géologie

Thématique

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DUVALIA POLYGONALIS (BLAINVILLE) HAUTERIVIAN TEKE DERE SHUMEN SOFIA UNIVERSITY 'ST. KLIMENT OHRIDSKI' MUSEUM OF PALEONTOLOGY AND HISTORICAL GEOLOGY

DUVALIA POLYGONALIS (BLAINVILLE) HAUTERIVIAN TEKE DERE SHUMEN SOFIA UNIVERSITY 'ST. KLIMENT OHRIDSKI' MUSEUM OF PALEONTOLOGY AND HISTORICAL GEOLOGY

musée Hauterivien géologie
Distoloceras belimelensis sp.n. Lower Hauterivian, Belimel, Montana Province, Cr1 970X1 (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

Distoloceras belimelensis sp.n. Lower Hauterivian, Belimel, Montana Province, Cr1 970X1 (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

musée Hauterivien géologie
Crioceratites (C.) villiersianum bituberculatum (Sarkar) Hauterivian, Belimel, Cr1 929X1 at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

Crioceratites (C.) villiersianum bituberculatum (Sarkar) Hauterivian, Belimel, Cr1 929X1 at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

musée Hauterivien géologie
Acrioceras (Aspinoceras) dilatatum (d'Orbigny) Upper Hauterivian, Belimel, Montana Province, (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

Acrioceras (Aspinoceras) dilatatum (d'Orbigny) Upper Hauterivian, Belimel, Montana Province, (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

musée Hauterivien géologie
Acanthodiscus vaceki (Neumayr & Uhlig) Lower Hauterivian, Dragoman, Bulgaria, Cr1 976X1 (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

Acanthodiscus vaceki (Neumayr & Uhlig) Lower Hauterivian, Dragoman, Bulgaria, Cr1 976X1 (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

musée Bulgarie Hauterivien géologie
Abrytusites julianyi (Honnorat-Bastide), Upper Hauterivian, Pali lula, Montana (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology
Intervalles Hauterivian

Abrytusites julianyi (Honnorat-Bastide), Upper Hauterivian, Pali lula, Montana (Coll. G. Mandov) at the Sofia University 'St. Kliment Ohridski' Museum of Paleontology and Historical Geology

musée Hauterivien géologie
Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London ..
Identifier: descriptivecatal02brit (find matches)
Year: 1910 (1910s)
Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924
Subjects: Reptiles, Fossil
Publisher: London, Printed by order of the Trustees
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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Text Appearing Before Image: 
CATAL.MARINE KEPT. OXFORD CLAY. PART II. PLATE I. pmcc.
Text Appearing After Image: 
>p77ia:. G.M.Woodward del. etlibh. West, Newman imp. PLIOSAURUS FEROX.

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Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London .. Identifier: descriptivecatal02brit (find matches) Year: 1910 (1910s) Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924 Subjects: Reptiles, Fossil Publisher: London, Printed by order of the Trustees Contributing Library: Smithsonian Libraries Digitizing Sponsor: Biodiversity Heritage Library View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: CATAL.MARINE KEPT. OXFORD CLAY. PART II. PLATE I. pmcc. Text Appearing After Image: >p77ia:. G.M.Woodward del. etlibh. West, Newman imp. PLIOSAURUS FEROX. Note About Images 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.

musée Oxford Clay fossile Liopleurodon +2
This image shows a 2.1 billion year old rock containing black-banded ironstone. The rock weighs about 8.5 tons, and is approximately two meters high, three meters wide, and one meter thick. It was found in North America and belongs to the National Museum of Mineralogy and Geology, Dresden, Germany. The rock is located at +51°2'34.84" +13°45'26.67".

This image shows a 2.1 billion year old rock containing black-banded ironstone. The rock weighs about 8.5 tons, and is approximately two meters high, three meters wide, and one meter thick. It was found in North America and belongs to the National Museum of Mineralogy and Geology, Dresden, Germany. The rock is located at +51°2'34.84" +13°45'26.67".

musée Allemagne géologie
Geological context of the Lower Cretaceous deposits of southeast England, focussing on the Purbeck Group and Wealden Supergroup.

