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Evidence of early bottom water current flow after the Messinian Salinity Crisis in the Gulf of Cadiz 5
Van Der Schee, Marlies; Sierro, F. J.; Jimenez-espejo, F. J.; Hernandez-molina, F. J.; Flecker, R.; Flores, J. A.; Acton, G.; Gutjahr, M.; Grunert, P.; Garcia-gallardo, A.; Andersen, N..
Integrated Ocean Drilling Program (IODP) Expedition 339 cored multiple sites in the Gulf of Cadiz in order to study contourite deposition resulting from Mediterranean Outflow water (MOW). One Hole, U1387C, was cored to a depth of 865.85 m below seafloor (mbsf) with the goal of recovering the latest Miocene to Pliocene transition in order to evaluate the history of MOW immediately after the end of the Messinian Salinity Crisis. To understand this history, an accurate age model for the succession is needed, but is challenging to construct, because the Miocene-Pliocene boundary is not marked by a clear biostratigraphic event in the Atlantic and coring gaps occur within the recovered stratigraphic record. These limitations are overcome by combining a variety...
Tipo: Text Palavras-chave: Miocene-Pliocene boundary; Gulf of Cadiz; IODP Expedition 339; Mediterranean outflow water; Messinian salinity crisis; Contourites.
Ano: 2016 URL: https://archimer.ifremer.fr/doc/00421/53217/54843.pdf
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