18

(5 Geological Journal

no. 25 p. 18 Murchison no break in life so complete as between Permian & Trias yet everywhere generally conformable –(good)

[Roderick Impey Murchison. 1851. The slaty rocks of the Sichon, or Northern end of the chain of the Forez in Central France, shown to be of Carboniferous age.]

p 32 Trimmer believes same mammals inhabited England before & after glacial

[Joshua Trimmer. 1851. On the origin of the soils which cover the chalk of Kent.]

no 26 Fraas p. 55 Suppl says ammonites radians present same in many localities even near each other; I do not think I have met with this before; yet must occur

p. 61 case of several species occuring in bed 4 ft thick together; which in others distinct – are invariably separated.

[Oscar Fraas. 1851. On the comparison of the German Jura formation with those of France and England.]

27 p. 166 Murchison, it is strange how same exact succession rest on Azoic strata in England & Bohemia

[R. I. Murchison. 1851. On the Silurian rocks of the South of Scotland.]

186 Bunbury, says it is exception to general rule that Ferns of Oolite are not more like recent than are carboniferous

- it is rather case of Heer's & Bronn, the very old types have not allied much, - a trench

If to common rule it be added, "when form of groups has been much modified'' it will hold true

[C. J. F. Bunbury. 1851. On some fossil plants from the Jurassic strata of the Yorkshire coast.]

no 28 p. 310 Strachey (1851) Extinction of glaciers on tertiary plain of Thibet, shows that extinction was post-tertiary – explains glacier by sea being washed foot of Himalaya & so made closest [minutes]

[Richard Strachey. 1851. On the geology of part of the Himalaya mountains and Tibet.]

p 267 Salter on coprolites in Lower Silurian, which almost certainly must have been from Vertebrates

[John William Salter. 1851. On the remains of Fish in the Silurian rocks of Great Britain.]

no 29 87 Hopkins paper on deflection of Gulf-stream N. B. a S. America boulder on the most recent Tertiary deposits -I think Boulder angular at Cauquenes

p 92 quote D'Orbigny from about doyen shell common to Europe & W Indies

[W. Hopkins. 1851. On the causes which may have produced changes in the Earth's superficial temperature.]

p 104 Mantell on Telerpeton Devonian Reptile – indicate a peculiar type. "which as in numerous other cases of extinct forms of the Class, osteological character are associated, which is existing oviparous quadrupeds are restricted to distinct order" Thus Labyrinthodont which in England are generally considered as Batrachian are regarded as Saurian by many eminent foreign palæontologist Meyer, Plieninger Pictet

[Gideon Algernon Mantell. 1852. Description of the telerpeton.]

no 31 p 197 Forbes on affinity of 2 land-shells to America & of others to W. Africa & our inhabitants

so (p198) St Helena marine mollusca point to connection in same line in very ancient time. How [illeg] – why if not transformed – no one wd expect identity

[Edward Forbes. 1852. On the extinct land-shells of St. Helena.]

p. 208 Phosphate nodules also [found] in some in Silurian of N. America

[W. E. Logan. 1852. On the foot-prints occurring in the Potsdam Sandstone of Canada.]

p 23 Suppl It really appears as if (Goeppert) the Flora of Carboniferous did endure long.

[H. R. Goeppert. 1852. On the flora of he transition rocks.]

no 32 p. 33 suppl. Barrande his recent Faunas & [illeg] of America has many representative species

[M. J. Barrande. 1852. On the three successive faunas, distinguished by their peculiar trilobites, in the lowest Palæozoic rocks.]

p 37 His Colonies

[M. J. Barrande. 1852. On the "Colonies" in the Silurian formation of Bohemia.]

no 34 p 60 Lyell on Land-shell in Coal measures & Reptile

[Charles Lyell. 1853. On the remains of a reptile (Dendrerpeton acadianum, Wyman and Owen, etc.)]

p 69 Owen sticks to Archegosaurus being Batiachian, of lowest kind.

ie perennibranchiate (& aquatic F. W)

[Prof. Owen.1853. Notice of Batrachoid fossil in British coal-shale.]

no 35 p. 130 Moore shown in distinct affinity of St Domingo fossil with W. America

[J. C. Moore. 1853. Notes on the fossil mollusca and fish from San Domingo.]

p 163 Ramsay Cambrian to Caradoc 42,000 ft thick conformable

168 – on conglomerate of various rocks, slate &c in oldest Cambrian bed

[Andrew C. Ramsay. 1853. On the physical structure and succession of some of the Lower Palæozoic rocks of North Wales, and part of Shropshire.]

19

(6 Geological Journal

no 37 p 2 suppl – Flora of Amber not tropical or sub-tropical.

