Articles | Volume 17, issue 8
https://doi.org/10.5194/bg-17-2381-2020
https://doi.org/10.5194/bg-17-2381-2020
Research article
 | 
30 Apr 2020
Research article |  | 30 Apr 2020

Evidence of changes in sedimentation rate and sediment fabric in a low-oxygen setting: Santa Monica Basin, CA

Nathaniel Kemnitz, William M. Berelson, Douglas E. Hammond, Laura Morine, Maria Figueroa, Timothy W. Lyons, Simon Scharf, Nick Rollins, Elizabeth Petsios, Sydnie Lemieux, and Tina Treude

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (19 Mar 2020) by S. Wajih A. Naqvi
ED: Publish subject to minor revisions (review by editor) (19 Mar 2020) by Katja Fennel (Co-editor-in-chief)
AR by Nathaniel Kemnitz on behalf of the Authors (24 Mar 2020)  Author's response   Manuscript 
ED: Publish as is (27 Mar 2020) by S. Wajih A. Naqvi
ED: Publish as is (27 Mar 2020) by Katja Fennel (Co-editor-in-chief)
AR by Nathaniel Kemnitz on behalf of the Authors (30 Mar 2020)
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Short summary
Our paper shows how sedimentation in a very low oxygen setting provides a unique record of environmental change. We look at the past 250 years through the filter of sediment accumulation via radioisotope dating and other physical and chemical analyses of these sediments. We conclude, remarkably, that there has been very little change in net sediment mass accumulation through the past 100–150 years, yet just prior to 1900  CE, sediments were accumulating at 50 %–70 % of today's rate.
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