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  Late Proterozoic rise in atmospheric oxygen concentration inferred from phylogenetic and sulphur-isotope studies

Canfield, D. E., & Teske, A. (1996). Late Proterozoic rise in atmospheric oxygen concentration inferred from phylogenetic and sulphur-isotope studies. Nature, 382(6587), 127-132. doi:10.1038/382127a0.

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Canfield_1996.pdf (Publisher version), 2MB
 
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 Creators:
Canfield, Donald E.1, Author              
Teske, Andreas2, Author              
Affiliations:
1Department of Biogeochemistry, Max Planck Institute for Marine Microbiology, Max Planck Society, Celsiusstraße 1, 28359 Bremen, DE, ou_2481693              
2Department of Molecular Ecology, Max Planck Institute for Marine Microbiology, Max Planck Society, ou_2481696              

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 Abstract: The evolution of non-photosynthetic sulphide-oxidizing bacteria was contemporaneous with a large shift in the isotopic composition of biogenic sedimentary sulphides between 0.64 and 1.05 billion years ago. Both events were probably driven by a vise in atmospheric oxygen concentrations to greater than 5-18% of present levels-a change that may also have triggered the evolution of animals.

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Language(s): eng - English
 Dates: 1996
 Publication Status: Published in print
 Pages: 6
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 Table of Contents: -
 Rev. Type: -
 Identifiers: ISI: A1996UW67200038
DOI: 10.1038/382127a0
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Title: Nature
  Abbreviation : Nature
Source Genre: Journal
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Publ. Info: London : Nature Publishing Group
Pages: - Volume / Issue: 382 (6587) Sequence Number: - Start / End Page: 127 - 132 Identifier: Other: 1476-4687
ISSN: 0028-0836
CoNE: https://pure.mpg.de/cone/journals/resource/954925427238