[Professor Goeppert. 1854. On the fossil plants found in Amber. Berlin Acad. Bull., 1853: 450-476, etc.]

no. 38 Forbes p. XXXIX Caradoc sandstone intermediate between Upper & lower Silurian

do XXII – Potsdam = Barrande primordial

XXIII is strong in ancient geographical Faunas with representative species

XXVI Barrande is strong on the same species appearing at slightly different stages in different countries – B. has discussion on the grain changes in Trilobites – progressive development of eyes – reduction of thorax &c stricture preceding granulation – then insignificant feature giving favia to Fauna Von Buch has said "the smallest difference acquires value by constancy".-

XII F. says "it will be more & more evident that the perishing of species is simply the result of the of the influence of physical changes in specific areas". Grey inn

without change of other species included in term physical

LXII – on unique genera time areas in Brachiopods

LXIII Leptæna now proved to be Liassic

LXVII on time-areas of Nummulites

p 188 Sharpe good remark on arguing in [inches] species distinct became in different formation

[Daniel Sharpe. 1854. On the age of the fossiliferous sands and gravels of Farringdon and its neighbourhood.]

p 6 class Barrande Bohemia very rich in species of Cephalopods, poor in genera – (evidence of increasing group) no cephalopods in Primordial Fauna

[M. J. Barrande. 1854. On the Silurian Crustracea, Pteropoda, and Cephalopoda of Bohemia.]

no 40 p 368 Müller shows that Heterocercy passes insensibly into Homocercy

p 369 Egerton case of homocercus ganoid below Lias

[Sir P. de M. Grey Egerton. 1854. Palichthyologic Notes. No. 6. On a fossil fish from the Upper Beds of the new Red Sandstone at Bromsgrove.]

388 Westwood gigantic ant in Lower Purbeck

[J. O. Westwood. 1854. Contributions to fossil entomology.]

431 Spalacotherium mammal from Purbeck – perhaps a placental insectivore – between Stonesfield & Eocene

[Professor Owen. 1854. On some fossil reptilian & mammalian remains form the Purbecks.]

no 42. p 125 Owen on Coccoteuthis – is a genera of Cephalopods with very intermediary "osculent character between the Sepiadæ & the Loliginidæ"

[Prof. Owen. 1855. Notice of a new species of an extinct genus of Dibranchiate Cephalopod (Cocoteuthis latipinnis) from the Upper Oolitic Shales at Kimmeridge.]

no 43 p 209 Prestwich on local phænomena modifying relation in allied & [synchron] beds

211 do Lower Clay not referenced in Paris basin, & yet there no appearance of link unifying – he enlarges how curious & striking this fact is

p 223 repeat this Brunton

p 240 Fragmentary as all not Tertiaries, believe they were connected as littoral deposits??

[Joseph Prestwich. 1855. On the correlation of the Eocene tertiaries of England, France, and Belgium. Read 21 June 1854.]

no 44 Murchison p. 450 on absolute uniformity of Permian & Trias throughout Germany & yet complete change of life

[Roderick Impey Murchison and J. Morris. 1855. On the Palæozoic and their associated rocks of the Thüringerwald and the Harz.]

p 464 Baily on S. African cretaceous fossils, somewhat like Indian, close affinity with some cretaceous species & one species identical., a Pecten

[William H. Baily. 1855. Description of some cretaceous fossils from South Africa, etc.]

515 at present level the Missouri have twice [inundated] the Red River; a small change of level wd produce resolution in line of drainage – so will with rivers

[A. K. Isbister. 1855. On the geology of the Hudson's Bay Territories, and of portions of the Arctic and North-western regions of America; with a coloured geological map.]

562 Hooker on some Eocene vegetation not showing tropical climate

[J. D. Hooker. 1855. On some minute seed-vessels (Carpolithes ovulum Brongniart) from the Eocene beds of Lewisham.]

20

(7  Geological Journal

no 45 p 26 Salter on 5 or 6 new Crust of large size in Lower Palæozoic

[J. W. Salter. 1855. On some new crustatea from the uppermost Silurian rocks.]

p 37 Huxley on distribution between larval & embryonic stages; view I think exaggerated = The above ancient Crustacean is a larval form.

[T. H. Huxley. 1855. Observations on the structure and affinities of Himantopterus.]

p 69 Austen on extension of Coal-shale – the proper impression in with idea that Eocene was during whole Secondary epoch like the Malay Archipelago, lower if succeeded by coral reefs

The St. Cassian beds show what a gap elsewhere

[R. Godwin-Austen. 1855. On the possible extension of the coal-measures beneath the South-eastern part of England.]

no 46 p. CI. Hamilton below lower Silurian, in N. America there seem to be 2 unconformable azoic formations – p do terrace 200 ft with recent shells on Red Sea I. of Suez

C.III. Ichthysaurian & ammonites in extreme N. Melville Isld Lias age

p. 128 Owen on decrease of Horn of Red Deer in Scotland, since Historical times

p 130 do Head Musk-deer been only fossil, it wd have reasonable to suppose it unfit for Arctic climes

[Professor Owen. 1855. Description of a fossil cranium of the musk-buffalo [Bubalus moschatus, Owen; Bos moschatus (Zimm. & Gmel.), etc.]

no 47 p 21 Suppl. The Aptian & Rhodanian are much more distinct on Continent & together make x English Lower Greensand – (this shows that other formation may include vast lapse of time

Blackdown Deposit have mingled Lower Greensand, [Gault] & Upper Greensand

[M. E. Renevier. 1856. On the lower Greensand and the Blackdown fossils of England.

no 48 p 313. Wright on Lias shows that the Cephalopods, Brachiopoda Echino[dermatan] generate mark scale & have fewer species in common than Cephalo[poda-bed] & Gasteropoda. The case of Brach offered only general rule that in each class, the higher change more rapidly – It is like in geographical distribution, some low as Carice are very local.

