Trilobite (Partial Cephalon)

Phacops sp. or Dalmanites sp. (cf. Phacopoid)Body fossil; Invertebrate (Arthropod)

Trilobite (Partial Cephalon)

Geological Period

Ordovician to Devonian

Estimated Age

Approx. 360 - 480 million years

Preservation Type

Replacement and carbonization; the darker central area suggests organic residue or mineral replacement within a fine-grained sedimentary cast.

Condition Assessment

Fair; the specimen is incomplete, missing the thorax and pygidium, and shows significant surface erosion/weathering.

Taxonomic Classification

Phylum: Arthropoda; Class: Trilobita; Order: Phacopida (likely); Family: Phacopidae or Dalmanitidae

Morphological Description

A partial cephalon (head section) displaying a prominent central glabella with visible furrows and a rounded anterior margin. Portions of the fixigenae (fixed cheeks) are present, though the specimen appears weathered and lacks clearly defined compound eyes or genal spines.

Rock Matrix

Silty mudstone or fine-grained shale, light grey to tan in color, consistent with typical trilobite-bearing deposits.

Formation & Location

Likely sourced from the Hamilton Group (New York, USA), the Jorf or Alnif regions (Morocco), or similar Paleozoic marine formations.

Size & Dimensions

Approx. 4-6 cm in width; typical of mid-sized Paleozoic benthic trilobites.

Value & Rarity

Estimated Market Value

$15 - $40 USD

Auction Estimate

$20 - $50 USD

Rarity Assessment

Common; trilobite fragments of this genus and preservation quality are widely distributed in the fossil record.

Scientific Significance

Provides evidence of Paleozoic marine benthic ecosystems and arthropod diversification; useful for local stratigraphic correlation within its original formation.

Preparation Recommendations

Keep in a low-humidity environment; no further mechanical preparation recommended as it may damage the soft matrix; display in current shadow box to prevent further breakage.

Notable Features

The distinct color contrast between the glabella and the surrounding matrix suggests selective mineralization or the presence of a carbonaceous film.

Identified on 5/10/2026