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LOT 2629
A Collection of Fossils
DEVONIAN-JURASSIC PERIOD, CIRCA 417-145 MILLION YEARS B.P.
3 - 6 1/8 in. (584 grams total, 7.4-15.5 cm).
Mixed group including Perisphinctids indogermanus ammonite, Goniatite and Orthoceras. [3, No Reserve]
ProvenanceFrom a collection acquired on the UK art market from various auction houses and collections mostly before 2000.
From an important Cambridgeshire estate; thence by descent.
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AUCTIONS:
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Unpolished Natural Amber Group
Oligocene Period, circa 45 million years B.PSold for (Inc. bp): £59
A large group of unpolished amber pieces, each pierced through the centre for stringing. 41 grams total, 8-21 mm
Ian Wilkinson collection, Nottinghamshire, UK, formed since 1985. -
Very Large Cut and Polished Mauve Agate Geode Slice
Sold for (Inc. bp): £910
Translucent with a thick band of white quartz crystals, dyed to enhance the internal structure. 640 grams, 23.3 cm
From Brazil. Ex Mineral Imports, London, UK. Gregory, Bottley & Lloyd (Gregory's), Harwich, UK. -
Campo Del Campo Cielo Meteorite
Fell 6000-5000 years B.P.Sold for (Inc. bp): £195
A nickel-iron meteorite (IAB). 76.6 grams, 49 mm
From a Lincolnshire, UK, collection.
A crater field of roughly 26 craters was found in the vicinity of this crater, which is estimated to date to 4-5 thousand years BP. The age of the meteorite itself is thought to be c.4.5 billion years, formed as part of the development of this solar system. The largest two fragments, the 30.8 ton Gancedo and 28.8 ton El Chaco, are among the heaviest meteorite masses ever recovered on Earth. In 1576, the governor of a province in Northern Argentina commissioned the military to search for a large mass of iron, which it was believed the local people claimed had fallen from the sky and which they used for their weapon production. The expedition discovered a large mass of metal which was assumed to be an iron mine and brought back a few samples, which were described as being of unusual purity. Following the legends, in 1774 Don Bartolomé Francisco de Maguna rediscovered the iron mass. He himself did not believe that the stone had fallen from the sky and assumed that it had formed by a volcanic eruption. However, he sent the samples to the Royal Society of London. In 1990 it became protected by law.