[Thomas Wright. 1856. On the Palæotological and stratigraphical relations of the so-called "sands of the inferior Oolite."]

no 49 p. 4 Owen calculates that the Stereognathus of Stonesfield was an Ungulate animal: It is not marsupial

p. 5 talk of "variety as non essential" (bis) as principle, explaining making one leaf to differ from other

[Professor Owen. 1856. On the affinities of the Stereognathus Ooliticus (Charlesworth) a mammal from the Oolitic slate of Stonesfield.]

p 69 Austen, number of the late change very imperfect- "least understood"

[R. Godwin-Austen. 1857. On the newer tertiary deposits of the Sussex coast. Read 7 November 1855.]

p 129 Prestwich, most curious talk of representative species almost same in number in Bracklesham & Calcaire grossier – Barton Clay & Sables Moyens, with only few identities

(a) yet if not separated by land, very strange such difference in so short a distance can they be really contemporaneous? How in Malay Archipelago?

p 132 (do) "it is very interesting to note how constant & steady in the proportion of change (in species) in its several subdivision of each formation. The disappearance & appearance quote apart for then quote breaks, which &c" – very good to quote. –

[J. Prestwich. 1857. On the correlation of the Eocene tertiaries of England, France, and Belgium. Read 18 June 1856.]

no 50 p xxv Woodward says that number of extinct molluscs to recent as 9 to 10 (& yet Brown calculates 30 renewal of species on earth? shows how imperfect record, & gaps –

p. 195 on different appearance of teeth in an ox & sheep

[Professor Owen. 1857. On the Dichodon cuspidatus, Owen.]

p 213 Prestwich on denudation of Weald – [illeg] axis varied somewhat during Cretea period

[Joseph Prestwich. 1857. On some fossiliferous ironstone occurring on the North Downs.]

7v

(a) How can in world an isthmus separating 2 marine corals, Faunas, & yet have often we seen in Books 2 fossil faunas which geologists by superposition believe to be of same age, & yet with so many representative species, that at so short a distance our present experience [wd] lead to double distinct, & so an isthmus is [illeg] – I suspect many more formations have to be intercalated. – If known type formation be later times is / in [lower] then it may well happen that many will have to be intercalated.

21

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no 51 p. 275 Falconer on Plagiaulex – a gneist with Microlestes

p 276 a most specialized form.

[H. Falconer. 1857. Description of two species of the fossil mammalian genus Plagiaulax from Purbeck.]

no 52 p. 310 p. 320 Falconer on blending of Elaphas & Mastodon, thought so distinct at extremes

p 319 species natural – all genera only artificial

[H. Falconer. 1857. On the species of mastodon and Elephant occuring in the fossil state in Great Britain. Part I.]

no. 53 p. 50 Murchison we all know how distinct the separation all in limited area, & how such separation vanishes when larger area examined

p 52 In Baltic Provinces of Russia, all Silurian strata only 200 ft thick & all conformable & nearly similar in composition & only to be separated by palæontologist

p 53 E. of Ural – Bohemia & Scandinavia have all representative species: is there another case of Isthmus?

[R. I. Murchison. 1857. The Silurian Rocks and fossils of Norway, as described by M. Theodor Kjerulf, those of the Baltic Provinces of Russia, etc.]

p 67 Owen, on general (not specialized) character of teeth of old Mammals

[Prof. Owen. 1857. Description of a small Lophiodont mammal (Pliolophus vulpiceps, Owen), from the London Clay, near Harwich.]

73 Salter, coniferous wood in Devonian Rocks

p 76 Lycopodium in passage rocks between Devonian & Silurian

[J. W. Salter. 1857. On some remains of terrestrial plants in the old Red Sandstone of Caithness.]

no 54 Falconer p 84 On Elephas primigenius in U. States,[re…] by distinct species in S. U. S.

[H. Falconer. 1857. On the species of mastodon and Elephant occuring in the fossil state in Great Britain. Part II.]

p 153 In Crimea (Baily) there in middle Tertiary with Caspian Cardium &c, & near Sevastopol a newer Tertiary, more marine

[William H. Baily. 1857. descriptions of fossil invertebrate from th Crimea.]

p 171 Trimmer In Norfolk an older [n…] Boulder Clay, & newer Oolite boulder drift.

[Joshua Trimmer. 1857. On the upper and lower boulder-clays of the Gorlston Cliffs in Norfolk.]

