{"created":"2023-07-27T06:50:19.862218+00:00","id":43069,"links":{},"metadata":{"_buckets":{"deposit":"2abf7eaa-c3f1-44c5-b1d5-ddc66acf03fd"},"_deposit":{"created_by":18,"id":"43069","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"43069"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00043069","sets":["2812:2813:2823"]},"author_link":["69278","11455"],"item_9_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2012-02-20","bibliographicIssueDateType":"Issued"},"bibliographicPageStart":"5p.","bibliographicVolumeNumber":"2008-2010","bibliographic_titles":[{"bibliographic_title":"平成22(2010)年度 科学研究費補助金 基盤研究(B) 研究成果報告書"},{"bibliographic_title":"2010 Fiscal Year Final Research Report","bibliographic_titleLang":"en"}]}]},"item_9_creator_33":{"attribute_name":"著者別表示","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{}],"nameIdentifiers":[{},{},{},{}]}]},"item_9_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"従来Cenomanian/Turonian境界であると考えられていた層準はCenomanianであり,同境界は従来Coniacianに近いと考えられていた層準であった.その層準は特異な赤色層により構成されており,同時代のテチス海,古大西洋において海洋無酸素事変(OAE2)が生じて黒色泥岩が堆積した状況とは正反対である.このことはOAE2のメカニズム解明に,南太平洋高緯度域が重要な意味を持っている(おそらく寒冷深層水の形成よる)ことを示唆している.","subitem_description_type":"Abstract"},{"subitem_description":"The horizon previously interpreted to be Cenomanian/Turonian boundary was not the boundary. We found that the real boundary located at horizon that believed to have been near Coniacian. The horizon was composed of remarkable red beds. Such condition is opposite to the contemporaneous proto-Atlantic and Tethyan oceanic condition. This finding suggests that Southern Pacific has significant importance for elucidating mechanism of OAE2. Cooler deep water formation near this region during OAE2 could explain the red beds formation.","subitem_description_type":"Abstract"}]},"item_9_description_22":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"研究課題/領域番号:20403016, 研究期間(年度):2008-2010","subitem_description_type":"Other"},{"subitem_description":"出典：研究課題「白亜紀海洋無酸素事変に対する顕著な負のフィードバック: 南西太平洋域の証拠」課題番号20403016\n（KAKEN：科学研究費助成事業データベース（国立情報学研究所）） \n（https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-20403016/20403016seika/）を加工して作成","subitem_description_type":"Other"}]},"item_9_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"金沢大学理工研究域自然システム学系","subitem_description_type":"Other"}]},"item_9_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.24517/00049416","subitem_identifier_reg_type":"JaLC"}]},"item_9_relation_28":{"attribute_name":"関連URI","attribute_value_mlt":[{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/search/?qm=50272943"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/search/?qm=50272943","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20403016/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-20403016/","subitem_relation_type_select":"URI"}},{"subitem_relation_name":[{"subitem_relation_name_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-20403016/20403016seika/"}],"subitem_relation_type_id":{"subitem_relation_type_id_text":"https://kaken.nii.ac.jp/report/KAKENHI-PROJECT-20403016/20403016seika/","subitem_relation_type_select":"URI"}}]},"item_9_version_type_25":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_ab4af688f83e57aa","subitem_version_type":"AM"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-12-21"}],"displaytype":"detail","filename":"SC-PR-HASEGAWA-T-keken 2012-5p.pdf","filesize":[{"value":"281.8 kB"}],"format":"application/pdf","licensetype":"license_11","mimetype":"application/pdf","url":{"label":"SC-PR-HASEGAWA-T-keken 2012-5p.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/43069/files/SC-PR-HASEGAWA-T-keken 2012-5p.pdf"},"version_id":"ecd09a91-6698-4d7a-bdb1-1fba44816f7e"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"research report","resourceuri":"http://purl.org/coar/resource_type/c_18ws"}]},"item_title":"白亜紀海洋無酸素事変に対する顕著な負のフィードバック: 南西太平洋域の証拠","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"白亜紀海洋無酸素事変に対する顕著な負のフィードバック: 南西太平洋域の証拠"},{"subitem_title":"Remarkable negative feedback against Cretaceous Oceanic Anoxic Event: evidence from Southwestern Pacific region","subitem_title_language":"en"}]},"item_type_id":"9","owner":"18","path":["2823"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-12-21"},"publish_date":"2017-12-21","publish_status":"0","recid":"43069","relation_version_is_last":true,"title":["白亜紀海洋無酸素事変に対する顕著な負のフィードバック: 南西太平洋域の証拠"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2023-07-27T13:18:29.772487+00:00"}