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Entry 132Filed under Breeding

About 360 Million Years Ago, the Seas Over Ohio Held a Predator With Bone Blades Instead of Teeth

About 360 million years ago, an armored fish called Dunkleosteus lived in the sea covering what is now Ohio. Its sharpened bone jaw edges—not true teeth—helped make it a formidable predator.
3-minute read By Animalso Team

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Dunkleosteus terrelli was a heavily armored fish that lived in the Late Devonian sea covering what is now Ohio. Its jaws were edged with sharpened bone rather than true teeth, giving it an imposing way to cut prey. “Cleveland” points to where its fossils are found today—not a city the animal ever inhabited.

Why is a prehistoric predator associated with Cleveland?

In the Late Devonian, roughly 375–359 million years ago, an inland sea covered the region that is now Ohio and connected to the open ocean. Rocks in the Cleveland Member of the Ohio Shale—where Dunkleosteus terrelli fossils occur—date to about 360–359 million years ago, according to the Ohio Department of Natural Resources’ Division of Geological Survey.

The modern geography can be misleading: Cleveland did not exist, and the animal did not swim through a city. The name reflects the fossils’ geological and museum context. The black shale formed as fine sediment and organic matter accumulated in the Appalachian Foreland Basin. Later movement of Earth’s plates helped bring those ancient deposits to their present location.

Did Dunkleosteus really have teeth?

No—not true teeth like those found in many other armored fishes of its time. Dunkleosteus had exposed, sharpened bony edges along its jaws, as well as fang-like bony projections called odontoids. The Ohio Geological Survey compares the upper and lower jaw edges to self-sharpening scissors. So “toothless” does not mean smooth-mouthed: its cutting surfaces were part of the jaw bones themselves.

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This arrangement was unusual among arthrodires, the group of armored fishes to which Dunkleosteus belonged. Many relatives had actual teeth. Bone-blade specializations also evolved independently in some other arthrodire groups, so one dramatic reconstruction should not stand in for every placoderm.

What did it eat, and how did it hunt?

The blade-like jaws are interpreted as adaptations for taking large prey, including other fishes. That is an inference from anatomy, not a preserved record of every meal or hunt. Claims about the precise mechanics of its feeding have also changed as researchers revisit its anatomy.

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A peer-reviewed study first published on November 20, 2025, reexamined specimens chiefly from the Cleveland Museum of Natural History. The authors infer that the skull contained substantially more cartilage than older reconstructions assumed and revise interpretations of jaw-muscle attachments. They argue that earlier claims for suction feeding are questionable and that older bite-force estimates need reassessment in light of the revised muscle reconstruction. A dramatic bite-force figure should therefore not be treated as settled fact.

How large was Dunkleosteus?

Published estimates differ. The Ohio Department of Natural Resources’ 2019 geological survey article gives an estimated maximum length of 6–8.8 meters (20–29 feet). Case Western Reserve University’s 2025 research announcement uses 14 feet. Those are attributed estimates, not a single agreed measurement; the available sources do not establish why the figures differ. Any length should be read with its source attached.

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What fossils have been found?

The species is known mainly from head and thoracic shields, along with some vertebrae and a pectoral fin. Black shale and low-oxygen conditions on the ancient sea floor favored preservation, but the fossil record remains incomplete. Armor and jaw elements are better represented than soft anatomy, so a full-body image necessarily includes reconstruction rather than direct fossil evidence.

That limitation matters when interpreting body shape, swimming, and feeding. The 2025 anatomical study updates ideas about cartilage and jaw muscles, but it does not turn incomplete remains into a complete record of the animal’s soft tissues or behavior.

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How were the Cleveland fossils discovered?

Ohio geological survey accounts credit Jay Terrell with finding fossils in 1867 in black shale along the Lake Erie shore at Sheffield Lake. Ohio geologist John Strong Newberry described them in 1873. The species name terrelli honors Terrell; the genus name Dunkleosteus honors Cleveland Museum of Natural History paleontologist David Dunkle.

The shale could be difficult to search. In a 1926 passage quoted by the Ohio Geological Survey, Professor Jesse Earle Hyde wrote: “It is almost useless for a man, untrained in the ways of the black shale, to come into the region hoping to find much.”

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