55 p 261 Godwin Austen believe even that the greater part of animal remains in Chalk have been floated there by same aging as boulder.

[Robert Godwin-Austen. 1857. On a boulder of granite found in the "White Chalk" near Croydon; etc.]

269 Huxley, quote Pander on existence of 2 species of Silurian Auchenaspis

p 279 Capital sketch of affinities of Ganoids – their relations between Teleosteans & Cartilaginous – 6 recent genera of Ganoids all F. water all in N. hemisphere

294 Huxley The Teleosauria, anatomically & chronologically bridge over distance between Nothosaurus & Alligator

[Thomas H. Huxley. 1857. On Cephalaspis and Pteraspis.]

330 Prestwich - it is clear Weald [illeg] axis of Elevation at commencement only Cretaceous period: if I use my case, I must say commencement of Chalk

[Joseph Prestwich. 1857. On the age of some Sands an Iron-Sandstones on the North Downs.]

p 25 Suppl – Bone bed of continent – is intermediate – so that Liassic shells lived with Triassic fishes.

[A. Oppel and Fred. Rolle. 1857. On the fossil Faunæ of the equivalent of the bone-bed between the Keuper and the Lias.]

56. p CIII Port-… number of Reptiles from Coal

p 395 Bigsby all the Palæozoic groups of her gull pass & easy organic gradation into each other

p 428 Bigsby 29 groups in U. S. of Palæozoic or ever more 430 each of to 13 main over a new centre of life

450 on few cases of transmission form over fauna to another.

[J. J. Bigsby. 1857. On the Palæozoic basin of the state of New York.]

536 Selwyn has seen no teeth of Glacial action Bones of Dingo (2)

[Alfred R. C. Selwyn. 1858. On the geology of the gold-fields of Victoria.]

22

(9 Geological Journal

57 p 7. Appendix Wesel & Weber on Brown Coal Flora – strange mixture of Australian & European Flora – if to be trusted Australia & S. Africa preserve wrecks of former life.

[Dr. P. Wesel and Dr. O. Weber. 1859. Contribution to the Tertiary flora of the Brown-Coal of the Lower Rhine.]

58 201 Ramsey on Glacial of Canada Silurian & great subsequent [duration] 3000 ft

203 Glacial deposits in Canada in parts 500-800 ft in thickness times!

211 White mountains trace of Glaciers

212 Erosion of Niagara began little before close of drift, & Lyells 35,000 year probably too little

[Andrew Ramsay. 1858. On some of the glacial phænomena of Canada and the North-eastern provinces of the United States during the drift-period.]

271 & 2 Bigsby on reappearance of same sp. in successive formations –

274 same forms recur in U. States & Wales – 275 do 276 do

p. 279 Rhizopodous tribe very common in lowest Silurian of Russia

279 Break in succession

280, 2 genera which appear earlier in Europe than in America

283 Law of appearance of form curiously same in America & Europe

59 287 Bigsby – several cases of closely adjoining districts of same formations with many species distinct – must be, I think, distinct ages good.

288 James Hall on species when extinct never recurring. Angelin on do.

290 on proportion of recurring or reappearing species

(a whole fauna never recurs)

292 on similarity of laws of appearance & disappearance in distinct basin the same

[J. J. Bigsby. 1858. On the Palæozoic basin of the state of New York. Part III.]

60. p. 16 Supplement. – Sporadic genera of Birds far older than those now having confined ranges. infers that anciently wide-… genera were local.

60 suppl p 610 on range of Chil….

61 48 Wright on 3 zones of life in Jurassic Oolite – because age

[Thomas Wright. 1859. On the subdivisions of the inferior Oolite in the South of England, etc.]

49 & 61 Owen Dicynodon Fauna confined to S. Africa, many genera & not genera if had wandered into Europe how abrupt it wd have appeared

[Professor Owen. 1859. On some reptilian fossils from South Africa.]

78 Hull – on Beds showing current very local – on one formation theory at the S. E (Even to look at beds of same age & [illeg] thickness spreading all over Europe)

[Edward Hull. 1859. On the South-easterly attenuation of the lower secondary formations of England, etc.]

62 Prof Phillips

XXXVIII in each zone of fossils poor origin, rich development & their decrease

XLIII on wide range of Palæozoic fossils

XIV on increase & decrease of groups

XLVII increase of new forms without replacement

XLVIII cases of replacement

LI changes of forms slower in old times

[John Phillips. 1860.Anniversary address of the President.]

p. 148 Selwyn on skull of Dingo in caves

[A. R. C. Selwyn. 1859. Notes on the geology of Victoria.]

p. 202 Glacial action in Vancouver Isld

[Hilary Bauerman. 1859. On the geology of the south-eastern part of Vancouver Island.]

Appendix p. 19 Good case of transitional ammonite bearing on above (24 new Cephalopods [illeg] ) objections by Phillips—

[Franz Ritter von Hauer. 1860. On new Triassic Cephalopoda from Halstatt.]

