Articles | Volume 10, issue 3
Earth Syst. Dynam., 10, 539–553, 2019
https://doi.org/10.5194/esd-10-539-2019
Earth Syst. Dynam., 10, 539–553, 2019
https://doi.org/10.5194/esd-10-539-2019

Research article 06 Sep 2019

Research article | 06 Sep 2019

Ocean phosphorus inventory: large uncertainties in future projections on millennial timescales and their consequences for ocean deoxygenation

Tronje P. Kemena et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (26 Feb 2019) by Axel Kleidon
AR by Tronje P. Kemena on behalf of the Authors (28 Feb 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (02 Mar 2019) by Axel Kleidon
RR by Anonymous Referee #2 (22 Mar 2019)
ED: Publish subject to minor revisions (review by editor) (11 Apr 2019) by Axel Kleidon
AR by Tronje P. Kemena on behalf of the Authors (18 Apr 2019)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (10 May 2019) by Axel Kleidon
AR by Tronje P. Kemena on behalf of the Authors (13 Jun 2019)  Author's response    Manuscript
ED: Publish as is (12 Jul 2019) by Axel Kleidon
Download
Short summary
Oceanic deoxygenation is driven by climate change in several areas of the global ocean. Measurements indicate that ocean volumes with very low oxygen levels expand, with consequences for marine organisms and fishery. We found climate-change-driven phosphorus (P) input in the ocean is hereby an important driver for deoxygenation on longer timescales with effects in the next millennia.
Altmetrics
Final-revised paper
Preprint