal tubercles:
7
38 FOSSIL MOLLUSCA OF THE CHALK.
when young, the ribs are about twelve in number, nearly equal, each bearing seven
tubercles; one large, close to the umbilicus; another, very large and conical, near the
side of the back ; and three on the back, which are smaller and compressed laterally : in
the middle stage there is occasionally one small rib, bearing three or five tubercles,
between the larger ones; and in the adult shell there are usually two such smaller tuber-
culated ribs between the principal ones, making about twenty ribs on the whorl, and the
tubercles are very unequal in size: back very broad: umbilicus small and deep, exposing
half the inner whorls: aperture transversely rhomboidal: septa with a very broad dorsal
saddle, and two lateral lobes, of which the superior is bifid ; the other has not been well
seen.
Diameter, 25 inches; height of last whorl, 14 inch; width of aperture, 13 inch.
Tolerably common in the Chalk with silicious grains of Lyme Regis, Dorsetshire ;
and Chardstock, Somersetshire.
Many of the Continental authors have united this species with 4. Rhotomagensis,
probably without having seen the shell, which appears to be confined to one bed in the
West of England. When very young the two shells are nearly alike; but 4. Aippocastanum
may be known by its greater breadth of whorl, and large lateral spines. As it increases
in size, it is distinguished by the rapid enlargement of its whorls, great breadth, and great
inequality of its ribs and tubercles; while 4. Rhotomagensis is, at all its stages, known by
their uniformity. 4. Cunningtoni has more affinity to 4. hippocastanum ; but not having
seen the young state of that shell, I am unable to compare them thoroughly.
24. Ammonrres Gouriuianus, D’Orbigny. Plate XVII, figs. 5, 6.
AmMonitEs Goupriianvs, D’Orbigny. Paléont. Frang. Terr. Crét., t. xciv, figs. 1—3.
A. testd discoided, compressa, carinatd, transversim undato-costatd ; costis depressis,
numerosis tnequalibus bicurvatis: dorso obtuso, carinato, producto: anfractibus tribus, ad
umbilicum dechivibus, sub-carinatis, deindé sub-sulcatis, compressis: umbilico mediocri :
apertura elongato-ovata: septorum lobis lateralibus 6, trifidis.
Shell discoidal, flattened on the sides, keeled; ornamented with numerous unequal,
flexuous ribs, which, rising from the raised edge of the umbilicus, incline forward for two
fifths of the width of the whorl, then bend slightly backwards, and again bend forward
near the back, and are produced forward at the keel, marking the outline of the mouth of
the shell at its successive stages of growth; a few of the ribs are stouter than the rest:
umbilicus of moderate size, exposing about one fourth of the inner whorls, and bounded
by nearly perpendicular walls: sides of the whorls depressed into a slight channel near the
umbilicus: back obtuse, with a sharp keel, and projecting in a point over the oval mouth:
septa with six trifid lateral lobes. In the youngest stage of growth seen, the larger ribs
AMMONITES. 39
rise into a tubercle near the umbilicus, and also on each side of the back : the old shell is
nearly smooth, with faintly marked obsolete ribs.
Diameter, 3 inches; height of the last whorl, 1¢ inch; width of aperture, | inch.
From the Grey Chalk of Hamsey, near Lewes. The only specimen seen is in the
British Museum, from the collection of Dr. Mantell. In France it has been found in the
Grey Chalk near Saumur, and in the Upper Green Sand of Mondragon, near Orange.
(D’ Orbigny, loc. cit., p. 319.)
With some general resemblance to the variety sub-plana of A. varians, this species is
distinguished from that and all the other known species of the Chalk by the depression of
the sides of the whorl near the umbilicus, and the peculiar sigmoidal flexure of the ribs,
in which characters it is related to 4. serpentinus, Schloth., and several other species of
the Lias and Lower Oolite.
25. me GNETES VeLLED#, Michelin. Plate XVII, fig. 7; and Plate XIX, fig. 6.
AMMONITES VELLED®, Michelin. Magasin de Zoologie, t. xxxv.
— — D' Orbigny. Paléont. Frang. Terr. Creét., vol. i, t. Lxxxii.
= — Pictet and Roux. Foss. des Grés Vert des env. de Geneve, t. ii, fig. 1.
A. tesid discoided, compressa, transversim subtilissimé costatd: anfractibus paucis,
lateribus complanatis, dorso rotundatis : costis tenuibus, rectiusculis, numerosissimis, anfrac-
tum totum amplectentibus: umbilico minimo: apertura elongato-ovatd, septorum lobis late-
ralibus trifidis.
Shell discoidal compressed, with few whorls, flattened on the sides, and rounded at
the back; crossed by numerous fine, equal, thread-like ribs, which embrace the whole
whorl: umbilicus very small :* aperture elliptical: lateral lobes of the septa trifid.
Diameter, 1? inch; height of the last whorl, 1 inch; width of aperture, 3 inch.
Found rarely in the Upper Chalk near Norwich, and in the Grey Chalk of Ventnor,
Isle of Wight. In France and Savoy itis found in beds of the age of the Gault, attaining
a diameter of 7 inches.
26. AwMontres NAVICULARIS, Mantell. Plate XVIII, figs. 1—3, 5, 8.
AMMONITES NAVIcULARIS, Mantell. Fossils of the South Downs, t. xxii, fig. 5.
— a Sowerby. Main. Conch., 555, fig. 2.
—_— — DOrbigny. Prodrome, vol. ii, p. 146.
— GENTONI, Brongniart. Env. de Paris, t. vi, fig. 6.
— Manrteui, D’Orbigny. Paléont. Frang. Terr. Crét., t. 103.
_ MILLeETIANUs, Dixon. Geol. of Sussex, t. xxix, fig. 15.
* Owing to the specimen, pl. xvii, fig. 7, consisting of very soft Chalk, the umbilicus has been too
much excavated, and is represented too large, *
40 FOSSIL MOLLUSCA OF THE CHALK.
A, testé inflaté, costatd, interdum tuberculatd: anfractibus rotundatis : costis rectis,
simplicibus, inequalibus, ud dorsum continuis ; junioribus tuberculatis; adultis angulatis,
vel rotundatis : dorso rotundato, transversim costato, juniore trituberculato : umbilico parvo,
profundo: apertura semi-ellipticd: septorum lobis lateralibus, primo inequaliter bifido,
ceteris trifidis : variat angulis, tuberculisque costalibus plus, minusvé conspicuis.
Shell inflated, with few rounded or angular whorls, crossed by numerous strong,
unequal ribs: back round, or angular at the sides: umbilicus small and deep, with
half the inner whorls visible: ribs alternately longer and shorter; the longer ribs
commence from a tubercle at the edge of the umbilicus, and sometimes bear a second
tubercle on each side of the whorl; the shorter ribs rise on the side of the whorl, nearer
to the umbilicus than to the back; all the ribs cross the back: in young shells there are
three tubercles on the dorsal part of each rib, which give a slight angularity to the back
and to the mouth; in older shells the rib is strong and prominent over the back, without
any tubercles, and the back and the mouth are rounded : the superior lateral lobe of the
septa is unequally bifid, the two others are trifid; only two lateral lobes are visible on the
side of the whorl, the second auxiliary lateral lobe being on the slope of the umbilicus.
Diameter, 43 inches; height of last whorl, 2 inches; width of aperture, 2 inches.
Common in the Lower Chalk of the South of England.
This species was first described by Dr. Mantell from a very imperfect specimen, but
was afterwards admirably figured in the ‘ Mineral Conchology ;’ nevertheless it was united
to A. Mantelli by D’Orbigny, Bronn, and other Continental writers. They are, however,
to be distinguished when young by the row of tubercles on the middle of the back of
A. navicularis, and when old by the nbs of that species continuing elevated over the
middle of the back; while in 4. Mantelli there is a depression on the middle of the back
at all periods of its growth. 4. Mantelli is usually flatter, more angular, and more
tuberculated than 4. navicularis, but there are varieties which differ in these respects.
The species are both found in the Lower Chalk ; but I have seen no specimens of 4. navi-
cularis from the Upper Green Sand. In the ‘ Prodrome de Paléontologie,’ M. D’Orbigny
has again separated the two species.
A. Gentoni of Defrance and Brongniart, is the young of 4. navicularis, in the con-
dition of my figure 5 c.
A. Milletianus of Dixon (not of D’Orbigny), is one of the many forms of this species,
nearly the same as my figure 5.
27 _ AMMONITES Manteu, Sowerby. Plate XVIII, figs. 4—7.
AmMONITES MANTELLI, Sowerby. Min. Conch., t. lv.
_ -- Mantell. Fossils of the South Downs, t. xxi, fig. 9; t. xxii, fig. 1.
— — D’Orbigny. Paléont. Frang. Terr. Crét., t. 104, figs. 1 and 2. (Not
t. 103.)
*
— — Id. Prodrome, vol. ii, p. 146.
AMMONITES. Al
A. testé discoided, costaté, tuberculaté : anfractibus angulatis: costis simplicibus, recti-
usculis, inequalibus ; ad dorsum subcontinuis vel obsoletis, bituberculatis ; ad latera 1, 2,
vel 3 tuberculatis: dorso angulato, medio depresso: umbilico parviusculo: aperturaé rhom-
boided : septorum lobis lateralibus, primo inequaliter bifido, ceteris trifidis.
Var. A. Anfractibus tumidis: aperturd octangulari ; costis rectis, majoribus 8 tubercu-
latis, minoribus 6 tuberculatis ; tuberculis spinosis.
Var. B. Anfractibus compressis : apertura angulato-ovali : costis subflexuosis : tuberculis
dorsalibus conspicuis, ceteris obsoletis.
Shell discoidal, with twenty to twenty-five tuberculated ribs, alternately long and
short: whorls angular, depressed or tumid: ribs simple and usually straight, the longer
ones commencing at a tubercle at the edge of the umbilicus, the shorter below the middle
of the whorl, and all continuing across the back, with a depression in the middle of the
back: tubercles varying from four to eight rows, of which the umbilical and dorsal rows
are always present, the lateral rows being either well or faintly marked, or altogether
absent: back depressed in the middle, with a row of tubercles on each side: umbilicus
small and deep, allowing half the inner whorls to be seen: aperture rhomboidal: septa
with three lateral lobes, the first unequally bifid, the others trifid.
Var. A. Whorls tumid: aperture octangular: ribs straight, with eight rows of large
tubercles.
Var. B. Whorls flattened : aperture nearly oval: ribs slightly flexuous: dorsal tubercles
distinct, the others nearly obsolete.
Diameter, 3 inches; height of last whorl, 1} to 13 inch; width of aperture, 14 to 12
inch, according to the variety.
Found in the Lower Chalk and the Upper Green Sand of the South of England, and
in beds of the same age throughout France.
The distinction between this species and 4. navicularis will be found after the descrip-
tion of that species.
1) fay
TOR \
28. Ammonites Runavxianus, D’Orbigny. Plate XIX, fig. 2.
AMMONITES RENAUXIANUS, D’Orbigny. Paléont. Franc. Terr. Crét., t. xxvii.
A. testéi discoided, compress, tuberculato-costatd : costis bi- vel tri-fidis, flecuosis, bi-
tuberculatis, ad dorsum sub-interruptis : dorso bituberculato ; juniore transversim sub-costato ;
adulto sub-carinato : umbilico mediocri : apertura truncato-ellipticd.
Shell discoidal, compressed, with few whorls, ribbed and tuberculated: ribs, about
fifteen, bifid or trifid, each springing from a large tubercle near the edge of the umbilicus,
and dividing into two or three flexuous branches, each of which bears another tubercle at
the edge of the back: in young shells the ribs are faintly continued across the back ; but
Oe ——————————————————— sc cc lc tt‘ Ct
42 FOSSIL MOLLUSCA OF THE CHALK.
in older specimens they end at the side of the back, and there is a slightly elevated ridge
along the middle of the back, with a row of tubercles on each side; these dorsal tubercles
are elongated transversely in the direction of the ribs: umbilicus shallow, leaving nearly
half of the inner whorls visible : aperture nearly elliptical.
Diameter of the figured specimen from the Grey Chalk, 15%; inch; height of the last
whorl, 56 inch; width of aperture, ;4> inch. /
Rare in the Grey Chalk of Ventnor, Isle of Wight. It is also found in the Upper
Green Sand, near Dorking, where it attains a diameter of 4 inches. In France it has
been found in the lower part of the “Craie Chloritée.”
Not having seen the young stage of any specimens of 4. Renauxianus found in the
Upper Green Sand, it is with some hesitation that I unite to that species these small
shells found in the Lower Chalk. On a side view, they closely resemble 4. varians, from
which they differ in the form of the back, which never rises into a decided keel as in that
species. ‘The dorsal tubercles are also different, as they slope with the rib; while in 4.
varians they are compressed transversely to the rib, and parallel to the keel.
29. Ammonites ocro-suLcatus, Sharpe. Plate XIX, fig. 3.
A. testé discoided: anfractibus complanatis ; dorso rotundatis, subtrilissimé costatis+
sulcis 8 transversis, rectiusculis, impressis ; costis numerosis, brevibus, dorsum amplectentibus :
umbilico mediocri: apertura semi-ovatd.
Shell discoidal ; with few whorls, flattened on the sides, and rounded on the back,
crossed by eight deep, very slightly flexuous furrows, between which are many short,
delicate ribs bending forward, and well defined on the back, fading away in the middle of
the sides of the whorl: umbilicus rather small, leaving a fourth of the inner whorls visible :
aperture semi-oval.
Diameter, 1 inch; width of aperture, 3 inch; height of last whorl, <4, inch.
Found in the Grey Chalk of Ventnor, in the Isle of Wight, and in the Chalk with
silicious grains, of Chardstock.