22

(10 Geological Soc. Journal

63 p 269 & 270 Dawson on land-shells T. Reptile & Myriapod in fossil coal-trees oldest myriapod Jurassic

270 1 terrestrial Devonian Plant. Sigillariæ

[J. W. Dawson. 1859. On a terrestrial mollusk, a Chilognathous Myriapod, and some new species of reptiles, from the coal-formation of Nova Scotia.]

64 Jamieson p 361 on ages since glacial in Scotland

p 366 3000 ft submergence during glacial period

370 summary of latest history of [illeg] in Scotland

[T. F. Jamieson. 1860. On the drift and rolled gravel of the North of Scotland.]

p 377 Wright on avicula bed

p 388 poverty of the zones in England in species; as zone get more divided, they in fact get poorer & the G. Record more imperfect

p. 392 do. – 398 403-409

p. 411 My conclusion.

[Thomas Wright. 1860. On the zone of Avicula Contorta, and the lower Lias of the South of England.]

p 441. Salter on wide range & size of Spitzbengen fossils

[J. W. Salter. 1860. Note on the fossils from Spitzbengen.]

458 on extreme antiquity of same variable forms of Foraminifera

[T. Rupert Jones. 1860. On some fossil foraminifera from Chellaston near Derby.]

491 Falconer on cave fossils all of same date & modern

[H. Falconer. On the Ossiferous caves of the Peninsula of Gower, in Glamoranshire, South Wales.]

494 Owen on Triassic mammal with probably Reptilian character; but case too doubtful.

[Professor Owen. 1860. On some small fossil vertebræ from near Frome, Somersetshire.]

65 63 Salter on increasing range of molluscs in Devonian, reaching maximum in Carboniferous p. – Palæozoic genera very wide range

[J. W. Salter. 1860. On the fossils, from the High Anders, collected by David Forbes.]

83 Huxley – Mammalia a generalized types yet recent – on non-correlation in ch to characters of cervical vertebræ, being camel-like & yet animal not a camel

[T. H. Huxley. 1860. On a new species of Macrauchenia (M. Boliviensis).]

Append p. 6 Suess on several changes in mammals in Vienna Basin whereas several hundred sea-shells still existing.

66 p XXXVIII L. Horner on excessive poverty of India beds, good

LV. on close relation of elevatory remnants, or rather disturbance & metamorphic action

LXVI. On depth between Sicily & Africa & Malta & do

67 305 on Permian shells at our stage being bigger

314 on small changes in the Permian succession

[James W. Kirkby. On the Permian rocks of South Yorkshire; and on their Palæontological relations.]

68 406 Erosions on West American coast

[James Hector. 1861. On the geology of the country between Lake Superior and the Pacific Ocean etc.]

474 on great range of some F. W. shells Corbicula –does not show greater worth after Glacial

[J. Gwyn Jeffreys . 1861. On the Corbicula (or Cyrena) fluminalis geologically considered.]

529 High Cretacean carried much further back – good

[J. W. Salter. 1861. On some of the higher crustatea from the British coal-measures.]

69 p. 6 six Reptiles & insects in Coal of Joggins – Pupa

[J. W. Dawson. 1861. Notice of the discovery of additional remains of land animals in the coal-measures of the South Joggins, Nova Scotia.]

p 34 28 carboniferous Brachiopods in Punjab of 13 common to Europe; but Punjab are larger shells

[T. Davidson. 1861. On some carboniferous Brachiopoda collected in India by A. Fleming and W. Purdon.]

70 p XIV on contemporaneity of Beds.

p XLIX on what orders extinct

p II old animals not endogenic – on specialization

71 p. 180 Jamieson in relation of glacier period to migration of mammals

[T. F. Jamieson. 1862. On the ice-worn rocks of Scotland.]

p 189 Ramsay – it is rarest thing in nature to find anticlinal or synclinal troughs with tops not denuded

p 191 On Miocene Glacial [illeg]

p 204. Ramsay thinks glacial epoch mundane.

[A. C. Ramsay. 1862. On the glacial origin of certain lakes in Switzerland, the Black Forest, Great Britain, Sweden, North America, and elsewhere.]

24

(11 Geolog Soc. Journal

71 p 243 Owen on affinity of Carboniferous Reptile of N. America to Fish, viz Ganoid.

[Professor Owen. 1862. Description of specimens of fossil reptilia discovered in the coal-measures of the South Joggin, Nova Scotia, by Dr. J. W. Dawson.]

72 Dawson p 305 on angiosperm wood Devonian

p 327 on number of Devonian plants

[J. W. Dawson. 1862. On the flora of the Devonian period in North-eastern America.]

Falconer p 353 Excellent on connection (by Descent) of canines & bones of leg in camels

p 365 on antiquity of Plagiaulax, judged by its specialization.

[Hugh Falconer. 1862. On the disrupted affinity of the mammalian genus Plagiaulax form the Purbeck beds.]

