{"created":"2023-06-19T08:42:16.220310+00:00","id":483,"links":{},"metadata":{"_buckets":{"deposit":"b90c1243-c390-4b80-aca2-424b2964bc92"},"_deposit":{"created_by":12,"id":"483","owners":[12],"pid":{"revision_id":0,"type":"depid","value":"483"},"status":"published"},"_oai":{"id":"oai:kgwu.repo.nii.ac.jp:00000483","sets":["1:70"]},"author_link":["1103","1104"],"item_10002_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1992","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"232","bibliographicPageStart":"217","bibliographicVolumeNumber":"3","bibliographic_titles":[{"bibliographic_title":"川村学園女子大学研究紀要"},{"bibliographic_title":"The journal of Kawamura Gakuen Woman's University","bibliographic_titleLang":"en"}]}]},"item_10002_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The stratigraphical and geographical distributions of Turonian collignoniceratid ammonites such as Collignoniceras woollgari (Mantell), C. bravaisianum (d'Orbigny), Subprionocyclus neptuni (Geinitz), S. minimus (Hayasaka & Fukada) and Lymaniceras planulatum Matsumoto, which are characteristically found in the Ishikari province, are described in detail. The validity of regional correlations based on their collignoniceratids in various sedimental conditions are also discussed. The differences among the distributions can be explaned by the changes in the sedimentary facies accompanied with transgression or regression. The distribution of Lymaniceras planulatum, which is probably regarded as a member of the \"Sobboreal fauna\", is characterized by its abundant occurrence in the northern areas of the Ishikari province in the Hokkaido Cretaceous. The limited distribution may be interpreted as a result of the upwelling from the Boreal Region where there is a cold water current.","subitem_description_type":"Abstract"}]},"item_10002_description_6":{"attribute_name":"内容記述","attribute_value_mlt":[{"subitem_description":"The stratigraphical and geographical distributions of Turonian collignoniceratid ammonites such as Collignoniceras woollgari (Mantell), C. bravaisianum (d'Orbigny), Subprionocyclus neptuni (Geinitz), S. minimus (Hayasaka & Fukada) and Lymaniceras planulatum Matsumoto, which are characteristically found in the Ishikari province, are described in detail. The validity of regional correlations based on their collignoniceratids in various sedimental conditions are also discussed. The differences among the distributions can be explaned by the changes in the sedimentary facies accompanied with transgression or regression. The distribution of Lymaniceras planulatum, which is probably regarded as a member of the \"Sobboreal fauna\", is characterized by its abundant occurrence in the northern areas of the Ishikari province in the Hokkaido Cretaceous. The limited distribution may be interpreted as a result of the upwelling from the Boreal Region where there is a cold water current.","subitem_description_type":"Other"}]},"item_10002_publisher_8":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"川村学園女子大学"}]},"item_10002_relation_12":{"attribute_name":"論文ID（NAID）","attribute_value_mlt":[{"subitem_relation_type_id":{"subitem_relation_type_id_text":"110000473204","subitem_relation_type_select":"NAID"}}]},"item_10002_source_id_11":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN10179111","subitem_source_identifier_type":"NCID"}]},"item_10002_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"09186050","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"二上, 政夫"},{"creatorName":"フタカミ, マサオ","creatorNameLang":"ja-Kana"}],"nameIdentifiers":[{"nameIdentifier":"1103","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Futakami, Masao","creatorNameLang":"en"}],"nameIdentifiers":[{"nameIdentifier":"1104","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":"2017-07-18"}],"displaytype":"detail","filename":"kiyou3-1 11 futakami.pdf","filesize":[{"value":"826.3 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"研究紀要3-1 11 二上","url":"https://kgwu.repo.nii.ac.jp/record/483/files/kiyou3-1 11 futakami.pdf"},"version_id":"b6cce348-0fa6-472c-8d5f-581a7ac809f1"}]},"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":"チュロニアン・コリンニョニケラス類アンモナイトの分布特性について : 特にメガ化石帯の対比の有効性に関連して","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"チュロニアン・コリンニョニケラス類アンモナイトの分布特性について : 特にメガ化石帯の対比の有効性に関連して"},{"subitem_title":"Distribution of Turonian Collignoniceratid Ammonites in the Ishikari Province of Central Hokkaido, with Special Reference to the Validity of Regional Correlations Based on the Zonal Indices","subitem_title_language":"en"}]},"item_type_id":"10002","owner":"12","path":["70"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-07-18"},"publish_date":"2017-07-18","publish_status":"0","recid":"483","relation_version_is_last":true,"title":["チュロニアン・コリンニョニケラス類アンモナイトの分布特性について : 特にメガ化石帯の対比の有効性に関連して"],"weko_creator_id":"12","weko_shared_id":-1},"updated":"2023-06-19T08:54:40.257661+00:00"}