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Fossils found along the cliffs of the Potomac River just south of D.C. are from Aquia formation, which is from the Selandian,
or late Paleocene. This time period markes the final ending of the supercontinent Pangaea, as the last vestige split apart into Antarctica and Australia. Also, at the end of the Paleocene, the climate was warming from the cool Paleocene climate into the tropical climate of the Eocene. Another special event marked in the Paleocene is the development of grass. Without the evolution of grass, mankind would have long perished from lack of cutting it. Again, as in the Eocene and Miocene, this area was just offshore in the young, and much narrower Atlantic Ocean. The fossiliferous deposits contain mainly shells, fish, and shark teeth (including the fiercest shark of the Paleocene, Otodus obliqqus), ray plates, and crocodile and turtle material. These deposists are to old to find marine mammals, as mammals did not return to the sea for another 4 - 6 million years, in the Eocene. |