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  1. B. 理工学域; 数物科学類・物質化学類・機械工学類・フロンティア工学類・電子情報通信学類・地球社会基盤学類・生命理工学類
  2. b 10. 学術雑誌掲載論文
  3. 1.査読済論文(理)

Non-Chained, Non-Interacting, Stable Single-Domain Magnetite Octahedra in Deep-Sea Red Clay: A New Type of Magnetofossil?

https://doi.org/10.24517/00067007
https://doi.org/10.24517/00067007
cddb831a-b02a-425d-bf7f-8e8bcb908583
名前 / ファイル ライセンス アクション
TE-PR-USUI-Y-22-e2021GC009770.pdf SC-PR-USUI-Y-22-e2021GC009770.pdf (2.8 MB)
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Item type 学術雑誌論文 / Journal Article(1)
公開日 2022-09-01
タイトル
タイトル Non-Chained, Non-Interacting, Stable Single-Domain Magnetite Octahedra in Deep-Sea Red Clay: A New Type of Magnetofossil?
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ journal article
ID登録
ID登録 10.24517/00067007
ID登録タイプ JaLC
著者 Usui, Yoichi

× Usui, Yoichi

WEKO 106521
e-Rad 20609862

Usui, Yoichi

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Yamazaki, Toshitsugu

× Yamazaki, Toshitsugu

WEKO 106522

Yamazaki, Toshitsugu

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著者別表示 臼井, 洋一

× 臼井, 洋一

臼井, 洋一

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提供者所属
内容記述タイプ Other
内容記述 金沢大学理工研究域地球社会基盤学系
書誌情報 Geochemistry, Geophysics, Geosystems

巻 22, 号 7, p. e2021GC009770, 発行日 2021-06-24
ISSN
収録物識別子タイプ ISSN
収録物識別子 1525-2027
DOI
関連タイプ isIdenticalTo
識別子タイプ DOI
関連識別子 10.1029/2021GC009770
出版者
出版者 American Geophysical Union, Geochemical Society / Wiley Open Access
抄録
内容記述タイプ Abstract
内容記述 Magnetic detection and classification of magnetofossils have been proposed as potential tools for paleoenvironmental studies. Magnetosomes in bacterial species living in different environmental conditions exhibit different grain morphologies and chain configurations, which determine their magnetic properties. Recently, abundant magnetofossils have been reported from unfossiliferous pelagic red clay. However, little is known about their geometry and magnetic properties. Here we report very low coercivity biogenic magnetite in red clay from Ocean Drilling Program (ODP) Site 777 in the northern Mariana Basin. Analyzed sediment showed non-interacting, stable single-domain-like magnetic behaviors. Acquisition of isothermal remanence was decomposed into five components, and a component with mean coercivity below 10 mT accounted for around 25 % of the remanence in some samples. Based on comparisons with semi-quantitative transmission electron microscopy observations of magnetic extracts, this component appears to be carried by octahedral grains with size and shape very similar to biogenic magnetite in red clay from other sites. Micromagnetic calculations indicated that isolated maghemite octahedra may be responsible for the observed low coercivity component. Based on these results, we conclude that the low coercivity component represents non-chained biogenic magnetite that has been oxidized to maghemite. The crystal morphology, geological setting, and lithology do not suggest unusual environmental conditions for ODP Site 777, so the relative amount of chained versus non-chained grains may represent subtle environmental differences. We suggest that non-chained magnetofossils may be widespread in deep-sea sediments. Some methods could overlook the presence of non-chained magnetite, affecting the identification and quantification of magnetofossils. © 2021. American Geophysical Union. All Rights Reserved.
権利
権利情報 Copyright © 2021. American Geophysical Union. All Rights Reserved.
著者版フラグ
出版タイプ VoR
出版タイプResource http://purl.org/coar/version/c_970fb48d4fbd8a85
関連URI
識別子タイプ URI
関連識別子 https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2021GC009770
関連名称 https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2021GC009770
関連URI
識別子タイプ URI
関連識別子 https://agupubs.onlinelibrary.wiley.com/journal/15252027
関連名称 https://agupubs.onlinelibrary.wiley.com/journal/15252027
関連URI
識別子タイプ URI
関連識別子 http://sites.agu.org/
関連名称 http://sites.agu.org/
関連URI
識別子タイプ URI
関連識別子 https://authorservices.wiley.com/open-research/open-access/index.html
関連名称 https://authorservices.wiley.com/open-research/open-access/index.html
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