Post-depositional formation of vivianite-type minerals alters sediment phosphorus records

Dijkstra, Nikki; Hagens, Mathilde; Egger, Matthias; Slomp, Caroline P.

doi:https://doi.org/10.5194/bg-15-861-2018

Articles | Volume 15, issue 3

https://doi.org/10.5194/bg-15-861-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/bg-15-861-2018

© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 15, issue 3

Research article

|

12 Feb 2018

Research article |

| 12 Feb 2018

Post-depositional formation of vivianite-type minerals alters sediment phosphorus records

Nikki Dijkstra, Mathilde Hagens, Matthias Egger, and Caroline P. Slomp

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Final revised paper (published on 12 Feb 2018)
Supplement to the final revised paper
Preprint (discussion started on 31 Aug 2017)
Supplement to the preprint

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

- Printer-friendly version

- Supplement

RC1: 'Review', Anonymous Referee #1, 29 Oct 2017
- AC1: 'Response to: Interactive comment by Anonymous Referee #1', Nikki Dijkstra, 02 Dec 2017
RC2: 'Revision of MS bg-2017-295', Anonymous Referee #2, 08 Nov 2017
- AC2: 'Response to: Interactive comment by Anonymous Referee #2', Nikki Dijkstra, 02 Dec 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (review by editor) (06 Dec 2017) by Silvio Pantoja

AR by Nikki Dijkstra on behalf of the Authors (10 Dec 2017) Author's response Manuscript

ED: Publish as is (28 Dec 2017) by Silvio Pantoja

AR by Nikki Dijkstra on behalf of the Authors (03 Jan 2018)

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Short summary

We show that post-depositional formation of iron(II) phosphate as vivianite strongly alters the phosphorus record in sediments of the Bornholm Basin (Baltic Sea). These minerals began to precipitate in the lake sediments just after the last lake–marine transition ~ 7.5 kyr BP, migrated downwards and are now a stable feature. Formation of vivianite may affect sedimentary phosphorus records in other systems as well. This should be considered when using such records to reconstruct past environments.