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Titlebook: Early Life on Earth; A Practical Guide David Wacey Book 2009 Springer Science+Business Media B.V. 2009 Archean.Biosignatures.Early Life.Mic

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˜3,490 Ma Dresser Formation, East Pilbara, Western Australias and draping chert layers. Their distribution could simply reflect the supply of supersaturated solutions from which they precipitated. Robust micro-textural and isotopic evidence for the involvement of any kinds of microbes in the growth of these stromatolites is still lacking.
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˜3,426–3,350 Ma, Strelley Pool Formation, East Pilbara, Western Australiaorings show slight constrictions along their margins suggestive of colonisation by individual cells (Fig. B43). The microborings do not extend into adjacent grains nor into the microcrystalline silica cement. Nano-scale geochemical mapping shows enrichments of carbon and nitrogen within and/or along
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> 3,700 Ma Isua Supracrustal Belt and Akilia Island, S.W. Greenland
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~3,460 Ma Apex Basalt, East Pilbara, Western Australia
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~3,450 Ma, Hoogenoeg Formation, Barberton, South Africa
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