Upper Jurassic Period, 150 million years BP. A fossil dorsal vertebra from an ichthyosaur, from the Kimmeridge Clay, Weymouth, Dorset, UK, mounted on a custom-made display stand. 640 grams, 15.5cm including stand (6"). From the collection of the palaeontologist R. Gledhill; collected between 1930 and 1960. [No Reserve] Fine condition.
18240 Preisdatenbank Los(e) gefunden, die Ihrer Suche entsprechen
18240 Lose gefunden, die zu Ihrer Suche passen. Abonnieren Sie die Preisdatenbank, um sofortigen Zugriff auf alle Dienstleistungen der Preisdatenbank zu haben.
Preisdatenbank abonnieren- Liste
- Galerie
-
18240 Los(e)/Seite
Eocene Period, 56-33 million years BP. A group of ten mixed species of fossil shark teeth including two Otodus obliquus, or Sand Shark teeth, from the Gregory, Bottley, and Lloyd collection. 16 grams including tray, 13-28mm (1/2 - 1"). From a historic ‘Victorian Museum’ collection; from the stock of Gregory, Bottley & Lloyd (1981-2014); formerly with Gregory, Bottley & Co. (1932-1981) and previously with J. R. Gregory & Co. (1898-1932); originally in the collection of the famous James Reynolds Gregory (1858-1898"). This item is part of a historic collection of fossils and minerals which has recently been reviewed by leading geological expert, Dr. Ronald Bonewitz. James Reynolds Gregory (1832-1899) was one of the principle London mineral and fossil dealers during the second half of the 19th century. The company he founded was one of the longest surviving geological suppliers in the world, second only to Kranz of Germany. In 1858 James Gregory established his business selling polished stones, minerals and fossils from premises in King William Street. A few years later he moved to premises in Golden Square, Soho. He won prize medals at exhibitions in Paris (1867), Sydney (1879) and London (1862 and 1883"). He also formed a superb collection of meteorites, which was later sold by his sons to the Natural History Museum, London. On the death of his father in 1899 Albert Gregory took over the business, dealing from premises in Kensington, then 30 Old Church Street in Chelsea. He eventually sold the company in 1932 to Percy Bottley, and after his death in 1982 the premises were sold. The company was then acquired by Brian Lloyd who had started the Natural History sales at Sotheby's before dealing from his own premises in Pall Mall. Gregory, Bottley & Lloyd, as it became known, traded from Ricket Street and later Seagrave Road in Fulham. In 2008 the business and all of the stock and Victorian cabinets were moved out of London to Walmer in Kent. On the eventual retirement of Brian and Mary Lloyd in 2014, with none of their family interested in taking over the business, the stock was sold and is now dispersed. [10, No Reserve] Extremely fine condition.
Eocene Period, 50-55 million years BP - Miocene Period, 23-5.3 million years BP. A group of two large fossil shark teeth comprising: one from Cosmopolitodus (Carcharodon) hastalis the extinct Giant White shark; one from Otodus obliquus from Morocco. 77 grams total, 60-81mm (2 1/4 - 3 1/4"). From the collection of the palaeontologist R. Gledhill; collected between 1930 and 1960. Cosmopolitodus (Carcharodon) hastalis is the largest of the Cosmopolitodus/Carcharodon lineage. The shark appeared in the Miocene Period and became extinct in the mid Pliocene.Cosmopolitodus hastalis have non-serrated teeth. The Otodus obliquus was the king of the early Eoceneand large examples of its teeth are not easily located in the phosphate pits in Atlas Mountains of Morocco. [2, No Reserve] Fine condition.
Eocene Period, 58-36 million years BP. A fossil fish Diplomystus from the Green River Formation, Lincoln County, Wyoming. 449 grams, 22cm (8 3/4"). From the Pradi Collection, Boston, USA; acquired during 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene Lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. [No Reserve] Fine condition.
