Geological evidence of oxygenic photosynthesis and the biotic response to the 2400-2200 Ma “Great Oxidation Event”

Title
Geological evidence of oxygenic photosynthesis and the biotic response to the 2400-2200 Ma “Great Oxidation Event”
Authors
Keywords
carbon isotopic fraction, cyanobacterial evolution, microfossils, oldest eucaryotes, oxygen-requiring biosynthesis, Precambrian, stromatolites
Journal
BIOCHEMISTRY-MOSCOW
Volume 79, Issue 3, Pages 165-177
Publisher
Pleiades Publishing Ltd
Online
2014-03-18
DOI
10.1134/s0006297914030018

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