73. 41 Remains in Cambrian few & low

p 42 Phosphatic nodule rocks strewn with them - Primordial [illeg] rich &c p. 51 do

[J. J. Bigsby. 1862. On the Cambrian and Huronian formations.]

p 67 Huxley on Carboniferous Reptiles

[T. H. Huxley. 1862. Description of Anthracosaurus russelli, a new Labyrinthodont from the Lanarkshire coal-field.]

92 Salter genealogical affinities of ancient Crustaceans.

[J. W. Salter. 1861. On Peltocaris, a new genus of Silurian Crustacea.]

74 p. XXXVL Ramsay whole paper grand on Bucks in ancient series

p 166 Davidson on genealogical succession in Brachiopods.

[Thomas Davidson. 1863. On the lower Carboniferous Brachiopoda of Nova Scotia.]

75 p 277 Salter on large Trilobites in lowest strata of Europe & N. America curious.

[J. W. Salter. 1863. On the discovery of Paradoxides in Britain.]

296 Day – on the many stages with distinct ammonites in the Lias

[E. C. H. Day. 1863 On the middle and upper Lias of the Dorsetshire coast.]

Append p. 20 Palæontology of N. Zealand. Tertiaries related to modern & peculiar shells of N. Zealand

[Dr. Zittel. 1863.On the Palæontology of N. Zealand.]

76 p 454 Duncan During Miocene age great changes in geography of W. Indies

455 W. Indian sea was affected by glacial period

456 Fossil corals then allied to Australian forms

[P. Martin Duncan. 1863. On the fossil corals of the West Indian Islands.]

468 Dawson on number of Devonian Plants

473 [Dawson] on 6 Reptiles in Carboniferous beds of N. America

[J. W. Dawson. 1863. Further observations on the Devonian plants of Maine Gaspé, and New York.]

512 Moore on shells of W. Indies, showing Panama formerly open

[J. Carrick Moore. 1863. on some tertiary shells from Jamaica.]

77 O

78 Ramsay's Address very valuable for breaks in Geolog. Succession.

79 199 Dr Bigsby

222 On breaks from emergence of land

224, 226, 232, all ditto

[J. J. Bigsby. 1864. On missing sedimentary formations, from suspension or removal of deposits.]

233 Mr Slater on important addition to the primordial fauna

[J. W. Salter. 1864. On some new fossils from the Lingula-flags of Wales.]

287 Salter on a barrier which divided the Scandinavian & mid-European areas during the Lower Silurian period

[J. W. Salter. 1864. On the fossils from the Budleigh Salterton Pebble-bed.]

80 409 Dorkings [Dawkins] on a new Mammal beneath the bone bed.

412 Ditto

[W. Boyd Dawkins. 1864. On the Rhætic beds of white Lias of western and central Somerset; and on the discovery of a new fossil mammal in the Grey Marlstones beneath the bone-bed.]

25

(p 12 Geolog. Soc. Journal

81 45 Sir W. Logan on the thickness of the Laurentian beds in Canada.

48 their fossils.

[Sir W. E. Logan. On the occurrence of organic remains in the Laurentian rocks of Canada.]

82 p. LIX Hamilton Pres. blindly argue that Laurentian strata contain first evidence of life.

LXZI Do – on two stages in Rhætic or Bona bed.

LXXI on relation of fossils to mineralogical deposit.

XCVII Do – quotes Owen on Mammalian character of teeth if Iguanodon.

83 O

84 362 Dr Duncan formerly species were not more widely distributed than at present.

362 On a persistent & anomalous form of Echinoderm which is the last in the Oolite & which is common to Arabia

p. 363 on another late form which departs a little from its type. This is like a species which departs from its range, departing also a little from its type.

[P. Martin Duncan. 1865. A description of the Echinodermata from the strata on the south-eastern coast of Arabia, etc.]

409 Stoliczka on cretaceous ammonites in India which have some Oolitic character & some few have even a Triassic character.

[F. Stoliczka. 1865. On the character of the Cephalopoda of the south-Indian Cretaceous rocks.]

443 Foster & Topley on superficial deposits of Medway

474 argues with much force that the Wealden has been formed by subaerial denudation; this perhaps gives even a greater idea of time than marine denudation.

[C. le Neve Foster and William Topley. 1865. On the superficial deposits of the valley of the Medway, with remarks on the denudation of the Weald.]

476 Lartet on remains of the ovibos in France 15° S. of its southern limit in N. America, where it is rarely found below 60°.

[Mons. E. Lartêt. Note o Ovibos moschatus, Blainville.]

477 Salter on additional fossils from the Lingula flags shewing that it is a distinct formation, so that the two Lingula flags & the Tremadoc slates form 3 formations with many genera even distinct

[J. W. Salter. On some additional fossils from the Lingula-flags.]

487 Woodward says that some Chiton are found in 25 fathoms water & extend back in time to the lower Silurian

[Henry Woodward. 1865. On some new species of crustatea belonging to the order Eurypterida.]

