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Where is Fossilized Crinoid Stem found?

Crinoidia (stem ossicle)

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Fossilized Crinoid Stem occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.

Where to find Fossilized Crinoid Stem

Midwestern United States (e.g., Indiana, Illinois, Kentucky, Missouri)

Abundant in Mississippian-age limestones, forming significant components of crinoidal limestones.

United Kingdom (e.g., Carboniferous Limestone of Northern England)

Commonly found in Carboniferous marine deposits, particularly in areas like County Durham (St. Cuthbert's Beads).

Germany (e.g., Eifel region)

Known for Devonian crinoid fossils, including well-preserved stem ossicles.

Morocco (e.g., Anti-Atlas Mountains)

Rich in Paleozoic marine fossils, including diverse crinoid remains.

Australia (e.g., Canning Basin, Western Australia)

Contains significant Paleozoic marine sequences with crinoid fossils.

Collecting tips

  1. Look in Limestones. Crinoid ossicles are most commonly found in limestones, especially those with a granular or fragmental texture. Examine weathered surfaces of limestone outcrops.
  2. Check Stream Beds and Gravel Pits. Erosion can concentrate durable fossils like crinoid ossicles in stream beds, river gravels, and gravel pits, where they may be found loose.
  3. Examine Shale and Calcareous Sandstone. While less common than in limestone, crinoid ossicles can also be found in shales and calcareous sandstones, often requiring careful splitting of the rock.
  4. Look for Distinctive Shapes. Search for small, disc-shaped, cylindrical, or star-shaped fragments with a central hole. The radial or pentameral symmetry on the articulating surfaces is a key identifier.
  5. Use a Hand Lens. Many ossicles are small, so a hand lens (10x magnification) can be very helpful for identifying their characteristic features.

Quick Check

Color:
White, gray, tan, brown, black
Luster:
Dull to vitreous, earthy
Streak:
White

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