WEKO3
インデックスリンク
アイテム
{"_buckets": {"deposit": "4aaa1334-c4f6-4084-bf08-beecf36aff99"}, "_deposit": {"created_by": 3, "id": "10459", "owners": [3], "pid": {"revision_id": 0, "type": "depid", "value": "10459"}, "status": "published"}, "_oai": {"id": "oai:kanazawa-u.repo.nii.ac.jp:00010459", "sets": ["937"]}, "author_link": ["15857", "15861", "15859", "11455", "15858", "15860", "15856"], "item_4_biblio_info_8": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2008-01-01", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "5", "bibliographicPageEnd": "888", "bibliographicPageStart": "878", "bibliographicVolumeNumber": "117", "bibliographic_titles": [{"bibliographic_title": "地學雜誌 = Journal of geography"}]}]}, "item_4_description_21": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Bulk organic carbon isotope (δ13Corg) analyses across the Cenomanian/Turonian boundary in Hokkaido, Japan, and high-resolution planktic foramiferal biostratigraphy indicate that the timing of the planktic foraminiferal disappearance in the northwestern Pacific was significantly earlier than that in the Atlantic region. δ13Corg shows a prominent ∼2‰ positive excursion, clear trough interval, steady plateau interval, and recovery interval, which can be used as very precise chemo-stratigraphic markers. Planktic foraminiferal biostratigraphy demonstrates a pair of diversity crisis at a horizon below the initial δ13Corg excursion and at the beginning of the plateau interval. This isolated double diversity crisis of planktic foraminifers has also been identified in the Western Interior region and northern Europe. The timings of this double diversity crisis in the Western Interior and Europe show quite good consistency on the basis of the δ13C chemo-stratigraphy. On the other hand, the double crisis in the northwestern Pacific is significantly earlier than those in the Western Interior and Europe. This offset indicates that expansion of the oxygen-depleted water mass in the northwestern Pacific preceded that in the Atlantic region.", "subitem_description_type": "Abstract"}]}, "item_4_publisher_17": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "東京地学協会 = Tokyo Geographical Society"}]}, "item_4_relation_12": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type": "isIdenticalTo", "subitem_relation_type_id": {"subitem_relation_type_id_text": "10.5026/jgeography.117.878", "subitem_relation_type_select": "DOI"}}]}, "item_4_relation_28": {"attribute_name": "関連URI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "http://www.geog.or.jp/", "subitem_relation_type_select": "URI"}}, {"subitem_relation_type_id": {"subitem_relation_type_id_text": "https://www.jstage.jst.go.jp/browse/jgeography/-char/ja/", "subitem_relation_type_select": "URI"}}]}, "item_4_rights_23": {"attribute_name": "権利", "attribute_value_mlt": [{"subitem_rights": "Copyright © 2008 Tokyo Geographical Society 東京地学協会 | 許可を得て登録"}]}, "item_4_source_id_11": {"attribute_name": "NCID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00322536", "subitem_source_identifier_type": "NCID"}]}, "item_4_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "0022-135X", "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": "守屋, 和佳"}], "nameIdentifiers": [{"nameIdentifier": "15856", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "60447662", "nameIdentifierScheme": "研究者番号", "nameIdentifierURI": "https://nrid.nii.ac.jp/nrid/1000060447662"}]}, {"creatorNames": [{"creatorName": "長谷川, 卓"}], "nameIdentifiers": [{"nameIdentifier": "11455", "nameIdentifierScheme": "WEKO"}, {"nameIdentifier": "50272943", "nameIdentifierScheme": "e-Rad", "nameIdentifierURI": "https://kaken.nii.ac.jp/ja/search/?qm=50272943"}, {"nameIdentifier": "50272943", "nameIdentifierScheme": "金沢大学研究者情報", "nameIdentifierURI": "http://ridb.kanazawa-u.ac.jp/public/detail.php?kaken=50272943"}, {"nameIdentifier": "50272943", "nameIdentifierScheme": "研究者番号", "nameIdentifierURI": "https://nrid.nii.ac.jp/nrid/1000050272943"}]}, {"creatorNames": [{"creatorName": "成瀬, 貴洋"}], "nameIdentifiers": [{"nameIdentifier": "15857", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "瀬尾, 草平"}], "nameIdentifiers": [{"nameIdentifier": "15858", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "根本, 俊文"}], "nameIdentifiers": [{"nameIdentifier": "15859", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "鈴木, 崇章"}], "nameIdentifiers": [{"nameIdentifier": "15860", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "森本, このみ"}], "nameIdentifiers": [{"nameIdentifier": "15861", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "ファイル情報", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2017-10-03"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "SC-PR-MORIYA-K-878.pdf", "filesize": [{"value": "3.8 