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Lower oolite Stock Photos and Images
Scene during the Lower Oolite period showing reconstructions of Ichthyosaurus, Plesiosaurus and a Marsupial. From 'The Popular Encyclopaedia' (London, 1888). Engraving. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-scene-during-the-lower-oolite-period-showing-reconstructions-of-ichthyosaurus-57289043.htmlRMD95MN7–Scene during the Lower Oolite period showing reconstructions of Ichthyosaurus, Plesiosaurus and a Marsupial. From 'The Popular Encyclopaedia' (London, 1888). Engraving.
ideal landscape of thr lower oolite period Oolite (egg stone) is a sedimentary rock formed from ooids, spherical grains composed Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-ideal-landscape-of-thr-lower-oolite-period-oolite-egg-stone-is-a-sedimentary-23004686.htmlRFB9BXKX–ideal landscape of thr lower oolite period Oolite (egg stone) is a sedimentary rock formed from ooids, spherical grains composed
Jurassic Landscape Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-jurassic-landscape-135042256.htmlRMHRKKNM–Jurassic Landscape
Scene during the Lower Oolite period showing reconstructions of Ichthyosaurus, Plesiosaurus and a Marsupial. From 'The Popular Encyclopaedia' (London, 1888). Engraving. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/scene-during-the-lower-oolite-period-showing-reconstructions-of-ichthyosaurus-plesiosaurus-and-a-marsupial-from-the-popular-encyclopaedia-london-1888-engraving-image483534134.htmlRM2K2JTM6–Scene during the Lower Oolite period showing reconstructions of Ichthyosaurus, Plesiosaurus and a Marsupial. From 'The Popular Encyclopaedia' (London, 1888). Engraving.
BRITISH FOSSILS. Lower Oolitic - Inferior Oolite. STANFORD 1904 old print Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-fossils-lower-oolitic-inferior-oolite-stanford-1904-old-print-image599849564.htmlRF2WRWE6M–BRITISH FOSSILS. Lower Oolitic - Inferior Oolite. STANFORD 1904 old print
LANDSCAPE OF THE LOWER OOLITE (BEFORE THE AGE OF MAN).— Drawn by Riou from volume 1 of Ridpath's Universal history : an account of the origin, primitive condition and ethnic development of the great races of mankind, and of the principal events in the evolution and progress of the civilized life among men and nations, from recent and authentic sources with a preliminary inquiry on the time, place and manner of the beginning by Ridpath, John Clark, 1840-1900 Published in 1897 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/landscape-of-the-lower-oolite-before-the-age-of-man-drawn-by-riou-from-volume-1-of-ridpaths-universal-history-an-account-of-the-origin-primitive-condition-and-ethnic-development-of-the-great-races-of-mankind-and-of-the-principal-events-in-the-evolution-and-progress-of-the-civilized-life-among-men-and-nations-from-recent-and-authentic-sources-with-a-preliminary-inquiry-on-the-time-place-and-manner-of-the-beginning-by-ridpath-john-clark-1840-1900-published-in-1897-image611362362.htmlRM2XEHXX2–LANDSCAPE OF THE LOWER OOLITE (BEFORE THE AGE OF MAN).— Drawn by Riou from volume 1 of Ridpath's Universal history : an account of the origin, primitive condition and ethnic development of the great races of mankind, and of the principal events in the evolution and progress of the civilized life among men and nations, from recent and authentic sources with a preliminary inquiry on the time, place and manner of the beginning by Ridpath, John Clark, 1840-1900 Published in 1897
Various Mid Jurassic fossil shell fish in limestone, Lower Inferior Oolite, Bridport, Dorset, England, UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-various-mid-jurassic-fossil-shell-fish-in-limestone-lower-inferior-24335078.htmlRFBBGFHX–Various Mid Jurassic fossil shell fish in limestone, Lower Inferior Oolite, Bridport, Dorset, England, UK.
Hardwicke's science-gossip : an illustrated medium of interchange and gossip for students and lovers of nature . Fig. J2. Otopteris dabia. four species of ferns from the Lower Oolite, derivedfrom their excellently-illustrated edition of FiguiersWorld before the Delude. Although all the. Fig. 73. Otopteris obtusu. present sketches are confined to one genus, severalothers are found in the same formation. The Eernsof this period are, however, inferior to those of the Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/hardwickes-science-gossip-an-illustrated-medium-of-interchange-and-gossip-for-students-and-lovers-of-nature-fig-j2-otopteris-dabia-four-species-of-ferns-from-the-lower-oolite-derivedfrom-their-excellently-illustrated-edition-of-figuiersworld-before-the-delude-although-all-the-fig-73-otopteris-obtusu-present-sketches-are-confined-to-one-genus-severalothers-are-found-in-the-same-formation-the-eernsof-this-period-are-however-inferior-to-those-of-the-image339221172.htmlRM2AKTT1T–Hardwicke's science-gossip : an illustrated medium of interchange and gossip for students and lovers of nature . Fig. J2. Otopteris dabia. four species of ferns from the Lower Oolite, derivedfrom their excellently-illustrated edition of FiguiersWorld before the Delude. Although all the. Fig. 73. Otopteris obtusu. present sketches are confined to one genus, severalothers are found in the same formation. The Eernsof this period are, however, inferior to those of the
'Boys at play', Robin Hood's Bay, North Yorkshire, England, UK Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-boys-at-play-robin-hoods-bay-north-yorkshire-england-uk-88257909.htmlRMF3GDT5–'Boys at play', Robin Hood's Bay, North Yorkshire, England, UK
. Fossil plants : for students of botany and geology . Paleobotany. 72 THE PKESERVATION OF PLANTS AS FOSSILS. [CH. leaf-cushions and leaf-scars of a Lepidodendron. The stem was embedded in soft sand, and as the latter became hard and set, an impression was obtained of the external markings of the Lepidodendron. Decay subsequently removed the substance of the plant.. Fig. 11. Equisetites columnaris Brongn. Prom a specimen in the Woodwardian Museum, Cambridge. ^ nat. size. In fig. 11 some upright stems of a fossil Horse-tail (Equi- setites columnaris) from the Lower Oolite rocks near Scarborough Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fossil-plants-for-students-of-botany-and-geology-paleobotany-72-the-pkeservation-of-plants-as-fossils-ch-leaf-cushions-and-leaf-scars-of-a-lepidodendron-the-stem-was-embedded-in-soft-sand-and-as-the-latter-became-hard-and-set-an-impression-was-obtained-of-the-external-markings-of-the-lepidodendron-decay-subsequently-removed-the-substance-of-the-plant-fig-11-equisetites-columnaris-brongn-prom-a-specimen-in-the-woodwardian-museum-cambridge-nat-size-in-fig-11-some-upright-stems-of-a-fossil-horse-tail-equi-setites-columnaris-from-the-lower-oolite-rocks-near-scarborough-image216386469.htmlRMPG1745–. Fossil plants : for students of botany and geology . Paleobotany. 72 THE PKESERVATION OF PLANTS AS FOSSILS. [CH. leaf-cushions and leaf-scars of a Lepidodendron. The stem was embedded in soft sand, and as the latter became hard and set, an impression was obtained of the external markings of the Lepidodendron. Decay subsequently removed the substance of the plant.. Fig. 11. Equisetites columnaris Brongn. Prom a specimen in the Woodwardian Museum, Cambridge. ^ nat. size. In fig. 11 some upright stems of a fossil Horse-tail (Equi- setites columnaris) from the Lower Oolite rocks near Scarborough
Devil's chimney Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/devils-chimney-image1287417.htmlRFAKA4FA–Devil's chimney
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36602969.htmlRMC3FBCW–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
Sectional in Middle Jurassic, vintage engraved illustration. Earth before man – 1886. Stock Vectorhttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sectional-in-middle-jurassic-vintage-engraved-illustration-earth-before-84300668.htmlRFEW46A4–Sectional in Middle Jurassic, vintage engraved illustration. Earth before man – 1886.
Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 408 MAMMALIA OF STONESFIELD OOLITE. [Oh. XX. and Phascolotherium have complicated crowns and two roots (see d, fig. 412), instead of being simple and with single fangs.* The only question, therefore, which conld fairly admit of contro- versy was limited to this point, whether the fossil mammalia found'in the Lower Oolite of Oxfordshire ought to be referred to the marsupial quadrupeds, or to the ordinary placental se Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-408-mammalia-of-stonesfield-oolite-oh-xx-and-phascolotherium-have-complicated-crowns-and-two-roots-see-d-fig-412-instead-of-being-simple-and-with-single-fangs-the-only-question-therefore-which-conld-fairly-admit-of-contro-versy-was-limited-to-this-point-whether-the-fossil-mammalia-foundin-the-lower-oolite-of-oxfordshire-ought-to-be-referred-to-the-marsupial-quadrupeds-or-to-the-ordinary-placental-se-image239641135.htmlRMRWTGKY–Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 408 MAMMALIA OF STONESFIELD OOLITE. [Oh. XX. and Phascolotherium have complicated crowns and two roots (see d, fig. 412), instead of being simple and with single fangs.* The only question, therefore, which conld fairly admit of contro- versy was limited to this point, whether the fossil mammalia found'in the Lower Oolite of Oxfordshire ought to be referred to the marsupial quadrupeds, or to the ordinary placental se
![. The earth in past ages . Fig. n—Belemnites Oweni, an internal shell of a kind f cuttle- fish. The "Guard'' is broken to shew the conical phi cone which penetratea into it. Oxford Clay, earthy limestone. Traced southward by Shot- over, it forms two divisions; and at Weymouth there is the sandy lower calcareous grit well de- fined, and an upper grit or sand which passes up to the Kimeridge clay. In Yorkshire this Oolite extends through the ilowardian Hills by Malton, through the Vale of Pickering to Filey. At Up- ware, on the river ('am, a small reef lull of corals appears to result from Stock Photo](https://c8.alamy.com/comp/MAARB3/the-earth-in-past-ages-fig-nbelemnites-oweni-an-internal-shell-of-a-kind-f-cuttle-fish-the-quotguard-is-broken-to-shew-the-conical-phi-cone-which-penetratea-into-it-oxford-clay-earthy-limestone-traced-southward-by-shot-over-it-forms-two-divisions-and-at-weymouth-there-is-the-sandy-lower-calcareous-grit-well-de-fined-and-an-upper-grit-or-sand-which-passes-up-to-the-kimeridge-clay-in-yorkshire-this-oolite-extends-through-the-ilowardian-hills-by-malton-through-the-vale-of-pickering-to-filey-at-up-ware-on-the-river-am-a-small-reef-lull-of-corals-appears-to-result-from-MAARB3.jpg ". The earth in past ages . Fig. n—Belemnites Oweni, an internal shell of a kind f cuttle- fish. The "Guard'' is broken to shew the conical phi cone which penetratea into it. Oxford Clay, earthy limestone. Traced southward by Shot- over, it forms two divisions; and at Weymouth there is the sandy lower calcareous grit well de- fined, and an upper grit or sand which passes up to the Kimeridge clay. In Yorkshire this Oolite extends through the ilowardian Hills by Malton, through the Vale of Pickering to Filey. At Up- ware, on the river ('am, a small reef lull of corals appears to result from Stock Photo")
. The earth in past ages . Fig. n—Belemnites Oweni, an internal shell of a kind f cuttle- fish. The "Guard'' is broken to shew the conical phi cone which penetratea into it. Oxford Clay, earthy limestone. Traced southward by Shot- over, it forms two divisions; and at Weymouth there is the sandy lower calcareous grit well de- fined, and an upper grit or sand which passes up to the Kimeridge clay. In Yorkshire this Oolite extends through the ilowardian Hills by Malton, through the Vale of Pickering to Filey. At Up- ware, on the river ('am, a small reef lull of corals appears to result from Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-earth-in-past-ages-fig-nbelemnites-oweni-an-internal-shell-of-a-kind-f-cuttle-fish-the-quotguard-is-broken-to-shew-the-conical-phi-cone-which-penetratea-into-it-oxford-clay-earthy-limestone-traced-southward-by-shot-over-it-forms-two-divisions-and-at-weymouth-there-is-the-sandy-lower-calcareous-grit-well-de-fined-and-an-upper-grit-or-sand-which-passes-up-to-the-kimeridge-clay-in-yorkshire-this-oolite-extends-through-the-ilowardian-hills-by-malton-through-the-vale-of-pickering-to-filey-at-up-ware-on-the-river-am-a-small-reef-lull-of-corals-appears-to-result-from-image178488103.htmlRMMAARB3–. The earth in past ages . Fig. n—Belemnites Oweni, an internal shell of a kind f cuttle- fish. The "Guard'' is broken to shew the conical phi cone which penetratea into it. Oxford Clay, earthy limestone. Traced southward by Shot- over, it forms two divisions; and at Weymouth there is the sandy lower calcareous grit well de- fined, and an upper grit or sand which passes up to the Kimeridge clay. In Yorkshire this Oolite extends through the ilowardian Hills by Malton, through the Vale of Pickering to Filey. At Up- ware, on the river ('am, a small reef lull of corals appears to result from
Bryozoans from the Jurassic Period. On the left is Adeona folifera, and on the right, two specimens of Cellaria loriculata. Illustration from Louis Figuier's The World Before the Deluge, 1867 American edition. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/bryozoans-from-the-jurassic-period-on-the-left-is-adeona-folifera-and-on-the-right-two-specimens-of-cellaria-loriculata-illustration-from-louis-figuiers-the-world-before-the-deluge-1867-american-edition-image246589771.htmlRMT953NF–Bryozoans from the Jurassic Period. On the left is Adeona folifera, and on the right, two specimens of Cellaria loriculata. Illustration from Louis Figuier's The World Before the Deluge, 1867 American edition.
BRITISH FOSSILS Lower Oolitic Great Oolite Stonesfield Slate Fuller's Earth 1904 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-fossils-lower-oolitic-great-oolite-stonesfield-slate-fullers-earth-1904-image599849565.htmlRF2WRWE6N–BRITISH FOSSILS Lower Oolitic Great Oolite Stonesfield Slate Fuller's Earth 1904
BRITISH FOSSILS. Lower Oolitic - Inferior Oolite. STANFORD 1907 old print Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-fossils-lower-oolitic-inferior-oolite-stanford-1907-old-print-image356272272.htmlRF2BKHGWM–BRITISH FOSSILS. Lower Oolitic - Inferior Oolite. STANFORD 1907 old print
The Quarterly journal of the Geological Society of London . a. Warp-drift; sandy loam. 6. Sand of the Crag. Fig. 4.—Section of Pipes filled with Boulder-clay, near Desborough,Northamptonshire (on the Harborough side of the village).. a. Boulder.clay : brown clay with chalk-flints, and rolled pebbles and scratched fragments of hard chalk. b. Whitish sand. i T /-> v. c. Ferruginous sandstone. } Lower Oolite. Fig. 5.—Section of Pipes in the Boulder-clay, at Hardingham,Norfolk. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-quarterly-journal-of-the-geological-society-of-london-a-warp-drift-sandy-loam-6-sand-of-the-crag-fig-4section-of-pipes-filled-with-boulder-clay-near-desboroughnorthamptonshire-on-the-harborough-side-of-the-village-a-boulderclay-brown-clay-with-chalk-flints-and-rolled-pebbles-and-scratched-fragments-of-hard-chalk-b-whitish-sand-i-t-gt-v-c-ferruginous-sandstone-lower-oolite-fig-5section-of-pipes-in-the-boulder-clay-at-hardinghamnorfolk-image338174828.htmlRM2AJ55CC–The Quarterly journal of the Geological Society of London . a. Warp-drift; sandy loam. 6. Sand of the Crag. Fig. 4.—Section of Pipes filled with Boulder-clay, near Desborough,Northamptonshire (on the Harborough side of the village).. a. Boulder.clay : brown clay with chalk-flints, and rolled pebbles and scratched fragments of hard chalk. b. Whitish sand. i T /-> v. c. Ferruginous sandstone. } Lower Oolite. Fig. 5.—Section of Pipes in the Boulder-clay, at Hardingham,Norfolk.
