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Freedom251 › Blog › CT imaging

What Evidence Can Identify Which Dinosaur Made a Fossil Bite Mark?

By Freedom251 Team · · 8 min read

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Identifying the maker of a fossil bite mark requires more than matching a hole to a dinosaur tooth. Researchers must first show that the feature is a tooth trace, document its three-dimensional geometry and microscopic details, exclude anatomy and pathology, compare it with teeth of animals that lived in the same place and time, and then state a conclusion no more specific than the evidence allows. The biter may be identifiable only as a broad group—or may not have been a dinosaur at all.

What a fossil bite mark can—and cannot—tell you

A tooth-marked bone records contact between a tooth and bone, but it does not automatically preserve the identity of the animal. Several different teeth can produce similar pits or grooves, and one animal can leave different traces depending on bite angle, force, tooth wear and whether the contact occurred during feeding, scavenging, defense or another interaction.

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The 2023 PeerJ study Bite and tooth marks on sauropod dinosaurs from the Morrison Formation puts the value of such evidence plainly: “Tooth-marked bones provide important evidence for feeding choices made by extinct carnivorous animals.” That evidence is strongest when multiple independent observations agree. A species-level name is justified only when the trace has features that distinguish one taxon from all credible alternatives.

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Step 1: Establish that the feature is really a tooth trace

Inspect the bone and its context before interpreting the mark

A depression, hole or channel can be a natural opening, a break, a disease-related lesion, insect damage, abrasion or another post-mortem alteration. The 2026 PLOS ONE study of a Maastrichtian Edmontosaurus annectens bonebed in Wyoming’s Lance Formation warns that neurovascular foramina and pathological lesions have been mistaken for tooth traces when context is ignored.

Examine the surrounding surface, the shape of the opening and the internal walls. A true tooth contact should fit a mechanical interaction with a tooth, while a foramen should connect with the bone’s vascular or nerve canals and a lesion may show abnormal bone growth, resorption or healing. These distinctions are not made from a photograph of one isolated mark; the host bone, preservation and nearby features matter.

Record every feature, not just the most dramatic one

For each suspected trace, document:

  • Outline and cross-section, including whether it is circular, oval, crescent-shaped, linear or irregular.
  • Length, width and maximum depth, measured in a stated unit and at a defined point.
  • Orientation relative to the bone’s long axis, joint surface and cortical structure.
  • Whether the feature is a pit, puncture, score, gouge, furrow or a combination.
  • Spacing and repetition: isolated marks, parallel sets, opposing pairs or repeated tooth rows.
  • Fine ridges or striations on the floor and walls.
  • Crushing, cracking, displaced bone or evidence that the surface was already damaged.
  • Whether the mark is healed, unhealed or too poorly preserved to determine.

No single shape is universally diagnostic. Interpretation comes from the combination of geometry, surface texture, arrangement and specimen context.

Step 2: Characterize tooth geometry and microscopic detail

Use dimensions and arrangement as a mechanical test

Measure traces in three dimensions where possible. A tooth’s cross-section, curvature and penetration depth constrain the shape of the mark, while spacing between repeated marks can reflect the spacing of teeth or movement of a jaw across bone. A broad, shallow scrape implies a different contact from a deep puncture; a paired groove may indicate a tooth edge or two interacting surfaces, but it is not automatically a dinosaur signature.

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Orientation also matters. A mark running along a bone can result from a tooth being dragged, whereas a near-perpendicular puncture may reflect direct loading. These interpretations remain hypotheses until they are tested against tooth morphology and alternative processes.

Look for serration striations

Minute parallel striations can be produced by denticles on a serrated tooth. The 2020 Proceedings of the Royal Society B study on a stressed Late Jurassic ecosystem used such patterns, together with larger trace features, to evaluate theropod feeding, scavenging and possible cannibalism. Striation spacing and orientation can help identify a tooth type and estimate a minimum tooth or animal size, but preservation must be good enough to show the ridges and the comparison must use appropriate reference teeth.

Step 3: Compare the trace with plausible teeth

Build a candidate set from the fossil ecosystem

Once a biological tooth origin is supported, list every animal that could plausibly have contacted the bone. Include carnivorous dinosaurs, other reptiles, mammals and non-biological alternatives that have not yet been excluded. Compare the trace with actual teeth or well-supported reconstructions from the relevant time and place rather than with a generic image of a “dinosaur tooth.”

Useful comparison questions include:

  • Can the candidate tooth produce the observed cross-section, depth and curvature?
  • Does its serration or denticle pattern match the microscopic striations?
  • Does tooth spacing fit repeated marks or paired grooves?
  • Is the candidate’s estimated tooth and body size compatible with the trace dimensions?
  • Could the candidate’s jaw movement create the observed orientation and surface damage?

Similarity is not proof. Several theropods may have overlapping tooth shapes, and a worn or broken tooth can leave an atypical mark.

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Step 4: Use geological, anatomical and assemblage context

Identify the host specimen

Record the host bone and host animal as precisely as preservation permits. A mark on a rib carries different mechanical implications from one on a dense limb shaft. Note the formation, geological age, geographic locality, depositional setting, preservation history and associated fossils. These data define which potential biters were present and whether the contact occurred before burial, during scavenging or after fossilization.

Check whether the candidate lived there and then

Context narrows the candidate list but does not independently identify the maker. A tooth that fits the geometry is a weak candidate if its animal is absent from the formation; conversely, a common predator remains only a possibility if another animal’s teeth fit the trace better.

