Priscacara liops

    SKU
    X485
    Out of stock
    $195.00
    Overview

    A very nice, Large Priscacara (Cockerellites) liops fish from the 18 inch layer. The Priscacara liops is an extinct Perch from the Eocene age (50 MYA), Green River Fm., Lincoln Co. Wyoming. This piece is from the 18 Inch Layer which is extremely hard and difficult to prepare. It also provides the most detailed, highly preserved fossils. Exceptional preservation and preparation. No repair. All natural. Plate size is 7-1/2" x 12".  A wonderful display piece!  Authenticity guaranteed.  Note - This item weighs 4.5 lbs. An international shipping surcharge will be applied to "Free Shipping". Please inquire for cost.

    X485                SIZE: 5"

     

    The Priscacara liops is an extinct Perch (a Priscacaridae fish). The Priscacara genus is the most popular of the Green River fish fossils and resembles a today's sunfish in shape. This specimen is from the 18" inch layer - the hardest layer that yields the highest quality for the Green River Fm. fish. This specimen shows incredible detail with incredible fin and other bone definition. Exceptional preservation and preparation. Wonderful display piece. The Priscacara is an  less common fish in the Green River Fm. This is an excellent quality fish from the ancient Lake Gosiute - Eocene age (50MYA). An excellent specimen!

    Note this fish was renamed as Cockereillites liops.

    Green River Formation - 

    The composition of the Green River rock formation consists of a group of sedimentary rock layers formed in a huge system of lakes. The source of the Green River Formation happened mostly during the Eocene Period between 59-33 million years ago. It's also located along the Green River of today, covering parts of Utah, Wyoming, and Colorado. In this post, we'll concentrate on the various layers that contain fossil fish.

    Streams exiting mountainous regions brought vast quantities of sand, silt, mud, and minerals dispersed into lakes that filled the intermountain foundation. Over time the lakes started to be infilled with sand, silt, and mud. The minerals dissolved also altered the reservoir waters' composition. Plentiful plants flourished in large swampy areas that formed along the lakeside margins.

    Most of the Green River Formation fossils in southwest Wyoming are extracted from Fossil Lake. This region was divided into two 'fossil zones' both of which include well-preserved fossil specimens. One layer is referred to as the “Split fish layer”, which is loaded fossil fish as well as other fossils. This layer is about 6 feet thick. The sediment was heavily laminated in the Split fish layer, meaning it has many layers that are easily separated to expose fossils. The second fossil zone is referred as the “18 Inch layer”. The 18 Inch layer is not a laminated layer and as expected it is about 18 inches thick. This second layer also contains abundant fossils which are exquisite, but the fossils are much more difficult to expose and prep since the layer is much denser and not layered.

    It can be very hard to determine the exact age for a rock structure. However, through the study of volcanic soil particles, the fossil bearing rocks of the Green River Formation were dated to be 53 to 48 million years ago. Volcanoes in what would become Yellowstone National Park to the north and the San Juan volcanic field to the south formed intermittent dust storms that fell in thin layers of volcanic ash into the still waters of the lake. These deposits of ash have been preserved and contain fine mineral grains that have crystallized mostly during a volcanic eruption. The researchers obtained specimens of these ash fall layers to date the Green River Formation fossils.

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    Size5"
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