Teeth, jaws and bite mechanics show what an extinct animal could process. Coprolites and gut contents sometimes show what one individual actually swallowed. They can preserve bone splinters, fish scales, plant cuticle, pollen, fungal tissue and microscopic fragments that would otherwise disappear from the fossil record.
This directness has strict limits. A coprolite is commonly found without its producer, digestion removes part of the meal, and one dropping records only a short interval. Material inside an articulated skeleton is easier to associate with the animal, but researchers must still rule out sediment, displaced bones and later contamination.
Interactive evidence guide
Four kinds of digestive evidence
Food residues have completed much or all of the digestive passage. Internal structure and chemistry may confirm the origin, but identifying the producer is usually difficult.
A compact mass preserves the approximate form and position of the intestine. Association can be strong when it lies within an articulated body cavity.
Recognisable prey bones or plant material can record a last meal. Researchers must demonstrate that the objects were inside the body before burial.
Material expelled through the mouth may contain less digested fragments. It can be difficult to distinguish from a coprolite or an ordinary concentration of debris.
Coprolite, cololite and regurgitated mass
A coprolite is fossilised faeces. A cololite is material preserved inside the intestinal tract, sometimes retaining a curved or segmented outline. Stomach contents occupy an earlier part of digestion. A regurgitalite contains expelled food. These categories describe a pathway through a body, not a particular texture or colour.
The distinction matters because digestion sorts evidence. Acids and enzymes attack soft tissues and small bones, while resistant fibres, scales and mineralised fragments survive. A cololite may preserve food before the final stages of processing; a coprolite may offer better chemical evidence that it passed through an intestine.
How a stone is identified as fossil dung
Shape alone is weak evidence. Sedimentary concretions, burrow fills and rolled pebbles can all be rounded or elongated. A secure diagnosis combines geological setting, repeated form, phosphatic or organic composition, a coherent outer boundary, internal folding and food inclusions.

Bone fragments, scales or plant tissues strengthen the digestive interpretation but do not identify the producer by themselves. Size, age, local fauna and expected gut diameter can narrow candidates. A large carnivore living in the formation is not automatically the source of every large bone-rich coprolite.
How the specimen is studied without destroying it
CT and micro-CT reveal dense inclusions and three-dimensional distribution before cutting. Surface microscopy identifies fibres, cells and small bone. Thin sections provide detailed tissues but permanently sample the specimen. Chemical analyses can detect phosphate, organic signatures and mineral replacement.
Each method has a bias. CT favours density contrasts; plant films may be difficult to distinguish. A thin section offers exquisite detail from one plane but can miss rare inclusions elsewhere. Good studies document position and sampling so later researchers can repeat the interpretation.
Bone in the dung of a large theropod
Large, phosphatic coprolites from the Late Cretaceous of Saskatchewan contain abundant crushed bone and have been attributed to a giant tyrannosaurid, plausibly Tyrannosaurus or a close ecological equivalent. The fragments show that a powerful predator ingested bone and that its digestive system did not dissolve every piece.
The producer remains an inference based on size, contents and the local fauna. Coprolites rarely preserve a biological label. They nevertheless complement the robust teeth and bite traces of Tyrannosaurus rex by recording food that travelled through a large carnivore.
Wood, fungi and crustaceans
Some large herbivore coprolites from Cretaceous deposits contain degraded conifer wood, fungal matter and occasional crustacean remains. The mixture challenges the simple picture of an animal eating only tender leaves. Decaying wood can carry fungi and invertebrates, and deliberate or accidental ingestion is not always distinguishable.
Even a surprising inclusion must be assessed against contamination and transport. If a small crustacean entered the dropping after deposition, it would not record diet. Repeated positioning within the mass and comparable specimens make ingestion more credible.
Plants and grasses in the Late Cretaceous
Plant-rich coprolites preserve microscopic cuticle, pollen and phytoliths. Some Indian examples contain grass-related phytoliths, indicating that grasses had diversified before the end-Cretaceous extinction. This does not mean vast modern grasslands or prove which dinosaur produced the droppings.
Coprolites may combine browsing evidence across several plant groups. They reveal food available at one place and time, while teeth and jaw mechanics indicate how it could have been gathered and processed.
How abdominal contents are verified
A credible last meal lies in the body cavity of an articulated or clearly associated skeleton, respects the anatomy and differs from the surrounding sediment. Researchers map every object, inspect whether ribs enclose it, compare mineralisation and ask whether water could have washed it into place.
Separated prey bones beside a disarticulated predator are weak evidence. They may represent a second carcass, scavenging or current transport. The stronger the behavioural claim, the tighter the spatial and taphonomic test must be.
A young Gorgosaurus selected parts of prey
A juvenile Gorgosaurus from Alberta preserves hind limbs of two small caenagnathid dinosaurs in its abdominal region. The association indicates two feeding events and suggests selective consumption of fleshy hindquarters. It is unusually direct evidence for prey choice in an individual young tyrannosaurid.

