Literature DB >> 17816370

Sulfur Isotopes in Swaziland System Barites and the Evolution of the Earth's Atmosphere.

E C Perry, J Monster, T Reimer.   

Abstract

Sedimentary barites from the Swaziland System of South Africa (more than 3000 million years old) have sulfur-34 ratios that are enriched by only 2.5 per mil with respect to contemporary sulfides. To explain this small fractionation, it is proposed that oxygen pressure in the earth's atmosphere was very low and that local oxidation occurred in a photosynthetic layer of the ocean.

Entities:  

Year:  1971        PMID: 17816370     DOI: 10.1126/science.171.3975.1015

Source DB:  PubMed          Journal:  Science        ISSN: 0036-8075            Impact factor:   47.728


  4 in total

Review 1.  Geological constraints on the origin of oxygenic photosynthesis.

Authors:  James Farquhar; Aubrey L Zerkle; Andrey Bekker
Journal:  Photosynth Res       Date:  2010-09-30       Impact factor: 3.573

Review 2.  Photosynthesis in the Archean era.

Authors:  John M Olson
Journal:  Photosynth Res       Date:  2006-02-02       Impact factor: 3.573

3.  Electron paramagnetic resonance study of a photosynthetic microbial mat and comparison with Archean cherts.

Authors:  M Bourbin; S Derenne; D Gourier; J-N Rouzaud; P Gautret; F Westall
Journal:  Orig Life Evol Biosph       Date:  2012-12-20       Impact factor: 1.950

4.  Antiquity and evolutionary status of bacterial sulfate reduction: sulfur isotope evidence.

Authors:  M Schidlowski
Journal:  Orig Life       Date:  1979-09
  4 in total

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