This species is nearly allied to 4. planulatus and A. Mayorianus, ‘of the Lower Chalk,
and to 4. Guettardi of the Neocomian of the South of France. It differs from the first
two in having the constrictions more numerous, and the inner whorls more concealed ;
and from the last, in having the furrows straighter, and projecting more forward, a rather
larger umbilicus, and flatter sides to the whorl. . Unfortunately the septa have not been
seen. A. Belus, D’Orbigny, las a similar form and ornaments, but the furrows incline
backwards on crossing the back ; while in all the other species just mentioned, they project
forwards at the middle of the back.
AMMONITES. 43
Haplecer aS
30. Ammonites Icenicus, Sharpe. Plate XIX, fig. 4.
A. testdé discoided, compressa, levi, inornatd : anfractibus paucis : umbilico mediocri :
dorso rotundato: aperturd ovatdé: septorum lobis lateralibus, primo trifido, teteris ine-
qualiter bifidis.
Shell discoidal, smooth ; with few whorls, flattened on the sides, and rounded on the
back: umbilicus of middling size, allowing two fifths of the inner whorls to be seen;
aperture ovate: septa with four lateral lobes, the first trifid, the others unequally bifid.
Diameter, 2 inches; height of last whorl, 1 inch ; width of aperture, 3 inch.
Rare in the Upper Chalk near Norwich.
The Ammonite here described has few characters by which it can be distinguished, and
may perhaps prove to be only a young shell. But the Upper Chalk contains so few
Ammonites, that it is desirable to place on record all that are known. It belongs to the
same group as 4. Lewesiensis.
f 4"
r\tay
31. Ammontres Devertanus, D’Orbigny. Plate XIX, fig. 5.
Ammonites Devertanus, D’Orbigny. Paléont. Frang. Terr. Crét., t. 111, figs. l and 2.
A. testa inflata, transversim tuberculato-costatd: anfractibus paucis, lateribus com-
pressis, dorso rotundatis: costis inequalibus, simplicibus vel bifurcatis, 9 tuberculatis: aper-
turd quadrato-rotundata : umbilico magno.
Shell discoidal ; with few whorls, flattened on the sides, and rounded at the back,
crossed by numerous tuberculated ribs, which are continued over the back: about half the
ribs commence at a tubercle on the edge of the umbilicus, and are either simple or bifur-
cating ; between these there is often a shorter rib, commencing on the middle of the side
of the whorl ; all are equal on the back: tubercles large and round, in nine rows; viz.,
three on each side, and three on the back ; the dorsal rows containing about twice as many
as the umbilical row: umbilicus very large, leaving nearly two thirds of the inner whorls
visible: aperture nearly square, with the corners rounded off.
Diameter, 4 inches ; height of last whorl, 1¢ inch; width of aperture, 13 inch.
From the Grey Chalk of Sussex. The only specimen seen is in the British Museum,
from the collection of F. Dixon, Esq. It has been found in France in the “ Craie Chlo-
ritée” of Uchaux.
This species is readily distinguished from all others by the number and position of the
tubercles.
= a
7
44 FOSSIL MOLLUSCA OF THE CHALK.
32. Ammonites RusTICUS, Sowerby. Plate XX, fig. 1.
AMMONITES RUSTICUS, Sowerby. Min. Conch., t. 177.
« _ — D Orbigny. Paleont. Frang. Terr. Crét., t. 111, figs. 1 and 2.
A. testé discoided, tuberculatd: anfractibus paucis, rotundatis : tuberculis 4 seriatis ;
2 lateralibus distantibus, maximis, conicis; 2 dorsalibus minoribus, depressis, numerosis :
umbilico maximo : dorso rotundato, medio plano.
Shell discoidal, tuberculated, with few rounded whorls: umbilicus very large, rounded
at the sides, exposing three fourths ofthe inner whorls: tubercles in four rows, viz., one on
each side of the whorl, a little above the middle, of ten or twelve very large, conical
tubercles ; and two on the back, of about twenty-four smaller, rounded, depressed tuber-
cles: aperture nearly round.
Diameter, 6 inches; height of last whorl, 23 inches; width of aperture, 2 inches.
A very rare shell, found in the Lower Chalk near Lyme Regis, Dursetshire.
33. Ammonites Runrvieri, Sharpe. Plate XX, fig. 2.
A. testé discoided, compressd : umbilico parvo: apertura truncato-hastatd : septorum
lobis lateralibus tribus trifidis: cetate juniore, undato-costatd, tuberculatd ; tuberculis 4
seriatis, ad umbilicum paucis, majoribus, dorsum versus elongatis, numerosis ; dorso subcari-
nato ; adulté omnino levi, dorso rotundato.
Shell discoidal, with few flat whorls: umbilicus small, leaving half the inner whorls
visible: mouth truncato-hastate: septa with three trifid lateral lobes: at the diameter of
four inches, as in the specimen figured, the whorls have their sides ornamented with about
ten ribs, each springing from a round tubercle at the edge of the umbilicus, reaching across
half the width of the whorl, and then changing to a flattened undulation, which ends at
the side of the back in a tubercle, elongated in the direction of the whorl ; alternating with
these ribs are similar flattened undulations, ending in similar tubercles: back faintly
keeled in the middle: in older specimens the sides are quite smooth, and the back
rounded. .
Diameter, 64 inches; height of last whorl, 34 inches , width of aperture, 2 inches.
Found in the Grey Chalk near Bonchurch, Isle of Wight, and near Devizes.
This species has probably been overlooked from its resemblance to some of the forms
of A. varians, from which it is to be distinguished by straighter and more simple ribbing,
and by the septa, which have the dorsal saddle divided into three parts, in a manner which
rarely occurs in this genus. I have named the species after M. E. Renevier, whose labours
among the Cretaceous Rocks of Switzerland deserve our warmest thanks, and who has
lately visited this country with the view of helping to bring into harmony the synonymy
of the Cretaceous Fossils of England and the Continent.
AMMONITES. A5
4
nA... ~
Copis res
34. Ammonrres Saxsu, Sharpe. Plate XX, fig. 3.
A. testa discoided, compressd, tuberculato-costata : anfractibus paucis, complanatis, an-
gulatis: dorso plano, bi-tuberculato : costis rectis 8—10 majoribus tri-tuberculatis, 20 mt-
_noribus bi-tuberculatis : aperturé rhomboided: septorum lobis lateralibus bifidis.
Shell discoidal, compressed ; whorls few, flattened on the sides: back flat, with angular
edges, and a row of tubercles on each side: ribs about thirty, straight, of which eight or
ten rise from a tubercle on the edge of the umbilicus, and the others begin on the middle
of the side of the whorl; all ending im a large tubercle at the side of the back, and also
bearing a smaller tubercle before reaching the back ; there being either two or three of the
smaller ribs between every two longer ones: aperture rhomboidal: umbilicus small,
bounded by steep sides, and allowing two thirds of the inner whorls to be seen: lateral
lobes of the septa bifid.
Diameter, 1 inch; height ofthe last whorl, $ inch; width of the aperture, 2 inch.
Rare in the Grey Chalk of Ventnor, Isle of Wight.
A pretty little shell, readily distinguished from all the varieties of A. varians by its
straight ribs and want of keel. It is named after S. Saxby, jun., Esq., who has rendered
me much assistance in collecting together the fossil species of the Chalk of the Isle of
Wight.
35. Ammonites Vectensts, Sharpe. Plate XX, fig. 4.
A. testa discoidedé: anfractibus, lateribus compressis, dorso rotundatis, transversim
costatis: costis inequalibus, flexuosis, supra dorsum continuis: umbilico mediocri ; aperturd
ovali.
Shell discoidal, with few whorls, which are flattened on the sides, rounded at the back,
and crossed by about twenty flexuous, slightly elevated ribs; the ribs commence at the
edge of the umbilicus, and slope forward to the middle of the side of the whorl, where
they bend backwards a little way, and then again slope forwards over the back ; besides
these there are about ten shorter ribs occasionally inserted between the former, which only
begin on the middle of the side, and equally cross over the back: umbilicus of moderate
size, leaving more than half the inner whorls exposed : aperture oval: septa not seen.
Diameter, 23 inch; height of last whorl, 1 inch; width of aperture, 3 inch.
Only one imperfect specimen has been seen, which was found in the Chloritic Marl,
near Ventnor, Isle of Wight.
This species is related to 4. consobrinus, D’Orbigny, and A. cinctus, Sowerby, but is not
in danger of being confounded with either. It is also related to 4. wndatus, Sowerby ; but
8
«
-
~_—
_
46 FOSSIL MOLLUSCA OF THE CHALK.
I find it impossible to compare them properly, for the original specimen of 4. wadatus
which Mr. J. de C. Sowerby has had the kindness to lend me, is so much crushed, that its
real characters cannot be distinguished; and that name had better be omitted from our
lists.
36. Ammonites Lewestensis, Mantell. Plate XXI, fig. 1. |
AmMONITES LewesIENsIs, Mantell. Fossils of the South Downs, t. 22, fig. 2.
— — D’ Orbigny. Paléont. Frang. Ters. Crét., t. 102, figs. 1, 2? note
t. 101.
A. testa subinflatd : anfractibus rotundatis, lateraliter sub-compressis, undato-costatis ;
dorso levi rotundato: umbilico parvo: aperturd ovatd: septorium lobis lateralibus 4
imequaliter trifidis.
Shell inflated: whorls few, with their sides a little flattened, and crossed by about
twelve broad, radiating undulations, or indistinct ribs, which commence at the edge of the
umbilicus, and die out before reaching the rounded, plain back: umbilicus rather small,
with steep sides, allowing above one third of the inner whorls to be seen: aperture oval ;
septa with four unequally trifid lateral lobes, and a very narrow dorsal lobe.
The young shell differs little from the adult; it has the same plain, round back, but
the undulations are hardly visible till it has reached a diameter of 4 to 6 inches: in very
old shells, of 2 feet in diameter, the outer whorl becomes quite smooth.
This is one of the largest species of Ammonite found in the Chalk, sometimes
exceeding two feet in diameter: the dimensions of the specimen figured are—diameter,
16 inches ; height of the last whorl, 6 inches; width of the opening, 5 inches.
Rather rare in the Grey Chalk near Lewes and Dover.
Three species have been published under the name of 4. Lewesiensis by Mantell,
Sowerby, and D’Orbigny. The description and figure given by the first are so imperfect
as to have made me almost despair of ascertaining what it represented, until Mr. Woodward
discovered Dr. Mantell’s original specimen in the vaults of the British Museum. The
specimen is very imperfect, a part of the back on the younger side of the whorl being
worn off, and the whole being so much crushed as to reduce the size of the umbilicus
considerably, and to render the whorls flatter, and the back less round, than in perfect
specimens: nevertheless it is sufficient to enable us to recognise the species with certainty.
A. Lewesiensis, when full grown, much resembles A. peramplus ; but it is flatter, and
the undulations are continued all across the side of the whorl, instead of stopping in the
middle of its side, as in 4. peramplus. The young shells of the two species have no
resemblance, 4. Lewesiensis being nearly smooth, and the other ornamented with nume-
rous ribs, which cross over the back. The form of the lateral lobes of the septa is nearly
the same in the two species; but in 4. Lewestensis the dorsal lobe is very narrow, while
AMMONITES. A7
in 4. peramplus the dorsal lobe is broad, and the superior lateral lobe thrown in conse-
quence farther from the middle of the back.
The 4. Lewesiensis of the Mineral Conchology (my A. leptophyllus) has flatter whorls,
a narrower aperture, more distinct ribs, an impressed line along the middle of the back,
and the lateral lobes of the septa branching into most complicated subdivisions, in strong
contrast with those of the true 4. Lewesiensis. Hitherto it has only been found in the
Upper Chalk.
M. D’Orbigny’s shell has no resemblance whatever to the 4. Lewesiensis of Mantell,
and very little to that of Sowerby. It is readily distinguished by a series of numerous
short ribs, which, commencing outside the middle of the whorl, are continued towards the
middle of the back, where they are suddenly interrupted by an impressed line: the septa
are as minutely subdivided as in J. /eptophyllus, but the lateral lobes are straight and
regularly trifid. It is stated in the ‘ Paléont. Franc.,’ that this species is found in France,
in the Lower Chalk: here I have only received it from the North of Ireland, from a bed
which I suspect to belong to the Upper Chalk. In the ‘ Prodrome de Paléontologie,’
p. 212, M. D’Orbigny, has named this species 4. Gollevillensis, having learned that it
differs from the 4. Lewestensis of Sowerby, and he removes its habitat from the Zerrain
Turonien, or Grey Chalk, wherein he quoted it in the ‘ Paléontologie Frangaise,’ to the
Terrain Sénonien, or White Chalk.
M. d’Archiac, in his ‘ Histoire du Progrés de la Géologie,’ quotes 4. Lewesiensis as
peculiar to the Lower Chalk of France; but I do not know to which of the three species
here mentioned he alludes.
37. Ammonites Wizsti1, Sharpe. Plate XXI, fig. 3.
A. testa discoided, costatdé: anfractibus paucis inflatis: costis 24—80 prominentibus,
imequalibus: dorso rotundato, costato: umbilico parviusculo, profundo: apertura semi-
ovata.
Shell discoidal, with few inflated whorls, ornamented with twenty-four to thirty strong,
rounded ribs of unequal length, of which ten rise near the edge of the umbilicus, and the
rest near the middle of the side of the whorl, and all are continued across the broad,
rounded back, where they incline a little backwards: umbilicus deep and rather small,
allowing half of the inner whorls to be seen: opening semi-ovate : the lobes of the septa
have not been seen.
Diameter, 23 inches ; height of the last whorl, 17 inch; width of the opening, 12 inch.
Very rare in the Chalk with silicious grains, Chardstock, Somersetshire.
I have seen only one specimen of this elegant Ammonite, which I have named after its
discoverer, J. Wiest, Esq., of Chardstock, from whom I have received great assistance in
the preparation of this work.