(A) Schematic geology of the Lower Cretaceous deposits of the Weald Sub-basin (southeast England), highlighting published spinosaurid finds (Charig & Milner, 1997; Salisbury & Naish, 2011; Turmine-Juhel et al., 2019). Based on Austen & Batten (2018: Fig. 2). Note that various additional spinosaurid teeth are known from the region but remain undescribed in detail (Fowler, 2007). (B) Simplified stratigraphic column of the Weald Group in southeast England, based on Batten & Austen (2011: Fig. 3.2). Note that the Grinstead Clay Formation, which subdivides the Tunbridge Wells Sands Formation in Batten & Austen (2011) and from which the “Suchosaurus cultridens” type specimen was discovered (Salisbury & Naish, 2011), is downgraded to a member of the latter formation in other works (Hopson, Wilkinson & Woods, 2008) and has not been included in this column. Spinosaurid silhouette courtesy of Dan Folkes (CC-BY 4.0).
Formations Durlston

Geological context of the Lower Cretaceous deposits of southeast England, focussing on the Purbeck Group and Wealden Supergroup. (A) Schematic geology of the Lower Cretaceous deposits of the Weald Sub-basin (southeast England), highlighting published spinosaurid finds (Charig & Milner, 1997; Salisbury & Naish, 2011; Turmine-Juhel et al., 2019). Based on Austen & Batten (2018: Fig. 2). Note that various additional spinosaurid teeth are known from the region but remain undescribed in detail (Fowler, 2007). (B) Simplified stratigraphic column of the Weald Group in southeast England, based on Batten & Austen (2011: Fig. 3.2). Note that the Grinstead Clay Formation, which subdivides the Tunbridge Wells Sands Formation in Batten & Austen (2011) and from which the “Suchosaurus cultridens” type specimen was discovered (Salisbury & Naish, 2011), is downgraded to a member of the latter formation in other works (Hopson, Wilkinson & Woods, 2008) and has not been included in this column. Spinosaurid silhouette courtesy of Dan Folkes (CC-BY 4.0).

Crétacé spécimen Spinosauridae Suchosaurus +2
Identifier: catalogueoffossi02bri (find matches)
Title: Catalogue of the fossil Reptilia and Amphibia in the British Museum (Natural history) ... By Richard Lydekker ..
Year: 1888 (1880s)
Authors:  British Museum (Natural History). Dept. of Geology Lydekker, Richard, 1849-1915
Subjects:  Reptiles, Fossil Amphibians, Fossil
Publisher:  London, Printed by order of the Trustees
Contributing Library:  Smithsonian Libraries
Digitizing Sponsor:  Biodiversity Heritage Library

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rface smooth; their terminal faces onlyslightly cupped, transversely ellipsoidal, and somewhat angulatod.Dorsals with longer centra, having nearly flat terminal faces, andforward overhang of upper part. Pectoral girdle of the general typeof Pliosaurus, with a small triangular omostornum between theventral plates of the scapula) (fig. 48), which have a strong ridge 1 Quart. Journ. Geol. Soc. vol. xlv. p. 49 (1889). 152 SATJKOPTERYGTA. dividing the ventral from the dorsal portion, and are thus more ofthe type of Thaumatosaurus. Pelvis (figs. 53, 54) like that ofPliosaurus, the pubis and ischium uniting to form an obturatorforamen. Relative lengths of humerus and femur unknown.Humerus articulating distally with only the radius and ulna, whichare relatively short, and separated only by a small interval (fig. 52) ;ulna and fibula subreniform, the former being considerably thelarger of the two. This genus may have been directly derived from the Longiros-trine group of Plesiosaurus. Fig. 49.
Text Appearing After Image:
Peloneustes philarchus.—Dorsal aspect of the coracoids; from the Oxford Clay of Bedford. Reduced, gl, glenoid cavity. (This and the preceding figure from the Quart. Joum. Geol. Soc.) Peloneustes sequalis (Phillips1). Syn. Pliosaurus cequalis, Phillips2.Pliosaurus sterrodirus, Seeley3. Imperfectly known. Cervical vertebrae with the neural canal•sunk into the centrum, and the pectorals with distinctly concaveterminal faces. Larger than typical examples of the next species. This species was founded upon a femur (fig. 50) from the Kime-ridge Clay of Oxfordshire, which so closely resembles the corre-sponding bone of P.jihilarchus as to indicate its generic identity; the 1 Geology of Oxford, p. 365 (1871).—Plesiosaurus. 2 Loc. cit. 3 Index to Ayes &c. in Cambridge Museum, p. 98 (1869).—No description. PLESI0SATJKIDJE, 153 length of this specimen is 0,572 (23 inches). The undermentionedvertebrae agree in relative size with this femur, and in genericcharacters with those of the ty

