書誌事項
- タイトル別名
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- Hypolimnetic Transitions and Sand-bar Development in Aso-kai Lagoon (Central Japan) during the Past 1,200 Years, Inferred from Benthic Foraminifera
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Paleoenvironmental changes during the last 1,200 years in Aso-kai Lagoon (central Japan) were inferred from the record of fossil benthic foraminifera in cores ASC2 (4 m length) and Aso4-2 (1.6 m length) taken from the center of the lagoon. Analysis of fossil foraminifera showed an alternation between bay environment and seasonally oxygen-poor brackish environment that was repeated twice in the lower part of these cores (before ∼380 cal BP). Year-round near-anoxia with occasional periods of increased oxygen level was established in the upper part of the cores (after ∼380 cal BP), indicating a restricted lagoon. The temporary increases of the dissolved oxygen level near the lagoon bottom in the upper part of the cores are probably related with sand-bar breaches and channel reopening due to extreme storms since seventeenth century.
収録刊行物
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- 第四紀研究
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第四紀研究 45 (5), 361-373, 2006
日本第四紀学会
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詳細情報 詳細情報について
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- CRID
- 1390282681473197696
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- NII論文ID
- 10023992152
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- NII書誌ID
- AN0034136X
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- ISSN
- 18818129
- 04182642
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- NDL書誌ID
- 8550452
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可