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LOT 2458
Natural History - Fossil Shrimp
CRETACEOUS PERIOD, CIRCA 145-65 MILLION YEARS B.P.
4 in. (113 grams, 10 cm).
Carpopenaeus sp. on a rectangular matrix. [No Reserve]
ProvenanceFrom a Lincolnshire, UK, 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 - Composite Fossil Mosasaur 'Marine Dinosaur' Jaw Pair
Cretaceous Period, circa 145-65 million years B.P.Sold for (Inc. bp): £130
Comprising a pair of Mosasaur prognathodon jaw section, each with three teeth. 1.16 kg, 19 cm
From a Cambridgeshire, UK, collection.
The Mosasaur is an extinct, large marine reptile dinosaur with a snake-like body, long snout and paddle-like limbs. found worldwide, they competed with other well-known sea predators of the Late Cretaceous, such as plesiosaurs and ichthyosaurs, for food, existing primarily on a diet of ammonoids, cuttlefish and fish. -
Natural History - Historic 'Naca, Mexico' Selenite Crystal Specimen
Sold for (Inc. bp): £20
Displaying large tabular crystals with fine examples if swallow-tail contact twins, collection number 533; purchased for £25.00 from the Natural History Museum Shop, in 1983. 139 grams, 71 mm
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 - Al Mahbas Fall Chondrite Meteorite
Sold for (Inc. bp): £98
An irregular stony meteorite. 183 grams, 74 mm
Found near Al Mahbas, Sahara Desert, Morocco.
Chondrites originated in the asteroid belt where collisions and gravitational perturbations put them into Earth-crossing orbits. Chondrites formed as part of the formation of their parent asteroids approximately 4.56 billion years ago. They also contain material that predates the formation of the solar system, including organic matter and tiny grains that formed around dying stars.
