Silicified Coral Fragment

Incertae sedis; cf. Lithostrotionella or Syringopora depending on internal structureBody fossil (Invertebrate); Permineralized/replaced colonial coral

Silicified Coral Fragment

Geological Period

Likely Carboniferous to Permian

Estimated Age

250 - 350 million years

Preservation Type

Silicification (Replacement); The original calcium carbonate skeleton has been entirely replaced by microcrystalline quartz/chalcedony.

Condition Assessment

Fair to Good; the specimen is a weathered fragment with significant conchoidal fracturing and loss of external diagnostic features.

Taxonomic Classification

Phylum: Cnidaria, Class: Anthozoa, Order: Rugosa or Tabulata

Morphological Description

The specimen exhibits a dense, waxy luster consistent with silica replacement (chalcedony). Visible are remnants of corallites (individual tubes) appearing as faint circular or hexagonal outlines on the fractured surfaces. The structure is massive/sub-massive with secondary vugs or small cavities.

Rock Matrix

The matrix is largely inseparable from the fossil due to complete mineral replacement, likely originating from a limestone or cherty limestone setting.

Formation & Location

Commonly found in the Mississippian/Pennsylvanian formations of the Central United States (e.g., Keokuk Limestone) or similar marine deposits globally.

Size & Dimensions

Approximately 6-8 cm in length; typical for a hand-sample fragment of a larger reef-building colony.

Value & Rarity

Estimated Market Value

$10 - $25 USD

Auction Estimate

$15 - $30 USD (as part of a bulk natural history lot)

Rarity Assessment

Common; silicified coral fragments are abundant in Paleozoic limestone regions and frequently found as surface float.

Scientific Significance

Provides evidence of ancient reef-building environments and high-energy shallow marine paleoecology. Silicified fossils are important for understanding secondary mineralization processes.

Preparation Recommendations

No chemical preparation needed due to silica hardness. Light polishing could enhance the visibility of internal corallite structures. Store in a dry environment.

Notable Features

Features high-quality chalcedony replacement and distinct conchoidal fracture patterns; contains small internal druzy quartz pockets in center vugs.

Identified on 5/10/2026
Silicified Coral Fragment - Incertae sedis; cf. Lithostrotionella or Syringopora depending on internal structure | Fossil Identifier