1.8" Fossil Pine Cone Equicalastrobus Replaced By Agate Eocene Age Seeds Fruit Glyptodon Their teeth were complex

Their teeth were complex

preventing organic decay and enabling the formation of finely laminated limestone layers

Members of Paralenorthis typically exhibit symmetrical

offering a rare window into the composition

Postosuchus was among the largest predators of its era

1.8" Fossil Pine Cone Equicalastrobus Replaced By Agate Eocene Age Seeds Fruit Glyptodon Their teeth were complexLocation: Talsine, Morocco Weight: 0. 5 Ounces Dimensions: 1. 8 Inches Long, 0. 7 Inches Wide The item pictured is the one you will receive. Equicalastrobus petrified pine cones are fossilized conifer seed cones primarily found in the Western Sahara of Morocco, particularly near Talsine and west of Boujdour. These fossils date back to the Eocene epoch, approximately 33 to 55 million years ago. The preservation of Equicalastrobus pine cones occurs