ネオジム同位体比分析による過去の海洋循環研究

研究成果: ジャーナルへの寄稿学術論文査読

抄録

Neodymium (Nd) isotopic compositions of ferromanganese (Fe–Mn) crusts, bulk sediment leachates, foraminiferal Fe–Mn hydroxides, biogenic apatite, and deep-sea corals have been used as a proxy of Nd isotopes in bottom seawater to reconstruct continental weathering and ocean circulation and mixing changes over various time scales. Proper understanding and appropriate use of this proxy are the basis for more detailed and accurate reconstructions of paleoceanographic variability recorded in marine sediments. In this review, I summarize current knowledge on the behavior of Nd isotopes in the modern ocean and the characteristics of bottom-water Nd isotope proxies to further advance the study of past ocean circulation. In addition, several noteworthy Nd isotope studies are presented to provide basic knowledge to researchers who will work on paleoceanography using Nd isotopes.

寄稿の翻訳タイトルStudies of past ocean circulation based on neodymium isotope analysis
本文言語日本
ページ(範囲)74-92
ページ数19
ジャーナル地球化学
57
2
DOI
出版ステータス出版済み - 2023/06/25

キーワード

  • ネオジム同位体

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