Articles | Volume 16, issue 2
https://doi.org/10.5194/bg-16-643-2019
https://doi.org/10.5194/bg-16-643-2019
Research article
 | 
01 Feb 2019
Research article |  | 01 Feb 2019

Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth

Hilde Pracht, Brett Metcalfe, and Frank J. C. Peeters

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Interactive discussion

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: Publish subject to minor revisions (review by editor) (01 Aug 2018) by Lennart de Nooijer
AR by Brett Metcalfe on behalf of the Authors (22 Aug 2018)  Manuscript 
ED: Publish subject to minor revisions (review by editor) (21 Sep 2018) by Lennart de Nooijer
AR by Brett Metcalfe on behalf of the Authors (05 Oct 2018)  Author's response   Manuscript 
ED: Publish as is (22 Oct 2018) by Lennart de Nooijer
AR by Brett Metcalfe on behalf of the Authors (01 Nov 2018)  Manuscript 

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Brett Metcalfe on behalf of the Authors (17 Jan 2019)   Author's adjustment   Manuscript
EA: Adjustments approved (17 Jan 2019) by Lennart de Nooijer
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Short summary
In palaeoceanography the shells of single-celled foraminifera are routinely used as proxies to reconstruct the temperature, salinity and circulation of the ocean in the past. Traditionally a number of specimens were pooled for a single stable isotope measurement; however, technical advances now mean that a single shell or chamber of a shell can be measured individually. Three different hypotheses regarding foraminiferal biology and ecology were tested using this approach.
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