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Identifier: catalogueoffossi02bri (find matches) Title: Catalogue of the fossil Reptilia and Amphibia in the British Museum (Natural history) ... By Richard Lydekker .. Year: 1888 (1880s) Authors: British Museum (Natural History). Dept. of Geology Lydekker, Richard, 1849-1915 Subjects: Reptiles, Fossil Amphibians, Fossil Publisher: London, Printed by order of the Trustees Contributing Library: Smithsonian Libraries Digitizing Sponsor: Biodiversity Heritage Library View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: rface smooth; their terminal faces onlyslightly cupped, transversely ellipsoidal, and somewhat angulatod.Dorsals with longer centra, having nearly flat terminal faces, andforward overhang of upper part. Pectoral girdle of the general typeof Pliosaurus, with a small triangular omostornum between theventral plates of the scapula) (fig. 48), which have a strong ridge 1 Quart. Journ. Geol. Soc. vol. xlv. p. 49 (1889). 152 SATJKOPTERYGTA. dividing the ventral from the dorsal portion, and are thus more ofthe type of Thaumatosaurus. Pelvis (figs. 53, 54) like that ofPliosaurus, the pubis and ischium uniting to form an obturatorforamen. Relative lengths of humerus and femur unknown.Humerus articulating distally with only the radius and ulna, whichare relatively short, and separated only by a small interval (fig. 52) ;ulna and fibula subreniform, the former being considerably thelarger of the two. This genus may have been directly derived from the Longiros-trine group of Plesiosaurus. Fig. 49. Text Appearing After Image: Peloneustes philarchus.—Dorsal aspect of the coracoids; from the Oxford Clay of Bedford. Reduced, gl, glenoid cavity. (This and the preceding figure from the Quart. Joum. Geol. Soc.) Peloneustes sequalis (Phillips1). Syn. Pliosaurus cequalis, Phillips2.Pliosaurus sterrodirus, Seeley3. Imperfectly known. Cervical vertebrae with the neural canal•sunk into the centrum, and the pectorals with distinctly concaveterminal faces. Larger than typical examples of the next species. This species was founded upon a femur (fig. 50) from the Kime-ridge Clay of Oxfordshire, which so closely resembles the corre-sponding bone of P.jihilarchus as to indicate its generic identity; the 1 Geology of Oxford, p. 365 (1871).—Plesiosaurus. 2 Loc. cit. 3 Index to Ayes &c. in Cambridge Museum, p. 98 (1869).—No description. PLESI0SATJKIDJE, 153 length of this specimen is 0,572 (23 inches). The undermentionedvertebrae agree in relative size with this femur, and in genericcharacters with those of the ty Note About Images 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.

musée fossile Peloneustes Pliosaurus +1
Identifier: catalogueoffossi02bri (find matches)
Title: Catalogue of the fossil Reptilia and Amphibia in the British Museum (Natural history) ... By Richard Lydekker ..
Year: 1888 (1880s)
Authors:  British Museum (Natural History). Dept. of Geology Lydekker, Richard, 1849-1915
Subjects:  Reptiles, Fossil Amphibians, Fossil
Publisher:  London, Printed by order of the Trustees
Contributing Library:  Smithsonian Libraries
Digitizing Sponsor:  Biodiversity Heritage Library

