Articles | Volume 16, issue 2
https://doi.org/10.5194/bg-16-643-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth
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- Final revised paper (published on 01 Feb 2019)
- Preprint (discussion started on 18 Apr 2018)
Interactive discussion
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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- Supplement
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RC1: 'Excellent Paper - Minor Suggestions', Jody Wycech, 08 May 2018
- AC3: 'Response to Reviewer 1', Brett Metcalfe, 17 Jul 2018
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EC1: 'waiting for reviewer 2', Lennart de Nooijer, 19 Jun 2018
- AC1: 'Correction of Figure 6 B', Brett Metcalfe, 17 Jul 2018
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RC2: 'Review of " Oxygen isotope composition of final chamber of planktic foraminifera provides evidence for vertical migration and depth integrated growth" by Pracht et al.', Takashi Toyofuku, 27 Jun 2018
- AC2: 'Response to Reviewer 2', Brett Metcalfe, 17 Jul 2018
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