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Belemnites are the fossilized internal shells (guards) of an extinct order of cephalopods, Belemnitida. These guards are typically bullet-shaped, conical, or cylindrical, and range in size from a few centimeters to over 30 centimeters in length. They are composed of calcium carbonate (calcite) and often exhibit a distinctive radial fibrous structure when broken. The anterior end of the guard often shows a conical cavity (alveolus) where the phragmocone (chambered shell) was housed. The surface can be smooth or exhibit longitudinal grooves or ridges.
How to Identify
- Color
- Typically light to dark brown, grey, black, or yellowish, depending on the surrounding sediment and diagenesis.
- Luster
- Dull to earthy on the exterior; can be vitreous to pearly on fresh breaks, especially along crystal faces.
- Texture
- Smooth to slightly rough on the exterior. Freshly broken surfaces often show a radial fibrous texture.
- Crystal Form
- Not a mineral crystal, but a biogenic structure. The overall form is typically bullet-shaped, conical, or cylindrical. Internally, it's composed of microcrystalline calcite with a radial arrangement.
- Cleavage
- No true mineral cleavage, but can fracture conchoidally or irregularly, often revealing the radial fibrous structure.
- Geological Environment
- Found in marine sedimentary rocks, particularly limestones, marls, shales, and chalks, deposited in shallow to deep marine environments. They are common in deposits from the Jurassic and Cretaceous periods.
Key Facts
- Hardness: 3-4 (Mohs scale) for the calcite guard, but can vary slightly due to diagenesis.
- Specific Gravity: Approximately 2.7-2.9 g/cm³
- Crystal System: Trigonal (calcite component)
- Color: Brown, grey, black, yellowish
- Luster: Dull to earthy (exterior), vitreous to pearly (fresh break)
- Transparency: Opaque
- Fracture: Conchoidal to irregular, often revealing radial fibrous structure
- Cleavage: None (as a fossil structure), but the constituent calcite has perfect rhombohedral cleavage
- Composition: Calcium carbonate (CaCO₃) in the form of calcite
Quick Check
- Color: Brown, grey, black, yellowish
- Luster: Dull to earthy (exterior), vitreous to pearly (fresh break)
- Streak: White
Physical Characteristics
- Crystal Habit: Not a mineral, but a biogenic structure. The internal calcite is microcrystalline with a radial fibrous arrangement.
- Cleavage Type: None (as a fossil), but the constituent calcite exhibits perfect rhombohedral cleavage in three directions.
- Fracture Type: Conchoidal to irregular, often revealing the internal radial structure.
- Tenacity: Brittle
- Luster Type: Dull to earthy on the exterior; vitreous to pearly on fresh breaks.
Formation
Belemnites are extinct marine cephalopods, closely related to modern squids and cuttlefish. The 'Belemnite' commonly found as a fossil is the internal, bullet-shaped, calcitic guard (rostrum) of the animal. This guard was located at the posterior end of the belemnite's body and served as a counterweight and possibly for muscle attachment. It is composed of densely packed, radially arranged calcite crystals, making it resistant to decomposition and fossilization.
Usage
Belemnite fossils are significant index fossils for dating Mesozoic marine sedimentary rocks. They are also popular among fossil collectors and are sometimes used in educational displays. Historically, they were sometimes ground into powder for medicinal purposes, though this practice has no scientific basis.
Age Distribution
Jurassic to Late Cretaceous periods (approximately 201 to 66 million years ago)
Where to Find
Dorset Coast, England
Part of the Jurassic Coast World Heritage Site, famous for abundant and well-preserved belemnite fossils, particularly in the Lias and Kimmeridge Clay formations.
Germany
Numerous localities, especially in Lower Saxony and Bavaria, yield belemnite fossils from Jurassic and Cretaceous marine deposits.
France
Significant occurrences in Jurassic and Cretaceous strata, particularly in regions like Normandy and the Paris Basin.
Russia
Extensive Mesozoic marine deposits across Russia contain numerous belemnite fossils.
United States
Found in Cretaceous marine sediments, particularly in states like Texas (e.g., Austin Chalk) and the Western Interior Seaway deposits.
Finding Tips
Look in Marine Sedimentary Rocks
Focus on outcrops of limestones, shales, marls, and chalks from the Jurassic and Cretaceous periods. Belemnites are rarely found in non-marine or igneous/metamorphic rocks.
Search for Distinctive Shapes
Keep an eye out for bullet-shaped, conical, or cylindrical objects. They often stand out from the surrounding matrix due to their denser composition.
Check Weathered Surfaces
Erosion can expose belemnites. Look for them on weathered rock faces, in scree slopes, or along shorelines where marine sediments are exposed.
Examine Broken Rock
Sometimes, a broken rock will reveal a cross-section of a belemnite, showing its characteristic internal structure.
Consult Geological Maps and Guides
Use local geological maps and fossil-hunting guides to identify specific formations and localities known for belemnite occurrences.
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Crinoidea (Class)
Also known as: Sea Lily Stem
Scientific Classification
- Mineral Class
- Not a mineral, but a fossilized biogenic structure.
- Group
- Cephalopoda (Class), Coleoidea (Subclass), Belemnitida (Order)
- Crystal System
- Trigonal (for the constituent calcite)
- Chemical Formula
- CaCO₃ (for the constituent calcite)
- Composition
- Calcium carbonate (calcite)
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