BRITISH FOSSILS. Lower Oolitic, Great Oolite, Stonesfield Slate. STANFORD 1880 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-fossils-lower-oolitic-great-oolite-stonesfield-slate-stanford-1880-image183052357.htmlRFMHPN45–BRITISH FOSSILS. Lower Oolitic, Great Oolite, Stonesfield Slate. STANFORD 1880
![. Fossil plants : for students of botany and geology . Paleobotany. XL] GINKGOITES 21 acuminata^. A deeply divided obcuiieate leaf, only 2—4 cm. broad, is figured by Dr Stopes^ from Jurassic strata (Lower Oolite) on the Sutherland coast at Brora (fig. 635, J). The specimen shown in fig. 633, also from the Sutherland coast, a few miles north of Brora and of Kimeridgian age, illustrates the type of leaf that may be conveniently referred to Ginkgoites digitata. var. Huttoni^. Heer's Jurassic species. Ginkgo Jaccardi^, from Switzerland is almost certainly Ginkgoites digitata. Arctic regions and no Stock Photo](https://c8.alamy.com/comp/PG170B/fossil-plants-for-students-of-botany-and-geology-paleobotany-xl-ginkgoites-21-acuminata-a-deeply-divided-obcuiieate-leaf-only-24-cm-broad-is-figured-by-dr-stopes-from-jurassic-strata-lower-oolite-on-the-sutherland-coast-at-brora-fig-635-j-the-specimen-shown-in-fig-633-also-from-the-sutherland-coast-a-few-miles-north-of-brora-and-of-kimeridgian-age-illustrates-the-type-of-leaf-that-may-be-conveniently-referred-to-ginkgoites-digitata-var-huttoni-heers-jurassic-species-ginkgo-jaccardi-from-switzerland-is-almost-certainly-ginkgoites-digitata-arctic-regions-and-no-PG170B.jpg ". Fossil plants : for students of botany and geology . Paleobotany. XL] GINKGOITES 21 acuminata^. A deeply divided obcuiieate leaf, only 2—4 cm. broad, is figured by Dr Stopes^ from Jurassic strata (Lower Oolite) on the Sutherland coast at Brora (fig. 635, J). The specimen shown in fig. 633, also from the Sutherland coast, a few miles north of Brora and of Kimeridgian age, illustrates the type of leaf that may be conveniently referred to Ginkgoites digitata. var. Huttoni^. Heer's Jurassic species. Ginkgo Jaccardi^, from Switzerland is almost certainly Ginkgoites digitata. Arctic regions and no Stock Photo")
. Fossil plants : for students of botany and geology . Paleobotany. XL] GINKGOITES 21 acuminata^. A deeply divided obcuiieate leaf, only 2—4 cm. broad, is figured by Dr Stopes^ from Jurassic strata (Lower Oolite) on the Sutherland coast at Brora (fig. 635, J). The specimen shown in fig. 633, also from the Sutherland coast, a few miles north of Brora and of Kimeridgian age, illustrates the type of leaf that may be conveniently referred to Ginkgoites digitata. var. Huttoni^. Heer's Jurassic species. Ginkgo Jaccardi^, from Switzerland is almost certainly Ginkgoites digitata. Arctic regions and no Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fossil-plants-for-students-of-botany-and-geology-paleobotany-xl-ginkgoites-21-acuminata-a-deeply-divided-obcuiieate-leaf-only-24-cm-broad-is-figured-by-dr-stopes-from-jurassic-strata-lower-oolite-on-the-sutherland-coast-at-brora-fig-635-j-the-specimen-shown-in-fig-633-also-from-the-sutherland-coast-a-few-miles-north-of-brora-and-of-kimeridgian-age-illustrates-the-type-of-leaf-that-may-be-conveniently-referred-to-ginkgoites-digitata-var-huttoni-heers-jurassic-species-ginkgo-jaccardi-from-switzerland-is-almost-certainly-ginkgoites-digitata-arctic-regions-and-no-image216386363.htmlRMPG170B–. Fossil plants : for students of botany and geology . Paleobotany. XL] GINKGOITES 21 acuminata^. A deeply divided obcuiieate leaf, only 2—4 cm. broad, is figured by Dr Stopes^ from Jurassic strata (Lower Oolite) on the Sutherland coast at Brora (fig. 635, J). The specimen shown in fig. 633, also from the Sutherland coast, a few miles north of Brora and of Kimeridgian age, illustrates the type of leaf that may be conveniently referred to Ginkgoites digitata. var. Huttoni^. Heer's Jurassic species. Ginkgo Jaccardi^, from Switzerland is almost certainly Ginkgoites digitata. Arctic regions and no
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36602919.htmlRMC3FBB3–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Aticula incequwalvis, Sow. Lower Oolite, and Lias. . Avicula cygnipes, Phil. Lias, Gloucestershire and Yorkshire. The peculiar aspect which is most characteristic of the Lias in England, France, and Germany, is an alternation of thin beds of blue or gray limestone, having a surface which becomes light-brown when weathered, these beds being separated by dark-colored, narrow argillaceous partings, so that the quarries Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-aticula-incequwalvis-sow-lower-oolite-and-lias-avicula-cygnipes-phil-lias-gloucestershire-and-yorkshire-the-peculiar-aspect-which-is-most-characteristic-of-the-lias-in-england-france-and-germany-is-an-alternation-of-thin-beds-of-blue-or-gray-limestone-having-a-surface-which-becomes-light-brown-when-weathered-these-beds-being-separated-by-dark-colored-narrow-argillaceous-partings-so-that-the-quarries-image239641536.htmlRMRWTH68–Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Aticula incequwalvis, Sow. Lower Oolite, and Lias. . Avicula cygnipes, Phil. Lias, Gloucestershire and Yorkshire. The peculiar aspect which is most characteristic of the Lias in England, France, and Germany, is an alternation of thin beds of blue or gray limestone, having a surface which becomes light-brown when weathered, these beds being separated by dark-colored, narrow argillaceous partings, so that the quarries
Bryozoans from the Jurassic Period. On the left is Adeona folifera, and on the right, two specimens of Cellaria loriculata. Illustration from Louis Figuier's The World Before the Deluge, 1867 American edition. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-bryozoans-from-the-jurassic-period-on-the-left-is-adeona-folifera-103984569.htmlRMG14WAH–Bryozoans from the Jurassic Period. On the left is Adeona folifera, and on the right, two specimens of Cellaria loriculata. Illustration from Louis Figuier's The World Before the Deluge, 1867 American edition.
The Quarterly journal of the Geological Society of London . Grandtdieri, R. B. Newton (sp. nov.).Cypricardia rostrata, J. Sowerby. ,, (allied to) bathonica, dOrbigny. Pseudotrapezium ventricosum, R. B. Newton (sp. nov.).„ depressum, R. B. Newton (sp. nov.). „ elongatum, R. B. Newton (sp. nov.). Trigonia pullus, J. de C. Sowerby. ,, costata, Parkinson.Astarte (allied to) angulata, Morris & Lycett.„ „ depressa, Miinster (Goldfuss). „ „ alia, Goldfuss. Lias. „ ,, Phyllis, dOrbigny. Oxfordian. ? Lower Oolite. „ ,, minima, Phillips. „ (?) Baroni, R. B. Newton. „ (allied to) excavata, J. Sowerby.Sph Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-quarterly-journal-of-the-geological-society-of-london-grandtdieri-r-b-newton-sp-novcypricardia-rostrata-j-sowerby-allied-to-bathonica-dorbigny-pseudotrapezium-ventricosum-r-b-newton-sp-nov-depressum-r-b-newton-sp-nov-elongatum-r-b-newton-sp-nov-trigonia-pullus-j-de-c-sowerby-costata-parkinsonastarte-allied-to-angulata-morris-lycett-depressa-miinster-goldfuss-alia-goldfuss-lias-phyllis-dorbigny-oxfordian-lower-oolite-minima-phillips-baroni-r-b-newton-allied-to-excavata-j-sowerbysph-image342736973.htmlRM2AWH0E5–The Quarterly journal of the Geological Society of London . Grandtdieri, R. B. Newton (sp. nov.).Cypricardia rostrata, J. Sowerby. ,, (allied to) bathonica, dOrbigny. Pseudotrapezium ventricosum, R. B. Newton (sp. nov.).„ depressum, R. B. Newton (sp. nov.). „ elongatum, R. B. Newton (sp. nov.). Trigonia pullus, J. de C. Sowerby. ,, costata, Parkinson.Astarte (allied to) angulata, Morris & Lycett.„ „ depressa, Miinster (Goldfuss). „ „ alia, Goldfuss. Lias. „ ,, Phyllis, dOrbigny. Oxfordian. ? Lower Oolite. „ ,, minima, Phillips. „ (?) Baroni, R. B. Newton. „ (allied to) excavata, J. Sowerby.Sph
BRITISH FOSSILS.Lower Oolitic Inferior Oolite.Molluscs.Ammonites.STANFORD 1880 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-fossilslower-oolitic-inferior-oolitemolluscsammonitesstanford-1880-image183052354.htmlRFMHPN42–BRITISH FOSSILS.Lower Oolitic Inferior Oolite.Molluscs.Ammonites.STANFORD 1880
Image taken from page 811 of 'Text-Book of Geology' Image taken from page 811 of 'Text-Book of Geology' Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-image-taken-from-page-811-of-text-book-of-geology-image-taken-from-130186317.htmlRMHFPDY9–Image taken from page 811 of 'Text-Book of Geology' Image taken from page 811 of 'Text-Book of Geology'
BRITISH FOSSILS Lower Oolitic Great Oolite Stonesfield Slate Fuller's Earth 1907 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/british-fossils-lower-oolitic-great-oolite-stonesfield-slate-fullers-earth-1907-image356272292.htmlRF2BKHGXC–BRITISH FOSSILS Lower Oolitic Great Oolite Stonesfield Slate Fuller's Earth 1907
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36588950.htmlRMC3ENG6–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Ammonites BraikenHdgvi, Sow. Ostrea Marshii. rtat. size. Oolite, Scarborough. Middle and Lower Oolite, or ranging Inf. Ool., Dundry ; Calvados; &c. from Coral Bay to Cornbrash. Palceontological relations of the Oolitic strata.—Observations have already been made, p. 345, on the distinctness of organic remains of the Oolitic and Cretaceous strata, and at pp. 398 and 401 of the proportion of species common to the Up Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-ammonites-braikenhdgvi-sow-ostrea-marshii-rtat-size-oolite-scarborough-middle-and-lower-oolite-or-ranging-inf-ool-dundry-calvados-c-from-coral-bay-to-cornbrash-palceontological-relations-of-the-oolitic-strataobservations-have-already-been-made-p-345-on-the-distinctness-of-organic-remains-of-the-oolitic-and-cretaceous-strata-and-at-pp-398-and-401-of-the-proportion-of-species-common-to-the-up-image239641408.htmlRMRWTH1M–Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Ammonites BraikenHdgvi, Sow. Ostrea Marshii. rtat. size. Oolite, Scarborough. Middle and Lower Oolite, or ranging Inf. Ool., Dundry ; Calvados; &c. from Coral Bay to Cornbrash. Palceontological relations of the Oolitic strata.—Observations have already been made, p. 345, on the distinctness of organic remains of the Oolitic and Cretaceous strata, and at pp. 398 and 401 of the proportion of species common to the Up
![The Quarterly journal of the Geological Society of London . Lower Oolite. Fig. 5.—Section of Pipes in the Boulder-clay, at Hardingham,Norfolk.. a. Loamy Warp-drift. b. Boulder-clay, r. The same materials as the Boulder-clay, viz. chalk and clay, butcontaining irregular seams of sand and gravel. 1854.] TRIMMER ON SAND-PIPES. 237 Fig. 5. A section of the Warp-drift and Boulder-clay near Hard-ingham, Norfolk. Here the depth of the furrows and pipes filledwith Warp-drift varies from 3 to 6 feet; one of the pipes, however,extending to the depth of 9 feet. If all the projecting points ofBoulder-clay Stock Photo](https://c8.alamy.com/comp/2AJ5592/the-quarterly-journal-of-the-geological-society-of-london-lower-oolite-fig-5section-of-pipes-in-the-boulder-clay-at-hardinghamnorfolk-a-loamy-warp-drift-b-boulder-clay-r-the-same-materials-as-the-boulder-clay-viz-chalk-and-clay-butcontaining-irregular-seams-of-sand-and-gravel-1854-trimmer-on-sand-pipes-237-fig-5-a-section-of-the-warp-drift-and-boulder-clay-near-hard-ingham-norfolk-here-the-depth-of-the-furrows-and-pipes-filledwith-warp-drift-varies-from-3-to-6-feet-one-of-the-pipes-howeverextending-to-the-depth-of-9-feet-if-all-the-projecting-points-ofboulder-clay-2AJ5592.jpg "The Quarterly journal of the Geological Society of London . Lower Oolite. Fig. 5.—Section of Pipes in the Boulder-clay, at Hardingham,Norfolk.. a. Loamy Warp-drift. b. Boulder-clay, r. The same materials as the Boulder-clay, viz. chalk and clay, butcontaining irregular seams of sand and gravel. 1854.] TRIMMER ON SAND-PIPES. 237 Fig. 5. A section of the Warp-drift and Boulder-clay near Hard-ingham, Norfolk. Here the depth of the furrows and pipes filledwith Warp-drift varies from 3 to 6 feet; one of the pipes, however,extending to the depth of 9 feet. If all the projecting points ofBoulder-clay Stock Photo")
The Quarterly journal of the Geological Society of London . Lower Oolite. Fig. 5.—Section of Pipes in the Boulder-clay, at Hardingham,Norfolk.. a. Loamy Warp-drift. b. Boulder-clay, r. The same materials as the Boulder-clay, viz. chalk and clay, butcontaining irregular seams of sand and gravel. 1854.] TRIMMER ON SAND-PIPES. 237 Fig. 5. A section of the Warp-drift and Boulder-clay near Hard-ingham, Norfolk. Here the depth of the furrows and pipes filledwith Warp-drift varies from 3 to 6 feet; one of the pipes, however,extending to the depth of 9 feet. If all the projecting points ofBoulder-clay Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-quarterly-journal-of-the-geological-society-of-london-lower-oolite-fig-5section-of-pipes-in-the-boulder-clay-at-hardinghamnorfolk-a-loamy-warp-drift-b-boulder-clay-r-the-same-materials-as-the-boulder-clay-viz-chalk-and-clay-butcontaining-irregular-seams-of-sand-and-gravel-1854-trimmer-on-sand-pipes-237-fig-5-a-section-of-the-warp-drift-and-boulder-clay-near-hard-ingham-norfolk-here-the-depth-of-the-furrows-and-pipes-filledwith-warp-drift-varies-from-3-to-6-feet-one-of-the-pipes-howeverextending-to-the-depth-of-9-feet-if-all-the-projecting-points-ofboulder-clay-image338174734.htmlRM2AJ5592–The Quarterly journal of the Geological Society of London . Lower Oolite. Fig. 5.—Section of Pipes in the Boulder-clay, at Hardingham,Norfolk.. a. Loamy Warp-drift. b. Boulder-clay, r. The same materials as the Boulder-clay, viz. chalk and clay, butcontaining irregular seams of sand and gravel. 1854.] TRIMMER ON SAND-PIPES. 237 Fig. 5. A section of the Warp-drift and Boulder-clay near Hard-ingham, Norfolk. Here the depth of the furrows and pipes filledwith Warp-drift varies from 3 to 6 feet; one of the pipes, however,extending to the depth of 9 feet. If all the projecting points ofBoulder-clay
![. Fossil plants : for students of botany and geology . Paleobotany. xxi] CYATHEACEAE 369 mens of fronds which afford no evidence as to the nature of the sori or sporangia. Some of the fronds referred by this author to Thyrsopteris rarinervis'^, which I examined in the Washington Museum, are in all probability examples of Onychiopsis, a, genus included in the Polypodiaceae. The fragments described by Lester Ward^ as species of Thyrsopteris from the Lower Cretaceous of the Black Hills of North America afford no. Fig. 272. Coniopteris hijmeiiophylloides. Specimen from the Inferior Oolite, Scarbor Stock Photo](https://c8.alamy.com/comp/PG15CY/fossil-plants-for-students-of-botany-and-geology-paleobotany-xxi-cyatheaceae-369-mens-of-fronds-which-afford-no-evidence-as-to-the-nature-of-the-sori-or-sporangia-some-of-the-fronds-referred-by-this-author-to-thyrsopteris-rarinervis-which-i-examined-in-the-washington-museum-are-in-all-probability-examples-of-onychiopsis-a-genus-included-in-the-polypodiaceae-the-fragments-described-by-lester-ward-as-species-of-thyrsopteris-from-the-lower-cretaceous-of-the-black-hills-of-north-america-afford-no-fig-272-coniopteris-hijmeiiophylloides-specimen-from-the-inferior-oolite-scarbor-PG15CY.jpg ". Fossil plants : for students of botany and geology . Paleobotany. xxi] CYATHEACEAE 369 mens of fronds which afford no evidence as to the nature of the sori or sporangia. Some of the fronds referred by this author to Thyrsopteris rarinervis'^, which I examined in the Washington Museum, are in all probability examples of Onychiopsis, a, genus included in the Polypodiaceae. The fragments described by Lester Ward^ as species of Thyrsopteris from the Lower Cretaceous of the Black Hills of North America afford no. Fig. 272. Coniopteris hijmeiiophylloides. Specimen from the Inferior Oolite, Scarbor Stock Photo")
. Fossil plants : for students of botany and geology . Paleobotany. xxi] CYATHEACEAE 369 mens of fronds which afford no evidence as to the nature of the sori or sporangia. Some of the fronds referred by this author to Thyrsopteris rarinervis'^, which I examined in the Washington Museum, are in all probability examples of Onychiopsis, a, genus included in the Polypodiaceae. The fragments described by Lester Ward^ as species of Thyrsopteris from the Lower Cretaceous of the Black Hills of North America afford no. Fig. 272. Coniopteris hijmeiiophylloides. Specimen from the Inferior Oolite, Scarbor Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fossil-plants-for-students-of-botany-and-geology-paleobotany-xxi-cyatheaceae-369-mens-of-fronds-which-afford-no-evidence-as-to-the-nature-of-the-sori-or-sporangia-some-of-the-fronds-referred-by-this-author-to-thyrsopteris-rarinervis-which-i-examined-in-the-washington-museum-are-in-all-probability-examples-of-onychiopsis-a-genus-included-in-the-polypodiaceae-the-fragments-described-by-lester-ward-as-species-of-thyrsopteris-from-the-lower-cretaceous-of-the-black-hills-of-north-america-afford-no-fig-272-coniopteris-hijmeiiophylloides-specimen-from-the-inferior-oolite-scarbor-image216385147.htmlRMPG15CY–. Fossil plants : for students of botany and geology . Paleobotany. xxi] CYATHEACEAE 369 mens of fronds which afford no evidence as to the nature of the sori or sporangia. Some of the fronds referred by this author to Thyrsopteris rarinervis'^, which I examined in the Washington Museum, are in all probability examples of Onychiopsis, a, genus included in the Polypodiaceae. The fragments described by Lester Ward^ as species of Thyrsopteris from the Lower Cretaceous of the Black Hills of North America afford no. Fig. 272. Coniopteris hijmeiiophylloides. Specimen from the Inferior Oolite, Scarbor
