Uranium isotopes as a proxy for primary depositional redox conditions in organic-rich marine systems
Abstract
In marine sediments, authigenic uranium (U) enrichments and U isotope compositions are important tools for interpreting changes in redox conditions, however, their use as paleoproxies requires a comprehensive understanding of the dominant processes that contribute to sediments becoming enriched or depleted. This study focuses on the U content and 238U/235U ratio of organic-rich surface sediments from the Namibian continental margin, where high...
Paper Details
Title
Uranium isotopes as a proxy for primary depositional redox conditions in organic-rich marine systems
Published Date
Jan 1, 2020
Volume
529
Pages
115878 - 115878
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