Gastroliths
Gastroliths are gizzard stones that are fossilized. This type of fossil is generally found by researchers who are studying reptiles. The stones are commonly found in the gizzards of organisms, but only considered gastroliths when found in reptilian remains. One way for a researcher to tell if a gastrolith is authentic is if the stone is found in bones and situated where the stomach should have been. The stones can reveal a lot about the feeding habits of ancient reptiles.
Mold and Cast
Mold and cast fossils are common types that occur when an organism is buried under many layers of sediment decays. The impression left behind is known as the mold, while an entire space left behind that has filled with sediment is called a cast. The bones of dinosaurs commonly fall into this category.
Carbonization
Carbonized fossils are another common fossil type, which occurs when carbon-containing organisms are buried and compressed. The result is a black mold that occurs when heat and pressure turn the organism to coal. Insects. leaves, feathers and fish are among the organisms found as carbonized fossils.
Tracks and Footprints
Tracks and footprints are commonly left behind when animals made their way through the mud during prehistoric times. The area where several preserved tracks from the same animal is known as a trackway. The path may also have impressions of the animal's tail or other body parts. Such tracks are commonly found in the states of Texas, Arizona and New Mexico.