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36589054.htmlRMC3ENKX–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 398 CORAL-KAG. [Ch. XX. m an upward direction, there is no similar discordance as we proceed downwards, and pass from one to another of the several members of the Jurassic group, the Upper, Middle, and Lower Oolite, and the Lias. Thus, for example, I find on consulting Mr. Etheridge's tables of British Fossils,* that of sixty species of all classes that lived in the period of the Kimmeridge clay, twenty, or about 33 Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-398-coral-kag-ch-xx-m-an-upward-direction-there-is-no-similar-discordance-as-we-proceed-downwards-and-pass-from-one-to-another-of-the-several-members-of-the-jurassic-group-the-upper-middle-and-lower-oolite-and-the-lias-thus-for-example-i-find-on-consulting-mr-etheridges-tables-of-british-fossils-that-of-sixty-species-of-all-classes-that-lived-in-the-period-of-the-kimmeridge-clay-twenty-or-about-33-image239640771.htmlRMRWTG6Y–Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 398 CORAL-KAG. [Ch. XX. m an upward direction, there is no similar discordance as we proceed downwards, and pass from one to another of the several members of the Jurassic group, the Upper, Middle, and Lower Oolite, and the Lias. Thus, for example, I find on consulting Mr. Etheridge's tables of British Fossils,* that of sixty species of all classes that lived in the period of the Kimmeridge clay, twenty, or about 33
![The Quarterly journal of the Geological Society of London . Michael i Mintein Bros . imp. JURASSIC MOLLUSCA FROM MADAGASCAR. Quart. Journ.Geol. Soc .Vol. LI. PL III.. /lichael dpi et lith. Mintem Bros . imp. JURASSIC M0LJAJ5CA FROM MADAGASCAR. Vol.51.] MK. E. B. NEWTON ON FOSSILS FROM MADAGASCAR. 91 Khynchonella (allied to) variabilis, Sehlotheim. „ plicatella J. de 0. Sowerby. I ^^ Oolite „ conctnna, J. bowerby. | „ obsoleta, J. Sowerby. J „ (allied to) tetrahedra, J. Sowerby. Lias & Lower Oolite. Echinodermata. Pentacrinus, sp. Lias (?). Acrosalcnia, sp. Lias. Stomechinus (allied to) bigranu Stock Photo](https://c8.alamy.com/comp/2AWH08G/the-quarterly-journal-of-the-geological-society-of-london-michael-i-mintein-bros-imp-jurassic-mollusca-from-madagascar-quart-journgeol-soc-vol-li-pl-iii-lichael-dpi-et-lith-mintem-bros-imp-jurassic-m0ljaj5ca-from-madagascar-vol51-mk-e-b-newton-on-fossils-from-madagascar-91-khynchonella-allied-to-variabilis-sehlotheim-plicatella-j-de-0-sowerby-i-oolite-conctnna-j-bowerby-obsoleta-j-sowerby-j-allied-to-tetrahedra-j-sowerby-lias-lower-oolite-echinodermata-pentacrinus-sp-lias-acrosalcnia-sp-lias-stomechinus-allied-to-bigranu-2AWH08G.jpg "The Quarterly journal of the Geological Society of London . Michael i Mintein Bros . imp. JURASSIC MOLLUSCA FROM MADAGASCAR. Quart. Journ.Geol. Soc .Vol. LI. PL III.. /lichael dpi et lith. Mintem Bros . imp. JURASSIC M0LJAJ5CA FROM MADAGASCAR. Vol.51.] MK. E. B. NEWTON ON FOSSILS FROM MADAGASCAR. 91 Khynchonella (allied to) variabilis, Sehlotheim. „ plicatella J. de 0. Sowerby. I ^^ Oolite „ conctnna, J. bowerby. | „ obsoleta, J. Sowerby. J „ (allied to) tetrahedra, J. Sowerby. Lias & Lower Oolite. Echinodermata. Pentacrinus, sp. Lias (?). Acrosalcnia, sp. Lias. Stomechinus (allied to) bigranu Stock Photo")
The Quarterly journal of the Geological Society of London . Michael i Mintein Bros . imp. JURASSIC MOLLUSCA FROM MADAGASCAR. Quart. Journ.Geol. Soc .Vol. LI. PL III.. /lichael dpi et lith. Mintem Bros . imp. JURASSIC M0LJAJ5CA FROM MADAGASCAR. Vol.51.] MK. E. B. NEWTON ON FOSSILS FROM MADAGASCAR. 91 Khynchonella (allied to) variabilis, Sehlotheim. „ plicatella J. de 0. Sowerby. I ^^ Oolite „ conctnna, J. bowerby. | „ obsoleta, J. Sowerby. J „ (allied to) tetrahedra, J. Sowerby. Lias & Lower Oolite. Echinodermata. Pentacrinus, sp. Lias (?). Acrosalcnia, sp. Lias. Stomechinus (allied to) bigranu Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-quarterly-journal-of-the-geological-society-of-london-michael-i-mintein-bros-imp-jurassic-mollusca-from-madagascar-quart-journgeol-soc-vol-li-pl-iii-lichael-dpi-et-lith-mintem-bros-imp-jurassic-m0ljaj5ca-from-madagascar-vol51-mk-e-b-newton-on-fossils-from-madagascar-91-khynchonella-allied-to-variabilis-sehlotheim-plicatella-j-de-0-sowerby-i-oolite-conctnna-j-bowerby-obsoleta-j-sowerby-j-allied-to-tetrahedra-j-sowerby-lias-lower-oolite-echinodermata-pentacrinus-sp-lias-acrosalcnia-sp-lias-stomechinus-allied-to-bigranu-image342736816.htmlRM2AWH08G–The Quarterly journal of the Geological Society of London . Michael i Mintein Bros . imp. JURASSIC MOLLUSCA FROM MADAGASCAR. Quart. Journ.Geol. Soc .Vol. LI. PL III.. /lichael dpi et lith. Mintem Bros . imp. JURASSIC M0LJAJ5CA FROM MADAGASCAR. Vol.51.] MK. E. B. NEWTON ON FOSSILS FROM MADAGASCAR. 91 Khynchonella (allied to) variabilis, Sehlotheim. „ plicatella J. de 0. Sowerby. I ^^ Oolite „ conctnna, J. bowerby. | „ obsoleta, J. Sowerby. J „ (allied to) tetrahedra, J. Sowerby. Lias & Lower Oolite. Echinodermata. Pentacrinus, sp. Lias (?). Acrosalcnia, sp. Lias. Stomechinus (allied to) bigranu
![. Fossil plants : for students of botany and geology . Paleobotany. xxi] CLADOPHLEBIS 345 sents an impression from the Inferior Oolite rocks of the Yorkshire coast in which the exposed upper surface of the pinnules shows a series of parallel ridges following the course of the lateral veins and no doubt formed by oblong son on the lower surface. There can be little doubt that the specimen figured by Lindley and Hutton and by others as Pecopteris undans^ is, as Nathorst suggests, a portion of a fertile frond of C. denticulata. A fertile specimen of a frond resembling in habit C. denticulata, whi Stock Photo](https://c8.alamy.com/comp/PG15FB/fossil-plants-for-students-of-botany-and-geology-paleobotany-xxi-cladophlebis-345-sents-an-impression-from-the-inferior-oolite-rocks-of-the-yorkshire-coast-in-which-the-exposed-upper-surface-of-the-pinnules-shows-a-series-of-parallel-ridges-following-the-course-of-the-lateral-veins-and-no-doubt-formed-by-oblong-son-on-the-lower-surface-there-can-be-little-doubt-that-the-specimen-figured-by-lindley-and-hutton-and-by-others-as-pecopteris-undans-is-as-nathorst-suggests-a-portion-of-a-fertile-frond-of-c-denticulata-a-fertile-specimen-of-a-frond-resembling-in-habit-c-denticulata-whi-PG15FB.jpg ". Fossil plants : for students of botany and geology . Paleobotany. xxi] CLADOPHLEBIS 345 sents an impression from the Inferior Oolite rocks of the Yorkshire coast in which the exposed upper surface of the pinnules shows a series of parallel ridges following the course of the lateral veins and no doubt formed by oblong son on the lower surface. There can be little doubt that the specimen figured by Lindley and Hutton and by others as Pecopteris undans^ is, as Nathorst suggests, a portion of a fertile frond of C. denticulata. A fertile specimen of a frond resembling in habit C. denticulata, whi Stock Photo")
. Fossil plants : for students of botany and geology . Paleobotany. xxi] CLADOPHLEBIS 345 sents an impression from the Inferior Oolite rocks of the Yorkshire coast in which the exposed upper surface of the pinnules shows a series of parallel ridges following the course of the lateral veins and no doubt formed by oblong son on the lower surface. There can be little doubt that the specimen figured by Lindley and Hutton and by others as Pecopteris undans^ is, as Nathorst suggests, a portion of a fertile frond of C. denticulata. A fertile specimen of a frond resembling in habit C. denticulata, whi Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fossil-plants-for-students-of-botany-and-geology-paleobotany-xxi-cladophlebis-345-sents-an-impression-from-the-inferior-oolite-rocks-of-the-yorkshire-coast-in-which-the-exposed-upper-surface-of-the-pinnules-shows-a-series-of-parallel-ridges-following-the-course-of-the-lateral-veins-and-no-doubt-formed-by-oblong-son-on-the-lower-surface-there-can-be-little-doubt-that-the-specimen-figured-by-lindley-and-hutton-and-by-others-as-pecopteris-undans-is-as-nathorst-suggests-a-portion-of-a-fertile-frond-of-c-denticulata-a-fertile-specimen-of-a-frond-resembling-in-habit-c-denticulata-whi-image216385215.htmlRMPG15FB–. Fossil plants : for students of botany and geology . Paleobotany. xxi] CLADOPHLEBIS 345 sents an impression from the Inferior Oolite rocks of the Yorkshire coast in which the exposed upper surface of the pinnules shows a series of parallel ridges following the course of the lateral veins and no doubt formed by oblong son on the lower surface. There can be little doubt that the specimen figured by Lindley and Hutton and by others as Pecopteris undans^ is, as Nathorst suggests, a portion of a fertile frond of C. denticulata. A fertile specimen of a frond resembling in habit C. denticulata, whi
Fossils on fallen rock on the beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-fossils-on-fallen-rock-on-the-beach-at-burton-bradstock-near-bridport-36603105.htmlRMC3FBHN–Fossils on fallen rock on the beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 PieropTiyllum comptum. Syn. Cycadites eomptus. Upper Sandstone and Shale, Gristhorpe, near Scarborough. Fig. 423. Hemitelites Broicnii, Goepp. Syn. Phlebopteris contigua, Lind. <fc Hntt. Upper Carbonaceous strata, Lower Oolite, Gristhorpe, Yorkshire. shales are well exposed in the sea-cliffs at Whitby, and are chiefly characterized by ferns and cycadese. They contain, also, a species of calamnite, and a fossil Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-pieroptiyllum-comptum-syn-cycadites-eomptus-upper-sandstone-and-shale-gristhorpe-near-scarborough-fig-423-hemitelites-broicnii-goepp-syn-phlebopteris-contigua-lind-ltfc-hntt-upper-carbonaceous-strata-lower-oolite-gristhorpe-yorkshire-shales-are-well-exposed-in-the-sea-cliffs-at-whitby-and-are-chiefly-characterized-by-ferns-and-cycadese-they-contain-also-a-species-of-calamnite-and-a-fossil-image239641301.htmlRMRWTGWW–Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 PieropTiyllum comptum. Syn. Cycadites eomptus. Upper Sandstone and Shale, Gristhorpe, near Scarborough. Fig. 423. Hemitelites Broicnii, Goepp. Syn. Phlebopteris contigua, Lind. <fc Hntt. Upper Carbonaceous strata, Lower Oolite, Gristhorpe, Yorkshire. shales are well exposed in the sea-cliffs at Whitby, and are chiefly characterized by ferns and cycadese. They contain, also, a species of calamnite, and a fossil
. The testimony of the rocks; . ven the mode of decay ofthis Zamia, as shown by the abrupt termination of its leaf-lets, exactly resembled that of its existing congeners. (Fig.134.) The withered points of the pinnae of recent Zamisedrop off as if clipped across with a pair of scissors; and infossil fronds of this Zamia of the Lias we find exactly thesame clipped-like appearance. (Fig. 135.) Another ScotchZamia (Fig. 136), which occurs in the Lower Oolite ofHelmsdale, resembles the Eathie one in the breadth of itsleaflets, but they are not wholly so rectilinear, diminishingslightly towards thei Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-testimony-of-the-rocks-ven-the-mode-of-decay-ofthis-zamia-as-shown-by-the-abrupt-termination-of-its-leaf-lets-exactly-resembled-that-of-its-existing-congeners-fig134-the-withered-points-of-the-pinnae-of-recent-zamisedrop-off-as-if-clipped-across-with-a-pair-of-scissors-and-infossil-fronds-of-this-zamia-of-the-lias-we-find-exactly-thesame-clipped-like-appearance-fig-135-another-scotchzamia-fig-136-which-occurs-in-the-lower-oolite-ofhelmsdale-resembles-the-eathie-one-in-the-breadth-of-itsleaflets-but-they-are-not-wholly-so-rectilinear-diminishingslightly-towards-thei-image370013398.htmlRM2CDYFT6–. The testimony of the rocks; . ven the mode of decay ofthis Zamia, as shown by the abrupt termination of its leaf-lets, exactly resembled that of its existing congeners. (Fig.134.) The withered points of the pinnae of recent Zamisedrop off as if clipped across with a pair of scissors; and infossil fronds of this Zamia of the Lias we find exactly thesame clipped-like appearance. (Fig. 135.) Another ScotchZamia (Fig. 136), which occurs in the Lower Oolite ofHelmsdale, resembles the Eathie one in the breadth of itsleaflets, but they are not wholly so rectilinear, diminishingslightly towards thei
![. Fossil plants : for students of botany and geology . Paleobotany. XXVIl] CTENOPTERIS 549 Frond bipinnate, broad rachis giving ofF branches at an acute angle; pinnules broadly linear, slightly falcate, with several slightly divergent forked veins. A frond very similar to the Lower Lias specimen from Dorsetshire represented in fig. 362 was described by Leckenby as Ctenis Leckenhyi (Bean MS.) from the Inferior Oolite of Yorkshire'- Leckenby recognised the possibility of a Cycadean. Fiu. 362. Ctenopteris eyeadea, Brongn. (^ nat. size.) From a specimen in the British Museum. [M.S.] affinity, but Stock Photo](https://c8.alamy.com/comp/PG0D4J/fossil-plants-for-students-of-botany-and-geology-paleobotany-xxvil-ctenopteris-549-frond-bipinnate-broad-rachis-giving-off-branches-at-an-acute-angle-pinnules-broadly-linear-slightly-falcate-with-several-slightly-divergent-forked-veins-a-frond-very-similar-to-the-lower-lias-specimen-from-dorsetshire-represented-in-fig-362-was-described-by-leckenby-as-ctenis-leckenhyi-bean-ms-from-the-inferior-oolite-of-yorkshire-leckenby-recognised-the-possibility-of-a-cycadean-fiu-362-ctenopteris-eyeadea-brongn-nat-size-from-a-specimen-in-the-british-museum-ms-affinity-but-PG0D4J.jpg ". Fossil plants : for students of botany and geology . Paleobotany. XXVIl] CTENOPTERIS 549 Frond bipinnate, broad rachis giving ofF branches at an acute angle; pinnules broadly linear, slightly falcate, with several slightly divergent forked veins. A frond very similar to the Lower Lias specimen from Dorsetshire represented in fig. 362 was described by Leckenby as Ctenis Leckenhyi (Bean MS.) from the Inferior Oolite of Yorkshire'- Leckenby recognised the possibility of a Cycadean. Fiu. 362. Ctenopteris eyeadea, Brongn. (^ nat. size.) From a specimen in the British Museum. [M.S.] affinity, but Stock Photo")
. Fossil plants : for students of botany and geology . Paleobotany. XXVIl] CTENOPTERIS 549 Frond bipinnate, broad rachis giving ofF branches at an acute angle; pinnules broadly linear, slightly falcate, with several slightly divergent forked veins. A frond very similar to the Lower Lias specimen from Dorsetshire represented in fig. 362 was described by Leckenby as Ctenis Leckenhyi (Bean MS.) from the Inferior Oolite of Yorkshire'- Leckenby recognised the possibility of a Cycadean. Fiu. 362. Ctenopteris eyeadea, Brongn. (^ nat. size.) From a specimen in the British Museum. [M.S.] affinity, but Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fossil-plants-for-students-of-botany-and-geology-paleobotany-xxvil-ctenopteris-549-frond-bipinnate-broad-rachis-giving-off-branches-at-an-acute-angle-pinnules-broadly-linear-slightly-falcate-with-several-slightly-divergent-forked-veins-a-frond-very-similar-to-the-lower-lias-specimen-from-dorsetshire-represented-in-fig-362-was-described-by-leckenby-as-ctenis-leckenhyi-bean-ms-from-the-inferior-oolite-of-yorkshire-leckenby-recognised-the-possibility-of-a-cycadean-fiu-362-ctenopteris-eyeadea-brongn-nat-size-from-a-specimen-in-the-british-museum-ms-affinity-but-image216369234.htmlRMPG0D4J–. Fossil plants : for students of botany and geology . Paleobotany. XXVIl] CTENOPTERIS 549 Frond bipinnate, broad rachis giving ofF branches at an acute angle; pinnules broadly linear, slightly falcate, with several slightly divergent forked veins. A frond very similar to the Lower Lias specimen from Dorsetshire represented in fig. 362 was described by Leckenby as Ctenis Leckenhyi (Bean MS.) from the Inferior Oolite of Yorkshire'- Leckenby recognised the possibility of a Cycadean. Fiu. 362. Ctenopteris eyeadea, Brongn. (^ nat. size.) From a specimen in the British Museum. [M.S.] affinity, but
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36588952.htmlRMC3ENG8–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 414: PAL^ONTOLOGICAL RELATIONS. [Ch. XX, but little information in regard to the condition of marine life, hav- ing yielded at present only 22 mollusca, as before mentioned (p. 412). While, therefore, the break between two great members of the Lower Oolite is expressed by saying that the proportion of species in common only amounts to 12 per cent., we have seen that there is a connection of 24 per cent, between the Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-414-palontological-relations-ch-xx-but-little-information-in-regard-to-the-condition-of-marine-life-hav-ing-yielded-at-present-only-22-mollusca-as-before-mentioned-p-412-while-therefore-the-break-between-two-great-members-of-the-lower-oolite-is-expressed-by-saying-that-the-proportion-of-species-in-common-only-amounts-to-12-per-cent-we-have-seen-that-there-is-a-connection-of-24-per-cent-between-the-image239641449.htmlRMRWTH35–Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 414: PAL^ONTOLOGICAL RELATIONS. [Ch. XX, but little information in regard to the condition of marine life, hav- ing yielded at present only 22 mollusca, as before mentioned (p. 412). While, therefore, the break between two great members of the Lower Oolite is expressed by saying that the proportion of species in common only amounts to 12 per cent., we have seen that there is a connection of 24 per cent, between the
. Geological magazine. (oh t^. A.SFoorddel. Mintern Bros. imp. Oxfordian L Lower Oolite Gasteropoda. (Ybrksliire) THE GEOLOGICAL MAGAZINE. NEW SERIES. DECADE III. VOL. I. No. VI.—JUNE, I.—Contributions to the PALiEONTOLOGY of the Toekshike Oolites. By Wilfrid H. Hudleston, M.A., F.E.S., F.G.S. (Continued from Decade III. Vol. I. p. 204.) (PLATE VIII.) Littorina and Amberleya. THE group of shells figured on Plate VIII. (excepting Fig. 12,whose position is doubtful) constitute a natural section of tur-binate or trochiform species, which should be classed under one andthe same genus, or at most o Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/geological-magazine-oh-t-asfoorddel-mintern-bros-imp-oxfordian-l-lower-oolite-gasteropoda-ybrksliire-the-geological-magazine-new-series-decade-iii-vol-i-no-vijune-icontributions-to-the-palieontology-of-the-toekshike-oolites-by-wilfrid-h-hudleston-ma-fes-fgs-continued-from-decade-iii-vol-i-p-204-plate-viii-littorina-and-amberleya-the-group-of-shells-figured-on-plate-viii-excepting-fig-12whose-position-is-doubtful-constitute-a-natural-section-of-tur-binate-or-trochiform-species-which-should-be-classed-under-one-andthe-same-genus-or-at-most-o-image370470915.htmlRM2CEMBC3–. Geological magazine. (oh t^. A.SFoorddel. Mintern Bros. imp. Oxfordian L Lower Oolite Gasteropoda. (Ybrksliire) THE GEOLOGICAL MAGAZINE. NEW SERIES. DECADE III. VOL. I. No. VI.—JUNE, I.—Contributions to the PALiEONTOLOGY of the Toekshike Oolites. By Wilfrid H. Hudleston, M.A., F.E.S., F.G.S. (Continued from Decade III. Vol. I. p. 204.) (PLATE VIII.) Littorina and Amberleya. THE group of shells figured on Plate VIII. (excepting Fig. 12,whose position is doubtful) constitute a natural section of tur-binate or trochiform species, which should be classed under one andthe same genus, or at most o
