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  1. 050 理学部
  2. 20 紀要
  3. 02 Science reports of Niigata University. (Geology)
  4. No.11
  1. 0 資料タイプ別
  2. 03 紀要論文

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/10191/47879
be3c76a1-b35e-4306-bb6c-5ebf8905fe1d
名前 / ファイル ライセンス アクション
11_13-33.pdf 11_13-33.pdf (10.1 MB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
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

WEKO 54576

Nguyen, Van Lap

Search repository
Kobayashi, Iwao

× Kobayashi, Iwao

WEKO 54577

Kobayashi, Iwao

Search repository
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
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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