26

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no 85 p. 18 causes leading to destruction of fossils

addend p. 10 fossil sp Cassian connecting Secondary & Palæozoic

no. 86 p LXVII on connecting links between Lophiodon & allies

XCII on great break in fishes & plants between Jurassic & Cretaceous

L on peculiar cretaceous flora of N. America

CXVI on close relation of Belemnites of N. Zealand with European & so in Trias

p 96 on thickness of coal-measures of N. Scotia viz 16,000 ft

p 103 on cycles of elevation & subsidence corresponding in Europe & N. Scotia

[J. W. Dawson. 1865. On the conditions of the deposition of coal, more especially as illustrated by the coal-formation of Nova Scotia and New Brunswick.]

no. 87 p. 316 groups between Ganoids & Teleosteans – Agassiz generalisation that apodal fish did not appear before chalk falls to ground.

[John Young. 1655. On the affinities of Platysomus and allied genera]

no 88 p 481 First evidence of Trilobites & Birch in England in rock repeating Lower Llandeilo

[R. Harkness and Henry Nicholson. 1866. Additional observations on the geology of the lake-country.]

p 585 On Atlantic having existed during Miocene or Eocene age

588 on relation of Miocene corals of W. Indies & Europe; & of identical & clearly analogous shells on opposite sides of Panama, & Fish

[R. J. Lechmere. 1866. On the relations of the tertiary formations of the West Indies.]

no 89. p. 1 Dinosaurian Reptiles of C. of Good Hope, of [Xiphosura]

[Professor Huxley, 1866. On some remains of large Dinosaurian reptiles from the Stormberg mountains, South Africa.]

p. 35 on longevity of Crust. form, of Xiphosura

[Henry Woodward. 1866. On some points in the structure of the Xiphosura., etc]

no 90 p. 7 Apx [Appendix] Unger 40 per cent of fossil plants of Eubœa are allied to S. Africa

[Prof. Unger. 1866. On the fossil flora of Eubœa.]

no. 91 p. 148 Jurassic fossil cycad at the Cape; previously known only in Europe

p 164 Certain Crustaceous fossils at Natal

p 165 Crassatella, until lately not found beneath Lower Greensand, no known in inferior Oolite

p 167 Oolites analogous fossils at Cape

[Ralph Tate. 1867. On some secondary fossils from South Africa.]

p 207 3 genera of terrestrial molluscs & Chara in Carboniferous age in England!!!

[Charles Moore. 1867. On abnormal conditions of secondary deposits when connected with the Somersetshire and South Wales coal-basin, etc.]

no 92 p 292 Spratt on line of connection of Malta & mainland (map)

[T. A. B. Spratt. 1867. On the bone-caves near Crendi, Zebbug, and Melliha, in the island of Malta.]

302 On planorbis ammonite some want real & general Pal character

[Ralph Tate. 1867. On the lower Lias of the north-east of Ireland.]

330 332 on new land mollusc in coal of [illeg]

[J. W. Dawson. 1867. On the discovery of a new Pulmonate mollusk… Nova Scotia.]

333 Salter when tracks abound, you need not expect to find fossils

[J. W. Salter. 1867. On some tracks of Pteraspis(?) in the Upper Ludlow Sandstone.]

340 do on fossil between upper & Lower Cambrian

[J. W. Salter. 1867. On a new Lingulella from the red Lower Cambrian Rocks of St. Davids.]

344 Haast Gneiss schist in Chatham Isld

[Julius Haast. 1867. Notes on the geology of the province of Canterbury, N.Z., etc.]

92* 471 Moore on fault in Ammonite years

473 a zoic only 6 inches thick, extend from England to Jura

475 beds only 18 inches thick, representing beds of great thickness elsewhere. do 476 good 477.

494. Moore on 3 genera of land molluscs, first in secondary Deposits!!!

510 on the recurrence of same sp. Where same conditions same – We may make their sequence of fossil in same area, but the sequence fails when extended area is considered.

[Charles Moore. 1867. On abnormal conditions of secondary deposits when connected with the Somersetshire and South Wales coal-basin; and on the age of the Sutton and Southerndown series.]

27

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no 93 p 29. Dr Duncan on relations of W. Indian fossil corals

[P. Martin Duncan. 1867. On the fossil corals (Madreporaria) of the West-Indian islands.]

Suppl. p 1-6 a sketch of Gaudry's fossil mammals from Attica Fauna is for the most part African.

[Albert Gaudry. 867. Fossil animals and geology of Attica. Part I. Translated.]

no 94 Warington Smith Ann. address

p LII on glacial action near Mt Sinai. Appear like great moraines.

no 95 p 214 B. Dawkins on Rhinoceros. The Etruscus species has dental characters represented by the milk-teeth of some other species sp. that lived after its extinction

p 216 Etruscus sp. is very isolated, the last representative of the Miocene type.

p 217 Caselli Nase proved that the cave-Hyena, mammoth bear &c passed S. & established themselves in the midst of the Italian pliocene fauna.

