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Radiolarian faunal change in the Middle Permian Gufeng Formation in the Liuhuang section, Chaohu, South China
http://hdl.handle.net/10191/22753
http://hdl.handle.net/10191/22753fdd8179e-abd2-4658-a864-538a2ac7bbd5
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
28_39-49.pdf (4.9 MB)
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| Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2013-07-23 | |||||
| タイトル | ||||||
| タイトル | Radiolarian faunal change in the Middle Permian Gufeng Formation in the Liuhuang section, Chaohu, South China | |||||
| タイトル | ||||||
| タイトル | Radiolarian faunal change in the Middle Permian Gufeng Formation in the Liuhuang section, Chaohu, South China | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | eng | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Radiolarian assemblage | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Middle Permian (Guadalupian) | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Gufeng Formation | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | Lower Yangtze region | |||||
| キーワード | ||||||
| 主題Scheme | Other | |||||
| 主題 | South China | |||||
| 資源タイプ | ||||||
| 資源 | http://purl.org/coar/resource_type/c_6501 | |||||
| タイプ | departmental bulletin paper | |||||
| 著者 |
Ito, Tsuyoshi
× Ito, Tsuyoshi× Feng, Qinglai× Matsuoka, Atsushi |
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| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | Middle Permian (Guadalupian) radiolarians were obtained from bedded siliceous rocks collected from the Gufeng Formation in the Liuhuang section in Chaohu, Anhui Province, South China. Three radiolarian assemblages, named as Pseudoalbaillella fusiformis, Follicucullus monacanthus, and Ruzhencevispongus uralicus, were recovered from the Liuhuang section in an ascending stratigraphic order. The quantitative analysis of radiolarian fauna in the Liuhuang section shows the following characteristics. Albaillellarians and spherical radiolarians occurred more commonly than stauraxon radiolarians, in the lower part; spherical radiolarians are extremely dominant in the middle part; and spherical and stauraxon radiolarians dominate the upper part. In other words, albaillellarians decrease upward in the Liuhuang section, whereas stauraxon and spherical radiolarians increase. This vertical radiolarian faunal change has been reported from the Gufeng Formation in other sections and areas in the Lower Yangtze region. Our findings are in keeping with previous reports, which supports a conclusion that radiolarian faunal change is common throughout the Gufeng Formation in the Lower Yangtze region. | |||||
| 書誌情報 |
Science reports of Niigata University. (Geology) en : Science reports of Niigata University. (Geology) 巻 28, p. 39-49, 発行日 2013-03 |
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| 出版者 | ||||||
| 出版者 | 新潟大学理学部 | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 13491237 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AA11436808 | |||||
| 著者版フラグ | ||||||
| 値 | publisher | |||||
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Cite as
Ito, Tsuyoshi, Feng, Qinglai, Matsuoka, Atsushi, 2013, Radiolarian faunal change in the Middle Permian Gufeng Formation in the Liuhuang section, Chaohu, South China: 新潟大学理学部, 39–49 p.
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