The transition from normal marine to evaporitic conditions recorded in a cold seep environment: The Messinian succession of Northern Italy

Messinian pre-evaporitic seep carbonates outcropping in the Tuscan-Romagna area share a common upward stratigraphic trend: massive seep carbonates rich in large lucinids, modiolids and planktonic foraminifera pass upward to horizontally laminated carbonates free of macrofauna and foraminifera. A tra...

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Veröffentlicht in:Marine and petroleum geology 2024-02, Vol.160, p.106617, Article 106617
Hauptverfasser: Conti, S., Argentino, C., Bojanowski, M., Fioroni, C., Giunti, S., Kremer, B., Fontana, D.
Format: Artikel
Sprache:eng
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