<?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:2011-001322</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=2011-001322</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Late Cenozoic history of sea level changes documented from high-resolution seismic data on the northern Sunda Shelf, South China Sea</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:2011-001322</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Zhong Guangfa</gco:CharacterString></individualName><organisationName><gco:CharacterString>Tongji University, Key Laboratory of Marine Geology of China Ministry of Education, Shanghai, China</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>Geng Jianhua</gco:CharacterString></individualName><organisationName><gco:CharacterString>Hamburg University, Germany</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>Zhou Zuyi</gco:CharacterString></individualName><organisationName><gco:CharacterString>Guangzhou Marine Geological Survey, China</gco:CharacterString></organisationName><role><CI_RoleCode 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lines acquired by German Sonne 115 Cruise in 1997. On the curve, about 36 cycles of sea level changes can be recognized with periods ranging from 0.08 Ma to 0.29 Ma, which are fallen into 4th order of sea level cycles. The curve is compared with the reprocessed deep-sea stable oxygen isotope data from benthic foraminifera on ODP sites 1,148 and 846 by resampling and filtering. Both of them matched well, which suggests that the 4th order of eustatic sea level changes during the last 5.33 Ma was probably controlled by changes in the sizes of the ice caps.</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 geology</gco:CharacterString></keyword><keyword><gco:CharacterString>Applied geophysics</gco:CharacterString></keyword><keyword><gco:CharacterString>Cenozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>deglaciation</gco:CharacterString></keyword><keyword><gco:CharacterString>eustacy</gco:CharacterString></keyword><keyword><gco:CharacterString>Foraminifera</gco:CharacterString></keyword><keyword><gco:CharacterString>geophysical methods</gco:CharacterString></keyword><keyword><gco:CharacterString>glacial geology</gco:CharacterString></keyword><keyword><gco:CharacterString>high-resolution methods</gco:CharacterString></keyword><keyword><gco:CharacterString>ice caps</gco:CharacterString></keyword><keyword><gco:CharacterString>Indonesian Seas</gco:CharacterString></keyword><keyword><gco:CharacterString>Invertebrata</gco:CharacterString></keyword><keyword><gco:CharacterString>isotope ratios</gco:CharacterString></keyword><keyword><gco:CharacterString>isotopes</gco:CharacterString></keyword><keyword><gco:CharacterString>Java Sea</gco:CharacterString></keyword><keyword><gco:CharacterString>microfossils</gco:CharacterString></keyword><keyword><gco:CharacterString>Neogene</gco:CharacterString></keyword><keyword><gco:CharacterString>O-18/O-16</gco:CharacterString></keyword><keyword><gco:CharacterString>Ocean Drilling Program</gco:CharacterString></keyword><keyword><gco:CharacterString>oxygen</gco:CharacterString></keyword><keyword><gco:CharacterString>Pacific Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>paleoclimatology</gco:CharacterString></keyword><keyword><gco:CharacterString>paleoenvironment</gco:CharacterString></keyword><keyword><gco:CharacterString>Pliocene</gco:CharacterString></keyword><keyword><gco:CharacterString>Protista</gco:CharacterString></keyword><keyword><gco:CharacterString>sea-level changes</gco:CharacterString></keyword><keyword><gco:CharacterString>seismic methods</gco:CharacterString></keyword><keyword><gco:CharacterString>seismic stratigraphy</gco:CharacterString></keyword><keyword><gco:CharacterString>South Pacific</gco:CharacterString></keyword><keyword><gco:CharacterString>Southwest Pacific</gco:CharacterString></keyword><keyword><gco:CharacterString>stable isotopes</gco:CharacterString></keyword><keyword><gco:CharacterString>Sunda Shelf</gco:CharacterString></keyword><keyword><gco:CharacterString>Tertiary</gco:CharacterString></keyword><keyword><gco:CharacterString>upper Cenozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>West Pacific</gco:CharacterString></keyword></MD_Keywords></descriptiveKeywords><language><gco:CharacterString>English</gco:CharacterString></language><topicCategory><MD_TopicCategoryCode>geoscientificInformation</MD_TopicCategoryCode></topicCategory><extent><EX_Extent><geographicElement><EX_GeographicBoundingBox><westBoundLongitude><gco:Decimal>106.0000</gco:Decimal></westBoundLongitude><eastBoundLongitude><gco:Decimal>116.0000</gco:Decimal></eastBoundLongitude><southBoundLatitude><gco:Decimal>-8.0000</gco:Decimal></southBoundLatitude><northBoundLatitude><gco:Decimal>-2.3000</gco:Decimal></northBoundLatitude></EX_GeographicBoundingBox></geographicElement><geographicElement><EX_GeographicDescription><geographicIdentifier><MD_Identifier><code><gco:CharacterString>Java Sea</gco:CharacterString></code></MD_Identifier></geographicIdentifier></EX_GeographicDescription></geographicElement></EX_Extent></extent></MD_DataIdentification></identificationInfo></MD_Metadata>