Articles | Volume 17, issue 11
https://doi.org/10.5194/bg-17-2923-2020
https://doi.org/10.5194/bg-17-2923-2020
Research article
 | 
03 Jun 2020
Research article |  | 03 Jun 2020

Southern California margin benthic foraminiferal assemblages record recent centennial-scale changes in oxygen minimum zone

Hannah M. Palmer, Tessa M. Hill, Peter D. Roopnarine, Sarah E. Myhre, Katherine R. Reyes, and Jonas T. Donnenfield

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (13 Feb 2020) by Tina Treude
ED: Reconsider after major revisions (17 Feb 2020) by Marilaure Grégoire (Co-editor-in-chief)
AR by Hannah Palmer on behalf of the Authors (24 Mar 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (25 Mar 2020) by Tina Treude
RR by Anonymous Referee #2 (30 Mar 2020)
ED: Publish subject to minor revisions (review by editor) (09 Apr 2020) by Tina Treude
ED: Publish subject to minor revisions (review by editor) (10 Apr 2020) by Marilaure Grégoire (Co-editor-in-chief)
AR by Hannah Palmer on behalf of the Authors (20 Apr 2020)  Author's response   Manuscript 
ED: Publish as is (21 Apr 2020) by Tina Treude
ED: Publish as is (22 Apr 2020) by Marilaure Grégoire (Co-editor-in-chief)
AR by Hannah Palmer on behalf of the Authors (28 Apr 2020)  Author's response   Manuscript 
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Short summary
Modern climate change is causing expansions of low-oxygen zones, with detrimental impacts to marine life. To better predict future ocean oxygen change, we study past expansions and contractions of low-oxygen zones using microfossils of seafloor organisms. We find that, along the San Diego margin, the low-oxygen zone expanded into more shallow water in the last 400 years, but the conditions within and below the low-oxygen zone did not change significantly in the last 1500 years.
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