Articles | Volume 23, issue 4
https://doi.org/10.5194/bg-23-1591-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
A simplified approach for measuring Rubisco carbon isotope fractionation and the first determination in marine haptophyte Gephyrocapsa oceanica
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- Final revised paper (published on 27 Feb 2026)
- Preprint (discussion started on 16 Oct 2025)
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
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RC1: 'Comment on egusphere-2025-5010', Kathleen Scott, 20 Oct 2025
- AC1: 'Reply on RC1', Reto Wijker, 19 Dec 2025
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RC2: 'Comment on egusphere-2025-5010', Anonymous Referee #2, 22 Oct 2025
- AC2: 'Reply on RC2', Reto Wijker, 19 Dec 2025
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RC3: 'Comment on egusphere-2025-5010', Anonymous Referee #3, 06 Nov 2025
- AC3: 'Reply on RC3', Reto Wijker, 19 Dec 2025
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to minor revisions (review by editor) (19 Dec 2025) by Jack Middelburg
AR by Reto Wijker on behalf of the Authors (25 Dec 2025)
Author's response
Author's tracked changes
Manuscript
ED: Publish subject to technical corrections (29 Dec 2025) by Jack Middelburg
AR by Reto Wijker on behalf of the Authors (05 Jan 2026)
Manuscript
General comments:
The manuscript describes an improved protocol for estimating isotope fractionation by RubisCO enzymes (though it could also be applied to other carboxylases, as long as they are mostly irreversible!). Improvements include 1) the convincing demonstration that absolute enzyme purification not necessary in some cases, as long as the appropriate controls are run in parallel (absence of substrate, e.g., RuBP). This is a huge benefit, since high enzyme activities are needed for these experiments, and extensive purification steps tend to diminish both yield and specific activity; 2) increased precision by sampling strategically along the timecourse, guided by modeling of carbon fixation; and 3) the introduction of instrumentation (Apollo-Picarro spectrometer) which permits the simultaneous quantification and isotope ratio determination for each sample, avoiding errors introduced by splitting a sample for measuring each of these parameters individually.
They reproduce epsilon values previously determined in the literature (spinach, Synechococcus) as well as a new one (coccolithophore G. oceanica) that compares favorably with the e value determined for coccolithophore E. huxleyi.
Their simplified partial purification protocol (run as they describe with the appropriate controls), as well as their simplification in instrumentation, and the modeling to improve sample timing, are all a great benefit for measuring this important parameter. Expanding the dataset of e values beyond the few that are currently available will be a huge benefit to the interpretation of d13C values of contemporary and fossil organic matter from a variety of habitats.
Specific comments:
The manuscript is very clearly written. My comments, accordingly, are few:
1. Line 122 what is PIC?
2. Line 425 issues with sample foaming during injection into analytic systems. This is not really a comment on the manuscript, just a suggestion for subsequent analyses: try adding antifoam A to the acid instead of using centrifugal filters; there will be less chance of introducing atmospheric CO2.