<?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:2003-060391</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>2011-06-23T00:00:00Z</gco:DateTime></dateStamp><dataSetURI><gco:CharacterString>http://sedis.iodp.org/pub-catalogue/index.php?id=2003-060391</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Review of the mineralogy of the Cretaceous-Tertiary boundary clay; evidence supporting a major extraterrestrial catastrophic event</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:2003-060391</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Ortega-Huertas, M.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Universidad de Granada, Departamento de Mineralogia y Petrologia, Granada, Spain</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>Martinez-Ruiz, F.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Universite de Lille, France</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>Palomo, I.</gco:CharacterString></individualName><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>Chamley, H.</gco:CharacterString></individualName><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><organisationName><gco:CharacterString>Mineralogical Society, London, United Kingdom</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_publisher">publisher</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><presentationForm><CI_PresentationFormCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_PresentationFormCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_PresentationFormCode_documentHardcopy">documentHardcopy</CI_PresentationFormCode></presentationForm><series><CI_Series><name><gco:CharacterString>Clay Minerals</gco:CharacterString></name><issueIdentification><gco:CharacterString>37 (3)</gco:CharacterString></issueIdentification><page><gco:CharacterString>395-411</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>The proposed impact event at the end of the Cretaceous resulted in mass extinctions and subsequently significant variations in the geochemical and mineralogical composition of the sediments marking the K/T boundary. The impact-generated material derived from target rocks produced the ejecta layer deposits around Chicxulub crater, which were subsequently diagenetically altered to mainly smectite in marine sections and to kaolinite in continental sections. The fireball layer represents the cosmic dust dispersed and deposited globally and contains smectite derived from the alteration of microkrystites and the finest fraction. The lowermost Danian clay layer, recognized in marine sections, resulted from the sudden decrease in ocean productivity and represents a reduced sedimentation deposit. Its clay mineral associations depend on local environmental conditions and diagenetic processes. Overall, the diagenetic alteration of the boundary materials resulted in a significant modification of original signatures. The composition of the clay mineral phases can, however, still be evidence of the nature of the precursor materials providing evidence for an extraterrestrial impact event.</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>Sedimentary petrology</gco:CharacterString></keyword><keyword><gco:CharacterString>Stratigraphy</gco:CharacterString></keyword><keyword><gco:CharacterString>alteration</gco:CharacterString></keyword><keyword><gco:CharacterString>Atlantic Ocean</gco:CharacterString></keyword><keyword><gco:CharacterString>Blake Nose</gco:CharacterString></keyword><keyword><gco:CharacterString>Blake Plateau</gco:CharacterString></keyword><keyword><gco:CharacterString>catastrophism</gco:CharacterString></keyword><keyword><gco:CharacterString>Cenozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>chemical composition</gco:CharacterString></keyword><keyword><gco:CharacterString>Chicxulub Crater</gco:CharacterString></keyword><keyword><gco:CharacterString>clay mineralogy</gco:CharacterString></keyword><keyword><gco:CharacterString>clay minerals</gco:CharacterString></keyword><keyword><gco:CharacterString>cosmic dust</gco:CharacterString></keyword><keyword><gco:CharacterString>Cretaceous</gco:CharacterString></keyword><keyword><gco:CharacterString>crystal chemistry</gco:CharacterString></keyword><keyword><gco:CharacterString>Deep Sea Drilling Project</gco:CharacterString></keyword><keyword><gco:CharacterString>diagenesis</gco:CharacterString></keyword><keyword><gco:CharacterString>ejecta</gco:CharacterString></keyword><keyword><gco:CharacterString>fireballs</gco:CharacterString></keyword><keyword><gco:CharacterString>formula</gco:CharacterString></keyword><keyword><gco:CharacterString>glass materials</gco:CharacterString></keyword><keyword><gco:CharacterString>impact features</gco:CharacterString></keyword><keyword><gco:CharacterString>K-T boundary</gco:CharacterString></keyword><keyword><gco:CharacterString>lower Paleocene</gco:CharacterString></keyword><keyword><gco:CharacterString>Mesozoic</gco:CharacterString></keyword><keyword><gco:CharacterString>metals</gco:CharacterString></keyword><keyword><gco:CharacterString>North Atlantic</gco:CharacterString></keyword><keyword><gco:CharacterString>Ocean Drilling Program</gco:CharacterString></keyword><keyword><gco:CharacterString>Paleocene</gco:CharacterString></keyword><keyword><gco:CharacterString>Paleogene</gco:CharacterString></keyword><keyword><gco:CharacterString>paleogeography</gco:CharacterString></keyword><keyword><gco:CharacterString>rare earths</gco:CharacterString></keyword><keyword><gco:CharacterString>SEM data</gco:CharacterString></keyword><keyword><gco:CharacterString>sheet silicates</gco:CharacterString></keyword><keyword><gco:CharacterString>silicates</gco:CharacterString></keyword><keyword><gco:CharacterString>smectite</gco:CharacterString></keyword><keyword><gco:CharacterString>stratigraphic boundary</gco:CharacterString></keyword><keyword><gco:CharacterString>Tertiary</gco:CharacterString></keyword><keyword><gco:CharacterString>Upper Cretaceous</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>-77.0000</gco:Decimal></westBoundLongitude><eastBoundLongitude><gco:Decimal>-76.0000</gco:Decimal></eastBoundLongitude><southBoundLatitude><gco:Decimal>29.3000</gco:Decimal></southBoundLatitude><northBoundLatitude><gco:Decimal>30.3000</gco:Decimal></northBoundLatitude></EX_GeographicBoundingBox></geographicElement><geographicElement><EX_GeographicDescription><geographicIdentifier><MD_Identifier><code><gco:CharacterString>Blake Nose</gco:CharacterString></code></MD_Identifier></geographicIdentifier></EX_GeographicDescription></geographicElement></EX_Extent></extent></MD_DataIdentification></identificationInfo></MD_Metadata>