48 FOSSIL MOLLUSCA OF THE CHALK.
38. AMMONITES LEPTOPHYLLUS, Sharpe. Plate XXI, fig. 2, and Plate XXII, fig. 1.
AMMONITES LEWESIENSIS, Sowerby. Mineral Conchology, t. 358.
— — D’ Orbigny. Prodrome de Paléontalogie, vol. ii, p. 189.
A. testa discoided, compressé, undulato-costaté : anfractibus lateraliter costatis, dorso
levibus: costis numerosis, paulum elevatis: dorso rotundato levi, lined angusta impresso :
umbilico parvo: apertura elevato-ellipticd: septorum lobis lateralibus ramosissimis, ramis
wrregulariter alternantibus.
Shell discoidal, flattened at the sides, rounded at the back : sides of the whorls crossed
by numerous radiating undulations, or low, broad ribs, which commence at the umbilicus,
and die out before they reach the back: umbilicus small, bounded by steep sides, allowing
more than half the imner whorls to be seen: back smooth and rounded, marked with a
narrow, impressed line: opening high and narrow: lobes of the septa much subdivided ;
the superior lateral lobe very large, with numerous irregularly alternate branches, ending
in long, pointed digits. In very old specimens the undulations are very faint, and
gradually disappear.
This species reaches a diameter of more than 23 feet. ‘I'he proportions of the specimen
figured are—diameter, 12 inches; height of the last whorl, 5 inches; width of the
aperture, 3 inches.
Found in the Upper Chalk of Brighton, Ramsgate, Greenhithe, &c.; but, from the
softness of the chalk in which it occurs, it is very seldom met with in good preservation.
This is not the species originally named by Dr. Mantell 4. Lewesiensis, nor is it the
species published under that name by M. D’Orbigny in the ‘ Paléontologie Frangaise,
which is now called 4. Gollevillensis ; but in his ‘ Prodrome de Paléontologie,’ that author
has so far corrected himself as to separate the last-named species from the one here
described.
As there have thus been three species passing under the name of 4. Lewesiensis, it is
impossible to know what is meant when this name is cited in geological works; a com-
parison of the three species is given, after the description of 4. Lewesiensis.
39. Ammonites GOLLEVILLENSIS, D’ Ord. Plate XVII, fig. 2.
AmMMONITES LEWESIENSIS, D’Orbigny. Paléont. Franc. Terr. Crét., t. 101.
— — Id. Prodrome de Paléontologie, vol. ii, p. 212.
A. testa discoided, compressa, costaté: anfractibus lateraliter levibus, dorso costatis :
costis brevibus, numerosis, equalibus, ad dorsum interruptis : dorso rotundato, costato, lined
AMMONITES. AQ
angustd, costas interrumpente, impresso: umbilico parviusculo: apertura ovatd: septum
lobis lateralibus trifidis ramosissimis.
Shell discoidal, whorls smooth and flattened on the sides, and ribbed on each side of
the rounded back ; ribs short, numerous, and equal, commencing beyond the middle of
the side of the whorl, and suddenly interrupted at the middle of the back by a narrow,
impressed line: umbilicus rather small, allowing about one third of the inner whorls to be
_ seen: aperture oval: septa very numerous, with minutely subdivided lobes; lateral lobes
trifid, with regularly opposite branches.
Diameter, 13 inch; height of the last whorl, 2 inches; width of the aperture,
1} inch.
Rare in the hard Chalk of the county of Londonderry, which is supposed to be of the
age of the Upper Chalk of England.
This species is closely related to 4. Oldhami, from which it is distinguished by its
short ribs, nearly confined to the back, and its smooth sides. In the ‘ Paléontologie
Frangaise,’, M. D’Orbigny confounded this Ammonite with Sowerby’s 4. Lewesiensis
(A. leptophyllus, Sharpe), and quoted it from the upper beds of the ‘“ Craie Chloritée,” or
on the level of our Grey Chalk. In his ‘ Prodrome’ he separates it from that species,
and considers the beds in which it is found as part of the Upper Chalk.
It is difficult to understand how two such different species could ever have been con-
founded, as the only character common to both is the impressed dorsal line. The lobes
of the septa of both are much subdivided, with spiked terminal digits, but in 4. Godlevil-
lensis they are trifid, with opposite and extremely regular branches. In A. eptophyllus
they bifurcate several times with very unequal alternating branches, and great irregularity.
oe
Mopites
40. AmMonrtus curvatus, Mantell. Plate VII, figs. 8, 9; Plate XXIII, fig. 1.
AMMONITES cuRVATUS, Mantell. Fossils of the South Downs, p. 118, t. 21, fig. 18.
— —_— Sowerby. Min. Conch., t. 579, fig. 2.
— FALcATUS? Pictet and Roux. Gres Verts des Env. de Geneve, t. 5, fig. 5.
A. testi discoided, sub-compressd, tuberculatd, plerumque costatd ; anfractibus paucis
sub-angulatis, lateribus depressis, tuberculatis ; dorso canaliculato, utringue bituberculato :
costis bicurvatis variantibus ; interdum paucis, latis, depressis ; interdum ad umbilicum
numerosis, dorsum versus paucis, latisque ; sepé omnino obsoletis: tuberculis utrinque tri-
sertalibus, ad umbilicum simplicibus, prope dorsum binis: umbilico parvo: aperturd rhom-
boided : septorum lobis lateralibus tribus trifidis.
Shell discoidal, flattened on the sides and back, with very few nearly rhomboidal
whorls; strongly tuberculated, and frequently ribbed: back with two rows of tubercles on
| ae ee
* +;
-~
_—
_
50 FOSSIL MOLLUSCA OF THE CHALK.
each side, and a hollow canal in the middle: ribs falcate, very variable in number and
size, and, rising from tubercles on the edge of the umbilicus, they extend forward to the
middle of the side of the whorl, then suddenly turn backward, and again curve forward
to the dorsal tubercles; sometimes they are five in number, broad and depressed; in
other specimens they are small and numerous on the inner half, and broad and few on
the outer half of the whorl; frequently they are well marked on young shells, and
gradually disappear with age; and in many specimens they are altogether wanting: three
rows of tubercles on each side of the whorl, one at the edge of the umbilicus, and two
near the edge of the back ; the umbilical tubercles vary both in size and number; when
there are no ribs, the tubercles are few in number, and very large; but they diminish in
size, and increase in number, in proportion to the development of the ribs; the dorsal
tubercles are usually large, but they vary in number from 15 to 30, being fewest and
largest where there are no ribs: umbilicus small and deep, allowing about one third of the
inner whorls to be seen: aperture rhomboidal: septa with three trifid lateral lobes on
each side.
Diameter, 13 inch; height of last whorl, 2 inch; width of aperture, 3 to 2 inch.
Found abundantly in the Chloritic Marl of the Isle of Wight; the Chalk with
silicious grains at Chardstock, Somersetshire; and the junction bed of the Chalk and
Upper Green Sand, near Warminster.
In the first part of this Memoir, I followed M. D’Orbigny and most other modern
paleontologists in uniting together the Ammonites falcatus and curvatus of Mantell and
Sowerby; but, as better materials have appeared, I have been obliged to separate them
again. Both are most variable species, and there are varieties which can only be distin-
guished with difficulty. The only invariable distinction which I have found between them
is in the termination of the superior lateral lobe, which is trifid in 4. cwrvatus and bifid in
A. falcatus ; see Pl. XXIII, figs. 1¢ and 2. In comparing the external forms, it will be
found that the more tuberculated varieties all belong to A. curvatus, the flatter, ribbed
varieties to A. falcatus; but there are intermediate forms combining falcate ribs with
dorsal tubercles, which can hardly be distinguished without the aid of the lateral lobe.
41. Ammonites Saurert, Sharpe. Plate XXIII, figs. 3 and 5.
A. testdé discoided, costatd, tuberculatd: costis ter-natis flecuosis, bi-tuberculatis, ad
dorsum interruptis: dorso utrinque tuberculato, tuberculis alternantibus : umbilico parvo :
apertura oblongd : septorum lobo dorsali longissimo.
Shell discoidal, with few whorls, ornamented with ribs and tubercles on their sides:
back plain, and slightly elevated in the middle, with a row of tubercles on each side ; these
j
e
og
»
\
yar
on ee Te
AMMONITES. 51
are not opposite to one another, but alternate: ribs flexuous, rising in threes from twelve
large tubercles which surround the umbilicus, forming an irregular zigzag pattern on the
side of the whorl, and ending at twenty-four rather smaller tubercles on the side of the
back: two rows of tubercles on each side of the shell: umbilicus small, allowing about
one third of the inner whorls to be seen: aperture oblong: septa with the dorsal lobe
considerably longer than the trifid superior lateral lobe.
Found by Mr. Wiest, in the Chalk with silicious grains, at Chardstock, Somersetshire.
42. Ammonites Ramsayranvs, Sharpe. Plate XXIII, fig. 4a—c.
A. testé discoided, costaté, tuberculaté: anfractibus paucis, sub-compressis ; costs
continuis, bi-tuberculatis, ad dorsum bifurcantibus : dorso lato, rotundato, costato, utrinque
tuberculato : umbilico parvo: apertura oblongd.
Shell discoidal, with few, slightly flattened whorls, and a broad, rounded back: the
whorls are ornamented on the sides by twenty ribs, each of which rise from a small tubercle
at the edge of the umbilicus, and bear another larger tubercle near the back ; at the latter
tubercle each rib divides into two smaller ribs, which continue across the back, and unite
again at the corresponding tubercle on the other side of the back: umbilicus small,
allowing nearly half of the inner whorls to be seen: aperture oblong: the septa have not
been seen.
Diameter, 14 inch; height of the last whorl, 3 inch; width of the aperture, 4 inch.
Very rare in the Chalk with silicious grains, at Chardstock, Somersetshire.
The only specimen which has been seen of this species is deformed, owing, without
doubt, to an accident met with when very young. In consequence of this malformation,
the two sides have very little resemblance to each other; and the specific character given
above may prove incorrect when more perfect specimens are met with.
A. Ramsayanus belongs to the group of the Coronarz, which, for the most part, belong
to the lower and middle divisions of the Oolitic series: its nearest congeners are perhaps
A. Humphriesianus and A. Brackenridgii. It is the second species of that group which
has been found in the Chalk ; 4. catinus having been the first.
This species is named after Professor Ramsay, of. the Geological Survey of Great
Britain.
n
4) t/ ” L
{AYA/TOp\\ Ces
43. AMMonItTES Frravpianus, D’Orb. Plate XXIII, fig. 6a—e.
[“ A. testd compressa, transversim costatd : costis inequalibus, rectis ; dorso complanato,
52 FOSSIL MOLLUSCA OF THE CHALK.
lateraliter angulato, anfractibus compressis, sub-quadrilateralibus, ultimo +2; ; apertura
oblonga, antice truncata.”—D Orbigny, ‘Terr. Crét.,’ t. i, p. 324.
The species thus described by M. D’Orbigny, in 1840, was said to have been dis-
covered by M. Emeric in the “Craie Chloritées” at Vergons, Basses-Alpes; but in a
later work, the ‘ Prodrome de Paléontologie,’ t. ii, p. 98, it is referred to the “* Néocomien
supérieur ou Urgonien.”
The specimen figured in Plate XXIII, fig. 6, was obtained by Mr. Sharpe from the
Grey Chalk at Ventnor, in the Isle of Wight, and named by him “ Feraudianus ;” but as
no memorandum exists to support this identification, it might possibly have been changed,
as it rests upon a single, crushed, and immature specimen. |
44. Ammonites Bravatsianus, D’ Orb. Plate XXIII, figs. 7a, 6, 8, and 9.
AMMONITES Bravaistanus, D’Orbigny. Paléontologie Francaise, Terrains Crétacés, t. 91,
figs. 3 and 4.
A. testa compressa, carinatd, costatd: costis inequalibus, simplicibus vel bifurcatis,
dorsum versus bituberculatis, interruptis: dorso carinato ; carind elevatd, acuta : umbilico
magno: aperturé oblonga.
Shell discoidal, with few depressed whorls, which are ornamented by about thirty
transverse, slightly flexuous ribs: back keeled: the ribs are unequal, either simple and
alternately long and short, or occasionally branching in pairs from the edge of the
umbilicus; each rib terminates at the side of the back, where it is ornamented with two
smaller tubercles: keel distinct, sharp, and elevated: umbilicus large, allowing two thirds
of the inner whorls to be seen: aperture oblong.
Diameter, 1 inch; height of last whorl, 2 inch; width of aperture, $ inch.
Found in a hard bed of the Middle Chalk, near Dover. In France it has been found
in the Upper Green Sand of the department of Vaucluse.
This pretty little Ammonite has some resemblance to 4. varians, from which it is at
once distinguished by the pair of tubercles at the termination of each rib. Moreover, its
ribs are simpler than in that species, and never fork on the middle of the side of the whorl.
As yet 4. Bravaisianus has only been found in this country in one bed of rather hard
Chalk, which occurs near the bottom of the Chalk with Flints, and contains 4. peramplus,
Scaphites, and several other species of Mollusca hitherto undescribed, and only known in
that bed.
Se
.
AMMONITES. 53
45. Ay monites Wixtonensis, Sharpe. Plate XXIII, fig. 10 a—e.
[4 testa compressa, transversim costatd, costis parvis, numerosis, obtusis, inequalibus ;
ape rturd elongata, antice rotundatd ; umbilico parvo. Lat. maj., 13 ; min., 11 ; alt., 6 lines.
This figure is taken from a small Ammonite in hard, gritty Chalk, with green stains,
_ stated: to have been found near Devizes, by Mr. W. Cunnington. The form is unusual
inthe Chalk; the ribs are simple, and sub-equal on the back of the shell, but many
e obsolete on the sides, the remainder becoming stronger at the umbilicus; the
‘sutural lobes are few and rather simple. |
oe
Ae “ udlryceros
46. rss Juxesti, Sharpe. Plate XXIII, fig. 11 a—e.
testd discoided, late umbilicatd, transversim costatd ; costis numerosis, acutis ; an-
ctibus sub-compressis, interdum constrictis ; aperturd ovata.
