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  1. 防災科研関係論文

87Sr/86Sr Isotopic Ratio of Ferromanganese Crusts as a Record of Detrital Influx to the Western North Pacific Ocean

https://nied-repo.bosai.go.jp/records/3851
https://nied-repo.bosai.go.jp/records/3851
a3b26f40-1c93-415d-8385-58370a116108
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 en
タイトル 87Sr/86Sr Isotopic Ratio of Ferromanganese Crusts as a Record of Detrital Influx to the Western North Pacific Ocean
言語
言語 eng
著者 Keishiro Azami

× Keishiro Azami

en Keishiro Azami

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Naoto Hirano

× Naoto Hirano

en Naoto Hirano

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Jun-Ichi Kimura

× Jun-Ichi Kimura

en Jun-Ichi Kimura

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Qing Chang

× Qing Chang

en Qing Chang

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Hirochika Sumino

× Hirochika Sumino

en Hirochika Sumino

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Shiki Machida

× Shiki Machida

en Shiki Machida

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Kazutaka Yasukawa

× Kazutaka Yasukawa

en Kazutaka Yasukawa

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Yasuhiro Kato

× Yasuhiro Kato

en Yasuhiro Kato

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抄録
内容記述タイプ Other
内容記述 In this study, the Sr isotope ratios (IRs; 87Sr/86Sr) of ferromanganese (Fe–Mn) crusts are analyzed through laser ablation inductively coupled plasma multiple-collector mass spectrometry. A sample collected from off Minamitorishima Island showed uniform Sr IRs (0.70906–0.70927) similar to that of present-day seawater with more than 36 mm thickness. Meanwhile, a detritus-rich sample collected from off northeast (NE) Japan showed a wide variation in Sr IRs (0.707761–0.709963). The Sr IR variation in the Fe–Mn crust from off NE Japan suggests detrital influx contributions from both the NE Japan arc (<0.708) and aeolian dust from China (>0.718). Detrital flux from the NE Japan arc increases from the bottom to middle layers, possibly due to the uplift of the Ou backbone range that occurred after ~2 Ma. The increased influx of the aeolian dust in the outer layer is attributable to global cooling in the Quaternary that increased the loess dust transportation from China to the western North Pacific Ocean. Meanwhile, the influence of the detrital influx on the sample from off Minamitorishima Island appeared to be negligible. The Sr IR analysis with high spatial resolution proposed in this study possibly improves the burial history of Fe–Mn nodules.
言語 en
書誌情報 en : Minerals

巻 12, 号 8, p. 943-943, 発行日 2022-07-27
出版者
言語 en
出版者 MDPI AG
ISSN
収録物識別子タイプ EISSN
収録物識別子 2075-163X
DOI
関連識別子 10.3390/min12080943
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