Cretaceous Period, 145-65 million years BP. A Cleoniceras besairiei ammonite showing opalescent lustre to the shell. See: Landman, Neil H; Tanabe, Kazushige; Davis, Richard Arnold (1996"). Ammonoid paleobiology ISBN 978-0-306-45222-2. 242 grams, 95cm (3 3/4"). From an old Bristol, UK, collection; acquired before 1960. Fine condition. [No Reserve]
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
Miocene period, 28-5 millon years BP. A museum quality reproduction of a large Carcharocles megalodon shark tooth. 143 grams, 13.6cm (5 1/4"). From Shark Tooth Hill, California, USA; from the collection of the palaeontologist R. Gledhill; collected between 1930 and 1960. Very fine condition. [No Reserve]
Eocene Period, 56-33 million years BP. A large fossil Knightia alta fish in a matrix. 559 grams, 19.7cm (8"). From Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A, from the Pradi Collection, Boston, USA; acquired 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. [No Reserve]
Eocene Period, 56-33 million years BP. A sandstone matrix including: a large smooth shelled ammonite with smaller ridge shelled ammonite, bivalve shells and section of coral stem. 2.7 kg, 27cm (11 1/2"). Property of a Welsh fossil collector; acquired on the UK art market. Very fine condition. [No Reserve]
Jurassic Period, 201-145 million years BP. A group of two shale matrix specimens each with numerous small ammonites with good shell structure and lustre; one sample with ink accession number: 'F.195.78'. See Landman, Neil H; Tanabe, Kazushige; Davis, Richard Arnold, 1996. Ammonoid paleobiology. 321 grams total, 10-13.5cm (4 - 5 1/4"). Property of a Welsh fossil collector; acquired on the UK art market. Very fine condition. [2, No Reserve]
Triassic Period, 251-199 million years BP. A cross section of a fossilised conifer tree trunk from Madagascar, with excellent grain preservation, and near the centre, the knots where branches have emerged. See Bonewitz, Dr. Ronald Louis, Rocks & Minerals, 2008, p.334-335. 624 grams, 17cm (6 3/4"). Found Madagascar; from the historic ‘Victorian Museum’ collection of Gregory, Bottley & Lloyd (Gregory's); formerly Gregory, Bottley & Co. (1932-1981) and previously J. R. Gregory & Co. (1898-1932); originally 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. The firm Gregory, Bottley and Lloyd (Gregory's), was acquired by TimeLine Auctions in 2016. London-born James Reynolds Gregory (1832-1899) founded the company, which is the second longest-running gem and fossil dealership in the world. James was educated at Archbishop Tennison's School, and afterward found employment in a jewellery company on Regent Street. In 1858 he established his own business in King William Street. A few years later he moved to ‘very extensive premises’ in Golden Square, Covent Garden. He was one of the best known dealers in London, exhibiting at major commercial shows throughout the world and winning awards for excellence in Paris in 1867, Sydney in 1879 and London in 1862, 1883 and 1884. James primarily bought his stock at auction, from collectors and other dealers, and supplied many major collectors and scientists of his day. He built superb personal collections, a selection going to the British Museum. He wrote many papers and was a member of several learned societies including the Society of Arts. The business became known as J.R. Gregory & Company in 1896, still under James' management with the assistance of his son Albert Gregory (b.1864"). When James died three years later, the business passed to Albert. At the end of the 19th century most London dealers had folded or retired, many selling out to J.R. Gregory & Co. Albert continued by acquiring Russell and Shaw (Est. 1848) in 1925 and Francis H. Butler (Est. 1884) in 1927. Percy Bottley (1904-1980) took