Articles | Volume 14, issue 10
Geosci. Model Dev., 14, 5999–6023, 2021
https://doi.org/10.5194/gmd-14-5999-2021
Geosci. Model Dev., 14, 5999–6023, 2021
https://doi.org/10.5194/gmd-14-5999-2021

Model description paper 07 Oct 2021

Model description paper | 07 Oct 2021

A model for marine sedimentary carbonate diagenesis and paleoclimate proxy signal tracking: IMP v1.0

Yoshiki Kanzaki et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on gmd-2020-405', David Archer, 11 May 2021
    • AC1: 'Reply on RC1', Yoshiki Kanzaki, 17 Aug 2021
  • RC2: 'Comment on gmd-2020-405', Anonymous Referee #2, 07 Jun 2021
    • AC2: 'Reply on RC2', Yoshiki Kanzaki, 17 Aug 2021
  • RC3: 'Comment on gmd-2020-405', Guy Munhoven, 15 Jun 2021
    • AC3: 'Reply on RC3', Yoshiki Kanzaki, 17 Aug 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Yoshiki Kanzaki on behalf of the Authors (17 Aug 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (01 Sep 2021) by Andrew Yool

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Yoshiki Kanzaki on behalf of the Authors (05 Oct 2021)   Author's adjustment   Manuscript
EA: Adjustments approved (06 Oct 2021) by Andrew Yool
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Short summary
Sedimentary carbonate plays a central role in regulating Earth’s carbon cycle and climate, and also serves as an archive of paleoenvironments, hosting various trace elements/isotopes. To help obtain true environmental changes from carbonate records over diagenetic distortion, IMP has been newly developed and has the capability to simulate the diagenesis of multiple carbonate particles and implement different styles of particle mixing by benthos using an adapted transition matrix method.