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Holocene Diatom Flora and Sedimentary Environment of the Echigo Plain, Central Honshu, Japan : Part 1 The Analysis of Fukushima-gata Well Core
http://hdl.handle.net/10191/47879
http://hdl.handle.net/10191/47879be3c76a1-b35e-4306-bb6c-5ebf8905fe1d
名前 / ファイル | ライセンス | アクション |
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11_13-33.pdf (10.1 MB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2017-08-31 | |||||
タイトル | ||||||
タイトル | Holocene Diatom Flora and Sedimentary Environment of the Echigo Plain, Central Honshu, Japan : Part 1 The Analysis of Fukushima-gata Well Core | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | Holocene Diatom Flora and Sedimentary Environment of the Echigo Plain, Central Honshu, Japan : Part 1 The Analysis of Fukushima-gata Well Core | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Holocene | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Diatom | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Sedimentary Environment | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Echigo Plain | |||||
キーワード | ||||||
主題Scheme | Other | |||||
主題 | Niigata | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
著者 |
Nguyen, Van Lap
× Nguyen, Van Lap× Kobayashi, Iwao |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Based on ecological spectra, diatoms of the Fukushima-gata well core are grouped into five diatom assemblages, namely marine, marine-brackish, brackish, fresh-brackish and fresh water diatom assemblages. The change of these assemblages is divided into six diatom divisions in ascending order; (1) Fresh water diatom division 1 (FD1) is characterized by a fresh water diatom assemblage.(2) Transitional division 1 (Tr1) is characterized by the alternation of marine and fresh water diatom assemblages. (3) Marine diatom division 1 (MD1) is dominated by a marine diatom assemblage reflecting Holocene transgression. (4) Transitional division 2 (Tr2) which composes of marine and fresh water diatom assemblages indicates a regression after the culmination of the maximum Holocene transgression. (5) Marine diatom division 2 (MD2) indicating a small transgression is dominated by marine diatoms. (6) Fresh water diatom division 2 (FD2) is dominated by fresh water diatoms. It is probably that each diatom division closely related to the development of sedimentation was caused by Holocene sea level and geomorphological changes. | |||||
書誌情報 |
Science reports of Niigata University. (Geology) en : Science reports of Niigata University. (Geology) 巻 11, p. 13-33, 発行日 1996-03 |
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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 |