WEKO3
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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
https://kgwu.repo.nii.ac.jp/records/483
https://kgwu.repo.nii.ac.jp/records/483a700e138-9a94-4365-be3c-0fcf0b420670
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2017-07-18 | |||||
タイトル | ||||||
タイトル | 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 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 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 | |||||
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 | departmental bulletin paper | |||||
著者 |
二上, 政夫
× 二上, 政夫× Futakami, Masao |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | 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. | |||||
内容記述 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 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. | |||||
書誌情報 |
川村学園女子大学研究紀要 en : The journal of Kawamura Gakuen Woman's University 巻 3, 号 1, p. 217-232, 発行日 1992 |
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出版者 | ||||||
出版者 | 川村学園女子大学 | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 09186050 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN10179111 | |||||
論文ID(NAID) | ||||||
識別子タイプ | NAID | |||||
関連識別子 | 110000473204 |