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18240 Los(e)/Seite
Rare unnamed Spalding "Ball Back Lofting Mashie" c.1897 - smf lofting iron with a large ball shaped weight to the back of the blade and stamped to the toe "Warranted forged" c/w full length leather grip Note See Jeff Ellis Auction catalogue lot 556 similar iron was first featured in the 1897 Spalding Catalogue Guide and quote "Less than 10 Ball Back Mashies are known to exist" realised $1650 incl BP 25%
1970 to 1980's Cricket Ashes Ephemera Album containing photos and photocards, of players and teams, team sheets including Australia 1972, 1977, 1979, 1980, 1981, M.C.C. 1974, 1976, 1979 and 1982, M.C.C. 1970-71 Christmas card, BP 1970-71 fixture card, Australia 1972 fixture card, assorted signatures on paper and photos including Snow, Shuttleworth, Luckhurst, Thomson, Steele, Hogg, Gooch, Bob Simpson, Hayes, Dilley, Border, Lillee, Alderman and others, approx. 60 total, signed match sheets, Boycott signed 8" x 10" photograph getting Hundredth 100 dated August 11th 1977, newspaper cuttings and photos, covers, cornhill cards etc.
Lower Jurassic Period, Toarcian Stage, Upper Lias, 180 million years BP. A large Harpoceras falciferum ammonite; presented on a custom-made display stand. 2.7 kg total, 29cm tall including stand (11 1/2"). From an old Bristol paleontological collection; acquired 1950s-1960s; from the Upper Lias, Seavington St. Mary, Illminster, Somerset, UK. [No Reserve] Fine condition.
Early Eocene Period, 50 million years BP. A group of fifty Odontaspis robusta and Otodus obliquus shark teeth; all with good enamel and roots. 109 grams total, 17-30mm (1/4 - 1 1/4"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; from Khouribga, Morocco. [50, No Reserve] Fine condition.
Upper Devonian to Palaeozoic Period, 385-350 million years BP. A group of four Orthoceras regulare (“straight horn”), a genus of extinct nautiloid cephalopod, together with two Sporadoceras sp. goniatites or primitive ammonites polished through the shell to reveal the calcite preserved inside and show the gas chambers (known as suture patterns) where they meet the surface giving a zig-zag pattern. 253 grams total, 50-80mm (2 - 3 1/3"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; from the Atlas Mountains, Central Morocco. [6, No Reserve] Fine condition.
Oligocene Period, 45 million years BP. A group of five pieces of polished clear Baltic amber, all containing flies or other insects together with other inclusions. 1.74 grams total, 10.85-18.65mm (1/4 - 3/4"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960. [5, No Reserve] Fine condition.
Upper Devonian Period, 385 to 359 million years BP. A Geesops sp. trilobite on matrix. 215 grams, 80mm (3 1/4"). From an old Bristol paleontological collection; acquired 1950s-1960s; previously with an old Oxfordshire fossil and mineral collection; from the Atlas Mountains, HamarLaghdad Formation, Pragian, (Alnif), Morocco. [No Reserve] Fine condition.
Oligocene Period, 45 million years BP. A group of two pieces of polished clear Baltic amber, both containing flies or other insects together with other inclusions. 1.64 grams total, 19.75-21.79mm (3/4 - 1"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960. [2, No Reserve] Fine condition.
Lower Cretaceous Period, 125 million years BP. A complete Sinohydrosaurus lingyuanensis, also known as Hyphalosaurus lingyuanensis, fossil reptile showing the full skeleton; presented in a display case. See Li Jianjun, 1999, Beijing Natural History Museum for information. 74 grams, 205 grams with case, 13.5cm, case 21 x 16cm (5 1/4"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; from the Yixian Formation, Lingyuan, Liaoning Province in Northeast China. The Sinohydrosaurus lingyuanensis is a more recently discovered and described marine lizard from the famous dinosaur fossil beds of Liaoning Province; believed to have descended from a land-dwelling ancestor, this was a fresh water aquatic reptile. Fine condition.
Lower Cretaceous Period, 125 million years BP. A complete Sinohydrosaurus lingyuanensis, also known as Hyphalosaurus lingyuanensis, fossil reptile showing the full skeleton; presented in a display case. See Li Jianjun, 1999, Beijing Natural History Museum for information. 54 grams, 110 grams with case, 13cm, case 16 x 13cm (5"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; from the Yixian Formation, Lingyuan, Liaoning Province in Northeast China. The Sinohydrosaurus lingyuanensis is a more recently discovered and described marine lizard from the famous dinosaur fossil beds of Liaoning Province; believed to have descended from a land-dwelling ancestor, this was a fresh water aquatic reptile. Fine condition.
