Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6024
AuthorsCorbí, H.* 
Caracuel, J. E.* 
Dinarès-Turell, J.* 
Lancis, C.* 
Pina, J. A.* 
Soria, J. M.* 
Tent-Manclús, J. E.* 
Yébenes, A.* 
TitleLa sección de San Miguel de Salinas (Cuenca del Bajo Segura). Significado paleoambiental de las asociaciones de foraminíferos en relación con la Crisis de Salinidad del Messiniense
Other TitlesThe San Miguel de Salinas section (Bajo Segura Basin). Palaeoenvironmental significance of the foraminiferal assemblages related to the Messinian Salinity Crisis
Issue Date2009
Series/Report no./ 46 (2009)
URIhttp://hdl.handle.net/2122/6024
KeywordsForaminifera
messinian salinity crisis
Pliocene
Bajo Segura Basin
palaeoenvironments
Subject Classification04. Solid Earth::04.04. Geology::04.04.08. Sediments: dating, processes, transport 
04. Solid Earth::04.04. Geology::04.04.10. Stratigraphy 
04. Solid Earth::04.05. Geomagnetism::04.05.06. Paleomagnetism 
AbstractIn the composite section of San Miguel de Salinas the following synthems are represented: MI (preevaporitic Messinan), MII (syn-evaporitic Messinian) and P (post-evaporitic Pliocene). The foraminiferal assemblages of these synthems have been studied in order to reveal the palaeoenvironmental changes related to the Mediterranean Salinity Crisis. The change between MI and MII synthems is characterized by the reduction of the foraminiferal biodiversity. Synthem MII records palaeoenvironmental stress related to the evaporitic deposition during the Salinity Crisis. Synthem P marks an abrupt increase of the foraminiferal biodiversity in coincidence with the Pliocene reflooding of the Mediterranean Sea.
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