Earth Record
Mineralogy and formation
Stromatolites are layered sedimentary structures built by cyanobacteria (blue-green algae), among the oldest evidence of life on Earth, with fossil examples dating to 3. 5 billion years ago. They form when microbial mats of cyanobacteria trap and bind sediment grains (typically calcium carbonate or silica) on their sticky surfaces. As each layer of sediment accumulates, the photosynthetic bacteria migrate upward toward light, establishing a new mat on top, creating successive laminae over time.
The internal structure shows fine, curved laminations, each layer represents a period of microbial growth and sediment trapping. Fossil stromatolites are composed of limestone, dolomite, or chert, depending on the original sediment composition and subsequent diagenesis. They are abundant in Precambrian rocks worldwide; their decline after the Cambrian Period correlates with the evolution of grazing animals that consumed the microbial mats.
Living stromatolites still form today in Shark Bay, Western Australia, and a few other hypersaline or alkaline environments where grazing competition is limited. Popular lapidary material comes from Precambrian formations in Australia, Bolivia, and the Great Lakes region.
Chemical FormulaVariable (SiO2 if silicified; CaCO3 if carbonate-dominated; biogenic sedimentary structure)Crystal SystemN/AMohs Hardness5Specific Gravity2.4-2.8 (varies with composition)LusterVaries -- waxy (chert), vitreous (quartz), dull to earthy (carbonate)ColorBrown-GreenIMA StatusrockIMA NumberNot IMA-approved Australia (Western Australia)Bolivia
Telling it apart
- Stromatolite is NOT a mineral. It is a biogenic sedimentary structure (a type of fossil). It has no fixed chemical formula, crystal system, or mineral classification. Listing it alongside minerals is a category error common in the crystal trade. - Common misconception: "All stromatolites are billions of years old." Stromatolites span the entire geological record from ~3. 48 Ga to the present.
Modern living stromatolites exist today. The age of a specific specimen depends on the geological formation it comes from. Most lapidary-market stromatolites are Proterozoic (0. 5-2. 5 Ga) from Montana or Western Australia. - Biogenicity debates: The oldest putative stromatolites (~3. 7-3. 8 Ga, Isua, Greenland; ~3. 48 Ga, Dresser Formation) are still debated. Some researchers argue certain ancient structures could be abiotic (formed by non-biological chemical precipitation).
The 3. 43 Ga Strelley Pool Formation stromatolites are more widely accepted. - "Kambaba jasper" confusion: "Kambaba jasper" (also "crocodile jasper") is sometimes marketed as fossilized stromatolite from Madagascar. Some specimens may indeed contain stromatolitic structures, but much of what is sold under this name is orbicular rhyolite or other volcanic rock with no biological origin.
Spotting the real thing
Stromatolite: layered sedimentary structure built by ancient cyanobacteria. The diagnostic feature is wavy, dome-shaped laminations visible in cross-section. These biological layering patterns are distinct from non-biological banded rock.
If the layers are perfectly parallel and uniform (like agate banding), it may be banded chert, not a biological stromatolite.
Cross-referenceMindat ↗