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36589056.htmlRMC3ENM0–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
![Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Ch. XX.] FOSSIL PLANTS OF GREAT OOLITE. 411 In the northwest of Yorkshire, the formation alluded to consists of an upper and a lower carbonaceous shale, abounding in impressions of plants, divided by a limestone considered by many geologists as the representative of the Great Oolite; but the scarcity of marine fossils makes all comparisons with the subdivisions adopted in the south extremely dim cult. A rich harvest Stock Photo](https://c8.alamy.com/comp/RWTGWT/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-ch-xx-fossil-plants-of-great-oolite-411-in-the-northwest-of-yorkshire-the-formation-alluded-to-consists-of-an-upper-and-a-lower-carbonaceous-shale-abounding-in-impressions-of-plants-divided-by-a-limestone-considered-by-many-geologists-as-the-representative-of-the-great-oolite-but-the-scarcity-of-marine-fossils-makes-all-comparisons-with-the-subdivisions-adopted-in-the-south-extremely-dim-cult-a-rich-harvest-RWTGWT.jpg "Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Ch. XX.] FOSSIL PLANTS OF GREAT OOLITE. 411 In the northwest of Yorkshire, the formation alluded to consists of an upper and a lower carbonaceous shale, abounding in impressions of plants, divided by a limestone considered by many geologists as the representative of the Great Oolite; but the scarcity of marine fossils makes all comparisons with the subdivisions adopted in the south extremely dim cult. A rich harvest Stock Photo")
Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Ch. XX.] FOSSIL PLANTS OF GREAT OOLITE. 411 In the northwest of Yorkshire, the formation alluded to consists of an upper and a lower carbonaceous shale, abounding in impressions of plants, divided by a limestone considered by many geologists as the representative of the Great Oolite; but the scarcity of marine fossils makes all comparisons with the subdivisions adopted in the south extremely dim cult. A rich harvest Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-elementsofgeolog00lyel-year-1868-ch-xx-fossil-plants-of-great-oolite-411-in-the-northwest-of-yorkshire-the-formation-alluded-to-consists-of-an-upper-and-a-lower-carbonaceous-shale-abounding-in-impressions-of-plants-divided-by-a-limestone-considered-by-many-geologists-as-the-representative-of-the-great-oolite-but-the-scarcity-of-marine-fossils-makes-all-comparisons-with-the-subdivisions-adopted-in-the-south-extremely-dim-cult-a-rich-harvest-image239641300.htmlRMRWTGWT–Elements of geology, or, The Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments elementsofgeolog00lyel Year: 1868 Ch. XX.] FOSSIL PLANTS OF GREAT OOLITE. 411 In the northwest of Yorkshire, the formation alluded to consists of an upper and a lower carbonaceous shale, abounding in impressions of plants, divided by a limestone considered by many geologists as the representative of the Great Oolite; but the scarcity of marine fossils makes all comparisons with the subdivisions adopted in the south extremely dim cult. A rich harvest
. Geological magazine. A S Foord del et Mh 5^. Oxfordian h. Lower Oolite Gasteropoda.(Ybrkshire.j Mintem Bros. imp. THE GEOLOGICAL MAGAZINE- NEW SERIES. DECADE III. VOL. I. So. v.—MAY, 1884. (D:EiXG-xi<rjL.Xj -A-is-tioXjIes. I.—Contributions to the Paleontology of the Yorkshire Oolites. By Wilfrid H. Hudleston, M.A., F.G.S. (Continued from Decade III. Vol. I. p. 154.) (PLATE VI. Figs. 11, lla; PLATE VII.) 40.—Alaria trifida/ Phillips, 1829. Plate VI. Figs. 11, lla;Plate VII. Figs. 1, la, 2, 3, 3a. 1829 and 1835. Rostellaria trifida, Bean MS. Phillips, G. T. p. 109, pi. v. fig. 14. 1842. Ros Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/geological-magazine-a-s-foord-del-et-mh-5-oxfordian-h-lower-oolite-gasteropodaybrkshirej-mintem-bros-imp-the-geological-magazine-new-series-decade-iii-vol-i-so-vmay-1884-deixg-xiltrjlxj-a-is-tioxjies-icontributions-to-the-paleontology-of-the-yorkshire-oolites-by-wilfrid-h-hudleston-ma-fgs-continued-from-decade-iii-vol-i-p-154-plate-vi-figs-11-lla-plate-vii-40alaria-trifida-phillips-1829-plate-vi-figs-11-llaplate-vii-figs-1-la-2-3-3a-1829-and-1835-rostellaria-trifida-bean-ms-phillips-g-t-p-109-pi-v-fig-14-1842-ros-image370492313.htmlRM2CENAM9–. Geological magazine. A S Foord del et Mh 5^. Oxfordian h. Lower Oolite Gasteropoda.(Ybrkshire.j Mintem Bros. imp. THE GEOLOGICAL MAGAZINE- NEW SERIES. DECADE III. VOL. I. So. v.—MAY, 1884. (D:EiXG-xi<rjL.Xj -A-is-tioXjIes. I.—Contributions to the Paleontology of the Yorkshire Oolites. By Wilfrid H. Hudleston, M.A., F.G.S. (Continued from Decade III. Vol. I. p. 154.) (PLATE VI. Figs. 11, lla; PLATE VII.) 40.—Alaria trifida/ Phillips, 1829. Plate VI. Figs. 11, lla;Plate VII. Figs. 1, la, 2, 3, 3a. 1829 and 1835. Rostellaria trifida, Bean MS. Phillips, G. T. p. 109, pi. v. fig. 14. 1842. Ros
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36589007.htmlRMC3ENJ7–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. Catalogue of the fossil plants of the Glossopteris flora in the Department of geology. Paleobotany -- Carboniferous; Paleobotany -- Catalogs and collections; Plants, Fossil -- Catalogs and collections. CLADOniLEBXS. 113 for the Indian fronds, as Feistmantel pointed out, closely resemble some of tliose known from the Lower Oolite of Britain and else- where. As a specific name I adopted 'Royleii in 1901 in honour of the first discoverer of this species. Fertile fronds of this species have been described and figured by Feistmantel. Tbe sporangia are inserted on the lateral veins of the leaflets Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-the-fossil-plants-of-the-glossopteris-flora-in-the-department-of-geology-paleobotany-carboniferous-paleobotany-catalogs-and-collections-plants-fossil-catalogs-and-collections-cladonilebxs-113-for-the-indian-fronds-as-feistmantel-pointed-out-closely-resemble-some-of-tliose-known-from-the-lower-oolite-of-britain-and-else-where-as-a-specific-name-i-adopted-royleii-in-1901-in-honour-of-the-first-discoverer-of-this-species-fertile-fronds-of-this-species-have-been-described-and-figured-by-feistmantel-tbe-sporangia-are-inserted-on-the-lateral-veins-of-the-leaflets-image233005346.htmlRMRF28KE–. Catalogue of the fossil plants of the Glossopteris flora in the Department of geology. Paleobotany -- Carboniferous; Paleobotany -- Catalogs and collections; Plants, Fossil -- Catalogs and collections. CLADOniLEBXS. 113 for the Indian fronds, as Feistmantel pointed out, closely resemble some of tliose known from the Lower Oolite of Britain and else- where. As a specific name I adopted 'Royleii in 1901 in honour of the first discoverer of this species. Fertile fronds of this species have been described and figured by Feistmantel. Tbe sporangia are inserted on the lateral veins of the leaflets
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36588943.htmlRMC3ENFY–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. Catalogue of the fossil plants of the Glossopteris flora in the Department of geology. Paleobotany -- Carboniferous; Paleobotany -- Catalogs and collections; Plants, Fossil -- Catalogs and collections. CLADOniLEBXS. 113 for the Indian fronds, as Feistmantel pointed out, closely resemble some of tliose known from the Lower Oolite of Britain and else- where. As a specific name I adopted 'Royleii in 1901 in honour of the first discoverer of this species. Fertile fronds of this species have been described and figured by Feistmantel. Tbe sporangia are inserted on the lateral veins of the leaflets Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-the-fossil-plants-of-the-glossopteris-flora-in-the-department-of-geology-paleobotany-carboniferous-paleobotany-catalogs-and-collections-plants-fossil-catalogs-and-collections-cladonilebxs-113-for-the-indian-fronds-as-feistmantel-pointed-out-closely-resemble-some-of-tliose-known-from-the-lower-oolite-of-britain-and-else-where-as-a-specific-name-i-adopted-royleii-in-1901-in-honour-of-the-first-discoverer-of-this-species-fertile-fronds-of-this-species-have-been-described-and-figured-by-feistmantel-tbe-sporangia-are-inserted-on-the-lateral-veins-of-the-leaflets-image233176911.htmlRMRFA3ER–. Catalogue of the fossil plants of the Glossopteris flora in the Department of geology. Paleobotany -- Carboniferous; Paleobotany -- Catalogs and collections; Plants, Fossil -- Catalogs and collections. CLADOniLEBXS. 113 for the Indian fronds, as Feistmantel pointed out, closely resemble some of tliose known from the Lower Oolite of Britain and else- where. As a specific name I adopted 'Royleii in 1901 in honour of the first discoverer of this species. Fertile fronds of this species have been described and figured by Feistmantel. Tbe sporangia are inserted on the lateral veins of the leaflets
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36589061.htmlRMC3ENM5–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
![. College collection of palaeontology. No. 334. Crassatella protexta, <?ou. This genus has the ligament internal. It commences in the Cretaceous and abounds to-day, and is the type of a family. Eocene,'Claiborne, Alabama. No. 335. Astarte obliqua, Desh. This genus is to-day represented by twenty species, widely distributed in the Northern seas; 285 fossil species are known, beginning with the Carbon- iferous. Family Astartidse. Lower Oolite, Bayeux, Calvados, France. No. 336. Venericardia rotunda, "Lea. This belongs to the family Astartidte, and the genus dates from the Creta- ceous. E Stock Photo](https://c8.alamy.com/comp/REHCD8/college-collection-of-palaeontology-no-334-crassatella-protexta-ltou-this-genus-has-the-ligament-internal-it-commences-in-the-cretaceous-and-abounds-to-day-and-is-the-type-of-a-family-eoceneclaiborne-alabama-no-335-astarte-obliqua-desh-this-genus-is-to-day-represented-by-twenty-species-widely-distributed-in-the-northern-seas-285-fossil-species-are-known-beginning-with-the-carbon-iferous-family-astartidse-lower-oolite-bayeux-calvados-france-no-336-venericardia-rotunda-quotlea-this-belongs-to-the-family-astartidte-and-the-genus-dates-from-the-creta-ceous-e-REHCD8.jpg ". College collection of palaeontology. No. 334. Crassatella protexta, <?ou. This genus has the ligament internal. It commences in the Cretaceous and abounds to-day, and is the type of a family. Eocene,'Claiborne, Alabama. No. 335. Astarte obliqua, Desh. This genus is to-day represented by twenty species, widely distributed in the Northern seas; 285 fossil species are known, beginning with the Carbon- iferous. Family Astartidse. Lower Oolite, Bayeux, Calvados, France. No. 336. Venericardia rotunda, "Lea. This belongs to the family Astartidte, and the genus dates from the Creta- ceous. E Stock Photo")
. College collection of palaeontology. No. 334. Crassatella protexta, <?ou. This genus has the ligament internal. It commences in the Cretaceous and abounds to-day, and is the type of a family. Eocene,'Claiborne, Alabama. No. 335. Astarte obliqua, Desh. This genus is to-day represented by twenty species, widely distributed in the Northern seas; 285 fossil species are known, beginning with the Carbon- iferous. Family Astartidse. Lower Oolite, Bayeux, Calvados, France. No. 336. Venericardia rotunda, "Lea. This belongs to the family Astartidte, and the genus dates from the Creta- ceous. E Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-no-334-crassatella-protexta-ltou-this-genus-has-the-ligament-internal-it-commences-in-the-cretaceous-and-abounds-to-day-and-is-the-type-of-a-family-eoceneclaiborne-alabama-no-335-astarte-obliqua-desh-this-genus-is-to-day-represented-by-twenty-species-widely-distributed-in-the-northern-seas-285-fossil-species-are-known-beginning-with-the-carbon-iferous-family-astartidse-lower-oolite-bayeux-calvados-france-no-336-venericardia-rotunda-quotlea-this-belongs-to-the-family-astartidte-and-the-genus-dates-from-the-creta-ceous-e-image232722932.htmlRMREHCD8–. College collection of palaeontology. No. 334. Crassatella protexta, <?ou. This genus has the ligament internal. It commences in the Cretaceous and abounds to-day, and is the type of a family. Eocene,'Claiborne, Alabama. No. 335. Astarte obliqua, Desh. This genus is to-day represented by twenty species, widely distributed in the Northern seas; 285 fossil species are known, beginning with the Carbon- iferous. Family Astartidse. Lower Oolite, Bayeux, Calvados, France. No. 336. Venericardia rotunda, "Lea. This belongs to the family Astartidte, and the genus dates from the Creta- ceous. E
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36589019.htmlRMC3ENJK–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 162 KADIATA. No. 795. Clypeus Davoustianus, Cott. This discoidal, inflated Urchin, with central ambulacral apex, is from the Great Oolite, Becheseul, Prance. Price, $0.35. No. 796. Clypeus (Nucleolites) Plotii, Klein. This is w ell characterized by its depressed shell with circular contour; large, lanceolate ambulacral areas ; and deep oval furrows, prolonged to the summit, which is eccentric. From the Lower Oolite, Cheltenham, England. Price, $0.50. No. 797. C Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-162-kadiata-no-795-clypeus-davoustianus-cott-this-discoidal-inflated-urchin-with-central-ambulacral-apex-is-from-the-great-oolite-becheseul-prance-price-035-no-796-clypeus-nucleolites-plotii-klein-this-is-w-ell-characterized-by-its-depressed-shell-with-circular-contour-large-lanceolate-ambulacral-areas-and-deep-oval-furrows-prolonged-to-the-summit-which-is-eccentric-from-the-lower-oolite-cheltenham-england-price-050-no-797-c-image233007779.htmlRMRF2BPB–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 162 KADIATA. No. 795. Clypeus Davoustianus, Cott. This discoidal, inflated Urchin, with central ambulacral apex, is from the Great Oolite, Becheseul, Prance. Price, $0.35. No. 796. Clypeus (Nucleolites) Plotii, Klein. This is w ell characterized by its depressed shell with circular contour; large, lanceolate ambulacral areas ; and deep oval furrows, prolonged to the summit, which is eccentric. From the Lower Oolite, Cheltenham, England. Price, $0.50. No. 797. C
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36589048.htmlRMC3ENKM–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
![. College collection of palaeontology. This fine specimen closely resembles A, coronatus, and belongs to the same group, " Goronati." It is from the Lower Oolite, Dorsetshire, England, and now in the Ward Collection, University of Rochester. Diameter, 7. No. 191. [476, Cast], Ammonites Birchii, Sow.. This elegant form, with the outer mark- ings of the shell visible upon all its whorls, and a double row of spines, belongs to the group " Armati." It is from the Lower Lias, Charmouth, England, and belongs to the Ward Collection, University of Rochester. Diameter, 8. No. 193. [ Stock Photo](https://c8.alamy.com/comp/REH26R/college-collection-of-palaeontology-this-fine-specimen-closely-resembles-a-coronatus-and-belongs-to-the-same-group-quot-goronatiquot-it-is-from-the-lower-oolite-dorsetshire-england-and-now-in-the-ward-collection-university-of-rochester-diameter-7-no-191-476-cast-ammonites-birchii-sow-this-elegant-form-with-the-outer-mark-ings-of-the-shell-visible-upon-all-its-whorls-and-a-double-row-of-spines-belongs-to-the-group-quot-armatiquot-it-is-from-the-lower-lias-charmouth-england-and-belongs-to-the-ward-collection-university-of-rochester-diameter-8-no-193-REH26R.jpg ". College collection of palaeontology. This fine specimen closely resembles A, coronatus, and belongs to the same group, " Goronati." It is from the Lower Oolite, Dorsetshire, England, and now in the Ward Collection, University of Rochester. Diameter, 7. No. 191. [476, Cast], Ammonites Birchii, Sow.. This elegant form, with the outer mark- ings of the shell visible upon all its whorls, and a double row of spines, belongs to the group " Armati." It is from the Lower Lias, Charmouth, England, and belongs to the Ward Collection, University of Rochester. Diameter, 8. No. 193. [ Stock Photo")
. College collection of palaeontology. This fine specimen closely resembles A, coronatus, and belongs to the same group, " Goronati." It is from the Lower Oolite, Dorsetshire, England, and now in the Ward Collection, University of Rochester. Diameter, 7. No. 191. [476, Cast], Ammonites Birchii, Sow.. This elegant form, with the outer mark- ings of the shell visible upon all its whorls, and a double row of spines, belongs to the group " Armati." It is from the Lower Lias, Charmouth, England, and belongs to the Ward Collection, University of Rochester. Diameter, 8. No. 193. [ Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-this-fine-specimen-closely-resembles-a-coronatus-and-belongs-to-the-same-group-quot-goronatiquot-it-is-from-the-lower-oolite-dorsetshire-england-and-now-in-the-ward-collection-university-of-rochester-diameter-7-no-191-476-cast-ammonites-birchii-sow-this-elegant-form-with-the-outer-mark-ings-of-the-shell-visible-upon-all-its-whorls-and-a-double-row-of-spines-belongs-to-the-group-quot-armatiquot-it-is-from-the-lower-lias-charmouth-england-and-belongs-to-the-ward-collection-university-of-rochester-diameter-8-no-193-image232714911.htmlRMREH26R–. College collection of palaeontology. This fine specimen closely resembles A, coronatus, and belongs to the same group, " Goronati." It is from the Lower Oolite, Dorsetshire, England, and now in the Ward Collection, University of Rochester. Diameter, 7. No. 191. [476, Cast], Ammonites Birchii, Sow.. This elegant form, with the outer mark- ings of the shell visible upon all its whorls, and a double row of spines, belongs to the group " Armati." It is from the Lower Lias, Charmouth, England, and belongs to the Ward Collection, University of Rochester. Diameter, 8. No. 193. [