Eocene Period, 58-36 million years BP. A fossil fish Diplomystus from the Green River Formation, Lincoln County, Wyoming, USA. 2.3 kg, 32.5cm (12 3/4"). From the Pradi Collection, Boston, USA; acquired during 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene Lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. Fine condition.
Eocene Period, 58-36 million years BP. A fossil fish Diplomystus from the Green River Formation, Lincoln County, Wyoming, U.S.A. 447 grams, 15.5cm (6"). From the Pradi Collection, Boston, USA; acquired during 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene Lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. [No Reserve] Fine condition.
Eocene Period, 58-36 million years BP. A group of three large fossil Knightia alta fish in matrix from Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A. 3.1 kg, 35cm (13 1/2"). From the Pradi Collection, Boston, USA; acquired during 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene Lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. Fine condition.
Eocene Period, 58-36 million years BP. A large fossil Knightia alta fish in matrix from Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A. 1.1 kg, 35cm (13 3/4"). From the Pradi Collection, Boston, USA; acquired during 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. [No Reserve] Fine condition.
Eocene Period, 58-36 million years BP. Two fossil Knightia alta fish in matrix from Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A. 561 grams, 18cm (7"). From the Pradi Collection, Boston, USA; acquired during the 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. [No Reserve] Fine condition.
Eocene Period, 58-36 million years BP. Two fossil Knightia alta fish in matrix from Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A. 824 grams, 21cm (8 1/4"). From the Pradi Collection, Boston, USA; acquired during the 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene Lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. [No Reserve] Fine condition.
Eocene Period, 58-36 million years BP. Two fossil Knightia alta fish and a third partial specimen in matrix from Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A. 657 grams, 18cm (7"). From the Pradi Collection, Boston, USA; acquired during the 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene Lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. [No Reserve] Fine condition.
Eocene Period, 58-36 million years BP. A group of five fossil Knightia alta fish in matrix from Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A. 1.1 kg, 26.5cm (10 1/2"). From the Pradi Collection, Boston, USA; acquired during 1980s. In southwest Wyoming (and parts of Colorado and Utah) in the Green River Formation are found some of the world's most outstanding specimens of fossil fish. The Green River system was composed of three lakes: Lake Ulinta, Lake Gosiute and Fossil Lake. These Eocene Lakes lay in a series of intermountain basins formed by geological events that uplifted the Rocky Mountains during the early Tertiary time. The climate was much different from the desert-like climate of this area today. Both the fauna (crocodiles, alligators, boa constrictors and some subtropical fish families) and the flora (such as large palm trees) indicate a climate much like that found along the Gulf Coast today. Large amounts of ash found in the sediments indicate that volcanoes were particularly active at this time. Fine condition.
Eocene Period, 58-36 million years BP. A large and well preserved example of a fossil fish Mioplosus labracoides from the Green River Formation, found at a quarry near Kemmerer, Wyoming, USA. 814 grams, 30.5cm (12"). From an old Bristol paleontological collection; acquired 1950s-60s. This specimen is highly detailed with the bone structure, vertebrae, fins and tail well preserved. [No Reserve] Fine condition. Rare.
Eocene Period, 56-33 million years BP. A group of fossil fish, three probably Knightia alta, the fourth a different species; in thin matrix tiles, suitable for framing or other display. 840 grams total, 12-16cm (4 3/4 - 6 1/4"). Property of a gentleman; acquired prior to 2000; from the Green River Formation, Wyoming, USA. [4, No Reserve] Fine condition.
Eocene Period, 56-33 million years BP. A group of fossil fish, three (one bearing two specimens) probably Knightia alta, the fourth another species; in thin matrix tiles, suitable for framing or other display. 995 grams total, 9.5-13cm (3 3/4 - 5"). Property of a gentleman; acquired prior to 2000; from the Green River Formation, Wyoming, USA. [4, No Reserve] Fine condition.
