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...
Guardado en:
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
|
Materias: | |
Acceso en línea: | https://doaj.org/article/4b9ea44d0f664016b1b2a7482b73670d |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
-
Bisnorgammacerane traces predatory pressure and the persistent rise of algal ecosystems after Snowball Earth
por: Lennart M. van Maldegem, et al.
Publicado: (2019) -
Orbital forcing of ice sheets during snowball Earth
por: Ross N. Mitchell, et al.
Publicado: (2021) -
Active methanogenesis during the melting of Marinoan snowball Earth
por: Zhouqiao Zhao, et al.
Publicado: (2021) -
Constraining the rise of oxygen with oxygen isotopes
por: B. A. Killingsworth, et al.
Publicado: (2019) -
Elevated CO2 degassing rates prevented the return of Snowball Earth during the Phanerozoic
por: Benjamin J. W. Mills, et al.
Publicado: (2017)