<?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:2009-027681</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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areas</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:2009-027681</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Williams, Trevor</gco:CharacterString></individualName><organisationName><gco:CharacterString>Lamont-Doherty Earth Observatory, Palisades, NY, United States</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" 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However, even though there have been many thermochronologic analyses of the onshore exposures, most of the East Antarctic coastline is ice-covered, and the onshore metamorphic provinces are not all well delimited. Roy et al. (2007) found that the thermochronologic signature of IRD from circum-Antarctic marine core-tops defined several geographic sectors with distinct provenance signals, thereby providing a base map for fingerprinting sediment sources from the Antarctic margin. We have subsequently used this base map to find the provenance of IRD back to 19 million years ago at ODP Site 1165, offshore of Prydz Bay, revealing ice-rafting conditions sometimes very different to today, with icebergs transported westwards from as far as the Adelie coast (Williams et al., 2007). 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