<?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:2001-079995</gco:CharacterString></fileIdentifier><parentIdentifier><gco:CharacterString>georefid:2001-079986</gco:CharacterString></parentIdentifier><contact><CI_ResponsibleParty><organisationName><gco:CharacterString>SEDIS Publication 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(editor), Klaus, A. (editor), Western North Atlantic Palaeogene and Cretaceous palaeoceanography</gco:CharacterString></name><issueIdentification><gco:CharacterString>183</gco:CharacterString></issueIdentification><page><gco:CharacterString>163-183</gco:CharacterString></page></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>Ocean Drilling Program Sites 1001A (Caribbean Sea) and 1050C (western North Atlantic) display obliquity and precession cycles throughout polarity zone C27 of the late Danian stage (earliest Cenozoic time). Sliding-window spectra analysis and direct cycle counting on downhole logs and high-resolution Fe variations at both sites yield the equivalent of 35-36 obliquity cycles. 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