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福井県越前海岸に分布する下部中新統国見層の生痕化石群集
http://hdl.handle.net/10098/00028609
http://hdl.handle.net/10098/000286097b83586b-8b2e-4e84-9995-ec8fcef63b27
名前 / ファイル | ライセンス | アクション |
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bd10125777 (33.9 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2021-03-02 | |||||
タイトル | ||||||
タイトル | 福井県越前海岸に分布する下部中新統国見層の生痕化石群集 | |||||
言語 | ||||||
言語 | jpn | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Kunimi Formation | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | trace fossil | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Early Miocene | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Fukui Prefecture | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Ophiomorpha nodosa | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Ophiomorpha ichnofacies | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Psilonichnus ichnofacies | |||||
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 | |||||
その他(別言語等)のタイトル | ||||||
その他のタイトル | Ichnofauna from the Lower Miocene Kunimi Formation along the Echizen Coast, Fukui Prefecture, central Japan | |||||
著者 |
中川, 登美雄
× 中川, 登美雄× 平山, 勝大× 小幡, 喜一 |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Trace fossils from the Lower Miocene (about 18 to 16 Ma) Kunimi Formation in the Echizen Coast area, Fukui Prefecture, central Japan. Ichnofacies clarified that the paleoenvironment in the Kunimi Formation are fluvial foot‒print ichnofacies, tidal flat Psilonichinus ichnofacies and shore Ophiomorpha ichnofacies. The foot‒print ichnofacies occurs in alternation of thin laminated fine‒grained sandstone and mudstone with black mudstone, and is characterized by foot‒print on the bedding plane. The Psilonichnus ichnofacies occurs in bioturbated sandy mudstone and muddy fine‒grained sandstone, and is characterized by vertical and horizontal sand pipe as Psilonichinus tubiformis, Psilonichinus cf. upsilon and Planolites isp. The Ophiomorpha ichnofacies occurs in medium to fine sandstone, and is characterized by Macaronichnus segregatis and Ophiomorpha nodosa. The ichnofacies show that the Kunimi Formation was formed by the repetition of the fluvial and shallow marine environment, and the sedimentary basin became deep gradually. |
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書誌情報 |
日本海地域の自然と環境 : 福井大学地域環境研究教育センター研究紀要 号 27, p. 27-51, 発行日 2020-12-01 |
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出版者 | ||||||
出版者 | 福井大学地域環境研究教育センター | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1343084X | |||||
書誌レコードID | ||||||
識別子タイプ | NCID | |||||
関連識別子 | AN10517316 | |||||
権利 | ||||||
権利情報 | 福井大学 | |||||
関連サイト | ||||||
識別子タイプ | URI | |||||
関連識別子 | https://karin21.flib.u-fukui.ac.jp/webopac/SB10010406 | |||||
関連名称 | 掲載刊行物所蔵情報へのリンク | |||||
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 | |||||
その他のID | ||||||
TD10125777 |