Part of a series of articles titled Grand Canyon Collections—Paleontology.
Previous: Fossil Tetrapod Foot Prints
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This particular fossil has a somewhat mysterious origin. It was found as a loose block that had tumbled down the side of a cliff. This makes it difficult to determine what this fossil’s original position among the many rock layers of the Grand Canyon was. A fossil’s location within a rock layer is used to determine how old it is, which is why it is important to leave any fossils you may find in place until it can be looked at by an expert. Our best guess for this fossil is that it is early Permian in age. It is also difficult to determine what animal this tooth plate belonged to, since the rest of the body is not preserved. It most likely belonged to a platysomid, an extinct group of fish that had deep bodies and large scales. Instead of individual structures arranged in neat rows, these fish had teeth that formed rough, bumpy plates. They probably hunted shelled animals, and used the tooth plates to crush the shells to get to the meat inside. As the teeth wore out, new ones would grow in from underneath to take their place.
This is mold of a Permian age fish plate. Fish plates are tooth-like structures found in early fish and are known from the Pennsylvanian to the Permian periods. They are somewhat common in the Kaibab limestone, and can be found in expouses in the Grand Canyon.
Information used to describe this fossil was sourced from: https://www.jstor.org/stable/1304267?refreqid=excelsior%3Aa2dba2d64ca0d7b0218fe21a1411aa5d&seq=1#metadata_info_tab_contents
This fossil is in the collections at Grand Canyon National Park, Arizona. Learn about paleontology in the National Park Service: https://www.nps.gov/subjects/fossils/index.htm
Learn more about Grand Canyon National Park’s Centennial: https://www.nps.gov/grca/getinvolved/centennial.htm
Part of a series of articles titled Grand Canyon Collections—Paleontology.
Previous: Fossil Tetrapod Foot Prints
Last updated: May 3, 2021