Abstract
Continuous X-ray fluorescence scanning of middle Eocene (~46 Ma) core M0002A-55X (~236–241 m
composite depth), recovered during Integrated Ocean Drilling Program Expedition 302, revealed a strong
cyclical signal in some major and trace geochemical elements. We performed a multiproxy study of the same
core, which included organic geochemical, sedimentological, and biological parameters, and
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