Petrography and stratigraphic Os isotopic ages of ferromanganese nodules from the Northwest Pacific east of Minamitorishima Island Article Swipe
Tatsuo Nozaki
,
Kosuke T. Goto
,
Yutaro Takaya
,
Kazuhiko Shimada
,
Akira Owada
,
Gen Shimoda
,
Jun‐Ichi Kimura
,
Qing Chang
,
Tetsuji Onoue
,
Shiki Machida
,
Teruaki Ishii
,
Kenji Shimizu
,
Naoto Hirano
,
Kazuhide Mimura
,
Moei Yano
,
Junichiro Ohta
,
Yasuhiro Kato
·
YOU?
·
· 2024
· Open Access
·
· DOI: https://doi.org/10.1016/j.jaesx.2024.100176
YOU?
·
· 2024
· Open Access
·
· DOI: https://doi.org/10.1016/j.jaesx.2024.100176
The area offshore of Minamitorishima Island, Northwestern Pacific Ocean, contains large amounts of seafloor mineral resources such as ferromanganese (Fe–Mn) nodules, Fe–Mn crusts, and rare-earth element and yttrium (REY)-rich muds. In this study, we applied stratigraphic Os isotopic dating to a Fe–Mn nodule for the first time to date its formation/depositional age, and mineralogical and texturally characterized a complementary nodule. Based on macroscopic and microscopic observations, the studied Fe–Mn nodules can be divided into three layers: Layers L2, L1, and L0 from core to rim. Under the microscope, the Fe–Mn nodules are dominated by vernadite and Fe-oxyhydroxide. In particular, Layer L1 is dominated by banded-columnar vernadite and contains lower amounts of clay minerals derived from the detrital component than Layers L2 and L0. The bulk major and trace element geochemical compositions of sampled layers in the Fe–Mn nodules all plotted in the hydrogenous field in several discrimination diagrams. The Os isotopic ages determined by fitting to the paleo-seawater 187Os/188Os curve can be divided into three clusters (35.7–31.0, 19.0–9.0, and 4.0–1.0 Ma, corresponding to Layers L2, L1, and L0, respectively). These Os isotopic ages indicate that two periods of very slow growth or growth hiatuses occurred during the formation of the Fe–Mn nodule; these age gaps are related to the intermittent (discontinuous) timings of the beginning of Fe–Mn nodule formation offshore Minamitorishima Island.
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- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1016/j.jaesx.2024.100176
- OA Status
- gold
- References
- 78
- Related Works
- 10
- OpenAlex ID
- https://openalex.org/W4392881004
All OpenAlex metadata
Raw OpenAlex JSON
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https://openalex.org/W4392881004Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1016/j.jaesx.2024.100176Digital Object Identifier
- Title
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Petrography and stratigraphic Os isotopic ages of ferromanganese nodules from the Northwest Pacific east of Minamitorishima IslandWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
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2024Year of publication
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2024-03-16Full publication date if available
- Authors
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Tatsuo Nozaki, Kosuke T. Goto, Yutaro Takaya, Kazuhiko Shimada, Akira Owada, Gen Shimoda, Jun‐Ichi Kimura, Qing Chang, Tetsuji Onoue, Shiki Machida, Teruaki Ishii, Kenji Shimizu, Naoto Hirano, Kazuhide Mimura, Moei Yano, Junichiro Ohta, Yasuhiro KatoList of authors in order
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https://doi.org/10.1016/j.jaesx.2024.100176Publisher landing page
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YesWhether a free full text is available
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goldOpen access status per OpenAlex
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https://doi.org/10.1016/j.jaesx.2024.100176Direct OA link when available
- Concepts
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Ferromanganese, Geology, Nodule (geology), Geochemistry, Petrography, Rare-earth element, Trace element, Seawater, Mineralogy, Manganese, Paleontology, Rare earth, Chemistry, Oceanography, Organic chemistryTop concepts (fields/topics) attached by OpenAlex
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0Total citation count in OpenAlex
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78Number of works referenced by this work
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10Other works algorithmically related by OpenAlex
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