Eocene Period, 56-33 million years BP. A group of fossil fish, two small and two larger, probably Knightia alta, in thin matrix tiles, suitable for framing or other display. 2.07 kg total, 10-25cm (4 - 10"). Property of a gentleman; acquired prior to 2000; from the Green River Formation, Wyoming, USA. [4, No Reserve] Fine condition.
Eocene Period, 56-33 million years BP. A group of fossil fish, probably Knightia alta, in thin matrix tiles, suitable for framing or other display. 885 grams total, 12-15.5cm (4 3/4 - 6"). Property of a gentleman; acquired prior to 2000; from the Green River Formation, Wyoming, USA. [4, No Reserve] Fine condition.
Eocene Period, 56-33 million years BP. A group of fossil fish, probably Knightia alta, in thin matrix tiles, suitable for framing or other display. 975 grams total, 12-15cm (4 3/4 - 6"). Property of a gentleman; acquired prior to 2000; from the Green River Formation, Wyoming, USA. [4, No Reserve] Fine condition.
Eocene Period, 56-33 million years BP. A group of three fossil fish, probably Knightia alta, with a spiral shell fossil; in thin matrix tiles, suitable for framing or other display. 1.47 kg total, 10-21cm (4 - 8 1/4"). Property of a gentleman; acquired prior to 2000; from the Green River Formation, Wyoming, USA. [4, No Reserve] Fine condition.
Eocene Period, 56-33 million years BP. A group of fossil fish, three probably Knightia alta, the fourth a different species; in thin matrix tiles, suitable for framing or other display. 1.22 kg, 13-16cm (5 - 6 1/4"). Property of a gentleman; acquired prior to 2000; from the Green River Formation, Wyoming, USA. [4, No Reserve] Fine condition.
45-70 million years BP. A collection of fossil fish and reptile teeth and vertebra from the phosphates of Khouribga, Morocco in a glazed wooden display frame, with identification labels. 1.7 kg, 49 x 29.5 x 3.5cm (19 1/4 x 11 1/2 x 1 1/2"). From an old Bristol paleontological collection; acquired 1950s-60s. [No Reserve] Fine condition.
Pliostene Period, 4-3 million years BP. A large mineralised vertebra from the extinct whale Cetotherium sp. showing the structure; with custom display stand. 1.7 kg, 24cm including stand (9 1/2"). From the Pradi Collection, Boston, USA; acquired during 1980s; found South Carolina, USA. Fine condition.
Pleistocene Period, 90,000-35,000 years BP. A complete juvenile molar tooth from an extinct mammoth, Mammuthus primigenius showing the characteristic enamel ridges, and retaining some root structure. 1.42 kg, 15cm (6"). Property of a Hampshire collector; collected by the vendor's father in the 1930s. See Adams, A. Leith, Monograph on the British Fossil Elephants, Palaeontographical Society, 1877. [No Reserve] Fine condition.
Pleistocene Period, 70,000-20,000 years BP. Two molar teeth from the extinct woolly rhinceros Coelodonta antiquitatis, with biting surfaces and root structures present; one lacking a cusp (about one quarter of upper surface), possibly resulting from injury during life; patination typical of British examples. 200 grams total, 50 - 60mm (2 - 2 1/2"). Property of a Hampshire collector; collected by the vendor's father in the 1930s. See Owen, Richard, A History of British Fossil Mammals and Birds, London, 1846, pp.325-383, for illustrations of similar teeth. [2, No Reserve] Fine condition. Scarce.
Late Pleistocene Period, 1.5 million-7,700 years BP. A large woolly rhinoceros lower leg bone Coelodonta antiquitatis from Brown Bank, Lowestoft, Suffolk, UK. 600 grams, 22cm (8 3/4"). From the collection of the palaeontologist R. Gledhill; collected between 1930 and 1960. [No Reserve] Fine condition.
