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...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Alexander J. Krause, Benjamin J. W. Mills, Shuang Zhang, Noah J. Planavsky, Timothy M. Lenton, Simon W. Poulton
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2018
Materias:
Q
Acceso en línea:https://doaj.org/article/09e019333c534aeb988b9ecee5d38252
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:09e019333c534aeb988b9ecee5d38252
record_format dspace
spelling oai:doaj.org-article:09e019333c534aeb988b9ecee5d382522021-12-02T16:50:06ZStepwise oxygenation of the Paleozoic atmosphere10.1038/s41467-018-06383-y2041-1723https://doaj.org/article/09e019333c534aeb988b9ecee5d382522018-10-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-06383-yhttps://doaj.org/toc/2041-1723The 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.Alexander J. KrauseBenjamin J. W. MillsShuang ZhangNoah J. PlanavskyTimothy M. LentonSimon W. PoultonNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-10 (2018)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Alexander J. Krause
Benjamin J. W. Mills
Shuang Zhang
Noah J. Planavsky
Timothy M. Lenton
Simon W. Poulton
Stepwise oxygenation of the Paleozoic atmosphere
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.
format article
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
title Stepwise oxygenation of the Paleozoic atmosphere
title_short 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_sort stepwise oxygenation of the paleozoic atmosphere
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/09e019333c534aeb988b9ecee5d38252
work_keys_str_mv AT alexanderjkrause stepwiseoxygenationofthepaleozoicatmosphere
AT benjaminjwmills stepwiseoxygenationofthepaleozoicatmosphere
AT shuangzhang stepwiseoxygenationofthepaleozoicatmosphere
AT noahjplanavsky stepwiseoxygenationofthepaleozoicatmosphere
AT timothymlenton stepwiseoxygenationofthepaleozoicatmosphere
AT simonwpoulton stepwiseoxygenationofthepaleozoicatmosphere
_version_ 1718383080329183232