<?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:2012-030509</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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T., Dewangan, Pawan, Hasegawa, Hitoshi, Hathorne, Edmund, Hayashi, Hiroki, Holbourn, Ann, Hovan, Steven, Iijima, Koichi, Ito, Takashi, Kimoto, Katsunori, Murphy, Daniel, Ogane, Kaoru, Romero, Oscar, Schneider, Leah, Sluijs, Appy, Jun Tian, Tsujimoto, Akira, Wade, Bridget, Wilkens, Roy, Yamamoto, Shinya, Yamazaki, Toshitsugu, Proceeding of the Integrated Ocean Drilling Program; Pacific Equatorial Age Transect; Expeditions 320 and 321 of the riserless drilling platform from and to Honolulu, Hawaii (USA); Sites U1331-U1336, 5 March-4 May 2009; and Honolulu, Hawaii (USA), to San Diego California (USA); Sites U1337-U1338, 4 May-22 June 2009</gco:CharacterString></name><issueIdentification><gco:CharacterString>320/321</gco:CharacterString></issueIdentification></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>We used X-ray fluorescence (XRF) scanning on Site U1338 sediments from Integrated Ocean Drilling Program Expedition 321 to measure sediment geochemical compositions at 2.5 cm resolution for the 450 m of the Site U1338 spliced sediment column. This spatial resolution is equivalent to approximately 2 k.y. age sampling in the 0-5 Ma section and approximately 1 k.y. resolution from 5 to 17 Ma. Here we report the data and describe data acquisition conditions to measure Al, Si, K, Ca, Ti, Fe, Mn, and Ba in the solid phase. We also describe a method to convert the data from volume-based raw XRF scan data to a normalized mass measurement ready for calibration by other geochemical methods. 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