Incomplete Brachiopod or Bivalve Shell Fragment

cf. Leiopteria sp. or Mucrospirifer fragmentBody fossil; Invertebrate (Macro-invertebrate)

Incomplete Brachiopod or Bivalve Shell Fragment

Geological Period

Devonian (likely Middle Devonian)

Estimated Age

385 to 400 million years

Preservation Type

Recrystallized shell material; original calcium carbonate replaced by stable calcite or silica.

Condition Assessment

Fair; the specimen is incomplete with significant breakage and a puncture, though growth lines are visible.

Taxonomic Classification

Phylum: Brachiopoda or Mollusca; Class: Articulata or Bivalvia; Order: Likely Spiriferida or Pterioida

Morphological Description

A sub-triangular shell fragment displaying concentric growth lines and a prominent, elongated posterior wing or auricle. The surface shows a light pearlescent or calcitic luster with some breakage toward the dorsal margin and a significant hole in the mid-shell region.

Rock Matrix

None (isolated find); likely weathered out of Devonian limestone or calcareous shale typical of the Dundee Limestone or Traverse Group.

Formation & Location

Dundee Limestone or Traverse Group; Sterling State Park, Monroe, Michigan, USA.

Size & Dimensions

Approximately 15-25mm; typical for small to medium Paleozoic brachiopods or bivalve shells.

Value & Rarity

Estimated Market Value

$1.00 - $5.00

Auction Estimate

$0.00 - $10.00 (generally sold in bulk lots)

Rarity Assessment

Common; fragments of this type are frequently found along the Lake Erie shoreline and in Michigan glacial drift.

Scientific Significance

Provides evidence of Paleozoic marine fauna in the Michigan Basin. These fossils represent a time when Michigan was covered by a warm, shallow tropical sea.

Preparation Recommendations

Minor cleaning with water and a soft brush; store in a dry, padded container to prevent further chipping of the brittle edges.

Notable Features

Features a distinct 'wing' shape common in certain Devonian bivalves and brachiopods; the hole may be the result of modern mechanical weathering or ancient bioerosion.

Notes

Found at Sterling State Park Michigan

Identified on 5/7/2026