The meal does not prove that every juvenile always hunted the same prey or that adults shared the preference. Ontogeny changed skull strength, body size and hunting opportunities, so juvenile and adult feeding niches may have differed.
Fish, lizards, birds and mammals
Exceptional small theropods and early birds preserve fish scales, lizard bones, small mammals or other birds inside the body. Such finds show that ecological networks were more complex than the labels “carnivore” and “herbivore”. One predator could take several kinds of small prey.
Direct contents are still snapshots. Seasonal availability, scavenging and age can alter a meal. A fish inside one specimen does not prove strict fish-eating, just as a mammal does not prove a specialised mammal hunter.
Borealopelta and selective plant feeding
The exceptionally preserved nodosaur Borealopelta contains a compact plant-rich abdominal mass. Fern material dominates, with other plants represented in smaller amounts, and charcoal occurs in the mixture. The specimen suggests selective browsing in a landscape recently affected by fire.
Its preservation links the contents securely to one animal, yet the seasonal and local context matters. It is evidence for a particular meal and feeding environment rather than an immutable menu for every nodosaur.
A convincing sauropod cololite
A compact plant mass preserved inside a sauropod body cavity provides one of the strongest cololite candidates for the group. Plant tissues and anatomical position make the digestive interpretation more persuasive than loose plant debris around a skeleton.
Because sauropods rarely preserve gut contents, the specimen tests long-standing inferences drawn from their teeth, necks and huge abdominal volume. It does not establish a single diet for all sauropods across more than one hundred million years.

Deinocheirus and a mixed diet
Deinocheirus combined a broad beak, enormous body and gut region containing gastroliths and fish remains. This supports an omnivorous diet with substantial plant intake and occasional aquatic prey. The anatomy and contents reinforce one another.
Fish remains alone would not determine the entire diet. The beak, jaw, body form, habitat and repeated evidence keep the reconstruction from depending on one inclusion.
What digestion hides
Soft flesh, delicate leaves and fluids are preferentially destroyed. Resistant bone, wood, scales and phytoliths become overrepresented. Large particles may have been deliberately avoided or broken before swallowing. Microbes continue modifying a dropping after deposition.
The absence of a food is therefore not proof it was never eaten. Digestive evidence is most powerful when combined with teeth, wear, isotopes, bite marks and functional anatomy.
One specimen is not a species-wide diet
A coprolite or gut mass records one individual, age, season and place. Species-level claims require multiple specimens and agreement with independent evidence. Assignment to a producer must also remain separate from identification of the consumed material.
This limitation does not make the find unimportant. A single secure meal can demonstrate that a food was eaten, reveal prey handling or show plant groups in the habitat. It simply cannot quantify how often that behaviour occurred.
Frequently asked questions
How is a dinosaur coprolite distinguished from an ordinary stone?
Researchers combine shape, composition, inclusions, internal structure and geological context. No single outward feature proves that a specimen is fossil dung.
Which is better evidence, a coprolite or gut contents?
Gut contents are linked more directly to an animal when preserved inside an articulated body. Coprolites can preserve processed food well but are usually harder to assign to a producer.
Can one coprolite reveal a dinosaur's whole diet?
No. It records one digestive event, and digestion preferentially destroys soft or fragile foods. A species-level diet requires repeated samples and independent anatomical evidence.
Has dinosaur DNA survived in coprolites?
No verified dinosaur DNA has been recovered from Mesozoic coprolites. Mineralisation and deep time destroy long DNA molecules even when microscopic food remains survive.

