Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery

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.

Bibliographic Details
Main Authors: M. O. Clarkson, R. A. Wood, S. W. Poulton, S. Richoz, R. J. Newton, S. A. Kasemann, F. Bowyer, L. Krystyn
Format: Article
Language:English
Published: Nature Publishing Group 2016-07-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/ncomms12236
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spelling doaj-cdbc83a48fe644389f3679677b23ef2e2021-05-11T11:21:11ZengNature Publishing GroupNature Communications2041-17232016-07-01711910.1038/ncomms12236Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recoveryM. O. Clarkson0R. A. Wood1S. W. Poulton2S. Richoz3R. J. Newton4S. A. Kasemann5F. Bowyer6L. Krystyn7School of GeoSciences, University of EdinburghSchool of GeoSciences, University of EdinburghSchool of Earth and Environment, University of LeedsInstitute of Earth Sciences, NAWI Graz, University of GrazSchool of Earth and Environment, University of LeedsDepartment of Geosciences and MARUM-Center for Marine Environmental Sciences, University of BremenSchool of GeoSciences, University of EdinburghInstitute for Palaeontology, Vienna UniversityOceanic 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.https://doi.org/10.1038/ncomms12236
collection DOAJ
language English
format Article
sources DOAJ
author M. O. Clarkson
R. A. Wood
S. W. Poulton
S. Richoz
R. J. Newton
S. A. Kasemann
F. Bowyer
L. Krystyn
spellingShingle 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
Nature Communications
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 Publishing Group
series Nature Communications
issn 2041-1723
publishDate 2016-07-01
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.
url https://doi.org/10.1038/ncomms12236
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AT rawood dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery
AT swpoulton dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery
AT srichoz dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery
AT rjnewton dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery
AT sakasemann dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery
AT fbowyer dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery
AT lkrystyn dynamicanoxicferruginousconditionsduringtheendpermianmassextinctionandrecovery
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