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LOT 2835
Group of Five Polished Fossil Coral Head Hearts
DEVONIAN PERIOD, CIRCA 417-354 MILLION YEARS B.P.
1 1/4 - 1 3/8 in. (115 grams total, 33-36 mm).
Each cut to a heart shape and polished to reveal the internal structure. [5, No Reserve]
ProvenanceFrom a Cambridgeshire, 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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Fossil Ammonite
Lower Jurassic, Toarcian Stage, circa 182-174 million years B.P.Sold for (Inc. bp): £39
A rounded nodule half containing a fossil specimen. 1.15 kg, 12.5 cm
From Whitby, Yorkshire, UK. From a Cambridgeshire, UK, collection.
The specimen is close to Pseudolioceras lythense (Young and Bird). -
Dawn Redwood Fossil Plant Group
Oligocene Period, circa 34-23 million years B.P.Sold for (Inc. bp): £20
Three irregular matrices containing dawn redwood fossils, showing twig and needle leaves. 164 grams total, 47-68 mm
Ex Lincolnshire, UK, collection. -
Fossil Knightia Fish in Matrix
Eocene Period, circa 58-36 million years B.P.Sold for (Inc. bp): £59
A Knightia alta fish on a rectangular limestone matrix with remains of another one on the reverse. 453 grams, 17.8 cm
From a Cambridgeshire, 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.