Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth

Large positive sulphur isotope excursions, recorded in the wake of the Marinoan glaciation have previously been interpreted assuming stable ocean sulphate concentrations. Here, using multiple sulphur isotopes, the authors instead suggest significant ocean sulphate drawdown, driven by increased pyrit...

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Autores principales: Pierre Sansjofre, Pierre Cartigny, Ricardo I. F. Trindade, Afonso C. R. Nogueira, Pierre Agrinier, Magali Ader
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2016
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Acceso en línea:https://doaj.org/article/4b9ea44d0f664016b1b2a7482b73670d
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spelling oai:doaj.org-article:4b9ea44d0f664016b1b2a7482b73670d2021-12-02T17:33:22ZMultiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth10.1038/ncomms121922041-1723https://doaj.org/article/4b9ea44d0f664016b1b2a7482b73670d2016-07-01T00:00:00Zhttps://doi.org/10.1038/ncomms12192https://doaj.org/toc/2041-1723Large positive sulphur isotope excursions, recorded in the wake of the Marinoan glaciation have previously been interpreted assuming stable ocean sulphate concentrations. Here, using multiple sulphur isotopes, the authors instead suggest significant ocean sulphate drawdown, driven by increased pyrite burial.Pierre SansjofrePierre CartignyRicardo I. F. TrindadeAfonso C. R. NogueiraPierre AgrinierMagali AderNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-8 (2016)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Pierre Sansjofre
Pierre Cartigny
Ricardo I. F. Trindade
Afonso C. R. Nogueira
Pierre Agrinier
Magali Ader
Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth
description Large positive sulphur isotope excursions, recorded in the wake of the Marinoan glaciation have previously been interpreted assuming stable ocean sulphate concentrations. Here, using multiple sulphur isotopes, the authors instead suggest significant ocean sulphate drawdown, driven by increased pyrite burial.
format article
author Pierre Sansjofre
Pierre Cartigny
Ricardo I. F. Trindade
Afonso C. R. Nogueira
Pierre Agrinier
Magali Ader
author_facet Pierre Sansjofre
Pierre Cartigny
Ricardo I. F. Trindade
Afonso C. R. Nogueira
Pierre Agrinier
Magali Ader
author_sort Pierre Sansjofre
title Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth
title_short Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth
title_full Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth
title_fullStr Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth
title_full_unstemmed Multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of Snowball Earth
title_sort multiple sulfur isotope evidence for massive oceanic sulfate depletion in the aftermath of snowball earth
publisher Nature Portfolio
publishDate 2016
url https://doaj.org/article/4b9ea44d0f664016b1b2a7482b73670d
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