Stromatolithe Paléoarchéen - MNHT.PAL.2009.10.1, by Didier Descouens, Taken on 30 July 2011
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Stromatolithe Paléoarchéen - MNHT.PAL.2009.10.1

Didier Descouens

Taken on 30 July 2011

Classification
Photograph
Museum
Wikimedia Commons
Rights
CC BY-SA 4.0, as the museum states it.
Who can see it
Teens profiles and older: its museum says too little about what it shows to place it for younger viewers. How works are placed

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About this work

Stromatolite Stromatolites are formed over the years by mats (1-10 mm in thickness) of microorganisms (cynobacteria among others) found in shallow, mainly marine waters. The microorganisms precipitate mineral particles, which makes the mat to thicken, but only the upper part survives. Most stromatolites display characteristically layered structures. Only the layers are visible to the naked eye. Stage : Paleoarchean from -3 600 à -3 200 Ma (million years ago). Locality: Strelley Pool Chert (SPC) (Pilbara Craton) - Western Australia.