<?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:2009-023084</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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Sea</gco:CharacterString></title><date><CI_Date><date><gco:Date>2001-01-01</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:2009-023084</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Tu Xia</gco:CharacterString></individualName><organisationName><gco:CharacterString>Chinese Academy of Sciences, South China Sea Institute of Oceanology, Guangzhou, China</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" 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Series D, Earth Sciences</gco:CharacterString></name><issueIdentification><gco:CharacterString>44 (10)</gco:CharacterString></issueIdentification><page><gco:CharacterString>865-870</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>High-resolution quantitative analysis of planktonic foraminifera and delta (super 18) O records of the section between 96.49-137.6 mcd at ODP Site 1144 on the continental slope of the northern South China Sea reveal an abrupt cooling event of sea surface temperature (SST) during the last interglacial (MIS 5.5, i.e. 5e). The range of the drop in winter SST may come to 7.5 degrees , corresponding to 1.2% of the delta (super 18) O value of sea surface water. This event is comparable with those discovered in Western Europe and the northern Atlantic Ocean, but is expressed in a more intensive way. 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