georefid:2012-006430georefid:2012-006358SEDIS Publication Catalogueana.macario@awi.dehttp://sedis.iodp.org/pub-catalogue/informationpointOfContact2013-07-08T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=2012-006430<gco:CharacterString>Quantification of the spatial enhancement of ocean anoxia during OAE2 and T-OAE using Mo and U isotope signatures</gco:CharacterString>2010-01-01publicationgeorefid:2012-006430Montoya-Pino, C.Goethe Universitat, Institut fuer Geowissenschaften, Frankfurt, GermanyauthorWeyer, S.Universitaet Koeln, GermanyauthorAnbar, A. D.Arizona State University, United Statesauthorvan de Schootbruggie, B.Deutsches GeoForchungsZentrum, GermanyauthorOschmann, W.authorPross, J.authorArz, H. W.authorDeutsche Forschungsgemeinschaft, Bonn, GermanypublisherdocumentHardcopyIn: Anonymous, IODP-ICDP Kolloquium 2010 IODP-ICDP colloquium 2010100-103completedStratigraphyIsotope geochemistryactinidesanaerobic environmentAtlantic OceanBlack Seablack shalecase studiesCenomanianchemical ratiosclastic rocksCretaceousDemerara RiseEast MediterraneanEhEquatorial AtlanticEuropegeochemistryglobalisotope fractionationisotope ratiosisotopesJurassicLeg 207Lower Jurassicmarine environmentMediterranean SeaMesozoicmetalsMo-97/Mo-95modern analogsmolybdenumNorth AtlanticNorthwest AtlanticOcean Drilling Programoceanic anoxic eventsODP Site 1261organic compoundspaleoenvironmentradioactive isotopessapropelsedimentary rocksstable isotopesToarciantrace metalsTuronianU-238/U-235Upper Cretaceousupper LiassicuraniumWest Atlanticurn:org.iodp:exp:207urnlargerWorkCitationcampaignurn:org.iodp:exp:207:site:1261urnlargerWorkCitationstudyurn:org.iodp:exp:207urnlargerWorkCitationcampaignEnglishgeoscientificInformation-54.1900-54.19009.03009.0300