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LOT 2636
Natural History - Fossil Ammonite Section
CRETACEOUS PERIOD, CIRCA 113-100 MILLION YEARS B.P.
7 in. (683 grams, 17.6 cm).
Showing the internal chambers of the ammonite. [No Reserve]
ProvenanceEnglish private collection.
CONDITIONTimeLine Auctions follows a vetting process to ensure the authenticity and legality of all items, reinforcing our commitment to integrity and responsible trading. Each antiquity, antique, and coin lot undergoes thorough examination by a vetting committee of at least ten external specialists, professional trade association members, scientists, and archaeologists: Our Vetting Process
AUCTIONS:
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Natural History - Amethyst Crystal Geode Section Group [20]
Sold for (Inc. bp): £20
Comprising large sections of geodes with variously sized amethyst crystals. 1.6 kg total, 45-64 mm
From Brazil. Ex Mineral Imports, London, UK. Gregory, Bottley & Lloyd (Gregory's). -
Natural History - Historic 'Corinto, Minas Gerais, Brazil' Quartz Crystal Specimen
Sold for (Inc. bp): £59
Displaying two large, almost colourless prismatic crystals with some smaller crystals; bought from Gregory, Bottley & Lloyd for £60.00 in the 1980s, with an old label. 217 grams, 13.6 cm
Acquired on the UK mineral and fossil market, since 1970. From the historic mineral collection of Richard Valentine Cain, London, UK, thence by descent. Accompanied by an original historic index file card. -
Natural History - Knightia Fossil Fish Group
Eocene Period, circa 56-33 million years B.P.Sold for (Inc. bp): £52
Comprising three rounded sandstone matrices, each with a Knightia alta specimen. 159 grams total, 75 mm each
From a Lincolnshire, UK, collection.
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.