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Text Appearing Before Image:
pterygian; from theKimeridge Clay of Ely. \. a, proximal, b, distal epiphysis ; c, shaft. 46792. Two still smaller specimens; from the Kimeridge Clay ofDevizes, Wiltshire. Cunnington Collection. R. 400. Two phalangeals; from the Oxford Clay of Weymouth,Dorsetshire. Presented by C. Westendarp, Esq., 1884. 150 SAUEOPTERIGIA. R. 1381. One longitudinal half of the humerus or femur of a me- (Ficj.) dium-sized form, with the inner surface cut and polished; from the Kimeridge Clay of Ely. This specimen is figured in the woodcut on the preceding page, and shows the two epiphyses almost meeting in the middle of the shaft. No history. R. 1381 a. The proximal half of a larger humerus or femur, longitu-dinally bisected; from the Kimeridge Clay of Ely. Thecontour of the proximal epiphysis is well displayed. No history. 46912. The proximal portion of a still larger humerus or femur,longitudinally bisected; from Shotover. The whole ofthe proximal epiphysis is displayed, of which the terminal Kg. 47.
Text Appearing After Image:
Sauropterygian mandibles.—A. Peloneustesphilarchus; from the Oxford Clay.\. B. Thaitmatosaurus indicus; from the Upper Jurassic of India. ).0. Pksiosaimcs dolichodirus; from the Lower Lias. f. (From the Kec.Geol. Surv. Ind.) PLESI0SAURID2E. 151 extremity appears to have been separated by a small va-cuity from that of the distal epiphysis. No history. 42097. One lateral half of a humerus or femur, with the inner sur- face cut; from the Neocomian bone-bed of Potton, Bed-fordshire. The extremity of one epiphysis is entire anddetached from the shaft, while a section is shown of thatat the opposite end. Purchased, 1870. 42098. A small imperfect femur, with the proximal epiphysis de- tached and lying loose in the cup of the shaft; fromPotton. Purchased, 1870. Genus PELONEUSTES, Lydekker \ Skull and teeth of the general type of Pliosaurus, but the mandible(fig. 47, A) with a longer symphysis, which includes more than adozen teeth. Neck short, with the anterior vertebras relativelyshort. Ve

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Identifier: catalogueoffossi02bri (find matches) Title: Catalogue of the fossil Reptilia and Amphibia in the British Museum (Natural history) ... By Richard Lydekker .. Year: 1888 (1880s) Authors: British Museum (Natural History). Dept. of Geology Lydekker, Richard, 1849-1915 Subjects: Reptiles, Fossil Amphibians, Fossil Publisher: London, Printed by order of the Trustees Contributing Library: Smithsonian Libraries Digitizing Sponsor: Biodiversity Heritage Library View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: pterygian; from theKimeridge Clay of Ely. \. a, proximal, b, distal epiphysis ; c, shaft. 46792. Two still smaller specimens; from the Kimeridge Clay ofDevizes, Wiltshire. Cunnington Collection. R. 400. Two phalangeals; from the Oxford Clay of Weymouth,Dorsetshire. Presented by C. Westendarp, Esq., 1884. 150 SAUEOPTERIGIA. R. 1381. One longitudinal half of the humerus or femur of a me- (Ficj.) dium-sized form, with the inner surface cut and polished; from the Kimeridge Clay of Ely. This specimen is figured in the woodcut on the preceding page, and shows the two epiphyses almost meeting in the middle of the shaft. No history. R. 1381 a. The proximal half of a larger humerus or femur, longitu-dinally bisected; from the Kimeridge Clay of Ely. Thecontour of the proximal epiphysis is well displayed. No history. 46912. The proximal portion of a still larger humerus or femur,longitudinally bisected; from Shotover. The whole ofthe proximal epiphysis is displayed, of which the terminal Kg. 47. Text Appearing After Image: Sauropterygian mandibles.—A. Peloneustesphilarchus; from the Oxford Clay.\. B. Thaitmatosaurus indicus; from the Upper Jurassic of India. ).0. Pksiosaimcs dolichodirus; from the Lower Lias. f. (From the Kec.Geol. Surv. Ind.) PLESI0SAURID2E. 151 extremity appears to have been separated by a small va-cuity from that of the distal epiphysis. No history. 42097. One lateral half of a humerus or femur, with the inner sur- face cut; from the Neocomian bone-bed of Potton, Bed-fordshire. The extremity of one epiphysis is entire anddetached from the shaft, while a section is shown of thatat the opposite end. Purchased, 1870. 42098. A small imperfect femur, with the proximal epiphysis de- tached and lying loose in the cup of the shaft; fromPotton. Purchased, 1870. Genus PELONEUSTES, Lydekker \ Skull and teeth of the general type of Pliosaurus, but the mandible(fig. 47, A) with a longer symphysis, which includes more than adozen teeth. Neck short, with the anterior vertebras relativelyshort. Ve Note About Images 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.

musée Oxford Clay fossile spécimen +2
Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London ..
Identifier: descriptivecatal02brit (find matches)
Year: 1910 (1910s)
Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924
Subjects: Reptiles, Fossil
Publisher: London, Printed by order of the Trustees
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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Text Appearing Before Image: 
78 MAEINE EEPTILES OF THE OXEOED CLAT. Test-fig. 30.
Text Appearing After Image: 
aa. Coracoids of Peloneustes evansi: A, from front; B, from above. (E. 3897, 1 nat. size.)  glenoid facet; p.e.a., postero-esternal angle; sc.f., facet for scapula; sym., symphysial surface.

