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dc.contributor.authorPoulton, Simon
dc.contributor.authorBekker, Andrey
dc.contributor.authorCumming, Vivien
dc.contributor.authorZerkle, Aubrey Lea
dc.contributor.authorCanfield, Donald
dc.contributor.authorJohnston, David
dc.date.accessioned2021-09-28T23:38:32Z
dc.date.available2021-09-28T23:38:32Z
dc.date.issued2021-03-29
dc.identifier.citationPoulton , S , Bekker , A , Cumming , V , Zerkle , A L , Canfield , D & Johnston , D 2021 , ' A 200-million year delay in permanent atmospheric oxygenation ' , Nature . https://doi.org/10.1038/s41586-021-03393-7en
dc.identifier.issn1476-4687
dc.identifier.otherPURE: 273038298
dc.identifier.otherPURE UUID: 10cad2d9-6a60-4a5b-bb69-33204524bb6f
dc.identifier.otherORCID: /0000-0003-2324-1619/work/91685959
dc.identifier.otherScopus: 85103318951
dc.identifier.otherWOS: 000634663900001
dc.identifier.urihttp://hdl.handle.net/10023/24041
dc.descriptionS.W.P. acknowledges support from a Leverhulme Research Fellowship and a Royal Society Wolfson Research Merit Award. A.B. acknowledges support from the University of Johannesburg in the form of a Distinguished Visiting Professorship. D.T.J. acknowledges support from a NASA Exobiology award (NNX15AP58G).en
dc.description.abstractThe rise of atmospheric oxygen fundamentally changed the chemistry of surficial environments and the nature of Earth’s habitability1. Early atmospheric oxygenation occurred over a protracted period of extreme climatic instability marked by multiple global glaciations2,3, with the initial rise of oxygen concentration to above 10−5 of the present atmospheric level constrained to about 2.43 billion years ago4,5. Subsequent fluctuations in atmospheric oxygen levels have, however, been reported to have occurred until about 2.32 billion years ago4, which represents the estimated timing of irreversible oxygenation of the atmosphere6,7. Here we report a high-resolution reconstruction of atmospheric and local oceanic redox conditions across the final two glaciations of the early Palaeoproterozoic era, as documented by marine sediments from the Transvaal Supergroup, South Africa. Using multiple sulfur isotope and iron–sulfur–carbon systematics, we demonstrate continued oscillations in atmospheric oxygen levels after about 2.32 billion years ago that are linked to major perturbations in ocean redox chemistry and climate. Oxygen levels thus fluctuated across the threshold of 10−5 of the present atmospheric level for about 200 million years, with permanent atmospheric oxygenation finally arriving with the Lomagundi carbon isotope excursion at about 2.22 billion years ago, some 100 million years later than currently estimated.
dc.format.extent17
dc.language.isoeng
dc.relation.ispartofNatureen
dc.rightsCopyright © 2021, The Author(s), under exclusive licence to Springer Nature Limited. This work has been made available online in accordance with publisher policies or with permission. Permission for further reuse of this content should be sought from the publisher or the rights holder. This is the author created accepted manuscript following peer review and may differ slightly from the final published version. The final published version of this work is available at https://doi.org/10.1038/s41586-021-03393-7en
dc.subjectGE Environmental Sciencesen
dc.subjectDASen
dc.subject.lccGEen
dc.titleA 200-million year delay in permanent atmospheric oxygenationen
dc.typeJournal articleen
dc.description.versionPostprinten
dc.contributor.institutionUniversity of St Andrews.School of Earth & Environmental Sciencesen
dc.contributor.institutionUniversity of St Andrews.St Andrews Centre for Exoplanet Scienceen
dc.contributor.institutionUniversity of St Andrews.St Andrews Isotope Geochemistryen
dc.identifier.doihttps://doi.org/10.1038/s41586-021-03393-7
dc.description.statusPeer revieweden
dc.date.embargoedUntil2021-09-29


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