Freshening of the Mediterranean Salt Giant: controversies and certainties around the terminal (Upper Gypsum and Lago-Mare) phases of the Messinian Salinity Crisis

The late Miocene evolution of the Mediterranean Basin is characterized by major changes in connectivity, climate and tectonic activity resulting in unprecedented environmental and ecological disruptions. During the Messinian Salinity Crisis (MSC, 5.97-5.33 Ma) this culminated in most scenarios first...

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Veröffentlicht in:	Earth-science reviews 2021-05, Vol.216, p.103577, Article 103577
Hauptverfasser:	Andreetto, F., Aloisi, G., Raad, F., Heida, H., Flecker, R., Agiadi, K., Lofi, J., Blondel, S., Bulian, F., Camerlenghi, A., Caruso, A., Ebner, R., Garcia-Castellanos, D., Gaullier, V., Guibourdenche, L., Gvirtzman, Z., Hoyle, T.M., Meijer, P.T., Moneron, J., Sierro, F.J., Travan, G., Tzevahirtzian, A., Vasiliev, I., Krijgsman, W.
Format:	Artikel
Sprache:	eng
Schlagworte:	Connectivity proxies Earth Sciences Lago-Mare Mediterranean stratigraphy Messinian Salinity Crisis Paleogeography Paratethys Sciences of the Universe
Online-Zugang:	Volltext
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