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1.4" Cardiospermum Coloradensis Balloon Vine Fossil Plant Leaf Eocene Age Utah

$ 11.61

Availability: 100 in stock
  • Item must be returned within: 30 Days
  • Condition: Location: Green River Formation, Uintah County Utah Weight: 2.9 Ounces Dimensions: 3 Inches Long, 2.1 Inches Wide, 0.5 Inches Thick (Plate) Leaf Dimensions: 1.4 Inches Long, 0.7 Inches Wide
  • All returns accepted: Returns Accepted
  • Country/Region of Manufacture: United States
  • Return shipping will be paid by: Seller
  • Restocking Fee: No
  • Refund will be given as: Money Back

    Description

    1.4" Cardiospermum Coloradensis Balloon Vine Fossil Plant Leaf Eocene Age Utah
    1.4" Cardiospermum Coloradensis Balloon Vine Fossil Plant Leaf Eocene Age Utah
    Location: Green River Formation, Uintah County Utah
    Weight: 2.9 Ounces
    Dimensions: 3 Inches Long, 2.1 Inches Wide, 0.5 Inches Thick (
    Plate
    )
    Leaf Dimensions: 1.4 Inches Long, 0.7 Inches Wide
    The item pictured is the one you will receive.
    This is a genuine fossil, not a replica.
    Eocene Age 56 million years ago
    Cardiospermum Coloradensis
    are fossil plant remains found in the famous Green River formation deposits, which are of Eocene age, dating them to between 53 to 48 million years old and were collected in Colorado, USA. This plant belongs to the soapberry family, which are often easily recognized in modern times due to their vibrant bright red fruit. The leaves themselves are a dark brown color, while the shale matrix, as expected of these fossils is pale sandy color.
    While the Green River Formation is a Lagerstätte most known for its exquisite fish fossils, the fossil flora and fauna are truly diverse, including plants, invertebrates, and vertebrates (including reptiles, mammals) with even Eocene stromatolites represented. This willow leaf shows nice venation. There is also a tiny insect, not so well preserved. Insects are not commonly seen in Green River fossils.
    Fossil representatives abundant in shales of the early Middle Eocene of the Green River Formation in Utah, Colorado, and Wyoming, and it is clear that the family was an important component of vegetation that surrounded the large lakes in which these shales were deposited.
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