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LOT 2737
Natural History - Fossil Seed Fern Pair Group
MIDDLE PENNSYLVANIAN PERIOD, CIRCA 300 MILLION YEARS B.P.
2 1/8 - 2 5/8 in. (175 grams total, 54-66 mm).
Comprising two Pecopteris sp. fossil seed fern pairs. [4, No Reserve]
ProvenanceFrom the Mazon Creek Fossil Beds, Braidwood, Illinois, USA.
Collected 1930-1960.
From the collection of the palaeontologist R Gledhill.
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AUCTIONS:
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LOT 2737
Natural History - Fossil Seed Fern Pair Group
Sold for (Inc. bp): £26
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Natural History - Fossil Ginko Leaf
Carboniferous Period, 359-299 million years B.P.Sold for (Inc. bp): £33
The light-coloured specimen on an irregular matrix. 88 grams, 73 mm
From a Cambridgeshire, UK, collection. -
Natural History - Mixed Historic Fossil Collection
Permian-Pliocene Period, circa 298-2.4 million years B.P.Sold for (Inc. bp): £33
Comprising fossilised wood, leaf fossils, a gastropod mollusc, sea urchin, nautilus shell, a bivalve, gastropods on a matrix, and a replica beetle on a matrix; all fossils with old labels. 1.62 kg total, 7.6-11.9 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. Each specimen accompanied by an original historic information 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.