Fossils on fallen rock on the beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-fossils-on-fallen-rock-on-the-beach-at-burton-bradstock-near-bridport-36603076.htmlRMC3FBGM–Fossils on fallen rock on the beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
![. College collection of palaeontology. 98 MOLLUSCA. No. 190. [475, Cast]. Ammonites Blagdeni, Sow.. This fine specimen closely resembles A, coronatus, and belongs to the same group, " Goronati." It is from the Lower Oolite, Dorsetshire, England, and now in the Ward Collection, University of Rochester. Diameter, 7. No. 191. [476, Cast], Ammonites Birchii, Sow.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Ward's Stock Photo](https://c8.alamy.com/comp/REH273/college-collection-of-palaeontology-98-mollusca-no-190-475-cast-ammonites-blagdeni-sow-this-fine-specimen-closely-resembles-a-coronatus-and-belongs-to-the-same-group-quot-goronatiquot-it-is-from-the-lower-oolite-dorsetshire-england-and-now-in-the-ward-collection-university-of-rochester-diameter-7-no-191-476-cast-ammonites-birchii-sow-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-wards-REH273.jpg ". College collection of palaeontology. 98 MOLLUSCA. No. 190. [475, Cast]. Ammonites Blagdeni, Sow.. This fine specimen closely resembles A, coronatus, and belongs to the same group, " Goronati." It is from the Lower Oolite, Dorsetshire, England, and now in the Ward Collection, University of Rochester. Diameter, 7. No. 191. [476, Cast], Ammonites Birchii, Sow.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Ward's Stock Photo")
. College collection of palaeontology. 98 MOLLUSCA. No. 190. [475, Cast]. Ammonites Blagdeni, Sow.. This fine specimen closely resembles A, coronatus, and belongs to the same group, " Goronati." It is from the Lower Oolite, Dorsetshire, England, and now in the Ward Collection, University of Rochester. Diameter, 7. No. 191. [476, Cast], Ammonites Birchii, Sow.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Ward's Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-98-mollusca-no-190-475-cast-ammonites-blagdeni-sow-this-fine-specimen-closely-resembles-a-coronatus-and-belongs-to-the-same-group-quot-goronatiquot-it-is-from-the-lower-oolite-dorsetshire-england-and-now-in-the-ward-collection-university-of-rochester-diameter-7-no-191-476-cast-ammonites-birchii-sow-please-note-that-these-images-are-extracted-from-scanned-page-images-that-may-have-been-digitally-enhanced-for-readability-coloration-and-appearance-of-these-illustrations-may-not-perfectly-resemble-the-original-work-wards-image232714919.htmlRMREH273–. College collection of palaeontology. 98 MOLLUSCA. No. 190. [475, Cast]. Ammonites Blagdeni, Sow.. This fine specimen closely resembles A, coronatus, and belongs to the same group, " Goronati." It is from the Lower Oolite, Dorsetshire, England, and now in the Ward Collection, University of Rochester. Diameter, 7. No. 191. [476, Cast], Ammonites Birchii, Sow.. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.. Ward's
Base of the sandstone cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-base-of-the-sandstone-cliffs-at-burton-bradstock-near-bridport-on-36602995.htmlRMC3FBDR–Base of the sandstone cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 162 KADIATA. No. 795. Clypeus Davoustianus, Cott. This discoidal, inflated Urchin, with central ambulacral apex, is from the Great Oolite, Becheseul, Prance. Price, $0.35. No. 796. Clypeus (Nucleolites) Plotii, Klein. This is w ell characterized by its depressed shell with circular contour; large, lanceolate ambulacral areas ; and deep oval furrows, prolonged to the summit, which is eccentric. From the Lower Oolite, Cheltenham, England. Price, $0.50. No. 797. C Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-162-kadiata-no-795-clypeus-davoustianus-cott-this-discoidal-inflated-urchin-with-central-ambulacral-apex-is-from-the-great-oolite-becheseul-prance-price-035-no-796-clypeus-nucleolites-plotii-klein-this-is-w-ell-characterized-by-its-depressed-shell-with-circular-contour-large-lanceolate-ambulacral-areas-and-deep-oval-furrows-prolonged-to-the-summit-which-is-eccentric-from-the-lower-oolite-cheltenham-england-price-050-no-797-c-image233180467.htmlRMRFA81R–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 162 KADIATA. No. 795. Clypeus Davoustianus, Cott. This discoidal, inflated Urchin, with central ambulacral apex, is from the Great Oolite, Becheseul, Prance. Price, $0.35. No. 796. Clypeus (Nucleolites) Plotii, Klein. This is w ell characterized by its depressed shell with circular contour; large, lanceolate ambulacral areas ; and deep oval furrows, prolonged to the summit, which is eccentric. From the Lower Oolite, Cheltenham, England. Price, $0.50. No. 797. C
Fossils on fallen rock on the beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-fossils-on-fallen-rock-on-the-beach-at-burton-bradstock-near-bridport-36603130.htmlRMC3FBJJ–Fossils on fallen rock on the beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. College collection of palaeontology. GASTEROPODA. 115 No. 295. Pleurotomaria sulcomarginata, Con. The sliell of this genus, the type of a family, is distingui.shed by its sub- quadrate aperture, with a slit in its outer lip; 400 species are known from the Palaeozoic and Mesozoic. Hamilton Group, Onondaga Co., New York. No. 296. Pleurotomaria ornata, Defrance. This species takes its name from the row of tubercles which crowns its spiral whorls. Oolite of Calvados, France. From the Inferior. No. 297. Pleurotomaria conoidea, Deshayes. Lower Oolite, Bayeux, France. No. 298. Murchisonia bellicina Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-gasteropoda-115-no-295-pleurotomaria-sulcomarginata-con-the-sliell-of-this-genus-the-type-of-a-family-is-distinguished-by-its-sub-quadrate-aperture-with-a-slit-in-its-outer-lip-400-species-are-known-from-the-palaeozoic-and-mesozoic-hamilton-group-onondaga-co-new-york-no-296-pleurotomaria-ornata-defrance-this-species-takes-its-name-from-the-row-of-tubercles-which-crowns-its-spiral-whorls-oolite-of-calvados-france-from-the-inferior-no-297-pleurotomaria-conoidea-deshayes-lower-oolite-bayeux-france-no-298-murchisonia-bellicina-image232722986.htmlRMREHCF6–. College collection of palaeontology. GASTEROPODA. 115 No. 295. Pleurotomaria sulcomarginata, Con. The sliell of this genus, the type of a family, is distingui.shed by its sub- quadrate aperture, with a slit in its outer lip; 400 species are known from the Palaeozoic and Mesozoic. Hamilton Group, Onondaga Co., New York. No. 296. Pleurotomaria ornata, Defrance. This species takes its name from the row of tubercles which crowns its spiral whorls. Oolite of Calvados, France. From the Inferior. No. 297. Pleurotomaria conoidea, Deshayes. Lower Oolite, Bayeux, France. No. 298. Murchisonia bellicina
The beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-the-beach-at-burton-bradstock-near-bridport-on-the-jurassic-coast-36589073.htmlRMC3ENMH–The beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 150 MOLLUSCA. No. 716. Terebratula intermedia, Sow. From the Lower Oolite of Calvados, France. Original in the Ward Museum of the University of Rochester. No. 717. Terebratula Lycetti, Dav. From the Lias of Ilminster, England. No. 718. Terebratula Mariae, D'Orb. From the Lias of Calvados, France. No. 719. Terebratula Moorei, Dav. From the Lias of Petherton, England. No. 720. Terebratula numismalis, Lam. From the Lias of Calvados, France. No. 721. Terebratula pe Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-150-mollusca-no-716-terebratula-intermedia-sow-from-the-lower-oolite-of-calvados-france-original-in-the-ward-museum-of-the-university-of-rochester-no-717-terebratula-lycetti-dav-from-the-lias-of-ilminster-england-no-718-terebratula-mariae-dorb-from-the-lias-of-calvados-france-no-719-terebratula-moorei-dav-from-the-lias-of-petherton-england-no-720-terebratula-numismalis-lam-from-the-lias-of-calvados-france-no-721-terebratula-pe-image233180521.htmlRMRFA83N–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 150 MOLLUSCA. No. 716. Terebratula intermedia, Sow. From the Lower Oolite of Calvados, France. Original in the Ward Museum of the University of Rochester. No. 717. Terebratula Lycetti, Dav. From the Lias of Ilminster, England. No. 718. Terebratula Mariae, D'Orb. From the Lias of Calvados, France. No. 719. Terebratula Moorei, Dav. From the Lias of Petherton, England. No. 720. Terebratula numismalis, Lam. From the Lias of Calvados, France. No. 721. Terebratula pe
The beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-the-beach-at-burton-bradstock-near-bridport-on-the-jurassic-coast-36589076.htmlRMC3ENMM–The beach at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. College collection of palaeontology. ECHINOIDEA. 139 No. 433. Echinobrissus (Nucleolites) cunucularis, Blaiuv. Lower Oolite, Youne, France. No. 424. Echinolampus afl&nis, Desm. Eocene, Vaiie;irard, France. No. 425. G-alerites albogalerus, Lam. This lofty, almost turreted form, with central mouth and marginal anus, is from the Upper Chalk, Kent, England.. No. 426. Hemicidaris intermedia, Fleming. This large, depressed genus belongs to the Cidari- dce with narrow ambulacra. The distinctive feature is the existence of small tubercles on the lower half of the ambulacra. The spines are cylind Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-echinoidea-139-no-433-echinobrissus-nucleolites-cunucularis-blaiuv-lower-oolite-youne-france-no-424-echinolampus-aflampnis-desm-eocene-vaiieirard-france-no-425-g-alerites-albogalerus-lam-this-lofty-almost-turreted-form-with-central-mouth-and-marginal-anus-is-from-the-upper-chalk-kent-england-no-426-hemicidaris-intermedia-fleming-this-large-depressed-genus-belongs-to-the-cidari-dce-with-narrow-ambulacra-the-distinctive-feature-is-the-existence-of-small-tubercles-on-the-lower-half-of-the-ambulacra-the-spines-are-cylind-image232722689.htmlRMREHC4H–. College collection of palaeontology. ECHINOIDEA. 139 No. 433. Echinobrissus (Nucleolites) cunucularis, Blaiuv. Lower Oolite, Youne, France. No. 424. Echinolampus afl&nis, Desm. Eocene, Vaiie;irard, France. No. 425. G-alerites albogalerus, Lam. This lofty, almost turreted form, with central mouth and marginal anus, is from the Upper Chalk, Kent, England.. No. 426. Hemicidaris intermedia, Fleming. This large, depressed genus belongs to the Cidari- dce with narrow ambulacra. The distinctive feature is the existence of small tubercles on the lower half of the ambulacra. The spines are cylind
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36588965.htmlRMC3ENGN–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
![. College collection of palaeontology. No. 430. Pygaster semisulcatus, Phil. Pea Grit (Lower Oolite), Chrichley Hill. England. No. 431. [789, Cast]. Rhabdocidaris copeoides, Desor. (Cidaris copeoides, Agass.). Three specimens op spines. This Urchin belongs to the Cidaridm having narrow umbulacra. The spines vary very much in size and form on different parts of the test, and at different stages of develop- ment. From the Oxfordian (Middle Oolite), Latrecy, France. No. 432. Scutella disca, Mather. This Amei'ican Clypeastroid is from the Tertiary of Georgia. No. 433. Toxaster Texana, Cretaceous, Stock Photo](https://c8.alamy.com/comp/REHC3A/college-collection-of-palaeontology-no-430-pygaster-semisulcatus-phil-pea-grit-lower-oolite-chrichley-hill-england-no-431-789-cast-rhabdocidaris-copeoides-desor-cidaris-copeoides-agass-three-specimens-op-spines-this-urchin-belongs-to-the-cidaridm-having-narrow-umbulacra-the-spines-vary-very-much-in-size-and-form-on-different-parts-of-the-test-and-at-different-stages-of-develop-ment-from-the-oxfordian-middle-oolite-latrecy-france-no-432-scutella-disca-mather-this-ameiican-clypeastroid-is-from-the-tertiary-of-georgia-no-433-toxaster-texana-cretaceous-REHC3A.jpg ". College collection of palaeontology. No. 430. Pygaster semisulcatus, Phil. Pea Grit (Lower Oolite), Chrichley Hill. England. No. 431. [789, Cast]. Rhabdocidaris copeoides, Desor. (Cidaris copeoides, Agass.). Three specimens op spines. This Urchin belongs to the Cidaridm having narrow umbulacra. The spines vary very much in size and form on different parts of the test, and at different stages of develop- ment. From the Oxfordian (Middle Oolite), Latrecy, France. No. 432. Scutella disca, Mather. This Amei'ican Clypeastroid is from the Tertiary of Georgia. No. 433. Toxaster Texana, Cretaceous, Stock Photo")
. College collection of palaeontology. No. 430. Pygaster semisulcatus, Phil. Pea Grit (Lower Oolite), Chrichley Hill. England. No. 431. [789, Cast]. Rhabdocidaris copeoides, Desor. (Cidaris copeoides, Agass.). Three specimens op spines. This Urchin belongs to the Cidaridm having narrow umbulacra. The spines vary very much in size and form on different parts of the test, and at different stages of develop- ment. From the Oxfordian (Middle Oolite), Latrecy, France. No. 432. Scutella disca, Mather. This Amei'ican Clypeastroid is from the Tertiary of Georgia. No. 433. Toxaster Texana, Cretaceous, Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-no-430-pygaster-semisulcatus-phil-pea-grit-lower-oolite-chrichley-hill-england-no-431-789-cast-rhabdocidaris-copeoides-desor-cidaris-copeoides-agass-three-specimens-op-spines-this-urchin-belongs-to-the-cidaridm-having-narrow-umbulacra-the-spines-vary-very-much-in-size-and-form-on-different-parts-of-the-test-and-at-different-stages-of-develop-ment-from-the-oxfordian-middle-oolite-latrecy-france-no-432-scutella-disca-mather-this-ameiican-clypeastroid-is-from-the-tertiary-of-georgia-no-433-toxaster-texana-cretaceous-image232722654.htmlRMREHC3A–. College collection of palaeontology. No. 430. Pygaster semisulcatus, Phil. Pea Grit (Lower Oolite), Chrichley Hill. England. No. 431. [789, Cast]. Rhabdocidaris copeoides, Desor. (Cidaris copeoides, Agass.). Three specimens op spines. This Urchin belongs to the Cidaridm having narrow umbulacra. The spines vary very much in size and form on different parts of the test, and at different stages of develop- ment. From the Oxfordian (Middle Oolite), Latrecy, France. No. 432. Scutella disca, Mather. This Amei'ican Clypeastroid is from the Tertiary of Georgia. No. 433. Toxaster Texana, Cretaceous,
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36588981.htmlRMC3ENH9–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. This and the next three forms belong to the Trigoniadce, the shell of which is equivalve and trigonal, with the uni- bones directed posteriorly. From the Lower Oolite, (Esch- ingen, Wirtemberg, and now in the Ward Museum, Uni- versity of Rochester. Price, $0.40. No. 680. Trigonia clavellata, Sow. From the Oxford Clay (Middle Oolite), Dives, France, and now in the pri- vate Geological Cabinet of Mr. Ward, Rochester. Price, $0.75. No. 681. Trigonia candata, Agass Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-this-and-the-next-three-forms-belong-to-the-trigoniadce-the-shell-of-which-is-equivalve-and-trigonal-with-the-uni-bones-directed-posteriorly-from-the-lower-oolite-esch-ingen-wirtemberg-and-now-in-the-ward-museum-uni-versity-of-rochester-price-040-no-680-trigonia-clavellata-sow-from-the-oxford-clay-middle-oolite-dives-france-and-now-in-the-pri-vate-geological-cabinet-of-mr-ward-rochester-price-075-no-681-trigonia-candata-agass-image233007860.htmlRMRF2BW8–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. This and the next three forms belong to the Trigoniadce, the shell of which is equivalve and trigonal, with the uni- bones directed posteriorly. From the Lower Oolite, (Esch- ingen, Wirtemberg, and now in the Ward Museum, Uni- versity of Rochester. Price, $0.40. No. 680. Trigonia clavellata, Sow. From the Oxford Clay (Middle Oolite), Dives, France, and now in the pri- vate Geological Cabinet of Mr. Ward, Rochester. Price, $0.75. No. 681. Trigonia candata, Agass
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36588960.htmlRMC3ENGG–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
. Fossil plants : for students of botany and geology . Paleobotany. 72 THE PKESERVATION OF PLANTS AS FOSSILS. [CH. leaf-cushions and leaf-scars of a Lepidodendron. The stem was embedded in soft sand, and as the latter became hard and set, an impression was obtained of the external markings of the Lepidodendron. Decay subsequently removed the substance of the plant.. Fig. 11. Equisetites columnaris Brongn. Prom a specimen in the Woodwardian Museum, Cambridge. ^ nat. size. In fig. 11 some upright stems of a fossil Horse-tail (Equi- setites columnaris) from the Lower Oolite rocks near Scarborough Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fossil-plants-for-students-of-botany-and-geology-paleobotany-72-the-pkeservation-of-plants-as-fossils-ch-leaf-cushions-and-leaf-scars-of-a-lepidodendron-the-stem-was-embedded-in-soft-sand-and-as-the-latter-became-hard-and-set-an-impression-was-obtained-of-the-external-markings-of-the-lepidodendron-decay-subsequently-removed-the-substance-of-the-plant-fig-11-equisetites-columnaris-brongn-prom-a-specimen-in-the-woodwardian-museum-cambridge-nat-size-in-fig-11-some-upright-stems-of-a-fossil-horse-tail-equi-setites-columnaris-from-the-lower-oolite-rocks-near-scarborough-image231994818.htmlRMRDC7N6–. Fossil plants : for students of botany and geology . Paleobotany. 72 THE PKESERVATION OF PLANTS AS FOSSILS. [CH. leaf-cushions and leaf-scars of a Lepidodendron. The stem was embedded in soft sand, and as the latter became hard and set, an impression was obtained of the external markings of the Lepidodendron. Decay subsequently removed the substance of the plant.. Fig. 11. Equisetites columnaris Brongn. Prom a specimen in the Woodwardian Museum, Cambridge. ^ nat. size. In fig. 11 some upright stems of a fossil Horse-tail (Equi- setites columnaris) from the Lower Oolite rocks near Scarborough
Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/stock-photo-sandstone-cliffs-at-burton-bradstock-near-bridport-on-the-jurassic-36588976.htmlRMC3ENH4–Sandstone Cliffs at Burton Bradstock near Bridport on the Jurassic Coast, Dorset England UK.