‘specimen figured is the fragment of an Ammonite which, when perfect, probably
2asUL ured 5 or 6 inches: in diameter ; it consists of about one third of the external volution
on b,c). The curvature of the ribs is convex towards ihe aperture ; but the figures
, not only reversed, but placed upside down. The outer whorl shows one of the
2 peri odic constrictions, and another is seen on the inner whorl when detached, and also a
more prominent rib on the posterior side of the constriction.
— Ammonites Jukesii was discovered by Colonel Portlock, R.E., in the hard Chalk of the
= ty of Londonderry. |
Genus—Artrycuus, H. Von Meyer. 1821.*
ry Cornei, Bestia of a single horny plate, of a semi-circular, scmi-ellipti, or
Beats vase form, marked by concentric wrinkles, with a semi-circular notch on the
middle of the straight side.
2. Imbricati, consisting of a pair of equal plates, each a quarter of a circle, or quarter
4 * The name Trigonellites, given by Parkinson, who described and figured several forms in 1811 (Org.
Rem.,’ ili, 184), ought to have been employed. Meyer added nothing to our knowledge respecting them.
9
A FOSSIL MOLLUSCA OF THE CHALK. ——
*
of an ellipse, in form, marked on one or both sides by strong concentric lines or wrin
produced by the imbricated growth of the shell; each plate has a fold along its s
side, the fold of one plate lapping over that of the other: the plates usually thin.
3. Cellulosi, consisting of a pair of plates, similar in form to those of the Imbricati,
and meeting in the same manner, but thick, and with the convex side cellular in structure. — ;
Few organic remains have given rise to more different opinions than these curious
bodies. [Professor Quenstedt regards them as the opercula of Ammonites, a view which
has been generally adopted in Germany. See Woodward’s ‘ Manual,’ 1851, p. 80, and
Owen’s ‘ Lectures on the Invertebrata,’ 2d edit., 1855, p. 596. In Part I, p. 19, of this
Monograph, the concave side of the Aptychus is incorrectly stated to have been external
instead of the convew side. |
All the Aptychi yet found in the Chalk belong to the group of the Jmbricati ; they
have all very thin shells, owing to which they are seldom found perfect ; and they are all
from the Upper or Middle Chalk.* As there is now little doubt that these bodies really
belong to some part of Ammonites, I have endeavoured to assign them to their respective
species of Ammonites, in which I have been guided by a comparison of the form and size
of the Aptychi with the apertures of the Ammonites found in the same beds of the Chalk
Formation, and in the same localities, for I am not aware that any Ammonite has yet been
found in the Chalk containing an Aptychus within it. As there are but few species of
Ammonites known in the Upper and Middle Chalk, the comparison is more satisfactory
than might have been anticipated ; but the result is only conjectural, as the discovery of ©
other species of Aptychus or of Ammonites might materially alter our conclusions on this
subject.
The species of Ammonites known in the Upper and Middle Chalk are 4. Grifithit and
A. Oldhamii, only known in Ireland, whence I have seen no Aptychi ; for which they are
excluded from the comparison.
A. Gollevillensis,* found in the Upper Chalk in Ireland and the North of France, and
which may consequently be expected to occur here.
A. Portlocki,*
a A. Icenicus,* )in the Upper Chalk of Norwich.
A. Fellede,* ‘
A. leptophyllus,* in the Upper Chalk of Kent and Sussex.
A. peramplus,*
* A. Woolgari, My: the Middle Chalk of our Southern Counties.
A. Bravaisianus,
The species marked * have round backs, and belong to Von Buch’s family of Ligati.
A. Woolgari has a serrated keel, and belongs to the Rothomagenses ; A. Bravaisianus
%* Mr. Flower has also found two species in Flint Pebbles in the Gravel, near Croydon.
APTYCHUS. 55
has a sharp keel, and may be excluded from the comparison, as it is too small to admit
any of the Aptychi yet found.
As yet we have only seven forms of Aptychus from the Chalk, six of which have so
many characters in common, that it is natural to suppose that they belong to Ammonites
of the same, or nearly allied groups; the remaining species, 4. rugosus, differs in having
the convex side strongly ribbed.
In Plate XXIV, which is devoted to this subject, are represented all the known
Aptychi of the Chalk, and outlines of the openings of the various Ammonites to which it
seems probable that the Aptychi may belong ; and, to facilitate the comparison, a dotted
line is drawn across each opening. It must be remembered that the two plates of the
Aptychi did not lie flat in the same plane, but were slightly inclined towards one another
_ {on the inner side], in which position the width they occupied would be rather less than
when they are represented lying side by side on the plate.
Among the Aptychi belonging to the Chalk, figured by Continental authors, Aptychus
eretaceus, of Miinster, so nearly approaches several of those which are here described, as
to show that they belong to nearly allied Ammonites. But sad confusion has been made
with that specific name. Geinitz gives three figures of Aptychus cretaceus (‘ Charakteristik
des Sachsischen Kreidegebirges,’ t. 17, figs. 25 a@ and 4 and 26), which evidently belong
to three different species; another distinct species is figured under the same name by
Reuss (‘ Versteinerungen der Bohmischen Kreideformation,’ t. 7, fig. 13), and both these
authors refer to Aptychus cretaceus, the plate described under the name of Anatifa convexa,
by Roemer (‘ Kreidegebirges,’ t. 16, fig. 7), which, if the figures are to be trusted, differs
from all the others.
APTYCHUS LEPTOPHYLLUs, Sharpe. Plate XXIV, fig. 1 a, 3.
A. bivalvis, subtruncato-ovatus ; valvis imbricatis, latere convexo levi, latere concavo
concentrice lineato ; plicd media inconspicud.
Bivalve, thin, the united valves ovate, with a slight truncation at the lower end; outer
edge reflected: the convex side smooth; the concave side delicately marked by very close,
concentric imbrications : medial fold narrow, and but little elevated.
Height, 14 inch; breadth of each valve, 4 inch.
Found in the Upper Chalk, near Brighton, by Mr. Morris.
The form of this Aptychus corresponds to that of the opening of Ammonites leptophyllus,
and which is also found in the Upper Chalk, near Brighton ; for these reasons it is probable
that it belongs to that species.
56 FOSSIL MOLLUSCA OF THE CHALK.
Aptycuus Portiocki, Sharpe. Plate XXIV, figs. 2, 3, and 4 (6?)
A. bivalvis, transversim semi-ellipticus ; valvis imbricatis, utrinque concentricé sulcatis ;
sulcis distantibus ; plicd medid elevatd.
Bivalve, the united valves forming, transversely, a semi-ellipse, with a uniform curve
to the outer margin; valves thin, marked on both sides by rather distant concentric
furrows, produced by the terminations of the broad imbricated additions to their outer
edges: medial fold large, and separated from the rest of the valve by a deep furrow.
Height, # inch; breadth of each valve, 3 inch.
Found in the Upper Chalk, near Norwich, by Mr. Bayfield; and in a Flint Pebble, in
the Gravel, near Croydon.
Of the Aptycht yet met with in the Upper Chalk, this species has the transverse
diameter of its united valves greatest in proportion to its height; and Ammonites Portlocki
is the only species known in the Upper or Middle Chalk which has the diameter of its
mouth greater than its height (see Plate XXIV, fig. 12). Moreover, the curves of the
respective outlines of the two nearly correspond, and both are found in the Upper Chalk,
near Norwich. The probability of this Aptychus belonging to A. Portlocki is therefore
very strong.
One of the three forms figured by Geinitz under the name of Aptychus cretaceus
(‘ Charakteristik, &c., des Sichsischen Kreidegebirges,’ t. 17, fig. 25 a) nearly resembles
A. Portlocki in outline, but, being a fragment, its proportions are not shown; and it is
distinguished by its closely set imbrications from our species.
Anatifa convera, Roemer, ‘ Kreidegeb.,’ t. 16, fig. 7, is the plate of an Aptychus
closely approaching 4. Portlocki ; but his figure and description do not enable me to
identify them.
AprycHus GoLLEVILLENSIS, Sharpe. Plate XXIV, fig. 5.
A. bivalvis, truncato-ovatus ; valvis imbricatis, utringue concentricé sulcatis ; sulcis
approximatis: plicd media elevatd.
Bivalve, truncato-ovate, the united valves forming about two thirds of the shape of an
egg; very convex, especially towards the outer edges: valves thin, marked on both sides
by closely set concentric furrows, produced by the terminations of the narrow imbricated
additions to the outer edges: medial fold elevated, and sharply separated from the rest of
the valve by a deep furrow.
ee Soe gg - gee
¢
APTYCHUS. 57
Height, 3 inch; breadth of each valve, 2 inch.
Found in the Upper Chalk of Norwich, by Mr. T. G. Bayfield, and in Flint Pebbles in
the Gravel, near Croydon.
_ Of the Ammonites found in the Upper Chalk, the one of which the outline of the
‘mouth most nearly resembles this Aptychus is A. Gollevillensis (Pl. XXIV, fig. 15). I
have not seen this species of Ammonite from Norwich; but as, besides being found in the
q North of Ireland, it occurs in France, in the Upper Chalk of the department of the
Manche, it may be expected to occur also on our side of the Channel; so that it is probable
__ that the Aptychus here described belongs to Ammonites Gollevillensis.
Of the varieties of Aptychus cretaceus figured by Geinitz, one form (/. c., t. 17, fig. 25 4)
_ approaches our species, but does not admit of absolute identification with it.
-
a>
s \ PTYCHUS IcENIcUs, Sharpe. Plate XXIV, fig. 7 a, 4.
% ie A. bivalvis, ovalis ; valvis imbricatis : latere convexo rugis paucis, latis, longitudinalibus,
:* -inconspicuis, ornato: plicd media parva.
s _ Bivalve, very thin; oval, with nearly straight sides: valves very convex, especially
: ~ towards the lower end: the convex side faintly marked by a few broad, longitudinal folds,
; which are not parallel to one another, and which cross the imbrications : medial fold small
and straight : the concave side has not been seen.
Height, § inch; breadth of each valve, } inch.
____ Found in the Upper Chalk, near Norwich, by Mr. T. G. Bayfield.
Ammonites Icenicus is the only species yet seen from the Upper Chalk which has its
ens corresponding to the peculiar outline of this Aptychus, which has its sides nearly
straight, and its two extremities nearly equal; and as both are found in the Upper Chalk,
j Pee Norwich, there is every probability that they must be connected.
. Aprycavs ruGosus, Sharpe. Plate XXIV, figs. 8 a, 4, and 9.
a
[ A. bivalvis, truncato-oblongus ; valvis imbricatis, latere convexo corrugatis, plicis dis-
tantibus, elevatis, tuberculatis, anticé angulariter inflectis.
Bivalve ; together oval or oblong, and notched at each end; separate plates nearly
- flat, thin, finely imbricated by lines of growth on the concave side, and ornamented with
_ elevated wrinkles on the outer surface; ridges from 4 line to 1 line apart, irregularly
ie Ms _ tuberculated, sub-parallel with the outer margin, and bent back at a sharp angle at the
_ upper end ; slightly irregular and flexuous, and becoming obsolete near the suture.
.
<a
58 FOSSIL MOLLUSCA OF THE CHALK.
Height of largest specimen (fig. 9), 24 inches; breadth of single valve, 11 lines. Small
pair (fig. 8), height, 14 inch; breadth, 1 inch.
From the Upper Chalk of Norwich, in the collections of Mr. John King and Mr.
T. G. Bayfield. |
Aprycuts PERAMPLUs, Sharpe. Plate XXIV, fig. 10, 6.
A. bivalvis ; truncato-ovatus ? valvis imbricatis, latere convexo corrugatis, latere concavo
subtiliter concentricé lineatis : plicd media elevata.
Bivalve ; truncato-ovate? valves imbricated, thin near the medial fold, thicker towards
the edge; convex side corrugated, the corrugations covered with irregular and unequal
tubercles ; concave side marked by fine concentric lines, indicating the edges of the closely
set imbrications : medial fold large.
From the Chalk, near Norwich, in the collection of Mr. Bayfield.
I have only one fragment of this Aptychus, 1$ inch in breadth, and can offer but an
imperfect description of it: the convex side is concealed in the specimen, and the direc-
tion of the corrugations cannot be seen. It is with great hesitation that I propose to
connect it with Ammonites peramplus.
[This specimen was described by Mr. Bayfield m 1851 (‘Annals and Magazine of
Natural History,’ 2d series, vol. vill, p. 236), being the first instance on record of the
occurrence of Z'rigonellites in the English Chalk. ]
Since the preceding descriptions of the species of Aptychus were in type, a memoir*
has appeared on the Cretaceous Fossils of Meudon, France, by M. Ed. Hébert, in which
three species of Aptychus are described; 4. odtusus, crassus, and insignis, the last form
being closely allied to, if not identical with, 4. rugosus, above noticed.
* Mém. Soc. Géol. de la France, vol. v, p. 367, pl. 28.
‘)"= IP
ty
Genus—TURRILITES, Lamarck. 1801.
Animal unknown: shell chambered, turreted, usually sinistral, with numerous angular
_ whor s, twisted spirally round a central cavity, and contiguous throughout on their upper
and lower sides: chambers separated by transverse, flexuous septa, deeply sinuated towards
he edges, and divided into six branching lobes, which are unsymmetrical, those on the
side of the whorls being much larger than the corresponding lobes on the inner side:
traversed by a continuous tube, situated on the outer side of the whorl, a little below
suture: mouth of the adult shell produced downwards, and bent over somewhat into
form of a hood.