Miocene Period, 20 million years BP. A group of 100 Microsolena excelsa fossil coral branches, in old white card tray with old label which states Microsolena excelsa, Great Oolite, Hampton, from the Gregory, Bottley, and Lloyd collection. 82 grams including tray, 8-23mm (1/4 - 1"). Found Great Oolite; Hampton Cliffs, near Bath, Buckinghamshire, UK, in the 19th century. From a historic ‘Victorian Museum’ collection; from the stock of Gregory, Bottley & Lloyd (1981-2014); formerly with Gregory, Bottley & Co. (1932-1981) and previously with J. R. Gregory & Co. (1898-1932); originally in the collection of the famous James Reynolds Gregory (1858-1898"). This item is part of a historic collection of fossils and minerals which has recently been reviewed by leading geological expert, Dr. Ronald Bonewitz. James Reynolds Gregory (1832-1899) was one of the principle London mineral and fossil dealers during the second half of the 19th century. The company he founded was one of the longest surviving geological suppliers in the world, second only to Kranz of Germany. In 1858 James Gregory established his business selling polished stones, minerals and fossils from premises in King William Street. A few years later he moved to premises in Golden Square, Soho. He won prize medals at exhibitions in Paris (1867), Sydney (1879) and London (1862 and 1883"). He also formed a superb collection of meteorites, which was later sold by his sons to the Natural History Museum, London. On the death of his father in 1899 Albert Gregory took over the business, dealing from premises in Kensington, then 30 Old Church Street in Chelsea. He eventually sold the company in 1932 to Percy Bottley, and after his death in 1982 the premises were sold. The company was then acquired by Brian Lloyd who had started the Natural History sales at Sotheby's before dealing from his own premises in Pall Mall. Gregory, Bottley & Lloyd, as it became known, traded from Ricket Street and later Seagrave Road in Fulham. In 2008 the business and all of the stock and Victorian cabinets were moved out of London to Walmer in Kent. On the eventual retirement of Brian and Mary Lloyd in 2014, with none of their family interested in taking over the business, the stock was sold and is now dispersed. [100, No Reserve] Extremely fine condition.
Cretaceous Period, 130-60 million years BP. A group of one hundred Orthopsis sp. fossil sea urchins, all well preserved and showing full shell details, in old white card tray. 156 grams including tray, 7-17mm (1/4 - 13/4"). From a historic ‘Victorian Museum’ collection; from the stock of Gregory, Bottley & Lloyd (1981-2014); formerly with Gregory, Bottley & Co. (1932-1981) and previously with J. R. Gregory & Co. (1898-1932); originally in the collection of the famous James Reynolds Gregory (1858-1898"). This item is part of a historic collection of fossils and minerals which has recently been reviewed by leading geological expert, Dr. Ronald Bonewitz. James Reynolds Gregory (1832-1899) was one of the principle London mineral and fossil dealers during the second half of the 19th century. The company he founded was one of the longest surviving geological suppliers in the world, second only to Kranz of Germany. In 1858 James Gregory established his business selling polished stones, minerals and fossils from premises in King William Street. A few years later he moved to premises in Golden Square, Soho. He won prize medals at exhibitions in Paris (1867), Sydney (1879) and London (1862 and 1883"). He also formed a superb collection of meteorites, which was later sold by his sons to the Natural History Museum, London. On the death of his father in 1899 Albert Gregory took over the business, dealing from premises in Kensington, then 30 Old Church Street in Chelsea. He eventually sold the company in 1932 to Percy Bottley, and after his death in 1982 the premises were sold. The company was then acquired by Brian Lloyd who had started the Natural History sales at Sotheby's before dealing from his own premises in Pall Mall. Gregory, Bottley & Lloyd, as it became known, traded from Ricket Street and later Seagrave Road in Fulham. In 2008 the business and all of the stock and Victorian cabinets were moved out of London to Walmer in Kent. On the eventual retirement of Brian and Mary Lloyd in 2014, with none of their family interested in taking over the business, the stock was sold and is now dispersed. [100, No Reserve] Extremely fine condition.