Early Pliocene Period, 5-2 million years BP. A large Carcharocles megalodon shark tooth; the specimen is well preserved and displays very good tooth enamel. 209 grams, 11cm (4 1/4"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960; from Georgia, USA. Very fine condition.
Early Jurassic Period, 200 million years BP. Four Coelophysis sp. dinosaur footprints preserved on a slab; with a model of this dinosaur species. 618 grams, 26cm (10 1/4"). Collected and verified by Dr Bretton Carter while working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution to help prove that Pangaea was a super-continent that existed during the late Palaeozoic and early Mesozoic eras; accompanied by a copy of a letter by Dr. Bretton Carter explaining circumstances and relevance of the discovery. This specimen was collected by, verified and used as part of a study by Dr Bretton Carter while working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution. A few miles from Urquhart Castle, there is a sedimentary deposit that yields schist, sandstones, and mudstones similar to those found in New Jersey, Connecticut, Massachusetts and Nova Scotia; these Scottish sedimentary deposits are also Late Triassic to Jurassic in age, and placed around the same time as the fossils that have been collected from New England. They hold the same species of dinosaurs, which means that the distribution of Coelophysis, Eubrontes, Dilophosaurus and the dinosaurs responsible for the Anchisauripus footprints was much more vast than ever previously thought. These Jurassic layers also extend into Shandwick Bay in Tain, Scotland, and even possibly further east into modern day Norway and Sweden. The Scottish localities have not been studied properly since the initial discovery of the tracks over 150 years ago, but the future preservation of these localities are quite promising. This specimen of Coelophysis in particular was discovered by Dr Bretton Carter, who spends much of his time studying the similarities of fossils between New England, Canada and the United Kingdom. Working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution, Bretton Carter has made it his mission to find concrete evidence of the vast distribution of the New England dinosaurs possibly having extended further northeast, and as of summer 2017, he may just have done that. Bretton Carter is gathering proof that Pangaea was a supercontinent that existed during the late Palaeozoic and early Mesozoic eras. Fine condition.
Eocene Period, 56-33 million years BP. A fine fossil Diplomystus sp. fish showing full detail and entire skeleton. 1.2 kg, 26.5cm (10 1/2"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; from the Green River Formation, Lincoln County, Wyoming, USA. [No Reserve] Fine condition.
Cambrian to Eocene Period, 525-36 million years BP. Group comprising: a natural iridescent rainbow shell Cleoniceras besairiei ammonite, Cretaceous; a brachiopod, Rhynchonella sp., Upper Jurassic; a Odontaspsis sp. shark tooth, Eocene; a Paralejurus sp. trilobite on a matrix, Upper Devonian; an agatised gastropod, Eocene; an Oreodont jaw section with teeth, Oligocene; a piece of oviraptor dinosaur eggshell, Upper Cretaceous; a Orthoceras, Upper Devonian; a section of polished dinosaur coprolite, Late Cretaceous; a section of polished fossilised wood from Madagascar, Triassic; two sea urchins, Echinolampas, Charente-Maritime, Eocene (36 million years); a Elrathia sp. trilobite, Utah, USA, Middle Cambrian (525 million years) and a Knightia alta fish from the Eocene from Warfield's Quarry, Kemmerer, Green River Formation, Wyoming, USA; with labels and card trays. 335 grams total, 24-98mm (1-4"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; acquired 1980s. [13, No Reserve] Very fine condition.
Jurassic Period, 200 million years BP. Four Coelophysis sp. dinosaur footprints, on a small slab. 685 grams, 17cm (6 3/4"). Collected and verified by Dr Bretton Carter while working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution to help prove that Pangaea was a super-continent that existed during the late Palaeozoic and early Mesozoic eras; accompanied by a copy of a letter by Dr. Bretton Carter explaining circumstances and relevance of the discovery. This specimen was collected by, verified and used as part of a study by Dr Bretton Carter while working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution. A few miles from Urquhart Castle, there is a sedimentary deposit that yields schist, sandstones, and mudstones similar to those found in New Jersey, Connecticut, Massachusetts and Nova Scotia. These Scottish sedimentary deposits are also Late Triassic to Jurassic in age, and placed around the same time as the fossils that have been collected from New England. Strangely enough, they hold the same species of dinosaurs, which means that the distribution of Coelophysis, Eubrontes, Dilophosaurus and the dinosaurs responsible for the Anchisauripus footprints was much more vast than ever previously thought. These Jurassic layers also extend into Shandwick Bay in Tain, Scotland, and even possibly further east into modern day Norway and Sweden. The Scottish localities have not been studied properly since the initial discovery of the tracks over 150 years ago, but the future preservation of these localities are quite promising. This specimen of Coelophysis in particular was discovered by Dr Bretton Carter, who spends much of his time studying the similarities of fossils between New England, Canada and the United Kingdom. Working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution, Bretton Carter has made it his mission to find concrete evidence of the vast distribution of the New England dinosaurs possibly having extended further northeast, and as of summer 2017, he may just have done that. Bretton Carter is gathering proof that Pangaea was a supercontinent that existed during the late Palaeozoic and early Mesozoic eras. Fine condition.