‘The genus Zurrilites, as it has been usually received, includes, in addition to the shells
he e classed in it, other chambered, turreted species, with contiguous, rounded whorls,
the siphuncle placed on the middle of the outer side of the whorl. I have ventured
to ave these species to the genus Helicoceras, with which they agree in the round form
who: rls Peaiguous instead of separate. The importance that difference is deena by
finding a species with rounded whorls, Helicoceras or Turrilites polyplocus, Roemer,
‘hich the whorls are separate during the early part of their growth, contiguous in
ee stage, and again ek when full grown ; in apmecapence of which it has been
| 2D i ites, and assigned their characters—lst, the rotwadati, which are those which I
r “ss se to unite to Helicoceras ; 2d, the angulati, which form the genus La as here
‘The produced, arched mouth has not yet been seen in all the Zwrrilites, but there are
indications of it in so many species, that it may be presumed to be universal in the genus.
iL can find no evidence that this mouth was formed more than once during the life of the
1 animal, as is conjectured by M. D’Orbigny (‘ Terr. Crét.,’ p. 570); on the contrary, we
hat, before the mouth is produced, there is always some modification in the form of
ribs which would betray the previous position of the produced mouth, if such had
bed and had been absorbed by the animal; but no specimens show any such irregu-
larity of the ribs in any of the upper whorls, so that we must conclude that the mouth
was only produced once, and the different size of individuals of the same species on
“which this occurs only show that some reached their adult form sooner than others.
_ There is very little difference in Zwrrilites between their forms and ornaments in the
young and older stages of their growth, excepting near the produced mouth; so that the
a
rs species may be recognised in specimens of any size or age. :
eee UT
, a
ae
60 FOSSIL MOLLUSCA OF THE CHALK.
None of the group of the rotwndati have been found with the produced mouth like the
Turrilites, and the only modification known in the adult shells of that group is a thicken-
ing of the edge of the mouth: probably this will be found to be another generic difference
between Zurrilites and Helicoceras.
Classification of Turrilites.
1. Rorunpati, D’ Orb. Whorls round; siphuncle near the middle of the exterior side
of the whorl; ribs simple ; mouth thickened.
Common in the Gault.
T. acuticostatus, D’Orb. C. C.
2. AneuLtati, D’Orb. Whorls angular; siphuncle near the suture; mouth covered
with a hood.
2 a. Lateral lobe trifid; ribs or tubercles not arranged in regular lines
across the whorl.
T. tuberculatus, Bosc. lL. Chalk.
T. Gravesianus, D’Orb. Pl. 144, fig. 3. L. Chalk.
T. Mantelli, Sharpe.
2aa. Lateral lobe trifid; tubercles in regular rows across the
whorl.
T. Bergeri, Brong. Gault and L. Chalk.
24. Lateral lobe bifid; tubercles or ribs arranged in regular lines
across the whorl.
T. catenatus, D’Orb. Pl. 140, fig. 1. Gault.
ZT. Puzosianus, D’Orb. Pl. 148, fig. 1. Gault.
T. Scheuchzerianus, Bosc. L. Chalk.
T. costatus, Lam. IL. Chalk.
T. Wiestii, Sharpe. . Chalk.
2c. Lateral lobe bifid; tubercles not in regular rows across the
whorl.
T. Morrisii, Sharpe. U. G. Sand and L. Chalk.
TURRILITES. 61
1. Turriites TuBERCULATUS, Bosc. Plate XXV, figs. 1 to4, and Pl. XXVI, figs. 15, 16.
TURRILITES TUBERCULATUS, Bose. Buff. da Déterville, Vers., t. 42, fig. 8.
— — Sow. Min. Conch., t. 74.
= — Mantell. Geol. of Sussex, t. 24, fig. 7.
— a D’ Orb. Pal. Frang. Terr. Crét., t. 144, figs. 1, 2.
== — Pictet and Roux. Foss. des Grés Vert de Genéve, t. 15, fig. 10.
_— vaRicosa, Bose. l.c., p. 190.
— GIGANTEUS, Haan. Mon. Amm. et Goniat., p. 78.
T. testa turritd, sinistrorsd : anfractibus numerosis, extra conveais, tuherculato-spinosis :
tuberculis 4-serialibus; serie superiort, in medio anfractuum, tuberculis 20 distantibus,
maximis, spinosis ; seriebus tribus inferioribus propé suturam tuberculis parvis, numerosis,
approximatis: angulo spiralt 16°—20°.
Shell turreted, with a spiral angle of 16° to 20°, sinistral: whorls numerous, rounded
externally, with one row of above 20 very large spinose tubercles near their middle, and
three rows of numerous small tubercles near their base, the lowest of which three rows is
concealed by the suture; the tubercles of the middle row have a rounded base, those of
the three lower rows are elongated in a direction parallel to the suture, and are of the
same number in each row: upper and lower sides of the whorls ornamented with faint,
radiating ribs, corresponding to the tubercles of the lowest row: umbilicus narrow:
section of the whorls nearly rhomboidal, with the outer side convex: mouth somewhat
produced, and rising to a blunt point on the inner side of the whorl, and surrounded by a
wing-shaped expansion, with a nearly semicircular outline.
‘The figures 1 and 4 represent the usual form of this species, with nearly twice as many
tubercles in the lower rows as there are in the upper one; but specimens are often found
like fig. 3, with less difference between the different rows in the size and number of the
tubercles, and with the two lower rows of tubercles almost coalescing. I have seen no
specimen in which these two varieties are found in the same individual, as is represented
m M. D’Orbigny’s fig. 1 ; but as the lobes of the septa of the two forms closely correspond,
we must presume that they belong to the same species. In very large individuals the
tubercles of the upper row are fewer in number, and proportionably larger.
The lobes of the septa are much divided and branching; the outer side of the whorl
holds half of the dorsal lobe, the dorsal saddle, and half of the superior lateral lobe, which
last has five principal branches ; the dorsal saddle is divided into two nearly equal parts,
aud each of these is divided into two nearly equal branches (fig. 15). ‘This is the character
by which 7. tuberculatus is best distinguished from 7. Gravesianus, which has the dorsal
saddle divided into two very unequal parts, only the upper of which is again divided.
The larger specimens of Zurrilites are never found perfect, so that their length must be
. 10
62 FOSSIL MOLLUSCA OF THE CHALK.
calculated. The specimen of this species figured in the ‘Mineral Conchology’ has a
diameter of 5 inches in the lower whorl, and must have been above 18 inches long. The
common-sized specimens have their largest diameter about 2} inches, and probably
reached 9 or 10 inches in length.
Common in the Grey Chalk of the South of England, and in the Chloritic Marl of the
Isle of Wight, and the Chalk with siliceous grains, of Dorset and Somerset.
2. Turritites Gravestanus, D’Orbigny. Plate XXV, fig. 7, and Plate XXVI, fig. 14.
TurriLites Gravestanvs, D’Orb. Pal. Frang. Terr. Crét., t. 144, figs. 3—5.
—_— TUBERCULATUS, Mantell. Geol. of Sussex, t. 24, fig. 6.
T. testé turrito-conicd, sinistrorsd ; anfractibus paucioribus, extra angulato-conveais,
tuberculato spinosis ; tuberculis 4 serialibus ; serie superiore, in medio anfractuum, tuber-
culis 10—12 mazximis, spinosis, distantibus; seriebus tribus inferioribus propé suturam
tuberculis parvis, numerosis, approaimatus ; angulo spirali 30°.
Shell conical, with a spiral angle of about 30°, sinistral: whorls few, externally convex,
and somewhat angular in the middle, with one row of 10 or 12 very large spinose tuber-
cles a little above their middles, and three rows of numerous small tubercles near their
base ; the two lowest of these rows are so near together that the tubercles almost coalesce,
and are partially concealed by the suture; the tubercles of the upper row have a rounded
base, those of the other three rows are elongated in a direction parallel to the suture, and
are of the same number in each row: upper and lower sides of the whorls ornamented with
radiating ribs, corresponding to the tubercles of the lowest row: umbilicus narrow : section
of the whorls somewhat pentagonal: the perfect mouth has not been seen.
The lobes of the septa are much divided, and form a very complicated pattern; the
dorsal lobe, dorsal saddle, and nearly two thirds of the superior lateral lobe are visible on
the outer side of the whorl; the latter has four principal branches, of very unequal size:
the dorsal lobe is short; the dorsal saddle is very large, and unevenly divided, the upper
half having two principal branches, of which the upper ends in three, the lower in two
terminal branchlets ; the lower half of the dorsal saddle has only one undivided straight
branch, parallel to the siphuncle: this peculiarity in the dorsal saddle distinguishes the
species from 7. tuberculatus ; the superior lateral lobe is veryelarge, and is divided into
five large branches (Plate XXVI, fig. 14).
Diameter of the largest whorl, 12 inch ; presumed length, 5 inches.
Rare in the Grey Chalk, near Lewes, and in the Chloritic Marl of Ventnor, Isle of
Wight.
The external form of this species is very similar to that of 7. tuberculatus, with which
TURRILITES. 63
it was long confounded. M. D’Orbigny pointed out the distinctions between them, which
consist in the shorter and blunter spire, fewer and larger tubercles of 7. Gravesianus.
Slightly crushed specimens of 7. ¢uberculatus are sometimes very difficult to distinguish
from 7. Gravesianus, unless the outline of the septa can be traced, when the different forms
of the dorsal saddles set all doubts on the subject immediately at rest.
3. Turrimites Manteu, Sharpe. Plate XXV, figs. 5 and 6.
T. testa turritd, sinistrorsd: anfractibus numerosis, extra convexis, tuberculatis : tuber-
culis 4 serialibus ; serie superiort, in medio anfractuum, tuberculis 20—24, basi rotundatis ;
seriebus tribus inferioribus, tuberculis 30 minoribus, basi elongatis, approximatis : angulo
spiralt 18°—20°.
Shell turreted, with a spiral angle of 18° to 20°, sinistral: whorls numerous, convex
externally, with one row of 20 to 24 tubercles near their middle, and three rows of about
30 smaller tubercles near their base, the lowest of which rows is hid by the suture; the
tubercles of the middle row have a rounded base, those of the three lower rows are
elongated in a direction parallel to the suture, and are of the same number in each row:
upper and lower sides of the whorls ornamented with radiating ribs, corresponding to the
tubercles of the lower row: umbilicus narrow: mouth somewhat produced, and rising to a
blunt point on the inner side of the whorl, and surrounded by a broad, wing-shaped
expansion of somewhat rhomboidal form.
Only a small part of the outline of a septum has been seen, which is shown on the
upper whorl of fig. 5; the dorsal saddle is divided into two unequal parts, which are inter-
mediate in form between those of 7. tuderculatus and T. Gravesianus, more nearly
resembling the latter.
Diameter of last whorl, 25 inches; probable length, 12 inches.
Rare in the Grey Chalk, near Lewes, Sussex.
This species is readily distinguished from 7. tuberculatus by the greater number and
smaller size of the tubercles of the upper row, which are almost as numerous as those of
the three lower rows. There is also a marked difference in the rhomboidal form of the
expanded margin of the mouth. ‘These distinctions will probably be strengthened when a
more complete view is obtained of the lobes of the septa.
The only specimens which I have seen were collected by Dr. Mantell, and are now in
the British Museum. ‘The specific name is therefore a just tribute to the memory of that
zealous geologist.
Tewari’ are
64 FOSSIL MOLLUSCA OF THE CHALK.
4. Turrinites Scnreucnzerianvus, Bosc. Plate XXVI, figs. 1—3.
TURRILITES SCHEUCHZERIANUS, Bose. Buffon du Deterville, vol. v, p. 190.
-- uNDULA1Us, Sow. Min. Con., t. 75, figs. 1—3.
— — Mantell. Fossils of the South Downs, t. 23, figs. 14 and 16; t. 24,
fig. 8.
= — Geinitz. Kreide, t. 13, figs. 1—3.
ao _ D’ Orb. Paléont. Frang. Terr. Crét., t. 146, figs. 3, 4.
—s DesnoyersI, D’Orb. Paléont. Frang. Terr. Cret., t. 146, figs. 1, 2.
T. testé turritd, sinistrorsd: anfractibus numerosis, extra rotundatis, costatis : costis
numerosis, sub-angulatis; junioribus interruptis; adultis continuis: angulo spirali
15°—18°.
Shell turreted, with a spiral angle of 15° to 18°, sinistral: whorls numerous, rounded
externally, crossed by 20 to 24 sharp, elevated ribs; on the upper whorls the ribs are
nearly straight, and broken into two unequal parts by a depression a little below their
middle ; towards the middle of the shell the depression gradually disappears, and on the
lower whorls the ribs continue uninterruptedly across the whorl, and become more and
more flexuous: upper and under sides of the whorls smooth: umbilicus very small: mouth
produced considerably downwards, partially arched over, and expanded towards the
umbilicus: the outline of the septa has not been seen.
Diameter of last whorl, 12 inch; estimated length, 8 inches.
Common in the Grey Chalk, wherever that bed occurs, in the South of England.
This species is so well distinguished from all the other Turrilites by its elongated form
and comparatively simple ribs, that it had remained free from all confusion, until M.
D’Orbigny unfortunately proposed the specific name of 7: Desnoyersi for its young form,
and gave an appearance of probability to his suggestion by representing both the young
and the old forms as full grown shells on his plate 146, without any variation in the ribs
during the growth of either.* Such errors are the natural consequence of what is called
restoring the entire form of a shell from a fragment, instead of representing what is actually
seen. Dr. Mantell had already given an admirable figure of a nearly perfect specimen,
exhibiting the change from the broken ribs of the upper whorls to the unbroken: ribs of
the older whorls, which ought to have preserved M. D’Orbigny from this unnecessary
addition of a synonym.
Figure 2 represents a young shell, with ribs still divided, which is already beginning
* Figures | and 3, plate 146, are both stated to be “restauré sur un échantillon de ma collection.’