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Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London .. Identifier: descriptivecatal02brit (find matches) Year: 1910 (1910s) Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924 Subjects: Reptiles, Fossil Publisher: London, Printed by order of the Trustees Contributing Library: Smithsonian Libraries Digitizing Sponsor: Biodiversity Heritage Library View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: 78 MAEINE EEPTILES OF THE OXEOED CLAT. Test-fig. 30. Text Appearing After Image: aa. Coracoids of Peloneustes evansi: A, from front; B, from above. (E. 3897, 1 nat. size.) glenoid facet; p.e.a., postero-esternal angle; sc.f., facet for scapula; sym., symphysial surface. Note About Images 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.

musée Oxford Clay fossile Peloneustes +1
Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London ..
Identifier: descriptivecatal02brit (find matches)
Year: 1910 (1910s)
Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924
Subjects: Reptiles, Fossil
Publisher: London, Printed by order of the Trustees
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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Text Appearing Before Image: 
CATAL,MARINE REPT. OXFORD CLAY. PART II. PLATE IV. col. — v.orb.
Text Appearing After Image: 
pas par. G.M.Woodward Aei.et litli. West.Newznsr. imp. PEEONEUSTES philarghus.

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Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London .. Identifier: descriptivecatal02brit (find matches) Year: 1910 (1910s) Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924 Subjects: Reptiles, Fossil Publisher: London, Printed by order of the Trustees Contributing Library: Smithsonian Libraries Digitizing Sponsor: Biodiversity Heritage Library View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: CATAL,MARINE REPT. OXFORD CLAY. PART II. PLATE IV. col. — v.orb. Text Appearing After Image: pas par. G.M.Woodward Aei.et litli. West.Newznsr. imp. PEEONEUSTES philarghus. Note About Images 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.

musée Oxford Clay fossile Peloneustes +1
Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London ..
Identifier: descriptivecatal02brit (find matches)
Year: 1910 (1910s)
Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924
Subjects: Reptiles, Fossil
Publisher: London, Printed by order of the Trustees
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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About This Book: Catalog Entry
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Text Appearing Before Image: 
CATAL.MARINE REPT. OXFORD CLAY. PART II. FLATE II.
Text Appearing After Image: 
G.M.Woodwa/p& del.etlitfL PLIOSAURUS PEROX. West, Newman imp.

Note About Images

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.

Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London .. Identifier: descriptivecatal02brit (find matches) Year: 1910 (1910s) Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924 Subjects: Reptiles, Fossil Publisher: London, Printed by order of the Trustees Contributing Library: Smithsonian Libraries Digitizing Sponsor: Biodiversity Heritage Library View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: CATAL.MARINE REPT. OXFORD CLAY. PART II. FLATE II. Text Appearing After Image: G.M.Woodwa/p& del.etlitfL PLIOSAURUS PEROX. West, Newman imp. Note About Images 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.

musée Oxford Clay fossile Liopleurodon +2
Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London ..
Identifier: descriptivecatal02brit (find matches)
Year: 1910 (1910s)
Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924
Subjects: Reptiles, Fossil
Publisher: London, Printed by order of the Trustees
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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About This Book: Catalog Entry
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Text Appearing Before Image: 
CATAL.MARINE KEPT. OXFORD CLAY. PART II. PLATE I. pmcc.
Text Appearing After Image: 
>p77ia:. G.M.Woodward del. etlibh. West, Newman imp. PLIOSAURUS FEROX.