[W. Boyd Dawkins. 1867. On the dentition of Rhinoceros Etruscus, Falc.]

p 327 Hull shews that 10,000 ft denuded before the deposition of the Permean strata.

p 328 that nearly 20,000 ft of carbonnif. strata denuded. This probably took place between the Carb. & permean periods. He adds "here is indeed a blank in the geolog. record"

[Edward Hull. 1868. On the thickness of the carboniferous rocks of the Pendle range of hills, Lancashire, etc.]

no 96 p 484 Mr R. Bruce Foote on stone implements in S. India

[R. Bruce Foote. 1868. On the distribution of stone implements in Southern India.]

p 499 Busk on the Asiatic elephant apparently having existed in Japan.

[A. Leith Adams. 1868. Has the Asiatic elephant been found in a fossil state? With additional remarks by G. Busk.]

no 97 p 53 Salter & Hicks on Menevian group. describes the metamorph. of a Trilobite, shewing that still earlier forms must have existed.

p 56 Describes a Paradoxides which has intermediate character between this genus & Anopolenus.

[J. W. Salter. 1868. On some fossils from the "Menevian group."]

no. 98 p 141 p 148 Huxley on Elgin Fossil Reptile – presidence thought World

p 147 affinities of Persistence of form.

p 151 Relation of New Zealand Fauna

p 152 on the antiquity of all 5 vertebrate types.

[T. H. Huxley. 1869. On hyperodapedon.]

Dawkins p 194 List of Post-glacial mammals

p. 211 sheep goat dog Bos longifrons Prehistoric

p 213 Lartet on immigration of Siberian Mammals

[W. Boyd Dawkins. 1869. On the distribution of the British postglacial mammals.]

28

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no. 99 p 238 to 247 Coquand on great bucks in Cretaceous formation correspondence with England – (is he trustworthy?)

[Henri Coquand. 1869. The Cretaceous strata of England, and the north of France compared with those of the west, etc.]

p 11 append. Heer Earliest Flora, lower cretaceous, with Dicotyledons.

[O. Heer. 1868. On the Cretaceous flora of Moletein, Moravia.]

p 14 – On generalized Chelonian – similar [2 words illeg] followed by Rutimeyer in query of existing species.

[C. Peters. 1869. On Chelonia from Eibiswald, in Styria.]

no. 101 p 28-31 – p 37 do Huxley on Bird affinities of Dinosaurian

[T. H. Huxley. 1869. Further evidence of the affinity between the Dinosaurian reptiles and birds.]

p 114 Dawson on the Graphital of the Laurentian beds, - organic –

[J. W. Dawson. 1869. On the graphite of the Laurentian of Canada.]

no 102. Huxley's address. p XXX – General proportions on relations = Fossil to formations – ages & extension

p XLIV on Persistent Types

p XIVI Progress – Greater intermediary types

P XIVII Zeuglodon - Equidæ affinities of various groups

p LV succession of types in lower areas

p LX – Relation to G. Distribution in past times

p. 230 Moore, Middle & upper Lias, Lava Oolite in W. Australia

p. 233 enormous Denudation – Australia.

[Charles Moore, 1869. Australian Mesozoic geology, and Palæontology.]

no. 103. p 408 & p 401 Ammonite zones only of series over limited areas

[Ralph Tate. 1870. On the Palæontology of the junction beds of the lower and middle Lias in Gloucestershire.]

no 104/0/ no 105/0/

no 106 Prestwich address

p LXIII on forms extensions of cretaceous occur in [permian] of Atlantic ocean

p LXIII on colonies Lyell's view

LXXIII all Tertiary deposit shallow seas

no 108 p. 437 Duncan on Persistence of Crustacean coral at bottom of Atlantic

p 439 Ammonites in Tertiary bed of America? Rupert Jones.

[P. Martin Duncan. 1871. On the persistence of Caryophyllia cylindracea, Reuss, sp., a Cretaceous species of coral, in the coral fauna of the deep sea.]

no 116 Descent of ammonites & their comparison with [Goniotobus] – parallel development in distinct group of ammonites

no 118 [p. 124-174.] Davidson. Evolution of the Trimerillidæ – perhaps important

[Thomas Davidson. 1874. On the Trimerillidæ, a Palæozoic family of the Palliobranchs or Brachiopoda.]

124 Blandford on Glacial Permian rock in India & S. Africa & on extension of Glaciers in the Himalaya.

p 540 Plat- bearing derives from Permian to present time – uninhabited land & caves.

- India & S. Africa & Australia connector – no connection with W. Asia

123 p. 63 (1876) Woodward list of Palæozoic Insects & Arachnida

[Henry Woodward. 1876. On a remarkable fossil Orthopterous insect from the cola-measures of Scotland. Read 3 November 1875.]

128 p 517 Guppy – conclusive evidence that Isthmus of Panama open Miocene age

[R. J. Lechmere Guppy. 1876. On the Miocene fossils of Haiti.]

130 p. 256 Belemnites Older Tertiaries of Italy

[Ralph Tate. 1877. On new species of Belemnites and Salenia from the middle tertiaries of South Australia.]