D’ Orb., ‘Terr. Creét.,’ vol. i, pp. 602 and 604.
i
a Za -
Ae
TURRILITES. 65
to form a mouth like an adult, with the ribs becoming flexuous. A still younger shell,
with the produced mouth completed, is shown in fig. 3; but as this specimen has the
lower side of the whorl strongly ribbed, it may be doubted whether it belongs to the
same species.
5. Turritites Morrisi, Sharpe. Plate XXVI, figs. 4—S.
T. testé turritd, sinistrorséd: anfractibus numerosis, extrd planiusculis tuberculatis ;
tuberculis 3 vel 4 serialibus; serie superiori, in medio anfractuum, tuberculis 8—\2
majoribus, distantibus ; seriebus inferioribus propé suturam, tuberculis minoribus, numerosis :
angulo spirali 15°.
Shell turreted, with a spiral angle of about 15°, sinistral: whorls numerous, nearly flat
externally, with one row of 8 to 12 large tubercles near their middle, and two or three
rows of above 20 smaller tubercles near the suture, all of them with a round base: upper
and lower sides of the whorls ornamented with faint, radiating ribs, corresponding to the
tubercles of the lowest row: umbilicus very narrow: section of the whorls rhomboidal :
septa with the superior lateral lobe bifid, with four branches on each side, and the dorsal
saddle divided into two very unequal parts: the perfect mouth has not been seen.
In the young shell the three lower rows of tubercles are usually distinct; in older shells
the tubercles of the two lower rows gradually coalesce, and at last hardly more than one
row can be distinguished, close to the suture.
Largest diameter, 14 inch; probable length, 6 inches.
Common in the Chloritic Marl of the Isle of Wight, and in the Chalk with siliceous
grains, Chardstock, Somersetshire.
6. Turritites Berceri, Brongniart. Plate XXVI, figs. 9—11.
TurRILITES BerGERI, Brong. Env. de Paris, t. 7, fig. 3.
—_— — D Orb. Pal. Frang. Terr. Cret., t. 143, figs. 3—6.
T. testa turritd, sinistrorsd (vel dextrorsé ?) : anfractibus paucioribus, rotundatis, tuber-
culatis: tuberculis 4 serialibus, equidistantibus, equalibus : apertura rotundato-rhomboided.
Shell turreted, turned to the left: whorls not very numerous, increasing rapidly in
size, rounded, and ornamented with four equidistant rows of numerous, rounded tubercles,
which are of the same number, and nearly the same size in each row; only three rows are
66 FOSSIL MOLLUSCA OF THE CHALK. [/
exposed, the upper one being covered by the next whorl; the tubercles are so placed as to
appear to form sloping, transverse bands across the whorls: section of the whorls somewhat
rhomboidal : septa, and position of the siphuncle, unknown.
Spiral angle about 35°.
Diameter of the largest specimens from Chardstock, in Mr. Wiest’s collection, 3 inches.
This is a well-marked shell, which can hardly be confounded with any other species.
We have not met with any specimen turned to the right like that figured by M. D’Orbigny,
t. 143, fig. 6.
Abundant in the Chalk with green grains, at Chardstock. (Wr Wiest.)
7. Turritires Becu, Sharpe. Plate XXVI, fig. 13.
T. testa turritd, sinistrorsd: anfractibus paucioribus, extrd rotundatis, costatis, tubercu-
latisque: costis numerosis, superioribus, flecuosis, tenuibus, infrd interruptis: tuberculis
biserialibus, inferioribus, numero costarum equalibus : angulo spirali 30°.
Shell turreted, sinistral, with a spiral angle of 20°: whorls few, externally rounded,
prettily ornamented with numerous delicate, flexuous ribs, which extend from the suture
across the upper two thirds of the whorl, where they are interrupted by a smooth space,
in which are two rows of tubercles, elongated in the direction of the suture, and equal in
number to the ribs ; below these the ribs appear again, bending backwards over the lower
side of the whorl; thus each rib, with its corresponding pair of tubercles, forms a flexuous
line across the outer and the under sides of the whorl: umbilicus small: the outline of the
septa has only been partially seen; the dorsal saddle is divided into two slightly unequal
parts: the specimen figured shows the beginning of a produced mouth.
Diameter of last whorl, 1 inch; estimated length, 4 inches.
Only one specimen has been seen, which was found in the Chalk with siliceous grains,
near Lyme Regis, by Sir H. T. de la Beche, and by him presented to the British Museum :
it is named in honour of his memory.
S. Turritires cosratus, Lamarck. Plate XXVII, figs. 1—5, and 15, 16.
TurRILITES costatus, Lamk. 1801. An. sans Vert., p. 102.
— — Sowerby. 1813. Min. Conch., t. 36.
— — Brong. 1822. Env. de Paris, p. 83, t. 7, fig. 4.
_ — Mantell. 1822. Geol. of Sussex, t. 23, fig. 15.
— — DOrbigny. Paléont. Frang., Terr. Crét., t. 145.
_— TRIPLIcaTUS, J. Sow. In Dixon's Geol. of Sussex, t. 29, fig. 16.
o
=
“ ‘
">> > TURRILITES.. 67
l’ testa elongato-turritd, sinistrorsd, costatdé et tuberculatd ; anfractibus convewius culis,
inferné costatis, superné bituberculatis ; costis tuberculisque numero equalibus ; aperturd
vali ; umbilico minimo.
Shell turreted, turned to the left, with a spiral angle of about 25°; whorls slightly
, separated by a moderately impressed suture, and ornamented on their lower half
rous straight, elevated ribs, which rise at their upper ends into round tubercles,
then terminate abruptly at a smooth spiral band, which encircles the shell; above are
rows of tubercles, the upper of which are smaller, and concealed by the next whorl ;
id tubercles equal in number ; aperture oval, higher than broad; umbilicus very small.
complicated form of the septa in this species is represented in Pl. XX VII, fig. 15. }
In Dixon’s ‘ Geology of Sussex,’ a Turrilite is described under the name of 7. ¢ripli-
catus, J. Sow., which appears to be a variety of the above. [This specimen is figured in
: £1. XXVIL, fig. 15.]
Found in the Chalk Marl of Ventnor, Isle of Wight; and in the Chalk with green
grains, at Chardstock.
a
9. Turritires Birrons? D’Orb. Plate XX VII, figs. 6, 7.
‘
7. testa turritd, elongata, sinistrorsd ; anfractibus convexiusculis, sulco longitudinaliter
; transversim costatis: costis curvatis, interruptis, biseriatis, anterioribis ad
specimens figured differ from the ordinary examples of 7. costatus in the flatten-
the whorls, occasioned by the shallow furrow which divides the curved transverse
tc a double series: the ribs are simple, rounded, and about as wide as the inter-
; the lower series of ribs is again divided by a furrow exactly at the suture, forming
set of little tubercles, only visible on the base of the shell when broken.
_ Found in the Lower Chalk, of Ventnor, Isle of Wight. }
a
10. Turriires Wiesti, Sharpe. Plate XXVII, fig. 8, 9 a, , and fig. 17.
T. testé turritd, sinistrorsd ; anfractibus externis rotundatis, tuberculatis, intus levibus ;
dratd ; umbilico parvo.
Shell turreted, tuberculated; spine turned to the left, with a spiral angle of about 22°;
whorls rounded, separated by a deep, crenulated suture, ornamented with four rows of
conical tubercles, which are of the same number in each row, and set obliquely under one
a
68 FOSSIL MOLLUSCA OF THE CHALK.
another, without ribs between them; the tubercles of the two outer rows are smaller than
the others, and meet at the junction of the valves, forming a crenulated suture ; while the
tubercles of the two middle rows, which are nearly equal, are prominent on the side of the
whorls; surface of the whorls between the the tubercles smooth ; aperture nearly square ;
umbilicus small.
The largest specimen seen has a diameter of 14 inch, which requires a length of 4 or
5 inches.
As yet we have only seen it from the Chalk with green grains, where it is very
abundant.
This elegant shell is at once distinguished from 7. tuberculatus by having the same
number of tubercles in each row, in which it agrees with 7. Bergeri. From this it differs
in the shape of the whorl, and the position of the lower row of tubercles, which is at the
suture instead of projecting at the side of the whorl: in consequence of this, it has only
two rows of tubercles visible instead of three on the side of the whorl.
Found in the Grey Chalk, of Ventnor, Isle of Wight; and also in the Chalk with green
grains, at Chardstock, Somersetshire ; and at Chaldon and Man-of- War Cove, Dorsetshire.
1). Turrizites Puzosianus, D’Oré., var.? Plate XXVIL, fig. 11.
? TurRILites Puzosranus, D’Orbigny. Terr. Crét., pl. 143, figs. 1, 2.
7. testa turrita, sinistrorsd ; anfractibus externi planiusculis, costulatis, tuberculatis ;
costis numerosis, flecuosis, obliquis, superné interruptis tuberculatisque ; tuberculis bi-seriali-
bus, sertis supertoris binis, inferioris longitudinaliter compressis ; apertura ovali; umbilico
parvo.
Shell turreted; spine turned to the left, with a spiral angle of about 15°; whorls
flattish, with the lower angle rounded off, separated by a moderate suture, and ornamented
with numerous oblique, flexuous, slight ribs, interrupted near the top of the whorl by a
smooth spiral band, on each side of which the ribs rise into longitudinally flattened
tubercles ; the tubercles of the upper row bifid or double, and stand at the angle of the
whorl ; aperture somewhat oval; umbilicus small.
I have as yet only seen one fragment of this shell. It resembles 7. Puzoscanus, D’Orb.,
in having ribs rising into tubercles on each side of a smooth band, which, running round
the upper part of the whorl, divides the ribs into two unequal parts. Our shell differs
from 7. Puzosianus in the flexure of the ribs, and in the position of the upper row of
tubercles, which, in that species, is placed at the suture, and thus concealed by the next
whorl; but in this one it is at the upper angle of the whorl, and always prominent. It
differs from 7’ costatus in the flexure of the ribs and flatness of the whorls.
Found in the Chloritic Mar], of Bonchurch, Isle of Wight.
*
PLATE L
Fig. PIBLOS sii
I, 2, and 3. BELEMNITELLA MucRoNATA’; from the Upper Chalk, near Norwich.
1. Ventral view, with the fissure.
2a and 6. Dorsal and lateral views of a specimen, in which the vascular
impressions are well seen.
2c. Alveolus from above.
3. Section of another specimen, showing the eccentric position of the
alveolus, and traces of the edges of the septa.
4,5, and 6. BELEMNITELLA LANcEOLATA; from the Upper Chalk, near Norwich.
4a, 6, and ec. Dorsal, lateral, and ventral views of one specimen.
4d. Alveolus from above.
5. Ventral view of a young specimen.
6. Section of another specimen, showing the central alveolus.
7. BELEMNITELLA QuaDRATA; from the Middle Chalk of Kent, in the collection of
Mr. J. G. Lowe; this specimen is broken at the top.
7a. Dorsal view.
74. Side view.
7c. Portion of the granulated surface, magnified.
8. BELEMNITELLA QuapRATA; from the Middle Chalk of Kent, in the collection of
Mr. Bowerbank.
8a. Dorsal view, showing the two lateral depressions.
84. The alveolar opening slightly broken away at the edges.
9. BELEMNITELLA QUADRATA; a young specimen from the Upper Chalk of Northfieet
in the collection of Mr. Morris, with the two vascular impressions strongly
marked.
9a. Dorsal view.
94. Lateral view.
10. BELEMNITELLA QUADRATA; alveolar opening from above, perfectly preserved. In the
collection of Mr. Bowerbank.
sr a
Fig. _
iL. BELEMNITELLA QUADRATA ; from the collection of Mr. Bowerbank.
lla. Section, showing the conical form of the lower part of the alveolar
opening, and the fissure.
114. The same, enlarged.
12, 13, 14, 15, and 16. BeLemniTeLLa PLENA; from the Grey Chalk, near Dorking.
12a. Dorsal view.
124. Upper end, with the lower part of the alveolus preserved.
13. A young specimen.
14. Section of a specimen, from which the alveolus is entirely broken off. _
‘15a. Dorsal view of a specimen, broken off at the apex of the alveolus.
154. Broken end of the last.
16. Section of a young specimen.
17. BeLeMNites uLtimus; from the Chloritic Marl of* Bonchurch in the Isle of Wight,
in the Collection of Mr. Saxby.
17a. Side view.
176. Ventral view.
17c. Outline of the opening.
2
Te bee
at Oe
spell
CO West, lth
PLATE -Tf.
Fig.
|. Navtitus Lavieatus; from the Chalk with siliceous grains of Chardstock, in the
collection of Mr. Wiest.
la. Side view.
14. Front view.
wo
. NAvTILus Lavieatus, young; from the Chloritic Marl of Bonchurch, in the col-
lection of Mr. Saxby.
Qa. Side view.
26. Front view, showing the position of the siphuncle.
3. Navutinus Expansus; from the Chalk with siliceous grains of Chardstock, in the
collection of Mr. Wiest.
3a. Front view.
34. Side view.
4. NAUTILUS EXPANSUS, young; from the Chalk, with siliceous grains of Chardstock,
in the collection of Mr. Weist.
4a. Side view.
44. Front view.
4c. Portion magnified, showing the cross striation.
or
. NAUTILUS EXPANSUS; view of one septum, showing the position of the siphuncle ;
from Mr. Bunbury’s collection.
or
4.
PLATESIAL
Fig.
tio as
a
1. Navriius DssLtonecuampsranus ; from the Grey Chalk near Lewes, in the collec
of Dr. Mantell.
la. Side view.
14. Back view.
2. NauriLus DEsLONGCHAMPSIANUS ; a fragment somewhat crushed, with the ¢ oss-rib-
bing well preserved. From the Grey Chalk, near Lewes. . |
3. NautiLus ELEGANS; from the Grey Chalk near Lewes, in the collection Mr.
Hudson. : i
The smooth part of this specimen has been enclosed in another whorl,
-
é
is partially broken away.
a ;
PLATE IV.
