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Shark teeth

Shark & ray teeth (fossils) • bioapatite → fluorapatite‑rich mineralization Hardest part of a shark • skeleton is cartilage → teeth dominate the fossil record Mohs ≈ 5 (apatite) • Luster: enamel(oid) glassy, root matte Age range: Devonian → Pleistocene → Recent shed teeth Famous: Otodus (Megalodon) giants • up to 7+ inches

Shark Teeth — Ocean Stories Written in Enamel

Shark teeth are the ocean’s postcards: small, durable, and everywhere sharks have hunted. Because sharks wear a cartilaginous skeleton that rarely fossilizes, their teeth carry most of the tale—tough caps of enameloid over dentine that survive burial, waves, and time. Shapes reveal diets (needles, blades, crushers), colors tell of sediments, and some specimens grow to palm‑filling legends. Put one in your hand and you’re holding a bite‑sized chapter of deep time. (No floss required.)

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Why so many
Sharks are polyphyodont: conveyor belts of teeth. Individuals can shed tens of thousands over a lifetime.
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What they’re made of
Enameloid + dentine (bioapatite). During fossilization, apatite is often enriched in fluorine and picks up sediment pigments.
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Why they survive
Hard, dense tissues resist decay; isolated teeth transport easily and concentrate in beaches, river gravels, and phosphate beds.

Identity & Anatomy 🔎

Tooth architecture

Each tooth has a crown (the functional cutting/holding surface) and a root (the anchor). The crown is sheathed in enameloid—a hard, fluorapatite‑rich tissue—over dentine. In many fossil forms you’ll notice a darker, triangular band at the crown’s base called the bourlette (common in large lamniform sharks).

A living conveyor belt

Sharks grow multiple rows of teeth. New teeth develop inside the jaw and roll forward as older ones are lost. That’s why teeth are abundant as fossils while cartilage skeletons are rare.

Left vs. right? Upper vs. lower? Tooth curvature, root shape, and the angle of the crown help place a tooth in the mouth. Upper anterior blades differ from lower laterals; symmetrical vs. slanted shoulders are clues.

How Fossilization Colors Teeth 🎨

Mineral swap

Original bioapatite persists but often trades ions with groundwater. Fluorine‑rich environments toughen the enamel; iron, manganese, and organic compounds tint crowns and roots.

Palette by sediment

  • Jet/charcoal — phosphate sands, tannin‑rich rivers.
  • Slate/steel grey — marine clays and limestones.
  • Honey/russet — iron‑bearing sands.
  • Bone‑tan — arid, carbonate‑rich settings.

Color reflects chemistry and burial—not simply age—so black doesn’t automatically mean “older.”

Tumbling & texture

River and surf polish can round roots and soften serrations; teeth from consolidated strata may keep crisp edges and a matte root texture.

Think of each tooth as a tiny mineralogical diary: chemistry writes the entries, water turns the pages.

Tooth Shapes & What They Mean 🦷

Three feeding strategies

  • Grasping: needle‑like, slender teeth for gripping fish and squid (many requiem sharks; sand tigers have long, curved daggers with small side cusplets).
  • Cutting: triangular, flattened, often serrated blades for shearing (white shark lineage; the extinct giant Otodus (Megalodon) shows massive, broad triangles with stout roots).
  • Crushing: pavement teeth, low domes forming mosaics for cracking shells (rays, guitarfish, horn sharks).

Field ID cues

  • Serrations present? Think cutting specialists (coarse vs. fine serrations help narrow lineage).
  • Side cusplets at the shoulders? Common in many Cretaceous and early Paleogene species.
  • Root shape: deep V‑notch vs. broad U; lobes symmetrical or angled.
  • Curvature: blade leaning strongly to one side often indicates lateral rather than anterior position.

Photo tip: Raking light makes serrations pop; a neutral grey card keeps enamel color honest.


Physical Details 🧪

Feature What to expect
Composition Bioapatite (hydroxy/fluorapatite) becoming fluorapatite‑rich during fossilization
Hardness (Mohs) ~5 (enameloid hardest; roots softer, more porous)
Luster Glassy on enamel(oid), matte/velvety on roots
Fracture Conchoidal chips on the crown; roots break more granular
Preservation Isolated teeth, partial roots, occasional associated vertebrae; cartilage rarely fossilizes
Size spectrum From millimeter micro‑teeth to multi‑inch giants (largest megalodon teeth exceed 7″)
Display note: a low, warm spotlight skims the serrations while a cool backlight reveals translucency near the tip—two moods, one tooth.

