{"created":"2023-07-27T07:00:44.295235+00:00","id":60771,"links":{},"metadata":{"_buckets":{"deposit":"e56d7a4b-fe66-4c07-8942-ba427d753d20"},"_deposit":{"created_by":18,"id":"60771","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"60771"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00060771","sets":["934:935:937"]},"author_link":["106585","106579","106521","106577","106581","106582","106580","106576","59247","106586","106578"],"item_4_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2020-06-18","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageStart":"9896","bibliographicVolumeNumber":"10","bibliographic_titles":[{"bibliographic_title":"Scientific Reports"}]}]},"item_4_creator_33":{"attribute_name":"著者別表示","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"臼井, 洋一"}],"nameIdentifiers":[{},{}]}]},"item_4_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The deep-sea clay that covers wide areas of the pelagic ocean bottom provides key information about open-ocean environments but lacks age-diagnostic calcareous or siliceous microfossils. The marine osmium isotope record has varied in response to environmental changes and can therefore be a useful stratigraphic marker. In this study, we used osmium isotope ratios to determine the depositional ages of pelagic clays extraordinarily rich in fish debris. Much fish debris was deposited in the western North and central South Pacific sites roughly 34.4 million years ago, concurrent with a late Eocene event, a temporal expansion of Antarctic ice preceding the Eocene–Oligocene climate transition. The enhanced northward flow of bottom water formed around Antarctica probably caused upwelling of deep-ocean nutrients at topographic highs and stimulated biological productivity that resulted in the proliferation of fish in pelagic realms. The abundant fish debris is now a highly concentrated source of industrially critical rare-earth elements. © 2020, The Author(s).","subitem_description_type":"Abstract"}]},"item_4_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"金沢大学理工研究域地球社会基盤学系","subitem_description_type":"Other"}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24517/00067016","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_17":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"Nature Research"}]},"item_4_relation_12":{"attribute_name":"DOI","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"10.1038/s41598-020-66835-8","subitem_relation_type_select":"DOI"}}]},"item_4_relation_28":{"attribute_name":"関連URI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"https://www.nature.com/articles/s41598-020-66835-8"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://www.nature.com/articles/s41598-020-66835-8","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://www.nature.com/srep/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://www.nature.com/srep/","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://www.nature.com/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://www.nature.com/","subitem_relation_type_select":"URI"}}]},"item_4_rights_23":{"attribute_name":"権利","attribute_value_mlt":[{"subitem_rights":"Copyright © The Author(s) 2020"},{"subitem_rights":"This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. Te images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/"}]},"item_4_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"2045-2322","subitem_source_identifier_type":"ISSN"}]},"item_4_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Ohta, Junichiro"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Yasukawa, Kazutaka"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Nozaki, Tatsuo"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Takaya, Yutaro"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Mimura, Kazuhide"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Fujinaga, Koichiro"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Nakamura, Kentaro"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Usui, Yoichi"}],"nameIdentifiers":[{},{}]},{"creatorNames":[{"creatorName":"Kimura, Jun-ichi"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Chang, Qing"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"Kato, Yasuhiro"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2022-09-02"}],"displaytype":"detail","filename":"SC-PR-USUI-Y-10-9896.pdf","filesize":[{"value":"3.0 MB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-USUI-Y-10-9896.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/60771/files/SC-PR-USUI-Y-10-9896.pdf"},"version_id":"742ffe03-3a8c-40ca-868e-cd2048ea2bb7"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"journal article","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"Fish proliferation and rare-earth deposition by topographically induced upwelling at the late Eocene cooling event","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Fish proliferation and rare-earth deposition by topographically induced upwelling at the late Eocene cooling event"}]},"item_type_id":"4","owner":"18","path":["937"],"pubdate":{"attribute_name":"公開日","attribute_value":"2022-09-02"},"publish_date":"2022-09-02","publish_status":"0","recid":"60771","relation_version_is_last":true,"title":["Fish proliferation and rare-earth deposition by topographically induced upwelling at the late Eocene cooling event"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T12:30:18.484723+00:00"}