The Morrison Formation study surveyed 68 sauropod bones with bite traces attributed to theropods. That figure is the size of that study’s sample, not a prevalence estimate for sauropod fossils and not a success rate for identifying individual biters. The authors also note that individual traces can be difficult to assign when multiple credible candidates occur in the same ecosystem.

Step 5: Test non-dinosaur explanations explicitly

A dinosaur bone does not guarantee a dinosaur biter

The identity of the victim and the identity of the biter are separate questions. Mammals, crocodile-line reptiles, insects and other animals can damage dinosaur bone, and physical processes can mimic biological traces. Every candidate should be tested against the same measurements and context.

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The Alberta paired-groove example

In a 2010 Palaeontology paper, Longrich and colleagues examined paired grooves on dinosaur bones from Late Cretaceous Alberta. They argued that mammals—most likely multituberculates—were the best candidates after comparing the traces with insect damage and other possible makers. The example demonstrates why “dinosaur bite” should not be built into the question before the evidence is examined.

A defensible analysis therefore asks, “Which animal best explains these traces?” rather than “Which dinosaur made them?” If a non-dinosaur explains the geometry, striations, size and local fauna more convincingly, it should remain the leading interpretation.

Step 6: Add imaging when it answers a specific question

Computed tomography

External inspection cannot show every consequence of a bite. CT can reveal internal cracks, displaced bone, tunnels or remodeling around a trace. In a 2015 Annales Societatis Geologorum Poloniae case study, CT visualization helped distinguish healed from non-healed bite-trace wounds and exposed internal morphology that was not visible at the surface.

CT strengthens the description of the injury and its timing. It does not, by itself, identify a unique dinosaur species: unrelated teeth can create similar internal damage, and imaging cannot supply a missing comparison tooth.

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Three-dimensional surface scanning

High-resolution three-dimensional scans can preserve surface relief, permit repeatable measurements and support comparison of striation patterns. Scanning is most useful when it answers a defined question—such as whether two grooves share a spacing pattern—not when it is treated as an automatic identification system. The available evidence does not establish one universal consumer device or workflow.

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How to compare candidates without overstating certainty

When several animals remain plausible, organize the evidence in a table or matrix. The axes below are comparisons to document, not a validated numerical scoring formula.

Evidence axis Question to answer What a strong result looks like
Trace geometry Can the candidate tooth create the outline, cross-section, depth and curvature? Physical or digital tooth comparisons reproduce the observed form.
Fine striations Do denticles or cutting edges match ridge spacing and orientation? Microscopic patterns agree in more than one trace.
Size Does the tooth and animal size fit the mark dimensions? The candidate is neither too small to reach the depth nor implausibly large for the setting.
Time and place Was the animal present in the formation and age represented by the bone? Fossil records place it in the relevant ecosystem.
Placement and orientation Could the animal’s jaw motion and feeding behavior reach this part of the bone? The location and direction fit a plausible interaction.
Alternative causes Have anatomy, pathology, insects, abrasion and non-dinosaur animals been tested? Each major alternative is contradicted by morphology or context.

Step 7: Separate three different identification claims

Reports should keep these questions distinct:

  1. Is it a tooth trace? The mark must be distinguished from a foramen, lesion, break or other alteration.
  2. What kind of tooth or animal group made it? Geometry, striations, size and ecology may support a theropod, mammal or another broad group.
  3. Can a particular dinosaur taxon be named? A genus or species requires distinctive evidence that excludes close alternatives.

Use calibrated wording. “Consistent with” means the observation does not conflict with a candidate. “Supports” means several observations favor it over alternatives. “Most likely” is appropriate when one candidate explains the evidence better but is not uniquely demonstrated. Reserve an unqualified species attribution for cases with genuinely diagnostic features and adequate comparative material.

A practical workflow for a specimen

  1. Document provenance. Record formation, age, locality, host bone, associated fauna and preservation history.
  2. Map the surface. Photograph and, where appropriate, scan every suspected mark with a scale and orientation reference.
  3. Measure the trace. Capture length, width, depth, cross-section, orientation, spacing and striation details.
  4. Inspect internal structure. Use CT if the question concerns hidden damage, remodeling or healing.
  5. Rule out look-alikes. Compare with foramina, pathology, fractures, insect traces and sedimentary abrasion on the same or comparable bones.
  6. Assemble candidates. Include all animals known from the time and place, not only dinosaurs.
  7. Compare teeth and mechanics. Test tooth shape, denticles, spacing, size and plausible jaw movement against the measured traces.
  8. Rank, then qualify. State the best-supported group or candidate and list the observations that keep alternatives alive.

What evidence cannot currently provide

There is no general success rate for assigning fossil bite marks to a maker, no universal threshold that guarantees species-level identification and no validated consumer test that returns an exact dinosaur identity. Preservation, incomplete fossil records, tooth wear, multiple sympatric predators and differences in how teeth contact bone all limit precision.

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Even a well-supported theropod attribution may stop at a broad group. Conversely, a mark may remain an unresolved tooth trace if the relevant teeth are unknown or the surface is too damaged. A scientifically useful conclusion makes that uncertainty explicit instead of converting a plausible match into a name the evidence cannot support.

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CT imagingdinosaursfossil evidencefossilsPaleontologytooth traces

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