Articles | Volume 14, issue 10
https://doi.org/10.5194/gmd-14-5999-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-14-5999-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Model description paper
| 
07 Oct 2021
Model description paper |
| 07 Oct 2021
| 07 Oct 2021
A model for marine sedimentary carbonate diagenesis and paleoclimate proxy signal tracking: IMP v1.0
Department of Earth and Planetary Sciences, University of California – Riverside, Riverside, CA 92521, USA
currently at: School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, GA 30332, USA
Dominik Hülse
Department of Earth and Planetary Sciences, University of California – Riverside, Riverside, CA 92521, USA
Sandra Kirtland Turner
Department of Earth and Planetary Sciences, University of California – Riverside, Riverside, CA 92521, USA
Andy Ridgwell
Department of Earth and Planetary Sciences, University of California – Riverside, Riverside, CA 92521, USA
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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
trueenvironmental 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.
Sedimentary carbonate plays a central role in regulating Earth’s carbon cycle and climate, and...
