Stepwise oxygenation of the Paleozoic atmosphere
The GEOCARBSULF model provides the most detailed reconstructions of Phanerozoic O2, but its predictions are not supported by geochemical data. Here, a GEOCARBSULF model rebuilt from first principles, with the addition of an amended sulphur cycle and the latest isotope records, supports a Paleozoic O...
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Format: | Article |
Language: | English |
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Nature Portfolio
2018-10-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-018-06383-y |
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author | Alexander J. Krause Benjamin J. W. Mills Shuang Zhang Noah J. Planavsky Timothy M. Lenton Simon W. Poulton |
author_facet | Alexander J. Krause Benjamin J. W. Mills Shuang Zhang Noah J. Planavsky Timothy M. Lenton Simon W. Poulton |
author_sort | Alexander J. Krause |
collection | DOAJ |
description | The GEOCARBSULF model provides the most detailed reconstructions of Phanerozoic O2, but its predictions are not supported by geochemical data. Here, a GEOCARBSULF model rebuilt from first principles, with the addition of an amended sulphur cycle and the latest isotope records, supports a Paleozoic Oxygenation Event. |
first_indexed | 2024-12-17T19:25:15Z |
format | Article |
id | doaj.art-09e019333c534aeb988b9ecee5d38252 |
institution | Directory Open Access Journal |
issn | 2041-1723 |
language | English |
last_indexed | 2024-12-17T19:25:15Z |
publishDate | 2018-10-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Nature Communications |
spelling | doaj.art-09e019333c534aeb988b9ecee5d382522022-12-21T21:35:24ZengNature PortfolioNature Communications2041-17232018-10-019111010.1038/s41467-018-06383-yStepwise oxygenation of the Paleozoic atmosphereAlexander J. Krause0Benjamin J. W. Mills1Shuang Zhang2Noah J. Planavsky3Timothy M. Lenton4Simon W. Poulton5School of Earth and Environment, University of LeedsSchool of Earth and Environment, University of LeedsDepartment of Geology and Geophysics, Yale UniversityDepartment of Geology and Geophysics, Yale UniversityEarth System Science Group, College of Life and Environmental Sciences, University of ExeterSchool of Earth and Environment, University of LeedsThe GEOCARBSULF model provides the most detailed reconstructions of Phanerozoic O2, but its predictions are not supported by geochemical data. Here, a GEOCARBSULF model rebuilt from first principles, with the addition of an amended sulphur cycle and the latest isotope records, supports a Paleozoic Oxygenation Event.https://doi.org/10.1038/s41467-018-06383-y |
spellingShingle | Alexander J. Krause Benjamin J. W. Mills Shuang Zhang Noah J. Planavsky Timothy M. Lenton Simon W. Poulton Stepwise oxygenation of the Paleozoic atmosphere Nature Communications |
title | Stepwise oxygenation of the Paleozoic atmosphere |
title_full | Stepwise oxygenation of the Paleozoic atmosphere |
title_fullStr | Stepwise oxygenation of the Paleozoic atmosphere |
title_full_unstemmed | Stepwise oxygenation of the Paleozoic atmosphere |
title_short | Stepwise oxygenation of the Paleozoic atmosphere |
title_sort | stepwise oxygenation of the paleozoic atmosphere |
url | https://doi.org/10.1038/s41467-018-06383-y |
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