Salt giants are massive salt deposits (hundreds of metres thick) that form during the
evaporation of semi-enclosed seas. The drivers of salt giant formation and their feedbacks …

This study describes the hydroclimate evolution of the eastern Mediterranean Basin during
the early Messinian (7.2 to 6.5 Ma) time-interval based on analysis of a succession at Agios …

This study intends to review and assess the middle to late Miocene Carbonate Crash (CC)
events in the low to mid latitudes of the Pacific, Indian, Caribbean and Atlantic Oceans as …

Integration of foraminiferal and geochemical data (stable isotope and elemental
composition) from West Alboran Basin (WAB) ODP Site 976 allowed evaluation of the effects …

The Lago Mare phase at the end of the Messinian Salinity Crisis (MSC) in the Mediterranean
has long been known for the Paratethyan affinities of its biota. The taxonomic level of these …

Abstract During the Messinian (7.24–5.33 Ma), the highly dynamic Mediterranean
environment was concomitantly governed by global climate changes and regional tectonic …

Sedimentological, micropalaeontological, and marine geological results from the Early
Jurassic to Eocene carbonate formations of the Ionian zone, from six localities of Epirus …

Field investigation, biostratigraphic, paleoecological, and sedimentary microfacies analyses,
as well as diagenetic processes characterization, were carried out in the Epirus region …

This study details new geochemical analysis from an outcrop in Crete to improve
understanding of the hydrocarbon potential of the southern margin of the Hellenic Arc along …

This study presents novel findings on the drivers of the calcitic planktonic foraminiferal and
aragonitic pteropod Holocene assemblages of the North Aegean Trough (northeastern …