<?xml version="1.0" encoding="UTF-8" ?><MD_Metadata xmlns="http://www.isotc211.org/2005/gmd" xmlns:gco="http://www.isotc211.org/2005/gco" xmlns:gml="http://www.opengis.net/gml" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.isotc211.org/2005/gmd http://www.isotc211.org/2005/gmd/gmd.xsd"><fileIdentifier><gco:CharacterString>georefid:2011-092182</gco:CharacterString></fileIdentifier><contact><CI_ResponsibleParty><organisationName><gco:CharacterString>SEDIS Publication Catalogue</gco:CharacterString></organisationName><contactInfo><CI_Contact><address><CI_Address><electronicMailAddress><gco:CharacterString>ana.macario@awi.de</gco:CharacterString></electronicMailAddress></CI_Address></address><onlineResource><CI_OnlineResource><linkage><URL>http://sedis.iodp.org/pub-catalogue/</URL></linkage><function><CI_OnLineFunctionCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode_information">information</CI_OnLineFunctionCode></function></CI_OnlineResource></onlineResource></CI_Contact></contactInfo><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_pointOfContact">pointOfContact</CI_RoleCode></role></CI_ResponsibleParty></contact><dateStamp><gco:DateTime>2013-07-08T00:00:00Z</gco:DateTime></dateStamp><dataSetURI><gco:CharacterString>http://sedis.iodp.org/pub-catalogue/index.php?id=2011-092182</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>A dynamic Cenozoic Arctic Ocean</gco:CharacterString></title><date><CI_Date><date><gco:Date>2008-01-01</gco:Date></date><dateType><CI_DateTypeCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_DateTypeCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_DateTypeCode_publication">publication</CI_DateTypeCode></dateType></CI_Date></date><identifier><MD_Identifier><code><gco:CharacterString>georefid:2011-092182</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Moran, Kathryn</gco:CharacterString></individualName><organisationName><gco:CharacterString>University of Rhode Island, United States</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_author">author</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Backman, Jan</gco:CharacterString></individualName><organisationName><gco:CharacterString>Stockholm University, Sweden</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_author">author</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Mayer, Larry A.</gco:CharacterString></individualName><organisationName><gco:CharacterString>University of New Hampshire, United States</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_author">author</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><citedResponsibleParty><CI_ResponsibleParty><organisationName><gco:CharacterString>[International Geological Congress], [location varies], International</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_publisher">publisher</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><presentationForm><CI_PresentationFormCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_PresentationFormCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_PresentationFormCode_documentHardcopy">documentHardcopy</CI_PresentationFormCode></presentationForm><series><CI_Series><name><gco:CharacterString>In: Anonymous, 33rd international geological congress; abstracts</gco:CharacterString></name><issueIdentification><gco:CharacterString>33</gco:CharacterString></issueIdentification></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>In 2004, the Integrated Ocean Drilling Program conducted the Arctic Coring Expedition (ACEX). This technically-challenging expedition recovered the first Cenozoic sediment record from the Arctic Ocean. The many results contributed by over 40 investigators from ACEX have transformed our view of the Arctic's paleoclimate. For example, during ACEX, the massulae from fresh water ferns were found at 49 Ma that suggests fresh water dominated the Arctic at that time. Ice-rafted debris was found to have occurred much earlier than previously thought during the Eocene and in an environment of high organic carbon content. Early analyses also revealed an unexpected hiatus that occurred between several of the most spectacular sediment cores in terms of color, e.g. turquoise, and structure, starkly contrasting black and white cross-bedding that is now dubbed the "zebra" core. The Paleocene-Eocene Thermal Maximum (PETM) was also recovered. Analyses have revealed surprisingly high Arctic Ocean surface water temperatures and a hydrologically active system during the PETM. ACEX results have also enabled interpretation of a major oceanographic reorganization at 17.5 Ma with ventilation of the Arctic Ocean to the North Atlantic through the Fram Strait. Here we summarize these transformational findings and the most recent results from the ACEX record that highlight sea ice and iceberg history reconstructions and descriptions of the age and depositional environments and their link to tectonic histories.</gco:CharacterString></abstract><status><MD_ProgressCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#MD_ProgressCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#MD_ProgressCode_completed">completed</MD_ProgressCode></status><descriptiveKeywords><MD_Keywords><keyword><gco:CharacterString>Stratigraphy</gco:CharacterString></keyword><keyword><gco:CharacterString>Arctic Coring EXpedition</gco:CharacterString></keyword><keyword><gco:CharacterString>Arctic Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>carbon</gco:CharacterString></keyword><keyword><gco:CharacterString>Cenozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>cores</gco:CharacterString></keyword><keyword><gco:CharacterString>cross-bedding</gco:CharacterString></keyword><keyword><gco:CharacterString>Fram Strait</gco:CharacterString></keyword><keyword><gco:CharacterString>ice</gco:CharacterString></keyword><keyword><gco:CharacterString>ice rafting</gco:CharacterString></keyword><keyword><gco:CharacterString>icebergs</gco:CharacterString></keyword><keyword><gco:CharacterString>Integrated Ocean Drilling Program</gco:CharacterString></keyword><keyword><gco:CharacterString>marine sediments</gco:CharacterString></keyword><keyword><gco:CharacterString>organic carbon</gco:CharacterString></keyword><keyword><gco:CharacterString>paleo-oceanography</gco:CharacterString></keyword><keyword><gco:CharacterString>Paleocene-Eocene Thermal Maximum</gco:CharacterString></keyword><keyword><gco:CharacterString>paleoclimatology</gco:CharacterString></keyword><keyword><gco:CharacterString>paleoenvironment</gco:CharacterString></keyword><keyword><gco:CharacterString>Paleogene</gco:CharacterString></keyword><keyword><gco:CharacterString>paleogeography</gco:CharacterString></keyword><keyword><gco:CharacterString>planar bedding structures</gco:CharacterString></keyword><keyword><gco:CharacterString>sea ice</gco:CharacterString></keyword><keyword><gco:CharacterString>sea-surface temperature</gco:CharacterString></keyword><keyword><gco:CharacterString>sedimentary structures</gco:CharacterString></keyword><keyword><gco:CharacterString>sediments</gco:CharacterString></keyword><keyword><gco:CharacterString>tectonics</gco:CharacterString></keyword><keyword><gco:CharacterString>Tertiary</gco:CharacterString></keyword><keyword><gco:CharacterString>ventilation</gco:CharacterString></keyword></MD_Keywords></descriptiveKeywords><language><gco:CharacterString>English</gco:CharacterString></language><topicCategory><MD_TopicCategoryCode>geoscientificInformation</MD_TopicCategoryCode></topicCategory><extent><EX_Extent><geographicElement><EX_GeographicBoundingBox><westBoundLongitude><gco:Decimal>-8.0000</gco:Decimal></westBoundLongitude><eastBoundLongitude><gco:Decimal>9.0000</gco:Decimal></eastBoundLongitude><southBoundLatitude><gco:Decimal>78.0000</gco:Decimal></southBoundLatitude><northBoundLatitude><gco:Decimal>81.0000</gco:Decimal></northBoundLatitude></EX_GeographicBoundingBox></geographicElement><geographicElement><EX_GeographicDescription><geographicIdentifier><MD_Identifier><code><gco:CharacterString>Fram Strait</gco:CharacterString></code></MD_Identifier></geographicIdentifier></EX_GeographicDescription></geographicElement></EX_Extent></extent></MD_DataIdentification></identificationInfo></MD_Metadata>