Florida has a very rich fossil record. Its geologic history is also complex. The rock underlying Florida was originally part of Gondwana and did not become part of North America until the Permian, when Pangaea formed. During the Mesozoic Pangaea began to divide again and Florida was left attached to North America. However, no dinosaur fossils are known from the state. In fact no fossils are known from surface deposits older than the Eocene. Nevertheless, the geologic record contributes to science’s ability to reconstruct the history of Florida’s changing Mesozoic environment. During the Cretaceous the Florida peninsula was much wider due to regions now submerged as continental shelf being exposed to the air. Later into the Cretaceous northern Florida was covered by rising seas connecting the Gulf of Mexico to the Atlantic. This passage of water was called the Suwannee Straits.
A shallow sea grew to cover most of the state during the Tertiary. Clams, echinoderms, and gastropods lived here. Cenozoic limestone formed in such environments is common in Florida and rich in fossils. The oldest fossil-bearing geologic deposits in Florida are of Eocene age. During the Eocene, primitive whales like Basilosaurus and Pontogenous swam over Florida. Other inhabitants included large numbers of shelled invertebrates, sharks, and sirenians. Oligocene fossils in Florida provide evidence for a diverse terrestrial fauna. During the early Miocene uplift and mountain building filled in the Suwannee Strait. At this point coral reefs were forming in the Florida Keys.The Thomas Farm Quarry is the richest source of Miocene mammal fossils in the eastern US. During the ensuing Pliocene, Florida was home to amphibians, bears, a variety of birds, camelids, crocodilians, deer, dogs, dugongs, at least six genera of horses, peccaries, porpoises, relatives of modern elephants, rays, saber toothed cats, seals, sharks, tapirs, turtles, and whales. The remains of all these creatures have been found in a region of Polk County called Bone Valley. Late Tertiary vertebrate fossils are known from southern Florida. during these animals’ lifetimes the southern 300 kilometers of Florida was still under water. Late Tertiary sediments of Gilchrist County preserve badgers, Kodiak bears, camels, dogs, horses, rhinos and more. Mammoths, mastodons, sloths, giant beavers, and ungulates were preserved near Gainesville.
The Pleistocene limestones of the Florida Keys are rich in fossils.The Pleistocene is the epoch of time best represented in Florida’s fossil record. In fact, Florida’s Pleistocene sediments are regarded as the best source of Pleistocene fossils in the world, especially for the mammals of that age. Also, Pleistocene Florida had a greater diversity of terrestrial vertebrates than any other place and time in North American history. At the time, the local sea level began to rise and fall along with the amount of water tied up in the glaciers covering the northern part of the continent. When the sea would withdraw savannas formed. Herds of American mastodon and Mammuthus floridanus browsed and grazes on the local foliage. The gigantic ground sloth Eremotherium was another contemporary large herbivore. Others included the antelope, bison, deer, armored glyptodonts, and the modern horse. These were preyed upon by predators like short-faced bears, saber-toothed cats, lions, and wolves.
- ^ a b c d e f “Florida,” Murray (1974); page 119.
- ^ a b “Florida,” Murray (1974); page 118.
- ^ a b c “Paleontology and geology,” Portell, Hulbert, Springer, and Scotchmoor (2005).
- ^ “Florida: A Great Place to Find Fossils,” Brown (2008); page 14.
- ^ a b c d e “Florida,” Murray (1974); page 121.
- ^ “Ancient Seascapes of the Coastal Plain: Muddy, oxygen-rich environments & Silty-sandy environments preserved as gray shale,” Picconi (2003); page 99.
- ^ “Terrestrial Environments: Intertidal areas, rivers, lakes, land preserved as sand, silt, clay,” Picconi (2003); page 100.
- ^ “Ice Age environments recorded by unconsolidated sediment,” Picconi (2003); page 101.
- ^ “Ancient Seascapes of the Coastal Plain: Clear, shallow environments preserved as limestone,” Picconi (2003); page 99.
- ^ “Florida,” Murray (1974); pages 118-119.
- ^ “Florida,” Murray (1974); pages 121-122.
- ^ “Florida,” Murray (1974); page 122.
- ^ a b c d e f “Appendix C: Major Fossil Clubs,” Garcia and Miller (1998); page 198.
- ^ “Appendix B: Major Fossil Shows,” Garcia and Miller (1998); page 196.