Evidence of Terrestrial Life and an O2-rich Atmosphere in the Oldest (~3.4 Ga) Paleosol in the East Pilbara Craton, Western Australia

Details Evidence of Terrestrial Life and an O2-rich Atmosphere in the Oldest (~3.4 Ga) Paleosol in the East Pilbara Craton, Western Australia Evidence of Terrestrial Life and an O2-rich Atmosphere in the Oldest (~3.4 Ga) Paleosol in the East Pilbara Craton, Western Australia

Apr 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010lpico1538.5424j&link_type=abstract

Astrobiology Science Conference 2010: Evolution and Life: Surviving Catastrophes and Extremes on Earth and Beyond, held April 2

Biology

Scientific paper

Elemental enrichment/depletion patterns in the Earth's oldest paleosol
in the East Pilbara Craton, Western Australia indicate that terrestrial
life flourished under an oxygenated atmosphere during pedogenesis at 3.4
Ga.

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