![. College collection of palaeontology. This elegant form, with the outer mark- ings of the shell visible upon all its whorls, and a double row of spines, belongs to the group " Armati." It is from the Lower Lias, Charmouth, England, and belongs to the Ward Collection, University of Rochester. Diameter, 8. No. 193. [478, CastJ. Ammonites Brongniarti, Sow. This curiously inflated species is from the Lower Oolite, Yeovil, England. Diameter 10. No. 193. [479, Cast]. Ammonites concavus, Sow. This species belongs to the group "Disci." From the Lower Oolite, Bridport, England, and Stock Photo](https://c8.alamy.com/comp/REH26H/college-collection-of-palaeontology-this-elegant-form-with-the-outer-mark-ings-of-the-shell-visible-upon-all-its-whorls-and-a-double-row-of-spines-belongs-to-the-group-quot-armatiquot-it-is-from-the-lower-lias-charmouth-england-and-belongs-to-the-ward-collection-university-of-rochester-diameter-8-no-193-478-castj-ammonites-brongniarti-sow-this-curiously-inflated-species-is-from-the-lower-oolite-yeovil-england-diameter-10-no-193-479-cast-ammonites-concavus-sow-this-species-belongs-to-the-group-quotdisciquot-from-the-lower-oolite-bridport-england-and-REH26H.jpg ". College collection of palaeontology. This elegant form, with the outer mark- ings of the shell visible upon all its whorls, and a double row of spines, belongs to the group " Armati." It is from the Lower Lias, Charmouth, England, and belongs to the Ward Collection, University of Rochester. Diameter, 8. No. 193. [478, CastJ. Ammonites Brongniarti, Sow. This curiously inflated species is from the Lower Oolite, Yeovil, England. Diameter 10. No. 193. [479, Cast]. Ammonites concavus, Sow. This species belongs to the group "Disci." From the Lower Oolite, Bridport, England, and Stock Photo")
. College collection of palaeontology. This elegant form, with the outer mark- ings of the shell visible upon all its whorls, and a double row of spines, belongs to the group " Armati." It is from the Lower Lias, Charmouth, England, and belongs to the Ward Collection, University of Rochester. Diameter, 8. No. 193. [478, CastJ. Ammonites Brongniarti, Sow. This curiously inflated species is from the Lower Oolite, Yeovil, England. Diameter 10. No. 193. [479, Cast]. Ammonites concavus, Sow. This species belongs to the group "Disci." From the Lower Oolite, Bridport, England, and Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-this-elegant-form-with-the-outer-mark-ings-of-the-shell-visible-upon-all-its-whorls-and-a-double-row-of-spines-belongs-to-the-group-quot-armatiquot-it-is-from-the-lower-lias-charmouth-england-and-belongs-to-the-ward-collection-university-of-rochester-diameter-8-no-193-478-castj-ammonites-brongniarti-sow-this-curiously-inflated-species-is-from-the-lower-oolite-yeovil-england-diameter-10-no-193-479-cast-ammonites-concavus-sow-this-species-belongs-to-the-group-quotdisciquot-from-the-lower-oolite-bridport-england-and-image232714905.htmlRMREH26H–. College collection of palaeontology. This elegant form, with the outer mark- ings of the shell visible upon all its whorls, and a double row of spines, belongs to the group " Armati." It is from the Lower Lias, Charmouth, England, and belongs to the Ward Collection, University of Rochester. Diameter, 8. No. 193. [478, CastJ. Ammonites Brongniarti, Sow. This curiously inflated species is from the Lower Oolite, Yeovil, England. Diameter 10. No. 193. [479, Cast]. Ammonites concavus, Sow. This species belongs to the group "Disci." From the Lower Oolite, Bridport, England, and
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 146 MOLLUSCA. No. 679. Trigonia costata, Park.. This and the next three forms belong to the Trigoniadce, the shell of which is equivalve and trigonal, with the uni- bones directed posteriorly. From the Lower Oolite, (Esch- ingen, Wirtemberg, and now in the Ward Museum, Uni- versity of Rochester. Price, $0.40. No. 680. Trigonia clavellata, Sow. From the Oxford Clay (Middle Oolite), Dives, France, and now in the pri- vate Geological Cabinet of Mr. Ward, Rochester Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-146-mollusca-no-679-trigonia-costata-park-this-and-the-next-three-forms-belong-to-the-trigoniadce-the-shell-of-which-is-equivalve-and-trigonal-with-the-uni-bones-directed-posteriorly-from-the-lower-oolite-esch-ingen-wirtemberg-and-now-in-the-ward-museum-uni-versity-of-rochester-price-040-no-680-trigonia-clavellata-sow-from-the-oxford-clay-middle-oolite-dives-france-and-now-in-the-pri-vate-geological-cabinet-of-mr-ward-rochester-image233180542.htmlRMRFA84E–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 146 MOLLUSCA. No. 679. Trigonia costata, Park.. This and the next three forms belong to the Trigoniadce, the shell of which is equivalve and trigonal, with the uni- bones directed posteriorly. From the Lower Oolite, (Esch- ingen, Wirtemberg, and now in the Ward Museum, Uni- versity of Rochester. Price, $0.40. No. 680. Trigonia clavellata, Sow. From the Oxford Clay (Middle Oolite), Dives, France, and now in the pri- vate Geological Cabinet of Mr. Ward, Rochester
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. This and the next three forms belong to the Trigoniadce, the shell of which is equivalve and trigonal, with the uni- bones directed posteriorly. From the Lower Oolite, (Esch- ingen, Wirtemberg, and now in the Ward Museum, Uni- versity of Rochester. Price, $0.40. No. 680. Trigonia clavellata, Sow. From the Oxford Clay (Middle Oolite), Dives, France, and now in the pri- vate Geological Cabinet of Mr. Ward, Rochester. Price, $0.75. No. 681. Trigonia candata, Agass Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-this-and-the-next-three-forms-belong-to-the-trigoniadce-the-shell-of-which-is-equivalve-and-trigonal-with-the-uni-bones-directed-posteriorly-from-the-lower-oolite-esch-ingen-wirtemberg-and-now-in-the-ward-museum-uni-versity-of-rochester-price-040-no-680-trigonia-clavellata-sow-from-the-oxford-clay-middle-oolite-dives-france-and-now-in-the-pri-vate-geological-cabinet-of-mr-ward-rochester-price-075-no-681-trigonia-candata-agass-image233180537.htmlRMRFA849–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. This and the next three forms belong to the Trigoniadce, the shell of which is equivalve and trigonal, with the uni- bones directed posteriorly. From the Lower Oolite, (Esch- ingen, Wirtemberg, and now in the Ward Museum, Uni- versity of Rochester. Price, $0.40. No. 680. Trigonia clavellata, Sow. From the Oxford Clay (Middle Oolite), Dives, France, and now in the pri- vate Geological Cabinet of Mr. Ward, Rochester. Price, $0.75. No. 681. Trigonia candata, Agass
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 146 MOLLUSCA. No. 679. Trigonia costata, Park.. This and the next three forms belong to the Trigoniadce, the shell of which is equivalve and trigonal, with the uni- bones directed posteriorly. From the Lower Oolite, (Esch- ingen, Wirtemberg, and now in the Ward Museum, Uni- versity of Rochester. Price, $0.40. No. 680. Trigonia clavellata, Sow. From the Oxford Clay (Middle Oolite), Dives, France, and now in the pri- vate Geological Cabinet of Mr. Ward, Rochester Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-146-mollusca-no-679-trigonia-costata-park-this-and-the-next-three-forms-belong-to-the-trigoniadce-the-shell-of-which-is-equivalve-and-trigonal-with-the-uni-bones-directed-posteriorly-from-the-lower-oolite-esch-ingen-wirtemberg-and-now-in-the-ward-museum-uni-versity-of-rochester-price-040-no-680-trigonia-clavellata-sow-from-the-oxford-clay-middle-oolite-dives-france-and-now-in-the-pri-vate-geological-cabinet-of-mr-ward-rochester-image233007865.htmlRMRF2BWD–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 146 MOLLUSCA. No. 679. Trigonia costata, Park.. This and the next three forms belong to the Trigoniadce, the shell of which is equivalve and trigonal, with the uni- bones directed posteriorly. From the Lower Oolite, (Esch- ingen, Wirtemberg, and now in the Ward Museum, Uni- versity of Rochester. Price, $0.40. No. 680. Trigonia clavellata, Sow. From the Oxford Clay (Middle Oolite), Dives, France, and now in the pri- vate Geological Cabinet of Mr. Ward, Rochester
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 150 MOLLUSCA. No. 716. Terebratula intermedia, Sow. From the Lower Oolite of Calvados, France. Original in the Ward Museum of the University of Rochester. No. 717. Terebratula Lycetti, Dav. From the Lias of Ilminster, England. No. 718. Terebratula Mariae, D'Orb. From the Lias of Calvados, France. No. 719. Terebratula Moorei, Dav. From the Lias of Petherton, England. No. 720. Terebratula numismalis, Lam. From the Lias of Calvados, France. No. 721. Terebratula pe Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-150-mollusca-no-716-terebratula-intermedia-sow-from-the-lower-oolite-of-calvados-france-original-in-the-ward-museum-of-the-university-of-rochester-no-717-terebratula-lycetti-dav-from-the-lias-of-ilminster-england-no-718-terebratula-mariae-dorb-from-the-lias-of-calvados-france-no-719-terebratula-moorei-dav-from-the-lias-of-petherton-england-no-720-terebratula-numismalis-lam-from-the-lias-of-calvados-france-no-721-terebratula-pe-image233007843.htmlRMRF2BTK–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. 150 MOLLUSCA. No. 716. Terebratula intermedia, Sow. From the Lower Oolite of Calvados, France. Original in the Ward Museum of the University of Rochester. No. 717. Terebratula Lycetti, Dav. From the Lias of Ilminster, England. No. 718. Terebratula Mariae, D'Orb. From the Lias of Calvados, France. No. 719. Terebratula Moorei, Dav. From the Lias of Petherton, England. No. 720. Terebratula numismalis, Lam. From the Lias of Calvados, France. No. 721. Terebratula pe
![. Fossil plants : for students of botany and geology . Paleobotany. XL] GINKGOITES 21 acuminata^. A deeply divided obcuiieate leaf, only 2—4 cm. broad, is figured by Dr Stopes^ from Jurassic strata (Lower Oolite) on the Sutherland coast at Brora (fig. 635, J). The specimen shown in fig. 633, also from the Sutherland coast, a few miles north of Brora and of Kimeridgian age, illustrates the type of leaf that may be conveniently referred to Ginkgoites digitata. var. Huttoni^. Heer's Jurassic species. Ginkgo Jaccardi^, from Switzerland is almost certainly Ginkgoites digitata. Arctic regions and no Stock Photo](https://c8.alamy.com/comp/RDBCNG/fossil-plants-for-students-of-botany-and-geology-paleobotany-xl-ginkgoites-21-acuminata-a-deeply-divided-obcuiieate-leaf-only-24-cm-broad-is-figured-by-dr-stopes-from-jurassic-strata-lower-oolite-on-the-sutherland-coast-at-brora-fig-635-j-the-specimen-shown-in-fig-633-also-from-the-sutherland-coast-a-few-miles-north-of-brora-and-of-kimeridgian-age-illustrates-the-type-of-leaf-that-may-be-conveniently-referred-to-ginkgoites-digitata-var-huttoni-heers-jurassic-species-ginkgo-jaccardi-from-switzerland-is-almost-certainly-ginkgoites-digitata-arctic-regions-and-no-RDBCNG.jpg ". Fossil plants : for students of botany and geology . Paleobotany. XL] GINKGOITES 21 acuminata^. A deeply divided obcuiieate leaf, only 2—4 cm. broad, is figured by Dr Stopes^ from Jurassic strata (Lower Oolite) on the Sutherland coast at Brora (fig. 635, J). The specimen shown in fig. 633, also from the Sutherland coast, a few miles north of Brora and of Kimeridgian age, illustrates the type of leaf that may be conveniently referred to Ginkgoites digitata. var. Huttoni^. Heer's Jurassic species. Ginkgo Jaccardi^, from Switzerland is almost certainly Ginkgoites digitata. Arctic regions and no Stock Photo")
. Fossil plants : for students of botany and geology . Paleobotany. XL] GINKGOITES 21 acuminata^. A deeply divided obcuiieate leaf, only 2—4 cm. broad, is figured by Dr Stopes^ from Jurassic strata (Lower Oolite) on the Sutherland coast at Brora (fig. 635, J). The specimen shown in fig. 633, also from the Sutherland coast, a few miles north of Brora and of Kimeridgian age, illustrates the type of leaf that may be conveniently referred to Ginkgoites digitata. var. Huttoni^. Heer's Jurassic species. Ginkgo Jaccardi^, from Switzerland is almost certainly Ginkgoites digitata. Arctic regions and no Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/fossil-plants-for-students-of-botany-and-geology-paleobotany-xl-ginkgoites-21-acuminata-a-deeply-divided-obcuiieate-leaf-only-24-cm-broad-is-figured-by-dr-stopes-from-jurassic-strata-lower-oolite-on-the-sutherland-coast-at-brora-fig-635-j-the-specimen-shown-in-fig-633-also-from-the-sutherland-coast-a-few-miles-north-of-brora-and-of-kimeridgian-age-illustrates-the-type-of-leaf-that-may-be-conveniently-referred-to-ginkgoites-digitata-var-huttoni-heers-jurassic-species-ginkgo-jaccardi-from-switzerland-is-almost-certainly-ginkgoites-digitata-arctic-regions-and-no-image231976796.htmlRMRDBCNG–. Fossil plants : for students of botany and geology . Paleobotany. XL] GINKGOITES 21 acuminata^. A deeply divided obcuiieate leaf, only 2—4 cm. broad, is figured by Dr Stopes^ from Jurassic strata (Lower Oolite) on the Sutherland coast at Brora (fig. 635, J). The specimen shown in fig. 633, also from the Sutherland coast, a few miles north of Brora and of Kimeridgian age, illustrates the type of leaf that may be conveniently referred to Ginkgoites digitata. var. Huttoni^. Heer's Jurassic species. Ginkgo Jaccardi^, from Switzerland is almost certainly Ginkgoites digitata. Arctic regions and no
![. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. CEPHALOPODA. 125 No. 517. Ammonites Martinsii, D'Orb. From the Lower Oolite, Bridport, England, and now in the private Geologi- cal Cabinet of Mr. Ward, Kochester. Diameter, 10in. Price, $1.50. No. 518. Ammonites Millesianus, D'Orb. From the Lower Chalk (Cretaceous), Rouen, France. Diameter, 8. Price, $1.50. No. 519. Ammonites modiolaris, Luid. ,^--^""'•" Also known as A sublmvis, Sow. From the Kelloway Rock, Wiltshire, England, and now in the Wa Stock Photo](https://c8.alamy.com/comp/RF2C2M/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-cephalopoda-125-no-517-ammonites-martinsii-dorb-from-the-lower-oolite-bridport-england-and-now-in-the-private-geologi-cal-cabinet-of-mr-ward-kochester-diameter-10in-price-150-no-518-ammonites-millesianus-dorb-from-the-lower-chalk-cretaceous-rouen-france-diameter-8-price-150-no-519-ammonites-modiolaris-luid-quotquotquot-also-known-as-a-sublmvis-sow-from-the-kelloway-rock-wiltshire-england-and-now-in-the-wa-RF2C2M.jpg ". Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. CEPHALOPODA. 125 No. 517. Ammonites Martinsii, D'Orb. From the Lower Oolite, Bridport, England, and now in the private Geologi- cal Cabinet of Mr. Ward, Kochester. Diameter, 10in. Price, $1.50. No. 518. Ammonites Millesianus, D'Orb. From the Lower Chalk (Cretaceous), Rouen, France. Diameter, 8. Price, $1.50. No. 519. Ammonites modiolaris, Luid. ,^--^""'•" Also known as A sublmvis, Sow. From the Kelloway Rock, Wiltshire, England, and now in the Wa Stock Photo")
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. CEPHALOPODA. 125 No. 517. Ammonites Martinsii, D'Orb. From the Lower Oolite, Bridport, England, and now in the private Geologi- cal Cabinet of Mr. Ward, Kochester. Diameter, 10in. Price, $1.50. No. 518. Ammonites Millesianus, D'Orb. From the Lower Chalk (Cretaceous), Rouen, France. Diameter, 8. Price, $1.50. No. 519. Ammonites modiolaris, Luid. ,^--^""'•" Also known as A sublmvis, Sow. From the Kelloway Rock, Wiltshire, England, and now in the Wa Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-cephalopoda-125-no-517-ammonites-martinsii-dorb-from-the-lower-oolite-bridport-england-and-now-in-the-private-geologi-cal-cabinet-of-mr-ward-kochester-diameter-10in-price-150-no-518-ammonites-millesianus-dorb-from-the-lower-chalk-cretaceous-rouen-france-diameter-8-price-150-no-519-ammonites-modiolaris-luid-quotquotquot-also-known-as-a-sublmvis-sow-from-the-kelloway-rock-wiltshire-england-and-now-in-the-wa-image233008012.htmlRMRF2C2M–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. CEPHALOPODA. 125 No. 517. Ammonites Martinsii, D'Orb. From the Lower Oolite, Bridport, England, and now in the private Geologi- cal Cabinet of Mr. Ward, Kochester. Diameter, 10in. Price, $1.50. No. 518. Ammonites Millesianus, D'Orb. From the Lower Chalk (Cretaceous), Rouen, France. Diameter, 8. Price, $1.50. No. 519. Ammonites modiolaris, Luid. ,^--^""'•" Also known as A sublmvis, Sow. From the Kelloway Rock, Wiltshire, England, and now in the Wa
![. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. CEPHALOPODA. 125 No. 517. Ammonites Martinsii, D'Orb. From the Lower Oolite, Bridport, England, and now in the private Geologi- cal Cabinet of Mr. Ward, Kochester. Diameter, 10in. Price, $1.50. No. 518. Ammonites Millesianus, D'Orb. From the Lower Chalk (Cretaceous), Rouen, France. Diameter, 8. Price, $1.50. No. 519. Ammonites modiolaris, Luid. ,^--^""'•" Also known as A sublmvis, Sow. From the Kelloway Rock, Wiltshire, England, and now in the Wa Stock Photo](https://c8.alamy.com/comp/RFA8BX/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-cephalopoda-125-no-517-ammonites-martinsii-dorb-from-the-lower-oolite-bridport-england-and-now-in-the-private-geologi-cal-cabinet-of-mr-ward-kochester-diameter-10in-price-150-no-518-ammonites-millesianus-dorb-from-the-lower-chalk-cretaceous-rouen-france-diameter-8-price-150-no-519-ammonites-modiolaris-luid-quotquotquot-also-known-as-a-sublmvis-sow-from-the-kelloway-rock-wiltshire-england-and-now-in-the-wa-RFA8BX.jpg ". Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. CEPHALOPODA. 125 No. 517. Ammonites Martinsii, D'Orb. From the Lower Oolite, Bridport, England, and now in the private Geologi- cal Cabinet of Mr. Ward, Kochester. Diameter, 10in. Price, $1.50. No. 518. Ammonites Millesianus, D'Orb. From the Lower Chalk (Cretaceous), Rouen, France. Diameter, 8. Price, $1.50. No. 519. Ammonites modiolaris, Luid. ,^--^""'•" Also known as A sublmvis, Sow. From the Kelloway Rock, Wiltshire, England, and now in the Wa Stock Photo")
. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. CEPHALOPODA. 125 No. 517. Ammonites Martinsii, D'Orb. From the Lower Oolite, Bridport, England, and now in the private Geologi- cal Cabinet of Mr. Ward, Kochester. Diameter, 10in. Price, $1.50. No. 518. Ammonites Millesianus, D'Orb. From the Lower Chalk (Cretaceous), Rouen, France. Diameter, 8. Price, $1.50. No. 519. Ammonites modiolaris, Luid. ,^--^""'•" Also known as A sublmvis, Sow. From the Kelloway Rock, Wiltshire, England, and now in the Wa Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/catalogue-of-casts-of-fossils-from-the-principal-museums-of-europe-and-america-with-short-descriptions-and-illustrations-fossils-cephalopoda-125-no-517-ammonites-martinsii-dorb-from-the-lower-oolite-bridport-england-and-now-in-the-private-geologi-cal-cabinet-of-mr-ward-kochester-diameter-10in-price-150-no-518-ammonites-millesianus-dorb-from-the-lower-chalk-cretaceous-rouen-france-diameter-8-price-150-no-519-ammonites-modiolaris-luid-quotquotquot-also-known-as-a-sublmvis-sow-from-the-kelloway-rock-wiltshire-england-and-now-in-the-wa-image233180750.htmlRMRFA8BX–. Catalogue of casts of fossils, from the principal museums of Europe and America, with short descriptions and illustrations. Fossils. CEPHALOPODA. 125 No. 517. Ammonites Martinsii, D'Orb. From the Lower Oolite, Bridport, England, and now in the private Geologi- cal Cabinet of Mr. Ward, Kochester. Diameter, 10in. Price, $1.50. No. 518. Ammonites Millesianus, D'Orb. From the Lower Chalk (Cretaceous), Rouen, France. Diameter, 8. Price, $1.50. No. 519. Ammonites modiolaris, Luid. ,^--^""'•" Also known as A sublmvis, Sow. From the Kelloway Rock, Wiltshire, England, and now in the Wa
. College collection of palaeontology. BRACHIOPODA. 127 No. 356. Terebratula semiglobosa, Sow. Chalk (Upper Cretaceous), Roueu, France. No. 357. Terebratula biplicata, Defr. Upper Greensand, Cambridge, Euglaud. No. 358. Terebratula sphaeroidalis, Sow. Fuller's Earth, Oolite, Noyen, France. No. 359. Terebratella umbonella, Lamk. Lower Oolite, Calvados, France. No. 360. Terebratula gregaria, Suess.' Lower Lias, Hindelang, Bavaria. No. 361. Leptocoelia hemispherica, Sow. A mass of rock composed entirely of this shell. From the Clinton Group, Rochester, N. Y. No. 362. Rensselaeria ovoides, Eaton. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-brachiopoda-127-no-356-terebratula-semiglobosa-sow-chalk-upper-cretaceous-roueu-france-no-357-terebratula-biplicata-defr-upper-greensand-cambridge-euglaud-no-358-terebratula-sphaeroidalis-sow-fullers-earth-oolite-noyen-france-no-359-terebratella-umbonella-lamk-lower-oolite-calvados-france-no-360-terebratula-gregaria-suess-lower-lias-hindelang-bavaria-no-361-leptocoelia-hemispherica-sow-a-mass-of-rock-composed-entirely-of-this-shell-from-the-clinton-group-rochester-n-y-no-362-rensselaeria-ovoides-eaton-image232722888.htmlRMREHCBM–. College collection of palaeontology. BRACHIOPODA. 127 No. 356. Terebratula semiglobosa, Sow. Chalk (Upper Cretaceous), Roueu, France. No. 357. Terebratula biplicata, Defr. Upper Greensand, Cambridge, Euglaud. No. 358. Terebratula sphaeroidalis, Sow. Fuller's Earth, Oolite, Noyen, France. No. 359. Terebratella umbonella, Lamk. Lower Oolite, Calvados, France. No. 360. Terebratula gregaria, Suess.' Lower Lias, Hindelang, Bavaria. No. 361. Leptocoelia hemispherica, Sow. A mass of rock composed entirely of this shell. From the Clinton Group, Rochester, N. Y. No. 362. Rensselaeria ovoides, Eaton.
