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File:Stromatolithe Paléoarchéen - MNHT.PAL.2009.10.1.jpg

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Summary

Stromatolithe Paléoarchéen

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Description
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.
institution QS:P195,Q422
Date Taken on 30 July 2011
Source Own work
Author Didier Descouens
Permission
(Reusing this file)
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I, the copyright holder of this work, hereby publish it under the following license:
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Camera location43° 35′ 38.03″ N, 1° 26′ 57.23″ E Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

Published in the press

The Japan Times nov 2013

Captions

Stromatolite of Paleoarchean age – 3, 600 to 3, 200 million years ago (Mya)

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30 July 2011

43°35'38.02980593962"N, 1°26'57.22698211670"E

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current08:30, 30 July 2011Thumbnail for version as of 08:30, 30 July 20115,185 × 3,655 (9.94 MB)Archaeodontosaurus{{Information |Description ={{en|1=x}} |Source ={{own}} |Author =Archaeodontosaurus |Date = |Permission = |other_versions = }}
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