TOOTH PROFILE / LIVING

Frilled sharktooth identification

Three long, slender, backward-curving cusps on a broad base, forming a trident-like tooth.

LivingChlamydoselachus anguineusLiving; lineage extends deep into the fossil record
FIELD VERDICT

Three long, slender, backward-curving cusps on a broad base, forming a trident-like tooth.

Fragile cusps break easily; incomplete teeth can resemble other primitive sharks.

01

ORIGINAL VISUAL PLATE

Front, edge and jaw position.

FRONT / LABIAL VIEWEDGE / PROFILESMOOTH EDGEPOSITION CHANGES SHAPE● ANTERIOR● LATERALTUFFSHARK ORIGINAL TOOTH PLATEDIAGRAMMATIC · NOT TO SCALE
Original TuffShark vector illustration. Trait emphasis is diagrammatic; it is not a specimen photograph or a substitute for an associated jaw.
02

IDENTIFICATION TRAITS

What to inspect.

Crown shape
Several cusps
Cutting edge
Smooth edge
Side cusplets
Several smaller cusps
Root
Wide / nearly flat root
Reference tooth height
About 518 mm, depending on age and jaw position
Jaw variation
Three-pronged teeth repeat through both jaws to trap soft prey.
03

ECOLOGY + SCALE

The shark behind the tooth.

Habitat
Deep outer shelves and continental slopes.
Diet
Squid, fishes and small sharks.
Estimated shark size
Usually 1.3–1.7 m (4–5.5 ft); maximum near 2 m.
Bite force
No reliable species-specific value is established; bite force changes with body size and bite point.
Fossil occurrence
Chlamydoselachid teeth occur in Cretaceous and younger deposits.
Time range
Living; lineage extends deep into the fossil record
04

FUNCTION

Form follows feeding.

Rows of delicate multi-cusped teeth form a prey-trapping array rather than a broad cutting blade.

05

LOOKALIKES

Do not stop at the first match.

AUTHORITATIVE REFERENCE

Smithsonian Ocean

The visual plate is original TuffShark artwork and is not copied from the reference. Use the source alongside formation age, locality and associated material.

Open source ↗
HAVE A TOOTH TO CHECK?

Put these traits into the identification flow.

Start a ranked identification →