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 3800000.0, "url": {"label": "SC-PR-MORIYA-K-878.pdf", "url": "https://kanazawa-u.repo.nii.ac.jp/record/10459/files/SC-PR-MORIYA-K-878.pdf"}, "version_id": "b22a5c19-1174-4f4a-9820-5d7922cec42d"}]}, "item_keyword": {"attribute_name": "キーワード", "attribute_value_mlt": [{"subitem_subject": "海洋無酸素事変", "subitem_subject_scheme": "Other"}, {"subitem_subject": "セノマニアン/チューロニン境界", "subitem_subject_scheme": "Other"}, {"subitem_subject": "炭素同位体比層序", "subitem_subject_scheme": "Other"}, {"subitem_subject": "浮遊性有孔虫化石層序", "subitem_subject_scheme": "Other"}, {"subitem_subject": "絶滅", "subitem_subject_scheme": "Other"}, {"subitem_subject": "北海道", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Oceanic Anoxic Event", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Cenomanian/Turonian boundary", "subitem_subject_scheme": "Other"}, {"subitem_subject": "carbon isotope stratigraphy", "subitem_subject_scheme": "Other"}, {"subitem_subject": "planktic foraminiferal biostratigraphy", "subitem_subject_scheme": "Other"}, {"subitem_subject": "extinction", "subitem_subject_scheme": "Other"}, {"subitem_subject": "Hokkaido", "subitem_subject_scheme": "Other"}]}, "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": "journal article", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "白亜紀中期・セノマニアン/チューロニアン境界の絶滅事変時における有孔虫化石群組成の超高解像度解析", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "白亜紀中期・セノマニアン/チューロニアン境界の絶滅事変時における有孔虫化石群組成の超高解像度解析"}, {"subitem_title": "Ultra-high Resolution Analyses of Foraminiferal Fossil Assemblages of the Cenomanian/Turonian Boundary (Mid-Cretaceous) Extinction Interval", "subitem_title_language": "en"}]}, "item_type_id": "4", "owner": "3", "path": ["937"], "permalink_uri": "http://hdl.handle.net/2297/36198", "pubdate": {"attribute_name": "公開日", "attribute_value": "2017-10-03"}, "publish_date": "2017-10-03", "publish_status": "0", "recid": "10459", "relation": {}, "relation_version_is_last": true, "title": ["白亜紀中期・セノマニアン/チューロニアン境界の絶滅事変時における有孔虫化石群組成の超高解像度解析"], "weko_shared_id": -1}
白亜紀中期・セノマニアン/チューロニアン境界の絶滅事変時における有孔虫化石群組成の超高解像度解析
http://hdl.handle.net/2297/36198
http://hdl.handle.net/2297/36198481ec8cb-1c23-461a-a86f-b3e2678e63b5
名前 / ファイル | ライセンス | アクション |
---|---|---|
SC-PR-MORIYA-K-878.pdf (3.8 MB)
|
|
Item type | 学術雑誌論文 / Journal Article(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2017-10-03 | |||||
タイトル | ||||||
タイトル | 白亜紀中期・セノマニアン/チューロニアン境界の絶滅事変時における有孔虫化石群組成の超高解像度解析 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Ultra-high Resolution Analyses of Foraminiferal Fossil Assemblages of the Cenomanian/Turonian Boundary (Mid-Cretaceous) Extinction Interval | |||||
言語 | ||||||
言語 | jpn | |||||
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 | |||||
著者 |
守屋, 和佳
× 守屋, 和佳× 長谷川, 卓× 成瀬, 貴洋× 瀬尾, 草平× 根本, 俊文× 鈴木, 崇章× 森本, このみ |
|||||
書誌情報 |
地學雜誌 = Journal of geography 巻 117, 号 5, p. 878-888, 発行日 2008-01-01 |
|||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0022-135X | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00322536 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.5026/jgeography.117.878 | |||||
出版者 | ||||||
出版者 | 東京地学協会 = Tokyo Geographical Society | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Bulk organic carbon isotope (δ13Corg) analyses across the Cenomanian/Turonian boundary in Hokkaido, Japan, and high-resolution planktic foramiferal biostratigraphy indicate that the timing of the planktic foraminiferal disappearance in the northwestern Pacific was significantly earlier than that in the Atlantic region. δ13Corg shows a prominent ∼2‰ positive excursion, clear trough interval, steady plateau interval, and recovery interval, which can be used as very precise chemo-stratigraphic markers. Planktic foraminiferal biostratigraphy demonstrates a pair of diversity crisis at a horizon below the initial δ13Corg excursion and at the beginning of the plateau interval. This isolated double diversity crisis of planktic foraminifers has also been identified in the Western Interior region and northern Europe. The timings of this double diversity crisis in the Western Interior and Europe show quite good consistency on the basis of the δ13C chemo-stratigraphy. On the other hand, the double crisis in the northwestern Pacific is significantly earlier than those in the Western Interior and Europe. This offset indicates that expansion of the oxygen-depleted water mass in the northwestern Pacific preceded that in the Atlantic region. | |||||
権利 | ||||||
権利情報 | Copyright © 2008 Tokyo Geographical Society 東京地学協会 | 許可を得て登録 | |||||
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 | http://www.geog.or.jp/ | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | https://www.jstage.jst.go.jp/browse/jgeography/-char/ja/ |