![. College collection of palaeontology. ACROGENS. 169 ISTo. 546. Stigmaria ficoides, Brngt. This geuus may represent the subterrauean stems and roots of Sigilhira and other plants, or perhaps some forms may be the stems of floating plants. Coal Measures, Scranton, Pa. No. 547. [1326, Cast]. Stigmaria ficoides, Brugt. Coal Measures, South Joggins, Nova Scotia. Size, 10 X 5. FAMILY EaUISETACE^. No. 548. Ancylogonatum carbonacium, Rom. Lower Oolite, Whitby, England. No. 549. Annularia longifolia, Brngt. Coal Measures, Mazou Creek, Grundy Co., 111. No. 550. [1329, Cast]. Calamites. The family—Equis Stock Photo](https://c8.alamy.com/comp/REHBM5/college-collection-of-palaeontology-acrogens-169-isto-546-stigmaria-ficoides-brngt-this-geuus-may-represent-the-subterrauean-stems-and-roots-of-sigilhira-and-other-plants-or-perhaps-some-forms-may-be-the-stems-of-floating-plants-coal-measures-scranton-pa-no-547-1326-cast-stigmaria-ficoides-brugt-coal-measures-south-joggins-nova-scotia-size-10-x-5-family-eauisetace-no-548-ancylogonatum-carbonacium-rom-lower-oolite-whitby-england-no-549-annularia-longifolia-brngt-coal-measures-mazou-creek-grundy-co-111-no-550-1329-cast-calamites-the-familyequis-REHBM5.jpg ". College collection of palaeontology. ACROGENS. 169 ISTo. 546. Stigmaria ficoides, Brngt. This geuus may represent the subterrauean stems and roots of Sigilhira and other plants, or perhaps some forms may be the stems of floating plants. Coal Measures, Scranton, Pa. No. 547. [1326, Cast]. Stigmaria ficoides, Brugt. Coal Measures, South Joggins, Nova Scotia. Size, 10 X 5. FAMILY EaUISETACE^. No. 548. Ancylogonatum carbonacium, Rom. Lower Oolite, Whitby, England. No. 549. Annularia longifolia, Brngt. Coal Measures, Mazou Creek, Grundy Co., 111. No. 550. [1329, Cast]. Calamites. The family—Equis Stock Photo")
. College collection of palaeontology. ACROGENS. 169 ISTo. 546. Stigmaria ficoides, Brngt. This geuus may represent the subterrauean stems and roots of Sigilhira and other plants, or perhaps some forms may be the stems of floating plants. Coal Measures, Scranton, Pa. No. 547. [1326, Cast]. Stigmaria ficoides, Brugt. Coal Measures, South Joggins, Nova Scotia. Size, 10 X 5. FAMILY EaUISETACE^. No. 548. Ancylogonatum carbonacium, Rom. Lower Oolite, Whitby, England. No. 549. Annularia longifolia, Brngt. Coal Measures, Mazou Creek, Grundy Co., 111. No. 550. [1329, Cast]. Calamites. The family—Equis Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/college-collection-of-palaeontology-acrogens-169-isto-546-stigmaria-ficoides-brngt-this-geuus-may-represent-the-subterrauean-stems-and-roots-of-sigilhira-and-other-plants-or-perhaps-some-forms-may-be-the-stems-of-floating-plants-coal-measures-scranton-pa-no-547-1326-cast-stigmaria-ficoides-brugt-coal-measures-south-joggins-nova-scotia-size-10-x-5-family-eauisetace-no-548-ancylogonatum-carbonacium-rom-lower-oolite-whitby-england-no-549-annularia-longifolia-brngt-coal-measures-mazou-creek-grundy-co-111-no-550-1329-cast-calamites-the-familyequis-image232722341.htmlRMREHBM5–. College collection of palaeontology. ACROGENS. 169 ISTo. 546. Stigmaria ficoides, Brngt. This geuus may represent the subterrauean stems and roots of Sigilhira and other plants, or perhaps some forms may be the stems of floating plants. Coal Measures, Scranton, Pa. No. 547. [1326, Cast]. Stigmaria ficoides, Brugt. Coal Measures, South Joggins, Nova Scotia. Size, 10 X 5. FAMILY EaUISETACE^. No. 548. Ancylogonatum carbonacium, Rom. Lower Oolite, Whitby, England. No. 549. Annularia longifolia, Brngt. Coal Measures, Mazou Creek, Grundy Co., 111. No. 550. [1329, Cast]. Calamites. The family—Equis
. Geology and mineralogy considered with reference to natural theology. 9 * N N. /» fl Lower Jaws and Teeth of Didelphysfrom the Oolite of Stonesfield, Oxon, Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/geology-and-mineralogy-considered-with-reference-to-natural-theology-9-n-n-fl-lower-jaws-and-teeth-of-didelphysfrom-the-oolite-of-stonesfield-oxon-image336827732.htmlRM2AFYR5T–. Geology and mineralogy considered with reference to natural theology. 9 * N N. /» fl Lower Jaws and Teeth of Didelphysfrom the Oolite of Stonesfield, Oxon,
. Geology and mineralogy considered with reference to natural theology. /» fl Lower Jaws and Teeth of Didelphysfrom the Oolite of Stonesfield, Oxon,. 1 Lower Jaw of Dinotherium giganteum. <2 Lower and part of upper Jaw of Dinotherium medium. 3 Molar Teeth of Dinotherium medium. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/geology-and-mineralogy-considered-with-reference-to-natural-theology-fl-lower-jaws-and-teeth-of-didelphysfrom-the-oolite-of-stonesfield-oxon-1-lower-jaw-of-dinotherium-giganteum-lt2-lower-and-part-of-upper-jaw-of-dinotherium-medium-3-molar-teeth-of-dinotherium-medium-image336827553.htmlRM2AFYPYD–. Geology and mineralogy considered with reference to natural theology. /» fl Lower Jaws and Teeth of Didelphysfrom the Oolite of Stonesfield, Oxon,. 1 Lower Jaw of Dinotherium giganteum. <2 Lower and part of upper Jaw of Dinotherium medium. 3 Molar Teeth of Dinotherium medium.
The Tanganyika problem; an account of the researches undertaken concerning the existence of marine animals in Central Africa . Chytra kirkii, upper, compared with a marine Jurassic onitstus, lower. by an Oolitic fossil genus Purpuroidia, from which it isvery difficult, if not impossible, on conchological grounds,to distinguish it. From these comparisons it will be seenthat we have numerous genera of gastropods belonging tothe halolimnic series of Tanganyika, which are concho-logically indistinguishable from an equal number character-istic of the Oolite seas, and it will certainly be admittedth Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-tanganyika-problem-an-account-of-the-researches-undertaken-concerning-the-existence-of-marine-animals-in-central-africa-chytra-kirkii-upper-compared-with-a-marine-jurassic-onitstus-lower-by-an-oolitic-fossil-genus-purpuroidia-from-which-it-isvery-difficult-if-not-impossible-on-conchological-groundsto-distinguish-it-from-these-comparisons-it-will-be-seenthat-we-have-numerous-genera-of-gastropods-belonging-tothe-halolimnic-series-of-tanganyika-which-are-concho-logically-indistinguishable-from-an-equal-number-character-istic-of-the-oolite-seas-and-it-will-certainly-be-admittedth-image339088853.htmlRM2AKJR85–The Tanganyika problem; an account of the researches undertaken concerning the existence of marine animals in Central Africa . Chytra kirkii, upper, compared with a marine Jurassic onitstus, lower. by an Oolitic fossil genus Purpuroidia, from which it isvery difficult, if not impossible, on conchological grounds,to distinguish it. From these comparisons it will be seenthat we have numerous genera of gastropods belonging tothe halolimnic series of Tanganyika, which are concho-logically indistinguishable from an equal number character-istic of the Oolite seas, and it will certainly be admittedth
. Elements of astronomy: accompanied with numerous illustrations, a colored representation of the solar, stellar, and nebular spectra, and celestial charts of the northern and the southern hemisphere. s as follows:— Cainozoic, or Tertiary Upper Lowerf UpperMesozoic, or Secondary : < t ower Palaeozoic, or Primary: Upper Lower ( Alluvium. Drift.( Crag.Eocene. Cretaceous.Oolite.Lias.Trias. Permian. Carboniferous. Devonian. Silurian. Cambrian. Laurentian. 195. That these beds have been deposited by water,and principally by the sea, is proved by two facts: First,that in their formation they res Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-astronomy-accompanied-with-numerous-illustrations-a-colored-representation-of-the-solar-stellar-and-nebular-spectra-and-celestial-charts-of-the-northern-and-the-southern-hemisphere-s-as-follows-cainozoic-or-tertiary-upper-lowerf-uppermesozoic-or-secondary-lt-t-ower-palaeozoic-or-primary-upper-lower-alluvium-drift-crageocene-cretaceousooliteliastrias-permian-carboniferous-devonian-silurian-cambrian-laurentian-195-that-these-beds-have-been-deposited-by-waterand-principally-by-the-sea-is-proved-by-two-facts-firstthat-in-their-formation-they-res-image336725891.htmlRM2AFR58K–. Elements of astronomy: accompanied with numerous illustrations, a colored representation of the solar, stellar, and nebular spectra, and celestial charts of the northern and the southern hemisphere. s as follows:— Cainozoic, or Tertiary Upper Lowerf UpperMesozoic, or Secondary : < t ower Palaeozoic, or Primary: Upper Lower ( Alluvium. Drift.( Crag.Eocene. Cretaceous.Oolite.Lias.Trias. Permian. Carboniferous. Devonian. Silurian. Cambrian. Laurentian. 195. That these beds have been deposited by water,and principally by the sea, is proved by two facts: First,that in their formation they res
. Geology of parts of Wiltshire and Gloucestershire, (sheet 34). , and in the deep cuttings of the Great WesternRailway in the Golden Valley. The Inferior Oolite frequentlyforms tabulated spurs bounded by abrupt banks which areplanted with beech trees and pines; of such there are goodexamples in Slaughterford Valley. The following subdivisions jnay be observed in this district,and can be distinguished both by lithological and fossilcharacters:— Inferior Oolite. Rodborough Common. Upper ragstone. (Clypeus grit.) Coarse rubbly white oolite, withTerebratula globata, Clypeus, Serpula . Lower rag Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/geology-of-parts-of-wiltshire-and-gloucestershire-sheet-34-and-in-the-deep-cuttings-of-the-great-westernrailway-in-the-golden-valley-the-inferior-oolite-frequentlyforms-tabulated-spurs-bounded-by-abrupt-banks-which-areplanted-with-beech-trees-and-pines-of-such-there-are-goodexamples-in-slaughterford-valley-the-following-subdivisions-jnay-be-observed-in-this-districtand-can-be-distinguished-both-by-lithological-and-fossilcharacters-inferior-oolite-rodborough-common-upper-ragstone-clypeus-grit-coarse-rubbly-white-oolite-withterebratula-globata-clypeus-serpula-lower-rag-image337046573.htmlRM2AG9P9H–. Geology of parts of Wiltshire and Gloucestershire, (sheet 34). , and in the deep cuttings of the Great WesternRailway in the Golden Valley. The Inferior Oolite frequentlyforms tabulated spurs bounded by abrupt banks which areplanted with beech trees and pines; of such there are goodexamples in Slaughterford Valley. The following subdivisions jnay be observed in this district,and can be distinguished both by lithological and fossilcharacters:— Inferior Oolite. Rodborough Common. Upper ragstone. (Clypeus grit.) Coarse rubbly white oolite, withTerebratula globata, Clypeus, Serpula . Lower rag
The deposits of the useful minerals & rocks; their origin, form, and content . pharosideritic clay-ironstone ofthe Upper Lias and Lower Dogger, on the south slope of the range ; (2) the 1020 ORE-DEPOSITS clayey iron oolite seam in the hanging-wall of the Macrocephalus sandstone—Upper Dogger—west of the Porta ; and (3) the oolitic haematite in theCoral Rag, east of the Porta. 1. The clay-ironstone nodules of the Upper Lias form several bedsof variable thickness lying one above the other; one sample contained31-5 per cent of iron. ^ These deposits are at present of no economicimportance. 2. Imme Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-deposits-of-the-useful-minerals-rocks-their-origin-form-and-content-pharosideritic-clay-ironstone-ofthe-upper-lias-and-lower-dogger-on-the-south-slope-of-the-range-2-the-1020-ore-deposits-clayey-iron-oolite-seam-in-the-hanging-wall-of-the-macrocephalus-sandstoneupper-doggerwest-of-the-porta-and-3-the-oolitic-haematite-in-thecoral-rag-east-of-the-porta-1-the-clay-ironstone-nodules-of-the-upper-lias-form-several-bedsof-variable-thickness-lying-one-above-the-other-one-sample-contained31-5-per-cent-of-iron-these-deposits-are-at-present-of-no-economicimportance-2-imme-image340215673.htmlRM2ANE4FN–The deposits of the useful minerals & rocks; their origin, form, and content . pharosideritic clay-ironstone ofthe Upper Lias and Lower Dogger, on the south slope of the range ; (2) the 1020 ORE-DEPOSITS clayey iron oolite seam in the hanging-wall of the Macrocephalus sandstone—Upper Dogger—west of the Porta ; and (3) the oolitic haematite in theCoral Rag, east of the Porta. 1. The clay-ironstone nodules of the Upper Lias form several bedsof variable thickness lying one above the other; one sample contained31-5 per cent of iron. ^ These deposits are at present of no economicimportance. 2. Imme
. Annual report of the regents of the university of the state of New York on the condition of the State Cabinet of Natural History and the historical and antiquarian collection annexed thereto. No. 4. Apiocrinvs parldnsoni,^ Pear Encrinite. Speci-men with Caljx, stem and root complete. Great Oolite: Hampton, England. IG.. No. 5. Ancyloceras {Scaphiies) gigas.^^ Afall-grown and unusually perfectspecimen. , Lower Grseusand: Atherfield, Isle of Wight,Kn glands Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annual-report-of-the-regents-of-the-university-of-the-state-of-new-york-on-the-condition-of-the-state-cabinet-of-natural-history-and-the-historical-and-antiquarian-collection-annexed-thereto-no-4-apiocrinvs-parldnsoni-pear-encrinite-speci-men-with-caljx-stem-and-root-complete-great-oolite-hampton-england-ig-no-5-ancyloceras-scaphiies-gigas-afall-grown-and-unusually-perfectspecimen-lower-grseusand-atherfield-isle-of-wightkn-glands-image370398260.htmlRM2CEH2N8–. Annual report of the regents of the university of the state of New York on the condition of the State Cabinet of Natural History and the historical and antiquarian collection annexed thereto. No. 4. Apiocrinvs parldnsoni,^ Pear Encrinite. Speci-men with Caljx, stem and root complete. Great Oolite: Hampton, England. IG.. No. 5. Ancyloceras {Scaphiies) gigas.^^ Afall-grown and unusually perfectspecimen. , Lower Grseusand: Atherfield, Isle of Wight,Kn glands
. The Tanganyika problem; an account of the researches undertaken concerning the existence of marine animals in Central Africa . Chytra kirkii, upper, compared with a marine Jurassic toiiislits, lower. by an Oolitic fossil genus Purpuroidia, from which it isvery difficult, if not impossible, on conchological grounds,to distinguish it. From these comparisons it will be seenthat we have numerous genera of gastropods belonging tothe halolimnic series of Tanganyika, which are concho-logically indistinguishable from an equal number character-istic of the Oolite seas, and it will certainly be admitt Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-tanganyika-problem-an-account-of-the-researches-undertaken-concerning-the-existence-of-marine-animals-in-central-africa-chytra-kirkii-upper-compared-with-a-marine-jurassic-toiiislits-lower-by-an-oolitic-fossil-genus-purpuroidia-from-which-it-isvery-difficult-if-not-impossible-on-conchological-groundsto-distinguish-it-from-these-comparisons-it-will-be-seenthat-we-have-numerous-genera-of-gastropods-belonging-tothe-halolimnic-series-of-tanganyika-which-are-concho-logically-indistinguishable-from-an-equal-number-character-istic-of-the-oolite-seas-and-it-will-certainly-be-admitt-image369681410.htmlRM2CDCCBE–. The Tanganyika problem; an account of the researches undertaken concerning the existence of marine animals in Central Africa . Chytra kirkii, upper, compared with a marine Jurassic toiiislits, lower. by an Oolitic fossil genus Purpuroidia, from which it isvery difficult, if not impossible, on conchological grounds,to distinguish it. From these comparisons it will be seenthat we have numerous genera of gastropods belonging tothe halolimnic series of Tanganyika, which are concho-logically indistinguishable from an equal number character-istic of the Oolite seas, and it will certainly be admitt
