georefid:2007-126742SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-06-23T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2007-126742The world-wide sea level including the Mediterranean Sea at the late Miocene period (Messinian Stage) was 2,000m lower than that of present2004-01-01publicationgeorefid:2007-126742
Hanada, MasaakiTokai University, Institute of Oceanic Research and Development, Tokai, Japanauthor[International Geological Congress], [location varies], InternationalpublisherdocumentHardcopyIn: Anonymous, Italia 2004; 32nd international geological congress; abstracts32, Part 1772completedStratigraphyAlboran SeaAtlantic OceanCenozoicchemically precipitated rocksDeep Sea Drilling ProjectevaporitesGorringe BankIPODLeg 13Mediterranean SeaMessinianMioceneNeogeneNorth AtlanticOcean Drilling Programpaleo-oceanographypaleoenvironmentpaleogeographysalinitysea-level changessedimentary rockssedimentationTertiaryupper MioceneWest Mediterraneanurn:org.iodp:exp:13
urnlargerWorkCitationcampaignEnglishgeoscientificInformation-5.0000-3.000035.300036.3000