Upper Devonian Period, 385-359 million years BP. A Reedops sp. trilobite on matrix clearly showing the external structures. 268 grams, 80mm (3"). From an old Bristol paleontological collection; acquired 1950s-1960s; previously with an old Oxfordshire fossil and mineral collection; from the Atlas Mountains, Hamar Laghdad Formation, Pragian, (Alnif), Morocco. [No Reserve] Fine condition.
Jurassic Period, 200 million years BP. A single Coelophysis sp. dinosaur footprint, on a small slab. 85 grams, 13cm (5"). Collected and verified by Dr Bretton Carter while working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution to help prove that Pangaea was a super-continent that existed during the late Palaeozoic and early Mesozoic eras; accompanied by a copy of a letter by Dr. Bretton Carter explaining circumstances and relevance of the discovery. This specimen was collected by, verified and used as part of a study by Dr Bretton Carter while working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution. A few miles from Urquhart Castle, there is a sedimentary deposit that yields schist, sandstones, and mudstones similar to those found in New Jersey, Connecticut, Massachusetts and Nova Scotia. These Scottish sedimentary deposits are also Late Triassic to Jurassic in age, and placed around the same time as the fossils that have been collected from New England. Strangely enough, they hold the same species of dinosaurs, which means that the distribution of Coelophysis, Eubrontes, Dilophosaurus and the dinosaurs responsible for the Anchisauripus footprints was much more vast than ever previously thought. These Jurassic layers also extend into Shandwick Bay in Tain, Scotland, and even possibly further east into modern day Norway and Sweden. The Scottish localities have not been studied properly since the initial discovery of the tracks over 150 years ago, but the future preservation of these localities are quite promising. This specimen of Coelophysis in particular was discovered by Dr Bretton Carter, who spends much of his time studying the similarities of fossils between New England, Canada and the United Kingdom. Working with the University of Glasgow, University of Massachusetts and the Smithsonian Institution, Bretton Carter has made it his mission to find concrete evidence of the vast distribution of the New England dinosaurs possibly having extended further northeast, and as of summer 2017, he may just have done that. Bretton Carter is gathering proof that Pangaea was a supercontinent that existed during the late Palaeozoic and early Mesozoic eras. Fine condition.
Ordovician Period, 450 million years BP. A mortality plate displaying five large brittlestars, Ophiura sp. showing much detail. 1.9 kg, 28cm (11"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; acquired 1980s; from Kataoua formation, Blekus, Morocco. Fine condition.
Lower Jurassic Period, 172 million years BP. A large group of Dactylioceras sp. ammonites in matrix; presented on a custom-made display stand. 4.1 kg total, 33cm including stand (13"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960; from Schlieffhausen (near Nuremberg), Germany. Fine condition.
Albian Cretaceous Period, 113-100 million years BP. A large A-grade cut and polished pair of Cleoniceras sp. ammonite displaying the distinctive pattern of the chambers; with card tray. 429 grams total, 12.5cm (5"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960; from Madagascar. [2, No Reserve] Very fine condition.
Upper Cretaceous Period, 66 million years BP. A group of samples of the carbonised material from the K-T Boundary, resulting from the asteroid impact with the earth that triggered the extinction of the dinosaurs. 56 grams total, 5-45mm (1/4-1 3/4"). From the Pradi Collection, Boston, USA; acquired during the 1980s; from Trochu, Alberta, Canada. Essentially carbon, this material also sometimes contains Cretaceous aged amber. Further evidence of the impact of an asteroid as the cause of this last great extinction can be determined from the presence of the element iridium found within this layer. Iridium of this concentration does not form naturally on the earth, but is commonly found in celestial objects such as asteroids. [45+, No Reserve] Fine condition.
Upper Miocene Period, 11-5 million years BP. A mortality insect plate with three complete dragonfly nymphs, Libelluladoris sp., the dragonfly “skimmer” with excellent preservation; presented in a display case. 39.4 grams, 247 grams with case, 13.3cm, case 21 x 16cm (5 3/4"). From an old Bristol paleontological collection; acquired 1950s-1960s; from Piedmont Area, Italy. [No Reserve] Fine condition.
