Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery
Oceanic anoxia is invoked for driving the Permo-Triassic Mass Extinction, but the timing, distribution and chemical state are poorly understood. Here, the authors show that fluctuations of anoxic, non-sulfidic (ferruginous) conditions were important for the delayed biotic recovery in the Neo-Tethys.
Guardado en:
Autores principales: | , , , , , , , |
---|---|
Formato: | article |
Lenguaje: | EN |
Publicado: |
Nature Portfolio
2016
|
Materias: | |
Acceso en línea: | https://doaj.org/article/cdbc83a48fe644389f3679677b23ef2e |
Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
id |
oai:doaj.org-article:cdbc83a48fe644389f3679677b23ef2e |
---|---|
record_format |
dspace |
spelling |
oai:doaj.org-article:cdbc83a48fe644389f3679677b23ef2e2021-12-02T14:38:35ZDynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery10.1038/ncomms122362041-1723https://doaj.org/article/cdbc83a48fe644389f3679677b23ef2e2016-07-01T00:00:00Zhttps://doi.org/10.1038/ncomms12236https://doaj.org/toc/2041-1723Oceanic anoxia is invoked for driving the Permo-Triassic Mass Extinction, but the timing, distribution and chemical state are poorly understood. Here, the authors show that fluctuations of anoxic, non-sulfidic (ferruginous) conditions were important for the delayed biotic recovery in the Neo-Tethys.M. O. ClarksonR. A. WoodS. W. PoultonS. RichozR. J. NewtonS. A. KasemannF. BowyerL. KrystynNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-9 (2016) |
institution |
DOAJ |
collection |
DOAJ |
language |
EN |
topic |
Science Q |
spellingShingle |
Science Q M. O. Clarkson R. A. Wood S. W. Poulton S. Richoz R. J. Newton S. A. Kasemann F. Bowyer L. Krystyn Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery |
description |
Oceanic anoxia is invoked for driving the Permo-Triassic Mass Extinction, but the timing, distribution and chemical state are poorly understood. Here, the authors show that fluctuations of anoxic, non-sulfidic (ferruginous) conditions were important for the delayed biotic recovery in the Neo-Tethys. |
format |
article |
author |
M. O. Clarkson R. A. Wood S. W. Poulton S. Richoz R. J. Newton S. A. Kasemann F. Bowyer L. Krystyn |
author_facet |
M. O. Clarkson R. A. Wood S. W. Poulton S. Richoz R. J. Newton S. A. Kasemann F. Bowyer L. Krystyn |
author_sort |
M. O. Clarkson |
title |
Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery |
title_short |
Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery |
title_full |
Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery |
title_fullStr |
Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery |
title_full_unstemmed |
Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery |
title_sort |
dynamic anoxic ferruginous conditions during the end-permian mass extinction and recovery |
publisher |
Nature Portfolio |
publishDate |
2016 |
url |
https://doaj.org/article/cdbc83a48fe644389f3679677b23ef2e |
work_keys_str_mv |
AT moclarkson dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery AT rawood dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery AT swpoulton dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery AT srichoz dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery AT rjnewton dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery AT sakasemann dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery AT fbowyer dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery AT lkrystyn dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery |
_version_ |
1718390980040720384 |