A model for marine sedimentary carbonate diagenesis and paleoclimate proxy signal tracking: IMP v1.0
<p>The preservation of calcium carbonate in marine sediments is central to controlling the alkalinity balance of the ocean and, hence, the ocean–atmosphere partitioning of <span class="inline-formula">CO<sub>2</sub></span>. To successfully address carbon cycle...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2021-10-01
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Series: | Geoscientific Model Development |
Online Access: | https://gmd.copernicus.org/articles/14/5999/2021/gmd-14-5999-2021.pdf |