Fig. p a -
1. NauTILus ELEGANS, reduced to two thirds; a front view of the inner portion of the
specimen figured Plate III, fig. 3, showing the position of the siphuncle.
2. NAUTILUS PSEUDO-BLEGANS; from the Grey Chalk near Lewes, in the collection of
the Geological Society. .
2a. Side view.
24. View of one septum, with the opening for the siphuncle.
PLATE. 4
Fig.
1. Navtitus rapratus; from the Chalk with siliceous grains of Chardstock, kindly
given me by Mr. Wiest.
la. Side view.
14. Front view, showing the position of the siphuncle, and the ventral
depression on the septum.
2. NAUTILUS RADIATUS; young specimen, with a portion of the cross-striation of the
young shell preserved. From the Chalk with siliceous grains of Chardstock,
in the collection of Mr. Morris.
3. Nautitus Neocomiznsis; from the Grey Chalk of Urchfont near Devizes, in the
collection of Mr. Cunnington.
3a. Side view.
36. Back view.
3c. Septum showing the position of the siphuncle.
4. NautiLus unDutatus; from the Chalk with siliceous grains of Chardstock, m the
collection of Mr. Wiest.
4a. Side view.
46. Front view.
4c. Septum showing the position of the siphuncle.
—————————— =
Yr
Sue
~~
°
PLATE “FX.
Fig.
1, NAUTILUS LARGILLIERTIANUS ; from the Chalk with siliceous grains of Chardstock, in
the collection of Mr. Wiest.
la. Side view.
14. Front view.
. NAUTILUS LARGILLIERTIANUS ; a fragment from the Chalk with siliceous grains of
Chaldon, in the collection of Mr. Morris.
bo
2a. Side view, with a commencement of undulation on the back.
26. Septum, showing the position of the siphuncle.
3. Navutinus Fievriaustanus; from the Chalk with siliceous grains of Chardstock, in
the collection of Mr. Wiest.
3a. Side view.
36. Front view.
4. Navutitus Frrron1; from the Chalk with siliceous grains of Chardstock, in the
collection of Mr. Wiest.
4a. Side view.
4b. Back view.
4c. Septum showing the position of the siphuncle.
t~
~
. UY 73
a
}
Fig.
PLATE VII.
1—3. AMMONITES COMPLANATUS.
1. From the Grey Chalk of Hamsey ; in the British Museum, from the col-
lection of Dr. Mantell; the original specimen figured, t. 569, of the
‘Mineral Conchology,’ reduced to half its diameter.
la. Side view.
14. Front view.
2. A young specimen of the natural size; in the British Museum, from the
collection of Dr. Mantell.
3. Outline of the margin of a septum, copied from pl. xcv of the ‘Paléont.
Francaise Terrains Crétacées.’
dl. The dorsal lobe.
sll. The superior lateral lobe.
7Zl. The inferior lateral lobe.
aaa, Auxiliary lobes.
sd. The dorsal saddle.
Zs. The lateral saddle.
?. The position of the siphuncle on the middle of the back.
4. AmMMONITES oBTEcTUS; from the Chalk with siliceous grains of Chardstock, in the
collection of Mr. Wiest.
4a. Side view.
46. Front view.
4c. Portion of the outline of a septum, only extending to the
lateral saddle.
5—9. AMMONITES FALCATUS.
5. From the Grey Chalk of the Clayton Tunnel, on the Brighton Railway, in
the collection of Mr. Catt.
6a and 6. From the Chloritic Marl of Gore Cliff, Isle of Wight, in the
collection of Mr. Saxby.
7a and 6. A specimen in the collection of Mr. Morris, from the Chalk with
siliceous grains of Chaldon.
8a and 46. From the Chloritic Marl of Bonchurch, Isle of Wight; in the
collection of Mr. Saxby.
9. Outline of a septum of a young specimen.
Day &S0n, Lith™ to the Qucen
War
PLATE Vitq
Fig. :
1—4. Ammonites CovupeEl.
la and 4. Tuberculated variety; from the Chloritic Marl of Bonchurch,
Isle of Wight, in the collection of Mr. Saxby.
2a and 4. Commonest of the species; from the Chalk with siliceous grains
of Chardstock, in the collection of Mr. Wiest.
2c. Outline of the septum of a young specimen of the tuberculated variety.
3. Outline of the septum of the specimen, fig. 2a.
4, ‘'Tuberculated variety, young; from the Chalk with siliceous grains of
Chardstock, in the collection of Mr. Morris. The lateral tubercles
have been partially rubbed off.
5—10. AMMONITES VARIANS.
5a, 6, and c. Common form of the species; from the Chalk with siliceous
grains of Chardstock, m the collection of Mr. Morris.
6a and 4. Broken specimen of the same variety as fig. 5, showing the
form of the shell when young; from the Chalk with
siliceous grains of Chaldon, in the collection of Mr. Morris.
7a and 6. Ribbed variety with obsolete lateral tubercles ; from the Chalk
with siliceous grains of Chardstock, in the collection of
Mr. Morris.
8a and 6. Another variety; from the Chalk with siliceous grains near
Lyme Regis.
9a and 6. Smooth variety; from the Chalk with siliceous grains of
Chardstock, in the collection of Mr. Wiest.
10a, 6, and c. Young specimen of a smooth variety; from the Chloritic
Mar! of Bonchurch, Isle of Wight.
PLATE .1X.
Fig.
la and 6. Ammonites Couper; from the Grey Chalk near Devizes, in the collection of
Mr. Cunnington.
2a and 6. AMMoniTEs cincTus; from the Grey Chalk of Middleham, in the British
Museum, from the collection of Dr. Mantell: the original specimen de-
scribed by Dr. Mantell, and figured in the ‘ Mineral Conchology,’ pl. 564.
3a, 6,andc. Ammonites Bunsurianus ; from the Chalk with siliceous grains of Chard-
stock, in the Museum of Practical Geology, from the collection of Mr.
Bunbury.
Re lt
<
. an Bs
PLATE II.
Fig.
1. The brachial aponeurosis and spiral arms of Terebratula flavescens, showing the _
central part of the nervous system, with the brachial and beginning of the
pallial nerves. Magnified 6 diameters.
2. The peduncle and a large proportion of the soft parts of Zerebratula flavescens.
showing the principal ramifications of-the pallial nerves or the dorso-pallial fold
of the mantle. Magnified 12 diameters,
3. Some of the soft parts of Lingula anatina, exposed by the removal of the valve and
pallial lobe, answering to the ventral ones in Zerebratula, and of the digestive
organs, chiefly te show the trunks of the visceral and muscular nerves.
Magnified 4 diameters.
36
G West, lath.
“PLATE XI.
Fig. Prronotvopis
la and 4. AmMontres Woouieari; from the Grey Chalk near Lewes; the cea Pe
specimen in Dr. Mantell’s collection, figured in his work, and in the
‘Mineral Conchology,’ and now in the British Museum. The portions
= R are restored by the artist.
Py ie 1on Wig VvYO~P
2a and 4. ees Mascon? a young specimen from the Middle Chalk near Lewes ;
in the collection of Henry Catt, Esq., of Brighton. 7
3a, 6, and ec. aeons GRIFFITHII; internal cast from the Hard Chalk of the County
of Derry; fig. 3a has been completed in the inner whorls from another —
specimen, and fig. 3c drawn from a third specimen, all in the collection —
of the Museum of Practical Geology, in London.
ile e
PLAT# KIL
Fig. :
la and 4. Ammonites AvsTENI; reduced to one third its natural diameter ; from the Grey —
Chalk of Guildford; in the British Museum.
2. Ammonites AUSTENI; a young specimen, reduced to one half its diameter ; from the
Grey Chalk of Sussex ; in the collection of Henry Catt, Esq. a
Deswmacera$
3. AMMONITES PLANULATUS; from the Grey Chalk near Lewes ; formerly in the collection
of Dr. Mantell, and now in the British Museum; it is the original
specimen figured in the ‘ Mineral Conchology ;’ the parts marked R are _
restored by the artist. |
Desmoceras
4a, 6, and c. AMMONITES PLANULATUS; an internal cast from the Upper Green Sand near
Cambridge ; in the collection of Mr. L. Barrett.
he .*-
han ° of eee eee B. ora at +,
PLATE XIII.
Fig. ;
la and 4. AMMoNITEs CATINUS; reduced to one half its diameter; from the Grey Chalk
near Devizes; in the collection of William Cunnington, Esq., of that —
town.
a
Poche d isevs
2 and 3a, 4, c. Ped Nese Porriock! ; from the Hard Chalk of Tamlaght, in the County
of Derry ; in the Museum of Practical Geology, London.
FsevaaspiAocevas
4a, 6, and c. AMMONITES EUOMPHALUS; from the base of the Lower Chalk at Man of War
Cove, Dorsetshire ; in the collection of E. H. Bunbury, Esq.
=
=
~
>
~
~
.
:
PLATE, REY.
Fig. Sharpeiceras
la and 6. Ammonites LavicLavius; from the Grey Chalk of Bonchurch, in the Isle of
Wight ; in my possession.
2a, 6, and c. AMMonires OLtpHam1; from the Hard Chalk of Dungivan, in the County of
Derry ; in the Museum of Practical Geology, London. ‘The surface of
the original was waterworn, and has been a good deal restored in the
drawing.
3a and 46. AMMONITES LEPTONEMA ; from the Grey Chalk of Ventnor, in the Isle of Wight ;
in my possession.
— -_ -— OO ——————— ———— eee ee eS ee ee OG ee ee ae = Oe ee eee _ — is _ — —
PLATE XY:
Fig. rhea S
la, 6, c, and d. AMMoNITES SUSSEXIENSIS ; a specimen given me by Dr. Mantell, from the
Grey Chalk near Lewes ; reduced to two thirds its natural diameter.
2a, 6, and c. AMMoNITES CUNNINGTONI; from a specimen belonging to T. A. Falkner,
Esq., of Manningford, reduced to two thirds its natural diameter; from
the Grey Chalk of Upton Scudamore, near Warminster.
| = =
Geo West li
~~ le ee |
PLATE Ae
Fig. Metacart he Pp ites
la, 6, and c. AMmonites Ruoromacensis; from the Grey Chalk of Bonchurch, in the
3
possession.
la 7 16. Side and front views of the complete specimen.
le. Inner whorl of the same specimen.
2a and 4. Ammonites Ruotomacensis; from the Grey Chalk of Bonchureh ; of the
natural size ; in my possession.
3a and 4. AwMontres RHOTOMAGENSIS ; a very young specimen, from the Grey Chalk of
Bonchurch ; in my possession.
4. Ammonites Ruoromacensts; outline of the septum of a specimen from the Grey Chalk
near Lewes.
Isle of Wight; reduced to two thirds its natural diameter; in my
> — a
PLATE. .A29 11.
Fig.
iz and 6. Ammonites CenomANENSIS; from the Grey Chalk of Dover; reduced to two
thirds its natural diameter ; in the collection of J. S. Bowerbank, Esq.,
p. 37.
la, side view.
14, front view.
2. AMMONITES HIPPOCASTANUM ; from the Lower Chalk of Man of War Cove, Dorsetshire ;
in the collection of E. H. Bunbury, Esgq., p. 37.
3a and 6. AMMONITES HIPPOCASTANUM, young; from the Lower Chalk of Chardstock ; in
the collection of E. H. Bunbury, Esq., p. 37.
3a, side view.
30, front view.
4a, 6, and c. AMMONITES HIPPOCASTANUM; a fragment, from the Lower Chalk of Chard-
stock ; in the collection of E. H. Bunbury, Esq., p. 37.
4a, back view.
46, side view.
4c, outline of a septum.
5a and 6. Ammonites GoupiLianus; from the Lower Chalk of Sussex; in the British
Museum, from the collection of Dr. Mantell, p. 38.
6. Ammonites GovPiLiaNus; outline of a septum, copied from Pl. xciv of M. D’Orbigny’s *;
‘Paléont. Frang. Terr. Crét.,’ p. 38.
7a and 46, Ammonites VeLLep@; from the Upper Chalk near Norwich ; in the collection
of F. G. Bayfield, Esq., of Norwich, p. 39.
7a, side view. wN.B. The umbilicus is represented too large, the artist having
been deceived by the breaking away of the soft chalk. .
76, front view.
e
*
¢
Pa
.
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De
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a
iA
‘
as
ere
lantetlicevas CO vleny
6 4% ‘
LA. tutielion
PLATE XVIII.
Fig. eos
1. AMMONITES NAVicULARIS; from the Grey Chalk of White Nore, Dorsetshire; in the
collection of E. H. Bunbury, Esq., p. 39.
2, AMMONITES NAVICULARIS; from the Grey Chalk near Lewes; in the collection of
Henry Catt, Esq., p. 39. ‘4
3a and 6. AMMONITES NAVICULARIS; from the Lower Chalk of Chardstock ; in the collec-
tion of John Morris, Esq., p. 39.
3a, front view.
30, side view.
4a and 6, Ammoneres-Manauiia ; from the Grey Chalk of Bonchurch, Isle of Wight ; in
the collection of S. Saxby, jun., Esq., p. 40.
4a, side view.
46, front view.
‘5a, 6, and c. AMMONITES NAVICULARIS; from the Lower Chalk of Chardstock ; in the
collection of John Morris, Esq., p. 39.
5a, side view.
56, front view.
5c, front view of the inner whorl of the same specimen.
Mantelliceras
6a and 6. Awemonrres Manreri1; from the Chloritic Marl of the Isle of Wight; in the
collection of John Morris, Esq., p. 40.
6a, side view.
64, front view.
