{"created":"2023-07-25T10:29:45.831326+00:00","id":467,"links":{},"metadata":{"_buckets":{"deposit":"74ae2176-344a-42a0-90ab-9131c30a3b73"},"_deposit":{"created_by":3,"id":"467","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"467"},"status":"published"},"_oai":{"id":"oai:shizuoka.repo.nii.ac.jp:00000467","sets":["8:87:117"]},"author_link":["219","415"],"item_25_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Climatic and environmental changes through the Paleogene : review and discussion"}]},"item_25_biblio_info_5":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2003-07","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"58","bibliographicPageStart":"47","bibliographicVolumeNumber":"30","bibliographic_titles":[{"bibliographic_title":"静岡大学地球科学研究報告"}]}]},"item_25_description_30":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_25_description_9":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Climatic and environmental changes through the Paleogene are characterized by some unusual sedimentological and astronomical events. LPTM (Latest Paleocene Thermal Maximum) event is thought to have been produced by an abrupt dissociation of marine sedimentary hydrates along ocean mareins. The abrupt warming that took place 55.5 Ma is one of the pronounced climatic events in the geohistory. Sudden climate cooling event at the Eocene-01igocene boundary might have been caused by multiple or continuous impacts of extraterretrial materials. EXtraordinarily warm climate during the Eocene may have been brought by either vigorous erosion and oxidation of organic carbons exhumed from the early Himalayan orogeny, or by voluminous metamorohic C0_2 degassing due to the regional metaraorphism. Although the first two events (LPTM and E-O boundary event) certainly affected some environmental changes during each geologic time, a longer-term effect of global plate tectonics, particularly the Himalayan orogeny, is of paramount causal importance throughout the Paleogene. I summarize these views of cause and effect for circumstantial changes on the earth surface and duiscuss about them.","subitem_description_type":"Abstract"}]},"item_25_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.14945/00000397","subitem_identifier_reg_type":"JaLC"}]},"item_25_publisher_6":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"静岡大学地球科学教室"}]},"item_25_relation_22":{"attribute_name":"NII論文ID","attribute_value_mlt":[{"subitem_relation_type":"isIdenticalTo","subitem_relation_type_id":{"subitem_relation_type_id_text":"120000795139","subitem_relation_type_select":"NAID"}}]},"item_25_source_id_19":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"03886298","subitem_source_identifier_type":"ISSN"}]},"item_25_source_id_23":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00103190","subitem_source_identifier_type":"NCID"}]},"item_25_subject_8":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"456","subitem_subject_scheme":"NDC"}]},"item_25_version_type_32":{"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":"八木下, 晃司"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-12-14"}],"displaytype":"detail","filename":"KJ00000693012.pdf","filesize":[{"value":"1.6 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00000693012.pdf","url":"https://shizuoka.repo.nii.ac.jp/record/467/files/KJ00000693012.pdf"},"version_id":"351eccbb-98f0-46d1-bd95-2c63b88354f3"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"paleoclimate","subitem_subject_scheme":"Other"},{"subitem_subject":"LPTM","subitem_subject_scheme":"Other"},{"subitem_subject":"E-0 boundary event","subitem_subject_scheme":"Other"},{"subitem_subject":"extraterrestrial materials","subitem_subject_scheme":"Other"},{"subitem_subject":"CO_2","subitem_subject_scheme":"Other"},{"subitem_subject":"degassing Himalayan orogeny","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":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"古第三紀における気候変動 : 近年の研究動向","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"古第三紀における気候変動 : 近年の研究動向"}]},"item_type_id":"25","owner":"3","path":["117"],"pubdate":{"attribute_name":"公開日","attribute_value":"2008-01-25"},"publish_date":"2008-01-25","publish_status":"0","recid":"467","relation_version_is_last":true,"title":["古第三紀における気候変動 : 近年の研究動向"],"weko_creator_id":"3","weko_shared_id":3},"updated":"2024-02-19T05:38:18.360465+00:00"}