Under the Loupe 🔬

Serration story

At 10×, cutting teeth show micro‑serrations that can be coarse, fine, or mixed near the tip. Rounded or worn serrations suggest transport.

Enameloid vs. root

The crown’s surface is smooth and glassy; the root is porous with tiny vascular pits. Repairs or restorations often look glossier than natural roots.

Bourlette & shoulders

In large lamniform teeth, a darker bourlette band sits between crown and root. The “shoulders” may carry cusplets—handy for age and family placement.


Look‑Alikes & Mix‑ups 🕵️

Ray dental plates

Appear as flat, polygonal tiles rather than pointed crowns; surfaces show a braided or pebbly texture from fused tooth elements.

Fish & reptile teeth

Bony fish teeth are often smaller, conical, and lack the distinct shark root lobes; mosasaur teeth are thicker, enamelled cones with visible growth lines and separate bony roots.

Cast replicas

Resin casts may show mold seams, uniform “plastic” gloss, and bubble pits. Natural teeth show differing textures between crown and root and subtle mineral staining.

Re‑sharpened “fantasy” teeth

Over‑polished serrations, unnatural symmetry, or a glossy root can signal heavy reworking. A loupe is your best truth‑teller.

Mako vs. white shark

Mako teeth: unserrated, sleek triangles. White shark: serrated blades with strong shoulders. Simple, useful distinction.

Quick checklist

  • Glassy crown + porous root? → fossil tooth, not glass.
  • Serrations crisp and consistent? → cutting specialist lineage.
  • Tiles/pavement? → ray plate, not a shark cusp.

Localities & Ages 📍

Where they’re found

Abundant in marine sediments and reworked river gravels. Notable hunting grounds include the Atlantic Coastal Plain of the USA (beaches & rivers), phosphate mines of Morocco, North Sea dredge spoils, and many coastal cliffs and quarries worldwide. After storms or seasonal low water, fresh finds appear.

Time travel in a tray

Micro‑teeth sieved from sands can span millions of years in one pan—Cretaceous needles, Paleogene cusplets, Neogene blades. Label by formation + age + locality and your tray becomes a tidy timeline.

Labeling idea: “Shark tooth — [family/genus if known], locality, formation, age (e.g., Miocene). Crown length: ___ mm.” Simple, complete, and collector‑friendly.

Collecting & Cleaning 🧼

Finding methods

  • Beachcombing: scan the shell line; teeth sparkle like tiny black triangles among fragments.
  • River screening: shovel gravel into a sifter; gentle swishing reveals glossy crowns.
  • Micro‑teeth: dry sand on a white tray and swirl—dark specks with a triangular glint are candidates.

Cleaning basics

  • Soak in lukewarm water + mild soap; use a soft brush.
  • Avoid acids (can etch) and harsh bleach (can chalk roots).
  • Stubborn matrix: wooden toothpick or bamboo skewer; patience beats abrasion.

Stabilizing & display

  • Fragile roots can be consolidated with a reversible acrylic such as a thin B‑72 solution.
  • Shadow boxes with a neutral backing make serrations stand out.
  • Note any restoration on your label—future you will thank present you.
Photography tip: Place the tooth on matte slate or sand; one small light at ~30° for texture + a subtle reflector opposite for softness. Serrations will sing.

Hands‑On Demos 🔍

Serration spotlight

Hold a small flashlight at a low angle across the edge. Micro‑serrations cast tiny shadows you can count—great for comparing species.

Root vs. crown

Touch the tip to your lip (carefully): the crown feels glass‑cool, the root more chalk‑warm. Texture tells you where enamel ends and dentine begins.

Small joke: sharks don’t worry about misplacing a tooth—there’s another one checking in immediately.

Questions ❓

Are black teeth always ancient?
Not necessarily. Color is driven more by burial chemistry than age. A Holocene river tooth can be as black as a Miocene beach tooth.

How big did megalodon teeth get?
The largest verified crowns exceed 7 inches (~18 cm) from tip to root edge—coffee‑mug‑sized bite marks on history.

Can I ID to species?
Sometimes—especially with large, well‑preserved cutting teeth. Many finds are best labeled to family or genus (and that’s perfectly respectable science).

Why do some teeth have little “mini‑teeth” at the base?
Those are lateral cusplets, common in earlier lineages and in certain positions in the jaw.

Do freshwater sites have shark teeth?
Yes. Rivers rework marine sediments and transport fossil teeth inland, concentrating them in gravel bars and bends.

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