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LOT 2170
Natural History - Woolly Mammoth Bone Bead Necklace String
DEVENSIAN PERIOD, 110,000-12,000 YEARS B.P.
23 5/8 in. (163 grams, 60 cm long).
Restrung using recently polished Mammuthus primigenius bone beads. [No Reserve]
ProvenanceFrom a late Japanese specialist collector, 1970-2000s.
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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LOT 2170
Natural History - Woolly Mammoth Bone Bead Necklace String
Sold for (Inc. bp): £143
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Natural History - British Fossil Bison Bone Collection
Pleistocene Period, circa 2.6 million-11,700 years B.P.Sold for (Inc. bp): £7
Comprising sections of ribs, vertebrae and other bones from Bison priscus. 1.32 kg total, 7.5-40 cm
From Oxfordshire, UK. From a Norfolk, UK, collection. -
Natural History - Fossil Pine Cone
Eocene Period, circa 55-33 million years B.P.Sold for (Inc. bp): £91
A rare unidentified agatized Dicotaledon fruit specimen. 15.5 grams, 44 mm
From the Western Sahara Desert, Morocco, North Africa. Acquired 1950s-1960s. From an old Bristol, UK, palaeontological collection. -
Natural History - Knightia Fossil Fish Group
Eocene Period, circa 56-33 million years B.P.Sold for (Inc. bp): £20
Comprising three Knightia alta specimens, each on a rounded matrix. 177 grams total, 80-91 mm
From Wyoming (Green River Formation), USA. 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.
