<?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:2004-066671</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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Pacific Ocean)</gco:CharacterString></title><date><CI_Date><date><gco:Date>2003-01-01</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:2004-066671</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Marino, Maria</gco:CharacterString></individualName><organisationName><gco:CharacterString>Universita di Bari, Dipartimento di Geologia e Geofisica, Bari, Italy</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" 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Site 577 is located on the SW flank of the Shatsky Rise in the NW Pacific Ocean, in 2685m water-depth, and exhibits both good recovery and well-preserved nannofossil assemblages. Most conventional Pleistocene events have been recognised; moreover, quantitative investigations allowed the collection of further data on the stratigraphic distribution of some species (Gephyrocapsa omega &gt;4 mu m, Helicosphaera inversa, Reticulofenestra asanoi, Helicosphaera acuta), thus improving the Pleistocene biostratigraphy of the Shatsky Rise sediments. The available magnetostratigraphic data for Site 577 also allowed the proposal of age-assignments for the following events: the last occurrence of H. acuta, the beginning and end of the temporary disappearance of G. omega, the first occurrence, temporary disappearance, and last occurrence of H. inversa, and the first and last occurrences of R. asanoi.</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>Quaternary 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