Mantellicevas
Ta, 6, and c. Ammonzexs Manvreii1; from the Chloritic Marl of Bonchurch, Isle of
Wight ; in the collection of S. Saxby, jun., Esq., p. 40.
Za, side view.
76, front view.
7c, outline of septum.
8. AMMONITES*NAVICULARIS; outline of the septum of the specimen fig. 1, above.
Se te Tee
ma anit
:
i Se
na ~~ ae ada
PLATE XIX.
Fig.
la, 6, and ec. Ammonites Coupe; var., from the Grey Chalk of Ventnor, Isle of Wight ;
3a and 8.
4a and 6.
5a and 6.
in my possession, p. 23.
la, side view.
14, back view.
le, section of a whorl.
_ 2a, 6, and c. Ammonites Renavuxianus ; a young shell, from the Grey Chalk of Ventnor,
Isle of Wight ; im my possession, p. 41.
2a, side view.
24, back view.
3c, front view of inner whorl of the same specimen.
AMMONITES OCTO-sULCATUS ; from the Grey Chalk of Ventnor, Isle of Wight ;
in my possession, p. 42.
3a, side view.
36, front view.
Ammonitzs Icrenicus; from the Upper Chalk, near Norwich; in the collection
of Mr. King of Norwich, p. 43.
Aa, side view, showing the outline of a septum.
46, front view.
Ammonites Devertanus; from the Grey Chalk of Sussex; in the British
Museum, from the collection of F. Dixon, Esq., p. 43.
5a, side view.
56, front view.
6. Awmonttes VELLEDS; from the Grey Chalk of Ventnor, Isle of Wight; in my pos-
session, p. 39.
6, outline of a septum.
PS — at ff oo LA SD Ee at eae ai
. PLATE XxX.
Fig. \etasigaleeras
ae: 6, c. AMMONITES RUSTICUS ; from the Lower Chalk, near Lyme Regis ; in the Museum
of Practical Geology ; reduced to two thirds its natural diameter, p. 44.
The surface of the inner part has decayed away.
la, side view.
14, back view.
le, section of the outer whorl.
Acompsocevas
Jape by 2a, 6, and c. AMMoniTEs ReNEVvIERI; from the Grey Chalk, near Blackdown, Isle of
deh: oS Acempsrceres, Nyolt _ Wight; in the collection of E. Renevier, Esq., of Lausanne, p. 44.
2a, side view.
26, front view.
2c, outline of a septum.
3a and 6. AmMmonitzs Saxsri; from the Grey Chalk of Ventnor, Isle of Wight; in my
possession, p. 45.
3a, side view.
36, front view.
4a and 6. Ammonites Vectensis; from the Chloritic Marl of Ventnor, Isle of Wight ; in
my possession, p. 45.
Aa, side view.
44, front view.
3 diam.
2
West ith
~
eo.
PLATE 7xa40
Fig. 4 Anisce vas ;
la, 4, c. Ammonites Lewesiznsis; from the Grey Chalk, near Dover; in the coll
of S. J. Mackie, Esq., of Folkstone, p. 46. “ ‘
la, side view. |
14, front view.
lc, outline of a septum.
Uaplocevas +
2. AMMONITES LEPTOPHYLLUs ; outline of a septum of the specimen, , Plate sou :
3a, b, c. Ammonites Wresti1; from the Chalk with silicious grains, Char dst ock
Somersetshire ; in the collection of J. Wiest, Esq., p- 47.
3a, side view.
36, back view.
3c, section of a whorl.
Ee West lath ;
PLATE KXIL
Fig.
la, 6. AMMONITES LEPTOPHYLLUS ; from the Upper Chalk of Greenhithe, Kent; in the
collection of L. Barrett, Esq., reduced to two fifths its natural diameter,
p. 48.
la, side view.
14, front view.
oC : ae
“ uu OLS Cars
LAB PO
2a, 6, c. Ammonites GoLLEvILuENsis ; from the hard Chalk of Damlaght, in the county
of Derry, Ireland; in the Museum of Practical Geology ; reduced to
three fourths its natural diameter, p. 48.
2a, side view.
24, front view.
2c, outline of a septum.
eateries
ee ee
PLATE XXIIL
Fig.
la, 4, c. Ammonites curvatus; from the Grey Chalk of Ventnor, isle of Wight ; in my
possession, p. 49.
La, side view.
14, front view.
le, outline of a septum.
%. AMMONITES FALCATUS ; outline of the septum of a specimen from the Chloritic Marl of
Ventnor, Isle of Wight ; in my possession, p. 21.
3a, 6, c. AMMoniITEs Saurert; from the Chalk with siliceous grains, Chardstock,
Somersetshire ; in the collection of J. Wiest, Esq., p. 50.
3a, side view.
34, front view.
3c, outline of a septum.
4a, 6,c. AMMonires Ramsayanus; from the Chalk with siliceous grains, Chardstock,
Somersetshire ; in the collection of J. Wiest, Esq., p. 51.
Aa, view of the left side.
44, view of the right side.
4c, front view.
ja, 6. AMMonires Saureri; from the Chalk with siliceous grains, Chardstock, Somerset-
shire ; in the collection of J. Wiest, Esq., p. 50.
5a, side view.
56, front view.
6a, 6, c. Ammonites Feraupianus; from the Grey Chalk of Ventnor, Isle of Wight ; in
thy possession, p. 52. a
6a, side view.
64, front view.
6c, back view.
7a, 6. Ammonites Bravatstanus; copied from Plate XCI, figs. 3 and 4, of D’Orbigny’s
‘Paléontologie Francaise, Terrains Crétacés.’ p. 52.
8. Ammonites Bravaisitanus; from the Middle Chalk of Dover; in the collection of
of S. J. Mackie, Esq.: the specimen has been worn, and the tubercles
are nearly all rubbed off, p. 52.
9. Ammonites Bravaistanus; from the Middle Chalk of Dover; in the collection of
J. W. Flower: restored by the artist from a broken specimen, p. 52.
10a, 6, c. AMmMonitxs WiitoneEnsts; from the Grey Chalk, near Devizes, Wiltshire; in
the collection of W. Cunnington, Esq., of Devizes, p. 53.
10a, side view. ;
104, front view.
10c, outline of a septum.
lla, , c, d, e. Ammonrres Juxesi1; from the hard Chalk of the county of Londonderry ;
in the Museum of Practical Geology, p. 53.
lla, side view of a fragment, with part of three whorls.
114, side view of the two inner whorls of lla.
lle, back view of 116.
11d, section of the whorls restored.
lle, part of the outline of a septum.
ad
\
Geo West, kth.
— ees.
PLATE XXIV.
Fig.
la, 6. Aprycnus LEpTopHYLLUs; from the Upper Chalk of Brighton; in Mr. Sharpe’s
collection (Geol. Soc.), p. 55.
la, concave (internal) surface.
14, smooth, convex surface.
>
2, 3, 4. Aprycuus Porrtockir; from the Upper Chalk of Norwich; 2 and 3 in the col-
lection of Mr. Bayfield; 4 in the British Museum, p. 56.
5. Aprycnuus GoLLEVILLENSIs ; Upper Chalk, Norwich; in the collection of Mr. Bayfield,
p. 56. .
6. Aprycuus Portiocki1? p. 56.
7. Aprycuus Icunicus ; Upper Chalk, Norwick; Mr. Bayfield, p. 57.
8a, 6, and 9. Aprycuus rucosus; Upper Chalk, Norwich, p. 57.
8a, external, sculptured surface of a pair of valves; in the collection of Mr.
Bayfield, p. 57.
84, internal surface, showing lines of growth.
9, external surface of a large valve, in the collection of Mr. John King, of
Norwich, p. 57.
10a, 6. Aprycuus pERaAMPLUs ; Upper Chalk, Norwich; Mr. Bayfield, p. 58.
10a. internal, striated surface.
104, external surface of a fragment.
11. Outline of the aperture of AMMonrrss IceNtcus.
12. * . A. PorrLocktl.
13. i = A. LEPTOPHYLLUS.
14. r z A. PERAMPLUS.
15. m 4 A. GoLLEVILLENSIS.
‘P1.XXIV
Cine
SS US
CT eee
Geo. West, ith.
Ford & West, Imp
PLATE Bea,
Fig.
1. TurriLites TuBErcuLatus ; from the Grey Chalk of Ringmer, Sussex ; in the British
Museum, from the collection of Dr. Mantell, p. 61.
2. TURRILITES TUBERCULATUS, Showing the produced mouth; from the Grey Chalk, near
Lewes ; in the British Museum, from the collection of Dr. Mantell, p- 61.
3. 'TURRILITES TUBERCULATUS ; a fragment, showing the position of the lobes of a septum
on the outer side of a whorl; from the Grey Chalk of Ventnor, Isle of Wight, in
my possession, p. 61.
4. TURRILITES TUBERCULATUS ; a young specimen, from the Grey Chalk of Ventnor, Isle
of Wight ; in the collection of S. Saxby, jun., Esq., p. 61.
5. Turritires Manteui1; from the Grey Chalk, near Lewes; part of the outline of a
septum is shown on the upper whorl ; in the British Museum, from the collection
of Dr. Mantell, p. 63.
6a, 6. Turritires Mantetii; from the Grey Chalk, near Lewes; an adult individual,
showing the produced mouth ; in the British Museum, from the collection of Dr.
Mantell, p. 63.
7a, 6. Turritites GRAvEsIANus; from the Grey Chalk, near Lewes; the position of the
lobes of a septum is shown on the lower whorl of fig. 7a ; in the British Museum,
from the collection of Dr. Mantell, p. 62.
i —
4
wri
G.West Lith
PLATE XXVI.
1. Torriurrus Scurvcazerianus ; adult, with the mouth produced ; from the Grey Chalk
of Ventnor, Isle of Wight ; in my possession, p. 64.
2. TurRiLires SCHEUCHZERIANUS ; a young shell, on which part of the produced mouth
is preserved ; from the Grey Chalk of Ventnor, Isle of Wight ; in my possession}
p. 64.
3. Turriires ScHEUCHZERIANUS ? a very young shell, with the produced mouth com-
pletely formed ; from the Grey Chalk of Ventnor, Isle of Wight ; in my posses-
sion, p. 64.
4, 5a, 6, 6, 7a, 6, and 8. ‘Turritivzs Morrisi1; five specimens of different ages; from
the Chloritic Marl of Ventnor, Isle of Wight; in my possession, p. 65.
54, shows the base of the whorl of 5a.
76, is the outline of the septum of 7a.
9. Turritites Bercert; a fragment, showing part of the outline of a septum; from the
Chloritic Marl of Ventnor, Isle of Wight ; in my possession, p. 65.
10. Turritites Berceri; a fragment, from.the Grey Chalk, near Lewes; in the British
Museum, from the collection of Dr. Mantell, p. 65.
11. Turritires Brerceri; fragment of a young shell; from the Chalk with siliceous
grains, Chardstock, Somersetshire ; in the collection of J. Morris, Esq., p. 65.
12, a, 6. Turrtrres, species undetermined ; the last whorl of an adult shell, with the mouth
produced; from the Grey Chalk of Lewes; in the British Museum, from the
collection of Dr. Mantell.
13a, 6. Turriuires Brcnzr; from the Chalk with siliceous grains, near Lyme Regis;
part of the outline of a septum is seen on the second whorl; presented to the
British Museum by the late Sir H. T. de la Beche, p. 66.
14. Turritites Gravesianus; outline of part of a septum.
15. TurRILITES TUBERCULA'US ; outline of part of a septum.
16. TURRILITES TUBERCULATUS ; outline of part of a septum; from the Chloritic Marl of
Bonchurch, Isle of Wight ; in the collection of S. Saxby, jun., Esq., p. 61.
Z a Ar
fe ——. _ ee ‘
4 ana ee) re, ee
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< ¢ F $
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= 9
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¢
PLATE XXVII.
Fig.
1. TurriLitzs costatus; young, from the Grey Chalk of Ventnor, Isle of Wight; in
my possession, p. 66.
2a, 6. TurRILitEs costatus; adult, with the mouth completely formed; from the Grey
Chalk of Ventnor, Isle of Wight; in my possession, p. 66.
2a, side view.
26, view of the base, with the perfect mouth.
3 and 4. TurriLires costatus; two small specimens which have already formed the
produced mouth; from the Grey Chalk of Ventnor, Isle of Wight; in my
possession, p. 66.
5. TURRILITES costaTUS; young, from the Grey Chalk of Ventnor, Isle of Wight; in
my possession, p. 66.
6 and 7. Turrinites Birrons? D’Ord. ; from the Lower Chalk, Ventnor, p. 67.
8. Turriuites Wiesti1; from the Grey Chalk of Ventnor, Isle of Wight; in my posses-
sion, p. 67.
9a, 6. Turritites Wixsti1; young, from the Chalk with siliceous grains, Chardstock,
Somersetshire ; in the collection of Mr. John Morris, p. 67.
9a, side view.
94, base of a whorl.
10. Turritites Bercert? var.; from the Chloritic Marl of Bonchurch, Isle of Wight.
(Mr. Saxby.)
11. Turrinires Puzostanus, D’ Ord. var.; from the Chloritic Marl of Bonchurch, p. 68.
12. Turriites costatus, var.; from the Lower Chalk of Ventnor, Isle of Wight.
13. TuRRILITES TUBERCULATUS, var.; from the Lower Chalk of Ventnor.
These two figures (12, 13) are doubtfully referred to the above species, aud —
may hereafter prove to be distinct: the specimens are only fragments, and in
an imperfect state of preservation.
14a, 6. Turritites Wizstit, var.; from the Lower Chalk of Ventnor.
15. Turriuites costatus, var. 7. triplicatus, J. Sow. ; Lower Chalk, Sussex; from the
original in the British Museum, p. 66.
16. Septum of 7. costatus, p. 66.
17. Septum of 7. Wrestii, p. 67.
Pl] XXVIII
Geo West,ith
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