Upper Cretaceous Period, 80 million years BP. A fossil Centrosaurus sp. dinosaur tooth showing the structures, presented in a display case. 0.84 grams, 33 grams with case, 10mm, case 75 x 62mm (1/2"). From an old Bristol paleontological collection; acquired 1950s-1960s; from the Judith River Formation, Havre, Montana, USA. The Centrosaurus is distinguished by having two large hornlets which hook forwards over the frill; a pair of small upwards directed horns is also found over the eyes. The frills of Centrosaurus were moderately long, with fairly large fenestrae and small hornlets along the outer edges. [No Reserve] Fine condition.
Cretaceous Period, 90 million years BP. A group of eleven teeth from the predatory fish Enchodus sp. (sabre-toothed herring), all with good enamel. 28 grams total, 30-39mm (1 1/4 - 1 1/2"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; from the phosphatic deposits of Ouled Abdoum, Morocco. [11, No Reserve] Fine condition.
Cretaceous Period, 100-93 million years BP. A group of two Acanthoceras sp. ammonites, both having clean centres; presented on a custom-made display stand. 2.5 kg, 11-13.5cm, stand 26cm wide (4 1/4 - 5 1/4"). From an old Bristol paleontological collection; acquired 1950s-1960s; from Agadir, Morocco. [2, No Reserve] Fine condition.
Ordovician Period, 450 million years BP. A mortality plate displaying four large brittlestars, Ophiura sp. showing much detail. 1.7 kg, 29.5cm (11 1/2"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; acquired 1980s; from Kataoua formation, Blekus, Morocco. Fine condition.
Cretaceous Period, 99-93 million years BP. An example of Carcharodontosaurus saharicus, the African T-Rex; with clearly visible serration and good enamel. 42 grams, 62.68mm (2 1/2"). Property of a Lincolnshire gentleman; formerly in an old Lincoln collection; acquired 1980s; from the Tegana formation, Sahara Desert, Morocco. The Carcharodontosaurus saharicus was one of the largest predators (larger than its distant North American T-Rex cousin) of all time and is also related to the allosaurus and the South American giganotosaurus. Very fine condition.
Eocene Period, 58-36 million years BP. The group comprises a Knightia alta (upper) and a Diplomystus sp. (lower) fossil fish, on the matrix plaque. 612 grams, 22.5cm (8 3/4"). From the Pradi Collection, Boston, USA; acquired during the 1980s; from the Green River Formation, Wyoming, USA. Fine condition.
Cretaceous Period, 99-93 million years BP. A large tooth of the mid-sized Bahariasaurus ingens carnivore dinosaur; the tooth displays good serrated edges and excellent enamel. 22 grams, 65.59mm (2 1/2"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960; from the Tegana Formation, Morocco. Very fine condition.
Cretaceous Period, 125-113 million years BP. A group of five dinosaur teeth, from the dinosaur Spinosaurus maroccanus; of good size with excellent enamel. 46 grams, 39-52mm (1 1/2 - 2"). From the collection of the palaeontologist R Gledhill; collected between 1930 and 1960; from the Tegana Formation, Taouz, Morocco. The spinosaurus was both a beachcomber type scavenger and an active hunter, taking small stranded plesiosaurs, pterosaurs, turtles and large fish. [5, No Reserve] Fine condition.
Albian Cretaceous Period, 113-100 million years BP. A large A-grade cut and polished pair of Cleoniceras sp. ammonite displaying the distinctive pattern of the chambers; with card tray. 503 grams, 13cm (5"). From the collection of the palaeontologist R. Gledhill; collected between 1930 and 1960; from Madgascar. [2, No Reserve] Very fine condition.
Pleistocene Period, 40000-15000 BP. A partial atlas vertebra, probably Bos primigenius or aurochs. 870 grams, 24cm (9 1/2"). From an important London collection, acquired in the 1990s; from the North Sea, UK. The atlas vertebra is located immediately below the skull and links skull and spinal column. [No Reserve] Good condition; one side chipped.
Eocene Period, 55-33 million years BP. A group of three rare unclassified agatized Dicotaledon cone specimens clearly showing the external structures. 48 grams total, 4-5cm (1 1/2 - 2"). From an old Bristol paleontological collection; acquired 1950s-1960s; from the Western Sahara Desert, Morocco. These are a new species from the old that have been recently discovered. [3, No Reserve] Fine condition.

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18240 Los(e)/Seite