over the company in 1931, renaming it Gregory, Bottley & Company with respect to his predecessors. Percy’s company survived the 2nd World War by buying out all of its competitors, including the supplier to Pitt-Rivers, Samuel Henson (Est. 1840) and G.H. Richards (Est. 1897) in 1936. Percy also added many important collections to his stock including those of Rev. F. Holmes in 1940, and the Graves collection in 1943. Following Percy's death in 1981, the business was sold to Brian Lloyd, whereupon it became Gregory, Bottley & Lloyd. Brian had been Sotheby’s main Natural History expert in the 1960s and 1970s, and subsequently traded from Pall Mall. The business continued to thrive, and Brian purchased the Joseph Neeld (1789-1856) collection in 1974 and the historic gold collection of H.S. Gordon, first exhibited at the Empire Exhibition, South Africa in 1936. Brian moved the business to 12-13 Rickett Street in 1982, and to 13 Seagrave Road in 1993. He carried on the company's specialization in historic collections, most recently acquiring that of Robert Ferguson (1767-1840) in 2000. The business moved to Walmer in Kent in 2008, and was acquired by TimeLine in April 2016. Trading History Est. 1858 (59 Frith Street, Soho) 1859 - 1861 (3 King William Street, Strand) 1862 - 1866 (25 Golden Square, Covent Garden) 1866 - 1874 (15 Russell Street, Covent Garden) 1874 - 1895 (88 Charlotte Street, Fitzroy Square) 1896 - 1906 (1 Kelso Place, Kensington) 1907 - 1926 (139 Fulham Road, Chelsea) 1926 - 1981 (30 (Old) Church Street, Chelsea) 1982 - 1993 (12-13 Rickett Street, Fulham) 1993 - 2007 (13 Seagrave Road, Fulham) 2008 - 2015 (59 Liverpool Road, Walmer, Kent) 2016 - (363 Main Road, Harwich, Essex) Very fine condition. [No Reserve]
Early Pliocene Period, 5.3-2.8 million years BP. A large Carcharocles megalodon shark tooth with serrations on the edge and good enamel preservation. 200 grams, 12.5cm (5"). From Georgia, USA; from the collection of the palaeontologist R. Gledhill; collected between 1930 and 1960. Fine condition.
Cretaceous Period, 145-65 million years BP. A group of five large Spinosaurs maroccanus dinosaur teeth. 78 grams total, 45-73mm (1 3/4 - 2 3/4"). From Tegana Formation, Taouz, Morocco, from the collection of the palaeontologist R. Gledhill; collected between 1930 and 1960. The Spinosaurus was both a beachcomber type scavenger and an active hunter taking small stranded Plesiosaurs, Pterosaurs, Turtles and large fish. Fine condition. [5, No Reserve]
Eocene Period, 56-33 million years BP. A fossil Knightia alta fish in a matrix. 204 grams, 14cm (5 1/2"). From Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A, from the Pradi Collection, Boston, USA; acquired 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. [No Reserve]
Eocene Period, 56-33 million years BP. A large fossil Diplomystus fish in a matrix. 458 grams, 22.9cm (9"). From the Green River Formation, Lincoln County, Wyoming, USA; from the Pradi Collection, Boston, USA; acquired 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. [No Reserve]
A Corgi Classics die-cast model vehicle : 31005 Shell/BP Bedford S Type, together with fourteen further Corgi boxed sets and models. All parts boxed. (15) CONDITION REPORT: Light wear to external packaging, Hyster Challanger 800 model with considerable wear to packaging. Otherwise very good condition for all parts.
Paul Darby (British, b.1964) - 'Still Life, Jar of Flowers by Window'Acrylic on paper, signed, approx 40x32cm, mounted and framed.Provenance: This picture was used as the poster for the Wirksworth Art Festival 2015.NB: Paul Darby has previously exhibited at the Medici Gallery in London and was runner up in the BP sponsored Young European Artist of the Year in 1992. For further information please see www.paul-darby.com.
