Articles | Volume 20, issue 8
https://doi.org/10.5194/cp-20-1785-2024
https://doi.org/10.5194/cp-20-1785-2024
Research article
 | 
12 Aug 2024
Research article |  | 12 Aug 2024

Modelling Mediterranean ocean biogeochemistry of the Last Glacial Maximum

Katharina D. Six, Uwe Mikolajewicz, and Gerhard Schmiedl

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Short summary
We use a physical and biogeochemical ocean model of the Mediterranean Sea to obtain a picture of the Last Glacial Maximum. The shallowing of the Strait of Gibraltar leads to a shallower pycnocline and more efficient nutrient export. Consistent with the sediment data, an increase in organic matter deposition is simulated, although this is based on lower biological production. This unexpected but plausible result resolves the apparent contradiction between planktonic and benthic proxy data.