Rock Identifier
Stromatolite Fossil (Stromatolite (Cyanobacteria biogenic sedimentary structure)) — fossil
fossil

Stromatolite Fossil

Stromatolite (Cyanobacteria biogenic sedimentary structure)

Mohs hardness around 3 to 7 depending on silicification; dull to earthy luster; distinct fine, wavy, concentric, or undulating laminations/layers; grayish-tan, beige, brown, and yellowish-tan color tones.

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Physical properties

Mohs hardness around 3 to 7 depending on silicification; dull to earthy luster; distinct fine, wavy, concentric, or undulating laminations/layers; grayish-tan, beige, brown, and yellowish-tan color tones.

Formation & geological history

Formed by the trapping, binding, and cementation of sedimentary grains by microorganisms, specifically cyanobacteria (blue-green algae), in shallow aquatic environments. These are among the oldest records of life on Earth, ranging from Precambrian (up to 3.5 billion years old) to modern day.

Uses & applications

Extremely valuable as educational and scientific display specimens, lapidary cabochons, polished decorative bookends or display stones, and collector fossils.

Geological facts

Stromatolites are among the oldest known fossils on Earth, dating back over 3.5 billion years. Photosynthetic cyanobacteria that created stromatolites were responsible for producing the oxygen that transformed Earth's early atmosphere (the Great Oxidation Event).

Field identification & locations

Identified in the field by characteristic fine, wavy, microbial laminations that create dome-like or column-like layered structures. Found in marine sedimentary formations worldwide, including Western Australia (Shark Bay), the United States (Wyoming, Michigan, Montana), and South Africa.