Ordovician Period, 460 million years BP. A group of three Calymene sp. fossil trilobites, two in the defensive curling posture, from the Gregory, Bottley and Lloyd collection, in old white card tray. 278 grams total including tray, 46-65mm (1 3/4 - 2 1/2"). From a historic ‘Victorian Museum’ collection; from the stock of Gregory, Bottley & Lloyd (1981-2014); formerly with Gregory, Bottley & Co. (1932-1981) and previously with J. R. Gregory & Co. (1898-1932); originally in the collection of the famous James Reynolds Gregory (1858-1898"). This item is part of a historic collection of fossils and minerals which has recently been reviewed by leading geological expert, Dr. Ronald Bonewitz. [3, No Reserve] Fine condition.
Palaeozoic Period, 540 million years BP. A mixed group of juvenile Calymene sp. trilobite fossils from the Palaeozoic Period, in two old white card trays, from the Gregory, Bottley, and Lloyd collection. 238 grams including trays, 26-70mm (1 - 2 3/4"). From a historic ‘Victorian Museum’ collection; from the stock of Gregory, Bottley & Lloyd (1981-2014); formerly with Gregory, Bottley & Co. (1932-1981) and previously with J. R. Gregory & Co. (1898-1932); originally in the collection of the famous James Reynolds Gregory (1858-1898"). This item is part of a historic collection of fossils and minerals which has recently been reviewed by leading geological expert, Dr. Ronald Bonewitz. James Reynolds Gregory (1832-1899) was one of the principle London mineral and fossil dealers during the second half of the 19th century. The company he founded was one of the longest surviving geological suppliers in the world, second only to Kranz of Germany. In 1858 James Gregory established his business selling polished stones, minerals and fossils from premises in King William Street. A few years later he moved to premises in Golden Square, Soho. He won prize medals at exhibitions in Paris (1867), Sydney (1879) and London (1862 and 1883"). He also formed a superb collection of meteorites, which was later sold by his sons to the Natural History Museum, London. On the death of his father in 1899 Albert Gregory took over the business, dealing from premises in Kensington, then 30 Old Church Street in Chelsea. He eventually sold the company in 1932 to Percy Bottley, and after his death in 1982 the premises were sold. The company was then acquired by Brian Lloyd who had started the Natural History sales at Sotheby's before dealing from his own premises in Pall Mall. Gregory, Bottley & Lloyd, as it became known, traded from Ricket Street and later Seagrave Road in Fulham. In 2008 the business and all of the stock and Victorian cabinets were moved out of London to Walmer in Kent. On the eventual retirement of Brian and Mary Lloyd in 2014, with none of their family interested in taking over the business, the stock was sold and is now dispersed. [8, No Reserve] Extremely fine condition.
Ordovician Period, 485-444 million years BP-Upper Devonian Period, 385-359 million years BP. A mixed group of fossil trilobites comprising: a Diacalymene sp. trilobite from the Ordovician Period of Morocco; a Metacanthina barrandei trilobite on a matrix from the Upper Devonian Period of the Atlas Mountains, Hamar Laghdad Formation, Pragian, (Alnif), Morocco; a Crotalocephalina gibba trilobite on a matrix from the Upper Devonian Period, Alnif, Morocco. 1 kg total, 8.5-10cm (3 1/2 - 4"). Property of a Lincolnshire, UK, gentleman; acquired on the UK art market. [3, No Reserve] Fine condition.
Lower Jurassic to Devonian Period, 417-175 million years BP. A mixed group comprising: a geode fragment with amethyst to one face; four ammonite fossils, two on matrix; a trilobite fossil on matrix. 1.4 kg, 5.5-17cm (2 1/4 - 6 3/4"). Private collection, Cambridgeshire, UK; acquired prior to 2000. [6, No Reserve] Fine condition.

-
18240 Los(e)/Seite