<?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:2001-019136</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 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rates</gco:CharacterString></title><date><CI_Date><date><gco:Date>1999-01-01</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:2001-019136</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Ogg, James G.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Purdue University, Department of Earth and Atmospheric Sciences, West Lafayette, IN, United States</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" 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Upper Danian magnetic polarity zone C27 spans 35 to 36 obliquity cycles at both sites. The corresponding cycle-tuned duration of 1.47 million years is consistent with trends from astronomical tuning of lower Danian polarity chron C29 and revised 40Ar/39Ar age calibration of the Campanian through Eocene magnetic polarity time scale.The complete cycle-tuned Danian stage spans 3.65 m. y. (65.5 Ma to 61.85 Ma). Spreading rates on the synthetic South Atlantic marine magnetic profile that serves as a standard for scaling magnetic polarity chrons display progressive slowing during the Maastrichtian through Danian stages, a constant rate during the late Paleogene and early Eocene epochs, followed by a rapid acceleration during the middle Eocene.</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>Atlantic Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>Blake Nose</gco:CharacterString></keyword><keyword><gco:CharacterString>Blake 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