Articles | Volume 16, issue 12
https://doi.org/10.5194/bg-16-2467-2019
https://doi.org/10.5194/bg-16-2467-2019
Research article
 | 
19 Jun 2019
Research article |  | 19 Jun 2019

Biomarker evidence for the occurrence of anaerobic ammonium oxidation in the eastern Mediterranean Sea during Quaternary and Pliocene sapropel formation

Darci Rush, Helen M. Talbot, Marcel T. J. van der Meer, Ellen C. Hopmans, Ben Douglas, and Jaap S. Sinninghe Damsté

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (11 Apr 2019) by S. Wajih A. Naqvi
AR by Darci Rush on behalf of the Authors (16 May 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (22 May 2019) by S. Wajih A. Naqvi
RR by Cecile Blanchet (23 May 2019)
ED: Publish subject to technical corrections (27 May 2019) by S. Wajih A. Naqvi
AR by Darci Rush on behalf of the Authors (29 May 2019)  Author's response   Manuscript 
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Short summary
Sapropels are layers of sediment that regularly occur in the Mediterranean. They indicate periods when the Mediterranean Sea water contained no oxygen, a gas vital for most large organisms. This research investigated a key process in the nitrogen cycle (anaerobic ammonium oxidation, anammox), which removes nitrogen – an important nutrient to algae – from the water, during sapropel events. Using lipids to trace this process, we found that anammox was active during the no-oxygen times.
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