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Journal Abstract Search

626 related items for PubMed ID: 18368114

  • 1. Tracing the stepwise oxygenation of the Proterozoic ocean.
    Scott C, Lyons TW, Bekker A, Shen Y, Poulton SW, Chu X, Anbar AD.
    Nature; 2008 Mar 27; 452(7186):456-9. PubMed ID: 18368114
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  • 2. The transition to a sulphidic ocean approximately 1.84 billion years ago.
    Poulton SW, Fralick PW, Canfield DE.
    Nature; 2004 Sep 09; 431(7005):173-7. PubMed ID: 15356628
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  • 5. Ferruginous conditions dominated later neoproterozoic deep-water chemistry.
    Canfield DE, Poulton SW, Knoll AH, Narbonne GM, Ross G, Goldberg T, Strauss H.
    Science; 2008 Aug 15; 321(5891):949-52. PubMed ID: 18635761
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  • 7. Molybdenum isotope evidence for widespread anoxia in mid-Proterozoic oceans.
    Arnold GL, Anbar AD, Barling J, Lyons TW.
    Science; 2004 Apr 02; 304(5667):87-90. PubMed ID: 15066776
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  • 10. Geochemical evidence for widespread euxinia in the later Cambrian ocean.
    Gill BC, Lyons TW, Young SA, Kump LR, Knoll AH, Saltzman MR.
    Nature; 2011 Jan 06; 469(7328):80-3. PubMed ID: 21209662
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  • 13. Increased subaerial volcanism and the rise of atmospheric oxygen 2.5 billion years ago.
    Kump LR, Barley ME.
    Nature; 2007 Aug 30; 448(7157):1033-6. PubMed ID: 17728754
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  • 16. Onset of coupled atmosphere-ocean oxygenation 2.3 billion years ago.
    Ostrander CM, Heard AW, Shu Y, Bekker A, Poulton SW, Olesen KP, Nielsen SG.
    Nature; 2024 Jul 30; 631(8020):335-339. PubMed ID: 38867053
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