{"created":"2023-07-25T08:06:30.462934+00:00","id":5299,"links":{},"metadata":{"_buckets":{"deposit":"292bf6bf-d437-4875-a196-31425a86703b"},"_deposit":{"created_by":18,"id":"5299","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"5299"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00005299","sets":["228:257:5552","31:32:77"]},"author_link":["3738"],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1999-07-30","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"87","bibliographicPageStart":"81","bibliographicVolumeNumber":"32","bibliographic_titles":[{"bibliographic_title":"南太平洋海域調査研究報告","bibliographic_titleLang":"ja"},{"bibliographic_title":"Occasional papers","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"1999-07-30","subitem_date_issued_type":"Issued"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"Late Pleistocene marine sediments (the Shiroyama, Shirakawa, Kushira, and Natsui\nformations), overlain by the Ata Pyroclastic Flow, are sporadically distributed in\nKagoshima Prefecture. Various lines of information (stratigraphy, lithology, and\npaleontology) imply that these marine sediments are all of the same age, falling within\nOxygen Isotope Stage 7 or 5e. With the exception of the Natsui Formation, Which only\ncontains carbonate shells and tests entirely subjected to dissolution, the foraminiferal\nfaunas of these marine sediments are dominated by the abundant occurrence of Ammonia tepida, an index species of inner and brackish water environments, and Buccella frigida, an\nindex species of nearshore and cold water. The benthic foraminiferal assemblages and\nother fossils suggest that these marine sediments were deposited in inner bay or\nnearshore areas under the influence of brackish water. Foraminifera-bearing mud is\ngenerally 9-33m below the present sea level, with the sample horizons of fossil\nforaminifera in the Shiroyama Formation situated 30-35m above the present sea level.\nThe southern part of the Yoshino Plateau where the Shiroyama Formation is distributed\nhas been uplifted since the Late Pleistocene to tilt southwestward.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_7_relation_32":{"attribute_name":"関連（relation）","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16920","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16921","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16922","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16923","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16924","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16925","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16927","subitem_relation_type_select":"URI"}},{"subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16928","subitem_relation_type_select":"URI"}}]},"item_7_relation_33":{"attribute_name":"関連（isVersionOf）","attribute_value_mlt":[{"subitem_relation_type":"isVersionOf","subitem_relation_type_id":{"subitem_relation_type_id_text":"http://hdl.handle.net/10232/16919","subitem_relation_type_select":"URI"}}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"13450441","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN1013531X","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"450","subitem_subject_scheme":"NDC"}]},"item_7_text_44":{"attribute_name":"備考","attribute_value_mlt":[{"subitem_text_language":"ja","subitem_text_value":"標題紙: http://hdl.handle.net/10232/16919, ポスター: http://hdl.handle.net/10232/16920, はじめに: http://hdl.handle.net/10232/16921, 本文: http://hdl.handle.net/10232/16922, http://hdl.handle.net/10232/16923, http://hdl.handle.net/10232/16924, http://hdl.handle.net/10232/16925, http://hdl.handle.net/10232/16927, http://hdl.handle.net/10232/16928"}]},"item_7_version_type_14":{"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":"大木, 公彦","creatorNameLang":"ja"},{"creatorName":"OKI, Kimihiko","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"3738","nameIdentifierScheme":"WEKO"},{"nameIdentifier":"1000090041235","nameIdentifierScheme":"NRID","nameIdentifierURI":" 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paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"鹿児島県に分布する後期更新世海成層の堆積環境とネオテクトニクス","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"鹿児島県に分布する後期更新世海成層の堆積環境とネオテクトニクス","subitem_title_language":"ja"},{"subitem_title":"Paleoenvironments of the Late Pleistocene Marine Sediments in Kagoshima Prefecture and Neotectonics","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["5552","77"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2015-03-17"},"publish_date":"2015-03-17","publish_status":"0","recid":"5299","relation_version_is_last":true,"title":["鹿児島県に分布する後期更新世海成層の堆積環境とネオテクトニクス"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-07-04T06:03:51.246434+00:00"}