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Taxons Liopleurodon

Title: A descriptive catalogue of the marine reptiles of the Oxford clay. Based on the Leeds Collection in the British Museum (Natural History), London .. Identifier: descriptivecatal02brit (find matches) Year: 1910 (1910s) Authors: British Museum (Natural History). Dept. of Geology; Andrews, Charles William, 1866-1924 Subjects: Reptiles, Fossil Publisher: London, Printed by order of the Trustees Contributing Library: Smithsonian Libraries Digitizing Sponsor: Biodiversity Heritage Library View Book Page: Book Viewer About This Book: Catalog Entry View All Images: All Images From Book Click here to view book online to see this illustration in context in a browseable online version of this book. Text Appearing Before Image: CATAL.MARINE KEPT. OXFORD CLAY. PART II. PLATE I. pmcc. Text Appearing After Image: >p77ia:. G.M.Woodward del. etlibh. West, Newman imp. PLIOSAURUS FEROX. Note About Images 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.

musée Oxford Clay fossile Liopleurodon +2
Cast of a Scaphognathus crassirostris, a kind of pterosaur. On display as part of the exhibit "Pterosaurs: Flight in the Age of Dinosaurs" at the Cleveland Natural History Museum in Cleveland, Ohio, in the United States.
This animal lived about 150 million years ago. This fossil was found in the Solnhofen formation in Germany. This is a cast; the fossil itself is held by the Institute of Geology and Paleontology at the University of Bonn.

Cast of a Scaphognathus crassirostris, a kind of pterosaur. On display as part of the exhibit "Pterosaurs: Flight in the Age of Dinosaurs" at the Cleveland Natural History Museum in Cleveland, Ohio, in the United States. This animal lived about 150 million years ago. This fossil was found in the Solnhofen formation in Germany. This is a cast; the fossil itself is held by the Institute of Geology and Paleontology at the University of Bonn.

vol musée Allemagne États-Unis +7
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Actualités

Un énorme astéroïde s'est écrasé dans la mer du Nord et a déclenché un tsunami de 330 pieds
Éocène géologie
Les scientifiques ont enfin confirmé l'origine du mystérieux cratère Silverpit sous la mer du Nord. De nouvelles preuves montrent qu’un astéroïde d’environ 160 mètres de large a heurté le fond marin il y a environ 43 à 46 millions d’années. L'impact a déclenché un tsunami de plus de 100 mètres de haut et a laissé derrière lui un cratère dont les géologues ont débattu pendant des années.
30/06/2026 sciencedaily ⚙ Traduction automatique
La jeune Terre a été ravagée par les astéroïdes, mais cela aurait tout changé
La jeune Terre a été ravagée par les astéroïdes, mais cela aurait tout changé
Hadéen géologie
Il y a plus de 4 milliards d’années, la Terre subissait un bombardement intense d’astéroïdes. Longtemps considérées comme de simples agents de destruction, ces collisions pourraient pourtant avoir joué un rôle inattendu en créant des environnements favorables à l’émergence de la vie.
15/06/2026 futura-terre
Les chercheurs révèlent une structure géante cachée sous l’Antarctique depuis 160 millions d’années
Les chercheurs révèlent une structure géante cachée sous l’Antarctique depuis 160 millions d’années
Antarctique découverte géologie
Le Continent blanc n'a été découvert qu'au début du XIXe siècle. Des hommes n'explorent donc l'Antarctique que depuis deux siècles et ses nombreux secrets ne sont pas encore percés. Mais les moyens de détection modernes nous aident dans ce but, comme le montre une découverte récente qui a des...
10/06/2026 futura-terre
Des volcans déclarés « éteints » pourraient préparer en silence leur retour explosif
Des volcans déclarés « éteints » pourraient préparer en silence leur retour explosif
géologie étude volcanisme
Combien de temps un volcan peut-il rester endormi avant de se réveiller ? L’étude d’un volcan grec montre que même plus de 100 000 ans de silence ne suffisent pas forcément à le déclarer éteint.
09/06/2026 futura-terre
Une étude du MIT révèle que les premiers animaux de la Terre étaient probablement d’anciennes éponges de mer
empreintes découverte géologie étude
Les scientifiques du MIT ont trouvé des preuves chimiques convaincantes selon lesquelles les premiers animaux de la Terre étaient probablement d’anciennes éponges marines. Cachées à l’intérieur de roches vieilles de plus de 541 millions d’années se trouvent de rares « empreintes digitales » moléculaires qui correspondent aux composés fabriqués par les démosponges modernes. Après avoir testé des roches, des éponges vivantes et des molécules fabriquées en laboratoire, les chercheurs ont confirmé que les signaux provenaient de la vie et non de la géologie. Cette découverte suggère que les éponges prospéraient dans les océans bien avant l’apparition de la plupart des autres groupes d’animaux.
27/02/2026 sciencedaily-paleo ⚙ Traduction automatique
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