. The Quarterly journal of the Geological Society of London. eposit of the Lower Limestones, and ofthat Middle Grit which divides them from what is usually known asthe Coralline oolite *. Natural causes fortunately have provided uswith a section of the Hambleton massive in the escarpment whichbounds the Gilling-Coxwold erosion on the north, at the same timethat it forms an abrupt termination to the chain. The portion ofthe escarpment between Ampleforth Beacon and Oswaldkirk isperhaps the most instructive. In order to connect this section with the main Hambleton one * This will serve to explain Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/the-quarterly-journal-of-the-geological-society-of-london-eposit-of-the-lower-limestones-and-ofthat-middle-grit-which-divides-them-from-what-is-usually-known-asthe-coralline-oolite-natural-causes-fortunately-have-provided-uswith-a-section-of-the-hambleton-massive-in-the-escarpment-whichbounds-the-gilling-coxwold-erosion-on-the-north-at-the-same-timethat-it-forms-an-abrupt-termination-to-the-chain-the-portion-ofthe-escarpment-between-ampleforth-beacon-and-oswaldkirk-isperhaps-the-most-instructive-in-order-to-connect-this-section-with-the-main-hambleton-one-this-will-serve-to-explain-image370397792.htmlRM2CEH24G–. The Quarterly journal of the Geological Society of London. eposit of the Lower Limestones, and ofthat Middle Grit which divides them from what is usually known asthe Coralline oolite *. Natural causes fortunately have provided uswith a section of the Hambleton massive in the escarpment whichbounds the Gilling-Coxwold erosion on the north, at the same timethat it forms an abrupt termination to the chain. The portion ofthe escarpment between Ampleforth Beacon and Oswaldkirk isperhaps the most instructive. In order to connect this section with the main Hambleton one * This will serve to explain
. Memoirs of the Geological Survey of India . hesis Paljeozamia, pointed out the greatinterest attaching to them from their striking analogy with Stonesfield-slate fossils. DArchiac (Hist. deg. prog, a. 1 Geologic, VII, 624) pointedout the confusion in Captain Grant^s desijtiption, but accepting his state-ments referred the plant-bearing beds to the horizon of the lower sand-stone and shale of Phillips* divisions of the oolite, and the same lowerJurassic age has been accepted as established by several subseqiient writers.It is not improbable that further research may fully establish this con-c Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/memoirs-of-the-geological-survey-of-india-hesis-paljeozamia-pointed-out-the-greatinterest-attaching-to-them-from-their-striking-analogy-with-stonesfield-slate-fossils-darchiac-hist-deg-prog-a-1-geologic-vii-624-pointedout-the-confusion-in-captain-grants-desijtiption-but-accepting-his-state-ments-referred-the-plant-bearing-beds-to-the-horizon-of-the-lower-sand-stone-and-shale-of-phillips-divisions-of-the-oolite-and-the-same-lowerjurassic-age-has-been-accepted-as-established-by-several-subseqiient-writersit-is-not-improbable-that-further-research-may-fully-establish-this-con-c-image370175742.htmlRM2CE6XX6–. Memoirs of the Geological Survey of India . hesis Paljeozamia, pointed out the greatinterest attaching to them from their striking analogy with Stonesfield-slate fossils. DArchiac (Hist. deg. prog, a. 1 Geologic, VII, 624) pointedout the confusion in Captain Grant^s desijtiption, but accepting his state-ments referred the plant-bearing beds to the horizon of the lower sand-stone and shale of Phillips* divisions of the oolite, and the same lowerJurassic age has been accepted as established by several subseqiient writers.It is not improbable that further research may fully establish this con-c
. Annual report of the regents of the university of the state of New York on the condition of the State Cabinet of Natural History and the historical and antiquarian collection annexed thereto. No. 92. Elephas primigenius.^ Perfect lowerjaw of a young individual, with the molarteeth still in place. Pleistocene: Lippethal, Rhenish Prussia. No. 93. Rhinoceros schleyermacheri. Lower jaw, left ramus of adultspecimen. Miocene Tertiary: Germany. No. 94. Pterodactylus rhamphastinus. Skeleton nearly entire ; on aslah. Lithographic limestone (Upper Oolite): Darting, Bavaria. No. 95. Encrinus liliiformi Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annual-report-of-the-regents-of-the-university-of-the-state-of-new-york-on-the-condition-of-the-state-cabinet-of-natural-history-and-the-historical-and-antiquarian-collection-annexed-thereto-no-92-elephas-primigenius-perfect-lowerjaw-of-a-young-individual-with-the-molarteeth-still-in-place-pleistocene-lippethal-rhenish-prussia-no-93-rhinoceros-schleyermacheri-lower-jaw-left-ramus-of-adultspecimen-miocene-tertiary-germany-no-94-pterodactylus-rhamphastinus-skeleton-nearly-entire-on-aslah-lithographic-limestone-upper-oolite-darting-bavaria-no-95-encrinus-liliiformi-image370344432.htmlRM2CEEJ2T–. Annual report of the regents of the university of the state of New York on the condition of the State Cabinet of Natural History and the historical and antiquarian collection annexed thereto. No. 92. Elephas primigenius.^ Perfect lowerjaw of a young individual, with the molarteeth still in place. Pleistocene: Lippethal, Rhenish Prussia. No. 93. Rhinoceros schleyermacheri. Lower jaw, left ramus of adultspecimen. Miocene Tertiary: Germany. No. 94. Pterodactylus rhamphastinus. Skeleton nearly entire ; on aslah. Lithographic limestone (Upper Oolite): Darting, Bavaria. No. 95. Encrinus liliiformi
. Annual report of the regents of the university of the state of New York on the condition of the State Cabinet of Natural History and the historical and antiquarian collection annexed thereto. No. 3. Amorphczjum?* A fossil sponge a foot indiameter, with eleven beautifully radiating andrecurved hollow fingers. Lower Silurian i Franldin county, Kentucky.( vy Specimen still UndcsCribcd.) 30 EIGHTEENTH ANNUAL REPORT ON THE STATE CABINET.. No. 4. Apiocrinvs parldnsoni,^ Pear Encrinite. Speci-men with Caljx, stem and root complete. Great Oolite: Hampton, England. IG. Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/annual-report-of-the-regents-of-the-university-of-the-state-of-new-york-on-the-condition-of-the-state-cabinet-of-natural-history-and-the-historical-and-antiquarian-collection-annexed-thereto-no-3-amorphczjum-a-fossil-sponge-a-foot-indiameter-with-eleven-beautifully-radiating-andrecurved-hollow-fingers-lower-silurian-i-franldin-county-kentucky-vy-specimen-still-undcscribcd-30-eighteenth-annual-report-on-the-state-cabinet-no-4-apiocrinvs-parldnsoni-pear-encrinite-speci-men-with-caljx-stem-and-root-complete-great-oolite-hampton-england-ig-image370399091.htmlRM2CEH3PY–. Annual report of the regents of the university of the state of New York on the condition of the State Cabinet of Natural History and the historical and antiquarian collection annexed thereto. No. 3. Amorphczjum?* A fossil sponge a foot indiameter, with eleven beautifully radiating andrecurved hollow fingers. Lower Silurian i Franldin county, Kentucky.( vy Specimen still UndcsCribcd.) 30 EIGHTEENTH ANNUAL REPORT ON THE STATE CABINET.. No. 4. Apiocrinvs parldnsoni,^ Pear Encrinite. Speci-men with Caljx, stem and root complete. Great Oolite: Hampton, England. IG.
. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. Aticula incequwalvis, Sow. Lower Oolite, and Lias. Avicula cygnipes, Phil. Lias, Gloucestershire and Yorkshire. The peculiar aspect which is most characteristic of the Lias in England, France, and Germany, is an alternation of thin beds of blue or gray limestone, having a surface which becomes light-brown when weathered, these beds being separated by dark-colored, narrow argillaceous partings, so that the quarries of this rock, at a distance, assume a striped and rib Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-geology-aticula-incequwalvis-sow-lower-oolite-and-lias-avicula-cygnipes-phil-lias-gloucestershire-and-yorkshire-the-peculiar-aspect-which-is-most-characteristic-of-the-lias-in-england-france-and-germany-is-an-alternation-of-thin-beds-of-blue-or-gray-limestone-having-a-surface-which-becomes-light-brown-when-weathered-these-beds-being-separated-by-dark-colored-narrow-argillaceous-partings-so-that-the-quarries-of-this-rock-at-a-distance-assume-a-striped-and-rib-image231502894.htmlRMRCHT8E–. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. Aticula incequwalvis, Sow. Lower Oolite, and Lias. Avicula cygnipes, Phil. Lias, Gloucestershire and Yorkshire. The peculiar aspect which is most characteristic of the Lias in England, France, and Germany, is an alternation of thin beds of blue or gray limestone, having a surface which becomes light-brown when weathered, these beds being separated by dark-colored, narrow argillaceous partings, so that the quarries of this rock, at a distance, assume a striped and rib
. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. PieropTiyllum comptum. Syn. Cycadites eomptus. Upper Sandstone and Shale, Gristhorpe, near Scarborough. Fig. 423.. Hemitelites Broicnii, Goepp. Syn. Phlebopteris contigua, Lind. <fc Hntt. Upper Carbonaceous strata, Lower Oolite, Gristhorpe, Yorkshire. shales are well exposed in the sea-cliffs at Whitby, and are chiefly characterized by ferns and cycadese. They contain, also, a species of calamnite, and a fossil called Equisetum columnare, which main- tains an upri Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-geology-pieroptiyllum-comptum-syn-cycadites-eomptus-upper-sandstone-and-shale-gristhorpe-near-scarborough-fig-423-hemitelites-broicnii-goepp-syn-phlebopteris-contigua-lind-ltfc-hntt-upper-carbonaceous-strata-lower-oolite-gristhorpe-yorkshire-shales-are-well-exposed-in-the-sea-cliffs-at-whitby-and-are-chiefly-characterized-by-ferns-and-cycadese-they-contain-also-a-species-of-calamnite-and-a-fossil-called-equisetum-columnare-which-main-tains-an-upri-image231512345.htmlRMRCJ8A1–. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. PieropTiyllum comptum. Syn. Cycadites eomptus. Upper Sandstone and Shale, Gristhorpe, near Scarborough. Fig. 423.. Hemitelites Broicnii, Goepp. Syn. Phlebopteris contigua, Lind. <fc Hntt. Upper Carbonaceous strata, Lower Oolite, Gristhorpe, Yorkshire. shales are well exposed in the sea-cliffs at Whitby, and are chiefly characterized by ferns and cycadese. They contain, also, a species of calamnite, and a fossil called Equisetum columnare, which main- tains an upri
. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. Ammonites BraikenHdgvi, Sow. Ostrea Marshii. rtat. size. Oolite, Scarborough. Middle and Lower Oolite, or ranging Inf. Ool., Dundry ; Calvados; &c. from Coral Bay to Cornbrash. Palceontological relations of the Oolitic strata.—Observations have already been made, p. 345, on the distinctness of organic remains of the Oolitic and Cretaceous strata, and at pp. 398 and 401 of the proportion of species common to the Upper and Middle, and to the Middle and Lower Ooli Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-geology-ammonites-braikenhdgvi-sow-ostrea-marshii-rtat-size-oolite-scarborough-middle-and-lower-oolite-or-ranging-inf-ool-dundry-calvados-ampc-from-coral-bay-to-cornbrash-palceontological-relations-of-the-oolitic-strataobservations-have-already-been-made-p-345-on-the-distinctness-of-organic-remains-of-the-oolitic-and-cretaceous-strata-and-at-pp-398-and-401-of-the-proportion-of-species-common-to-the-upper-and-middle-and-to-the-middle-and-lower-ooli-image231502898.htmlRMRCHT8J–. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. Ammonites BraikenHdgvi, Sow. Ostrea Marshii. rtat. size. Oolite, Scarborough. Middle and Lower Oolite, or ranging Inf. Ool., Dundry ; Calvados; &c. from Coral Bay to Cornbrash. Palceontological relations of the Oolitic strata.—Observations have already been made, p. 345, on the distinctness of organic remains of the Oolitic and Cretaceous strata, and at pp. 398 and 401 of the proportion of species common to the Upper and Middle, and to the Middle and Lower Ooli
. Elements of geology. Geology. 218 LYELL'S ELEMENTS OF GEOLOGY. Fossils of Oolite Group. of the Jura, Alps, and other distant regions, where there is scarcely any hthological resemblance ; and yet some of the same fossils remain peculiar in each country to the Upper, Middle, and Lower Oolite formations respectively. Mr. Thurmann has shown how remarkably this fact holds true in the Bernese Jura, although the argillaceous divisions, so conspicuous in England, are feebly represented, and some entirely wanting. Amongst the characteristic fossils of the Upper Oolite, may be mentioned the Ostrea de Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-geology-218-lyells-elements-of-geology-fossils-of-oolite-group-of-the-jura-alps-and-other-distant-regions-where-there-is-scarcely-any-hthological-resemblance-and-yet-some-of-the-same-fossils-remain-peculiar-in-each-country-to-the-upper-middle-and-lower-oolite-formations-respectively-mr-thurmann-has-shown-how-remarkably-this-fact-holds-true-in-the-bernese-jura-although-the-argillaceous-divisions-so-conspicuous-in-england-are-feebly-represented-and-some-entirely-wanting-amongst-the-characteristic-fossils-of-the-upper-oolite-may-be-mentioned-the-ostrea-de-image231525105.htmlRMRCJTHN–. Elements of geology. Geology. 218 LYELL'S ELEMENTS OF GEOLOGY. Fossils of Oolite Group. of the Jura, Alps, and other distant regions, where there is scarcely any hthological resemblance ; and yet some of the same fossils remain peculiar in each country to the Upper, Middle, and Lower Oolite formations respectively. Mr. Thurmann has shown how remarkably this fact holds true in the Bernese Jura, although the argillaceous divisions, so conspicuous in England, are feebly represented, and some entirely wanting. Amongst the characteristic fossils of the Upper Oolite, may be mentioned the Ostrea de
. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. 408 MAMMALIA OF STONESFIELD OOLITE. [Oh. XX. and Phascolotherium have complicated crowns and two roots (see d, fig. 412), instead of being simple and with single fangs.* The only question, therefore, which conld fairly admit of contro- versy was limited to this point, whether the fossil mammalia found'in the Lower Oolite of Oxfordshire ought to be referred to the marsupial quadrupeds, or to the ordinary placental series. Cuvier had long ago pointed out a peculiarity Stock Photohttps://www.alamy.com/image-license-details/?v=1https://www.alamy.com/elements-of-geology-or-the-ancient-changes-of-the-earth-and-its-inhabitants-as-illustrated-by-geological-monuments-geology-408-mammalia-of-stonesfield-oolite-oh-xx-and-phascolotherium-have-complicated-crowns-and-two-roots-see-d-fig-412-instead-of-being-simple-and-with-single-fangs-the-only-question-therefore-which-conld-fairly-admit-of-contro-versy-was-limited-to-this-point-whether-the-fossil-mammalia-foundin-the-lower-oolite-of-oxfordshire-ought-to-be-referred-to-the-marsupial-quadrupeds-or-to-the-ordinary-placental-series-cuvier-had-long-ago-pointed-out-a-peculiarity-image231512353.htmlRMRCJ8A9–. Elements of geology, or, The ancient changes of the earth and its inhabitants as illustrated by geological monuments. Geology. 408 MAMMALIA OF STONESFIELD OOLITE. [Oh. XX. and Phascolotherium have complicated crowns and two roots (see d, fig. 412), instead of being simple and with single fangs.* The only question, therefore, which conld fairly admit of contro- versy was limited to this point, whether the fossil mammalia found'in the Lower Oolite of Oxfordshire ought to be referred to the marsupial quadrupeds, or to the ordinary placental series. Cuvier had long ago pointed out a peculiarity
