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Numerical model of the Messinian Mediterranean combining hydrological water balance, river erosion, and flexural isostasy: TISC code and input dataset for the Lago-Mare

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Jun 12, 2025 version files 243.55 MB
Jun 13, 2025 version files 243.55 MB

Abstract

We hereby share the code and input/output datasets for the numerical model of the Messinian Salinity Crisis published in the Science Advances paper linked to this submission.

The Messinian salinity crisis (MSC) was a short period of isolation of the Mediterranean Sea causing the precipitation of a million cubic kilometers of salt. The puzzling sedimentary record that formed after salt deposition yields conflicting levels of desiccation, ranging from a full exposure of most of the Mediterranean seafloor based on shallow sediment found in the abyss to a nearly full Mediterranean scenario as suggested by similar, fresher-water deposits ubiquitous along the coastline: the so-called Lago-Mare formation.

We use the TISC landscape evolution model (integrating fluvial drainage, hydrological balance in endorheic lakes, fluvial erosion, and flexural isostasy) to explore the expected evolution for the drawdown stage of the Messinian salinity crisis, known as the 'Lago-Mare'. The model is constrained by published climate and sediment budget estimates. 

The results show that the propagation of an erosional wave into the surrounding continents added a gradual sea level rise to the climatic oscillations of the Mediterranean. This retrogressive fluvial incision of the spillways of the Paratethys and the Pannonian basins also explains the Mediterranean transition to fresher water conditions during the MSC.