A collection of Tri-Ang Hornby including; OO gauge scale models, GWR 0-6-0 Pannier Tank Loco R253, 0-4-0 Diesel Dock Shunter, BR Testrol Wagon, Transfesa Ferry Van, Salmon Bogie R635 Freight and Inner BP Chemicals, Track Clearing Car, an open and goods wagon 2x Freight Linerwagons, a Twelve Ton Wagon, Milk Tank Wagon and Brake Van. (23)
Matchbox 75s - No1e, Mercedes Truck, turquoise body, orange canopy, black wheels; No2d Mercedes Trailer, turquoise body, orange canopy, black wheels; No3c Mercedes Benz "Binz Ambulance"; No4d Dodge Stake Truck; No5d London Bus, BP Visco-Static; No6c Euclid Quarry Truck; No7c Ford Refuse Truck; No8e Ford Mustang, white body, red interior, silver hubs, black tyres; No9d cabin Cruiser and Trailer; No 10d Pipe Truck with seven piped, red body, silver base and grille, all boxed (10)
Matchbox 75s - No31c Lincoln Continental, light sea green body, black wheels; No32c Leyland Tanker BP; No33b Ford Zephyr; No34c, Volkswagen Camper, silver, (Windowless Roof); No35b Snow-Trac Tractor; No36c Opel Diplomat; No37c Dodge Cattle Truck, orange/yellow cab; No38 c Honda Motorcycle & Trailer; No 39c Ford Tractor; 40c Hay Trailer, all boxed (10)
Caenozoic Period, 66 million years BP. A historic group of four fossil molluscs from the Gregory, Bottley and Lloyd reference collection, with old labels reading: '84, Barton Clay, Pectunculus sp., Barton, Hants'; '85, Barton Clay, Cardita sulcata, Barton, Hants'; '83, Barton Clay, Ostrea plicata, Barton, Hampshire'; '82, Crassatella sulcata, Barton, Hants.'; all in old white card trays. 24 grams total including trays, 18-35mm (3/4 - 1 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. Fine condition. [4, No Reserve]
Palaeolithic, circa 400,000 BP. A group of bifacial ovate flint handaxes with grey patination; one with inked 'MORETON 1925' inscription, the other with inked collection label 'MORETON 7/24'; both with typical water erosion. 1 kg total, 11-15cm (4 1/4 - 6"). Found Moreton, Dorset, UK; 1924-1925. Fine condition. [2]
Cretaceous Period, Aptian Stage, 125-113 million years BP. A group of four teeth from the dinosaur Spinosaurs maroccanus from the Tegana Formation, Taouz, Morocco. 140 grams total, 71-84mm (2 3/4 - 3 1/4"). From the collection of the palaeontologist R Gledhill, collected between 1930 and 1960. The Spinosaurus was both a beachcomber type scavenger and an active hunter taking small stranded plesiosaurs, pterosaurs, turtles and large fish. Fine condition. [4, No Reserve]
Jurassic Period, Bacocian Stage, 168-172 million years BP. An A-grade cut and polished Cleoniceras sp. ammonite in an old card tray, discovered at Arbala, Middle Atlas Mountains, Morocco. 593 grams, 14cm (5"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960. Fine condition. [No Reserve]
Jurassic Period, Bacocian stage, 168-172 million years BP. A large polished Oolite Sloenbachia sp. chambered ammonite, discovered at Arbala, Middle Atlas Mountains, Morocco. 234 grams, 10.5cm (4"). From the collection of the palaeontologist R Gledhill, collected between 1930 and 1960. Fine condition. [No Reserve]
Upper Carboniferous Period, 327-299 million years BP. A group of eight plant and seed fossils including Bothrodendron minutifolium and Lepidodendron sp. plant seeds in nodules. 143 grams total, 36-52mm (1 1/2 - 2"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960. Fine condition. [8, No Reserve]
A mixed group comprising: selenite rose specimens from Mexico; polished chalcopyrite from Peru; rutile crystals in polished quartz from Brazil; polished mugglestone from South Africa; polished stromatolite pebbles from the Pre-Cambrian age (2.7 billion years BP"). of the Salt Lake of Uyuni, Oruro state, Bolivia; bornite specimens (also known as peacock ore or chalcopyrite"). from Mexico; unusual green-coloured calcite from Chihuahua, Mexico; a small amethyst point from Brazil; a sphalerite and calcite specimen from Northumberland; a sphalerite specimen from Northumberland; a citrine specimen from Brazil. 2.6 kg total, 2.5-10.5cm (1 - 4"). Property of a Lady, Swaffham, UK; acquired 1970s. Mugglestone comprises three minerals - haematite, jasper and tiger eye. Fine condition. [57, No Reserve]
