Solitary Rugose Coral (Horn Coral)

Rugosa gen. et sp. indet. (cf. Zaphrentis or Heliophyllum)Body fossil (Internal/External Mold and Recrystallized Stem); Invertebrate

Solitary Rugose Coral (Horn Coral)

Geological Period

Paleozoic (likely Devonian to Carboniferous)

Estimated Age

300 - 400 million years

Preservation Type

Recrystallization and mineral replacement (likely calcite or silica) within a mold.

Condition Assessment

Fair; the specimen is highly weathered, partially obscured by the matrix, and lacks the fine detail of individual septa or the external theca.

Taxonomic Classification

Phylum: Cnidaria; Class: Anthozoa; Subclass: Rugosa; Order: Stauriida

Morphological Description

The specimen shows a cross-sectional view of a solitary coral. Visible features include a circular to sub-circular calyx area with faint evidence of radial septa (internal vertical plates) which are partially obscured by recrystallization. The 'horn' shape is suggested by the way the organism is embedded within the matrix.

Rock Matrix

Fine-grained, grey bioclastic limestone or calcareous siltstone with possible iron-oxide (limonite) staining in the vugs.

Formation & Location

Common in the Onondaga Formation (USA/Canada) or Carboniferous Limestones of the UK and Europe.

Size & Dimensions

Approximately 3-4 cm in diameter; typical for solitary rugose corals which usually range from 1 cm to 10 cm.

Value & Rarity

Estimated Market Value

$5.00 - $15.00 USD

Auction Estimate

$10.00 - $20.00 USD

Rarity Assessment

Common; solitary corals are ubiquitous in Paleozoic marine deposits globally.

Scientific Significance

Provides evidence of Paleozoic marine benthic environments. Rugose corals were major reef builders and are essential for dating Paleozoic strata and understanding ancient seawater chemistry.

Preparation Recommendations

Mechanical cleaning with a dental pick or air-scribe could reveal more septal detail. Avoid acid baths unless the fossil is silicified and the matrix is pure limestone.

Notable Features

The specimen exhibits a 'vug' or small cavity below the main fossil body containing reddish-pink mineral deposits (possibly calcite or iron-rich sediment).

Identified on 5/17/2026