What does the Messinian Salinity Crisis teach us about Mediterranean paleo-environmental upheavals?
ID:1592 View Protection:ATTENDEE Updated Time:2024-10-15 14:36:03 Hits:805 Poster Presentation

Start Time:2025-01-15 17:50(Asia/Shanghai)

Duration:15min

Session:S53 Session 53-Geological Analogues for Future Warm Ocean and Cimate » S53-PGeological Analogues for Future Warm Ocean and Climate

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Abstract
Between 5.96 Ma and 5.33 Ma, the brutal Messinian Salinity Crisis profoundly disrupted the environment of the Mediterranean basin and surrounding continental masses. This extraordinary crisis, one of the most spectacular that the Earth has known, is linked to the progressive closure of communications with the Atlantic Ocean at the Betic corridor then the Rif corridor. It had a considerable impact on sedimentation and therefore on paleo-environments: the margins brought to the outcrop by the fall in sea level of around 1500 meters were subjected to intense erosion and were cut by deep canyons, while the products of this erosion accumulated at the foot of the slope, in the form of detrital cones. During this period, very short on the geological time scale, a thick evaporitic series was deposited in the deep basins, with a mobile salt layer, subsequently creating intense gravity-driven tectonics all around the Mediterranean. The reflooding in the basal Pliocene (Zanclean) was dazzling following the sudden reestablishment of connections with the Atlantic Ocean at the Strait of Gibraltar. We present here a synthesis of studies on several Mediterranean margins. This integrated approach thus makes it possible to study the impact of the Messinian event on the margins and basins in varied tectono-sedimentary contexts, to overcome certain local control factors specific to each study area (type of margin, thickness/lithology of the eroded series, paleo-morphologies, size of the watershed, tectonic context) and to specify the modalities of the crisis (erosion and deposition processes, volumes involved, modalities of variation of the water body, role of Mediterranean thresholds, climatic variations). The geological recording of this major crisis in the history of the Mediterranean, thanks to the discrimination of proxies, thus offers keys to better understand the major environmental and oceanological changes that resulted from it.
Keywords
Messinian Salinity Crisis,paleoenvironmental change.,tectonics,geophysics
Speaker
Virginie Gaullier
Professor LOG - University of Lille

Submission Author
Virginie GAULLIER LOG - University of Lille
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Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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