Cretaceous Period, Aptian Stage, 125-113 million years BP. A group of eight large teeth from Spinosaurs maroccanus from Tegana Formation, Taouz, Morocco. 125 grams total, 51-63mm (2 - 2 1/2"). From the collection of the palaeontologist R Gledhill collected between 1930 and 1960. The Spinosaurus was both a beachcomber type scavenger and an active hunter taking small stranded plesiosaurs, pterosaurs, turtles and large fish. Fine condition. [8, No Reserve]
Palaeolithic, circa 400,000 BP. A group of flint bifacial handaxes, comprising: one ovate with grey patination, one pointed and one with significant original cortex with blue-grey patination; two with ink inscription 'MORETON 1925' and 'MORETON 1926, the third with inked collection label 'MORETON 6/24'; all with typical water erosion. 1.12 kg total, 13-16cm (5-6 1/4"). Found Moreton, Dorset, UK; 1924-1926. Fine condition. [3]
Palaeolithic, circa 400,000 BP. A group of ovate bifacial flint handaxes with cream-grey patination; two with inked collection labels 'MORETON 1923' and 'MORETON 7/24', the third with ink inscription 'MORETON 1922'. 1.1 kg total, 11-13.5cm (4 1/4 - 5 1/2"). Found Moreton, Dorset, UK; 1922-1924. Fine condition. [3]
Cretaceous Period (late Aptian), 125-113 million years BP. A group of five Spinosaurs maroccanus teeth. 95 grams total, 50-70mm (2 - 2 3/4"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960, from the Tegana Formation, Taouz, Morocco, North Africa. Fine condition, repaired. [5, No Reserve]
Cretaceous Period, 145-65 million years BP. A selection of fifteen pterosaur teeth, Siroccopteryx moroccensis, from south of Taouz, in the Moroccan Sahara. 9.73 grams total, 15-36mm (1/2 - 1 1/2"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960. So far, Siroccopteryx is the only named flying reptile from Africa and its narrow, curved teeth were probably used to catch fish. Fine condition. [15, No Reserve]
Cretaceous Period, 145-65 million years BP. A large Bahariasaurus ingens dinosaur tooth from a mid-sized carnivore, from Morocco. 21 grams, 66mm (2 3/4"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960. The teeth are different from Carcharodontosaurus in being thinner but having a thicker more triangular X-section. Fine condition.
Eocene Period, 58-36 million years BP. A large fossil Knightia alta fish on matrix from Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, U.S.A. 433 grams, 23.5 x 14.5cm (9 1/4 x 5 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. [No Reserve]
Jurassic Period, Bacocian stage, 168-172 million years BP. A large polished Beudanticeras sp. chambered ammonite, discovered at Arbala, Middle Atlas Mountains, Morocco. 458 grams, 12cm (4 3/4"). From the collection of the palaeontologist R Gledhill, collected between 1930 and 1960. Fine condition. [No Reserve]
Middle Miocene Period, 15.9-11.6 million years BP. A group of twenty five fish vertebra in an old white card collector's tray, from the Pungo River Formation, Lee Creek Phosphate Mine, Aurora, Beaufort County, N.C., USA. 59 grams total, 15-24mm (1/2 - 1"). From the Pradi Collection, Boston, USA acquired during 1980s. Fine condition, some chipped. [25, No Reserve]
Oligocene Period, 33-30 million years BP. A group of four whole eggs from the Stylemus nebrascaensis, turtle, from the White River Formation, Converse County, Wyoming, U.S.A. 21 grams total, 21-28mm (3/4 - 1 1/4"). From the Pradi Collection, Boston, USA acquired during 1980s. The Stylemus was a land tortoise. The eggs are found concentrated in rock layers together with the fossil turtle remains. Fine condition. [4, No Reserve]
Eocene Period, 58-36 million years BP. A fossil diplomystus fish in matrix from the Green River Formation, Lincoln County, Wyoming, U.S.A. 914 grams, 21.5 x 15.5cm (8 1/2 x 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. Fine condition. [No Reserve]
Eocene Period, 58-36 million years BP. A fossil Priscacara liops fish in matrix from the Green River Formation, Lincoln County, Wyoming, U.S.A. 1.5 kg, 24 x 19.5cm (9 1/2 x 7 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. Very 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. 1.5 kg, 23.5 x 16cm (5 1/4 x 6 1/4"). 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. [No Reserve]

-
18240 Los(e)/Seite