Articles | Volume 14, issue 4
https://doi.org/10.5194/cp-14-441-2018
© Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License.
Research article
| 
09 Apr 2018
Research article |
| 09 Apr 2018
| 09 Apr 2018
Salinity changes and anoxia resulting from enhanced run-off during the late Permian global warming and mass extinction event
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- Final revised paper (published on 09 Apr 2018)
- Supplement to the final revised paper
- Preprint (discussion started on 25 Oct 2017)
- Supplement to the preprint
Interactive discussion
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
- Printer-friendly version
- Supplement
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RC1: 'salinity: ecostratigraphy not biostratigraphy', Anonymous Referee #1, 18 Dec 2017
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AC1: 'response to reviewer #1', Els van Soelen, 18 Jan 2018
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AC1: 'response to reviewer #1', Els van Soelen, 18 Jan 2018
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RC2: 'Acritarchs, salinity and the end-Permian mass extinction', Anonymous Referee #2, 20 Dec 2017
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AC2: 'response to reviewer #2', Els van Soelen, 18 Jan 2018
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AC2: 'response to reviewer #2', Els van Soelen, 18 Jan 2018
Peer-review completion
AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (11 Feb 2018) by Arne Winguth
AR by Els van Soelen on behalf of the Authors (13 Feb 2018)
Author's response
Manuscript
ED: Publish as is (13 Mar 2018) by Arne Winguth
AR by Els van Soelen on behalf of the Authors (13 Mar 2018)
