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Highly Detailed Mimosite Coloradensis Fossil Plant Leaf Green River Eocene Age

$ 10.55

Availability: 100 in stock
  • Item must be returned within: 30 Days
  • Refund will be given as: Money Back
  • All returns accepted: Returns Accepted
  • Return shipping will be paid by: Seller
  • Restocking Fee: No
  • Condition: Location: Green River Formation, Uintah County Utah Weight: 1.9 Ounces Dimensions: 2.4 Inches Long, 1.6 Inches Wide, 0.4 Inches Thick (Plate) Leaf Dimensions: 1.5 Inches Tall, 0.4 Inches Wide
  • Country/Region of Manufacture: United States

    Description

    Highly Detailed Mimosite Coloradensis Fossil Plant Leaf Green River Eocene Age
    Highly Detailed Mimosite Coloradensis Fossil Plant Leaf Green River Eocene Age
    Location: Green River Formation, Uintah County Utah
    Weight: 1.9 Ounces
    Dimensions: 2.4 Inches Long, 1.6 Inches Wide, 0.4 Inches Thick (
    Plate
    )
    Leaf Dimensions: 1.5 Inches Tall, 0.4 Inches Wide
    Item pictured is the one you will receive.
    This is a genuine fossil, not a replica.
    Eocene Age 56 million years ago
    The family
    Fagaceae
    , or beech family, comprises about 600 species of both evergreen and deciduous trees and shrubs, which are characterized by alternate simple leaves with pinnate venation, unisexual flowers in the form of catkins, and fruit in the form of cup-like ( cupule) nuts. Fagaceous leaves are often lobed and both petioles and stipules are generally present. Fruits lack endosperm and lie in a scaly or spiny husk that may or may not enclose the entire nut, which may consist of one to seven seeds. The best-known group of this family is the oaks, genus
    Quercus
    , the fruit of which is a non-valved nut (usually containing one seed) called an acorn. The husk of the acorn in most oaks only forms a cup in which the nut sits.
    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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