Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event

The Great Oxidation Event (GOE) is considered to have occurred at 2.33–2.32 Ga based on the last occurrence of MIF-S in South Africa. Here, based on sulphur isotope analysis of samples from Western Australia, the authors show preservation of MIF-S beyond 2.31 Ga and call for a re-evaluation of GOE t...

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Autores principales:	Pascal Philippot, Janaína N. Ávila, Bryan A. Killingsworth, Svetlana Tessalina, Franck Baton, Tom Caquineau, Elodie Muller, Ernesto Pecoits, Pierre Cartigny, Stefan V. Lalonde, Trevor R. Ireland, Christophe Thomazo, Martin J. van Kranendonk, Vincent Busigny
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/93a9c072bdb94e9abd5bb84301b68084
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spelling	oai:doaj.org-article:93a9c072bdb94e9abd5bb84301b680842021-12-02T14:38:48ZGlobally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event10.1038/s41467-018-04621-x2041-1723https://doaj.org/article/93a9c072bdb94e9abd5bb84301b680842018-06-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-04621-xhttps://doaj.org/toc/2041-1723The Great Oxidation Event (GOE) is considered to have occurred at 2.33–2.32 Ga based on the last occurrence of MIF-S in South Africa. Here, based on sulphur isotope analysis of samples from Western Australia, the authors show preservation of MIF-S beyond 2.31 Ga and call for a re-evaluation of GOE timing.Pascal PhilippotJanaína N. ÁvilaBryan A. KillingsworthSvetlana TessalinaFranck BatonTom CaquineauElodie MullerErnesto PecoitsPierre CartignyStefan V. LalondeTrevor R. IrelandChristophe ThomazoMartin J. van KranendonkVincent BusignyNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-10 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Pascal Philippot Janaína N. Ávila Bryan A. Killingsworth Svetlana Tessalina Franck Baton Tom Caquineau Elodie Muller Ernesto Pecoits Pierre Cartigny Stefan V. Lalonde Trevor R. Ireland Christophe Thomazo Martin J. van Kranendonk Vincent Busigny Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event
description	The Great Oxidation Event (GOE) is considered to have occurred at 2.33–2.32 Ga based on the last occurrence of MIF-S in South Africa. Here, based on sulphur isotope analysis of samples from Western Australia, the authors show preservation of MIF-S beyond 2.31 Ga and call for a re-evaluation of GOE timing.
format	article
author	Pascal Philippot Janaína N. Ávila Bryan A. Killingsworth Svetlana Tessalina Franck Baton Tom Caquineau Elodie Muller Ernesto Pecoits Pierre Cartigny Stefan V. Lalonde Trevor R. Ireland Christophe Thomazo Martin J. van Kranendonk Vincent Busigny
author_facet	Pascal Philippot Janaína N. Ávila Bryan A. Killingsworth Svetlana Tessalina Franck Baton Tom Caquineau Elodie Muller Ernesto Pecoits Pierre Cartigny Stefan V. Lalonde Trevor R. Ireland Christophe Thomazo Martin J. van Kranendonk Vincent Busigny
author_sort	Pascal Philippot
title	Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event
title_short	Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event
title_full	Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event
title_fullStr	Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event
title_full_unstemmed	Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event
title_sort	globally asynchronous sulphur isotope signals require re-definition of the great oxidation event
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/93a9c072bdb94e9abd5bb84301b68084
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Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event

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