<?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:2009-028553</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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events</gco:CharacterString></title><date><CI_Date><date><gco:Date>2002-01-01</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:2009-028553</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Fang Nianqiao</gco:CharacterString></individualName><organisationName><gco:CharacterString>Chinese University of Geosciences, Institute of Marine Geology and Geophysics, Beijing, China</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" 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Using the identification of foraminiferal assemblages and an analysis of foraminiferal tests, combined with the previous sedimentary, geochemical, paleomagnetic and micropaleontological data, we made an integrated analysis of ridge records since 9 Ma, represented by ODP Site 758. Some significant signals of a variable marine environment, which responded to the phased uplift of the plateau from 3.7 Ma to 3.2 Ma, 0.8 Ma to 0.6 Ma, and 0.17 Ma to 0.16 Ma, can be recognized in the records. We point out that the intensity of the Indian winter monsoon is a key symptom mirroring the tectonics of the plateau. 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