<gco:CharacterString>A CO (sub 2) decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous oceanic anoxic event 2</gco:CharacterString>

georefid:2010-074517SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-07-06T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1016/j.epsl.2010.02.027<gco:CharacterString>A CO (sub 2) decrease-driven cooling and increased latitudinal temperature gradient during the mid-Cretaceous oceanic anoxic event 2</gco:CharacterString>2010-01-01publicationgeorefid:2010-074517doi:10.1016/j.epsl.2010.02.027Sinninghe Damste, Jaap S.Royal Netherlands Institute for Sea Research, Department of Marine Organic Biogeochemistry, Den Burg, Netherlandsauthorvan Bentum, Elisabeth C.Utrecht University, NetherlandsauthorReichart, Gert-JanUniversity of Frankfurt, Federal Republic of GermanyauthorPross, JoergauthorSchouten, StefanauthorElsevier, Amsterdam, NetherlandspublisherdocumentHardcopyEarth and Planetary Science Letters293 (1-2)97-103completedStratigraphyAtlantic OceanburialC-13/C-12carboncarbon dioxideCenomaniancoolingCretaceousgreenhouse effectisotope ratiosisotopeslatitudeLeg 210MesozoicmicrofossilsMiddle CretaceousNewfoundland BasinNorth AtlanticNorthwest AtlanticOcean Drilling Programoceanic anoxic eventsODP Site 1276organic carbonorganic compoundspaleoclimatologypaleotemperaturepalynomorphspartial pressuresea-surface temperaturestable isotopestemperaturetotal organic carbonTuronianUpper Cretaceousurn:org.iodp:exp:210urnlargerWorkCitationcampaignurn:org.iodp:exp:210:site:1276urnlargerWorkCitationstudyurn:org.iodp:exp:210urnlargerWorkCitationcampaignEnglishgeoscientificInformation-44.4700-44.470045.240045.2400Supplementary data available in online version