<?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:2010-041937</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>2011-07-06T00:00:00Z</gco:DateTime></dateStamp><dataSetURI><gco:CharacterString>http://sedis.iodp.org/pub-catalogue/index.php?id=10.2204/iodp.proc.303306.208.2010</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Data report; Pleistocene paleomagnetic and rock magnetic records from IODP Site U1312 on the southern flank of the King's Trough</gco:CharacterString></title><date><CI_Date><date><gco:Date>2010-01-01</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:2010-041937</gco:CharacterString></code></MD_Identifier></identifier><identifier><MD_Identifier><code><gco:CharacterString>doi:10.2204/iodp.proc.303306.208.2010</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Kanamatsu, Toshiya</gco:CharacterString></individualName><organisationName><gco:CharacterString>Japan Agency for Marine-Earth Science and Technology, Institute for Research on Earth Evolution, Yokosuka, Japan</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>Acton, Gary D.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Japan Agency for Marine-Earth Science and Technology, Japan</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>Evans, Helen</gco:CharacterString></individualName><organisationName><gco:CharacterString>Akita University, Japan</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>Guyodo, Yohan J. 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T., Kanamatsu, Toshiya, Sato, Tokiyuki, Stein, Ruediger, Zarikian, Carlos A. Alvarez, Malone, Mitchell J., Robinson, Stuart, de Abreu, Lucia, Bartoli, Gretta Linda, Chiyonobu, Shun, Damuth, John E., De Vernal, Anne, Ennyu, Atsuhito, Esmerode, Estela Vazquez, Funakawa, Satoshi, Henderson, Samuel S., Hodell, David A., Ito, Masashi, Kawamura, Kiichiro, Kawamura, Noriko, Krissek, Lawrence A., Leigh, Sasha N. B., Liu Chuanlian, Mazaud, Alain, Obrochta, Stephen, Romero, Oscar E., Schiebel, Ralf, Shimada, Chieko, Stoner, Joseph S., Wilkens, Roy H., Wright, James D., Yamasaki, Makoto, Higgins, Sean M., Aboud, Essam, Acton, Gary D., Akimoto, Kazumi, Bailey, Ian, Bjorklund, Kjell R., Evans, Helen, Fang Nianqiao, Ferretti, Patrizia, Gruetzner, Jens, Guyodo, Yohan J. B., Hatakeda, Kentaro, Harris, Robert, Hagino, Kyoko, Hefter, Jens Norbert, Judge, Shelley A., Kulhanek, Denise K., Nanayama, Futoshi, Nielsen, Simon H. H., Ohno, Masao, Rashid, Harunur, Sanchez, Francisco J. Sierro, Voelker, Antje, Zhai, Qiumin, Proceedings of the Integrated Ocean Drilling Program; North Atlantic climate; Expeditions 303 and 306 of the riserless drilling platform; St. John's, Newfoundland, to Ponta Delgada, Azores; Sites U1302-U1308, 25 September-17 November 2004; and Ponta Delgada, Azores, to Dublin, Ireland, 2 March-26 April 2006</gco:CharacterString></name><issueIdentification><gco:CharacterString>303/306</gco:CharacterString></issueIdentification><page><gco:CharacterString>1-9</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>Paleomagnetic and rock magnetic studies were conducted on sediment obtained from Integrated Ocean Drilling Program Site U1312 in order to construct an age model for understanding spatial and temporal changes in North Atlantic paleoceanography. Paleomagnetic directions suggest that the sedimentary sequence from 0 to 59.6 m composite depth (mcd) covers geomagnetic polarities from 0 to 3.6 Ma. 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