Timescale: Stromatolites have been around since Precambrian times, more than 542 million years ago.

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Stromatolites are layered accretionary structures formed in shallow water by the trapping, binding, and cementation of sedimentary grains by biofilms of microorganisms, especially cyanobacteria (commonly known as blue-green algae). Very few ancient stromatolites contain fossilized microbes. While features of some stromatolites are suggestive of biological activity, others possess features that are more consistent with "abiotic" (non-organic) precipitation. |
© Jo Edkins 2008 - Return to Fossils index