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Holocene lake sediments and sea-level change at Mt. Riiser-Larsen
https://doi.org/10.15094/00003032
https://doi.org/10.15094/00003032061c70cf-2892-41ee-b113-b1a13ba06423
名前 / ファイル | ライセンス | アクション |
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KJ00000044149 (1.0 MB)
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1998-10-01 | |||||
タイトル | ||||||
タイトル | Holocene lake sediments and sea-level change at Mt. Riiser-Larsen | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | sea-level | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | lake sediment | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | raised beach | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Holocene | |||||
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 | |||||
ID登録 | ||||||
ID登録 | 10.15094/00003032 | |||||
ID登録タイプ | JaLC | |||||
ページ属性 | ||||||
内容記述タイプ | Other | |||||
内容記述 | P(論文) | |||||
著者名(英) |
Zwartz, Daniel Peter
× Zwartz, Daniel Peter× Miura, Hideki× Takada, Masashi× Moriwaki, Kiichi |
|||||
著者所属(英) | ||||||
en | ||||||
Research School of Earth Sciences, The Australian National University/National Institute of Polar Research/Department of Socio-geographical and Environmental Studies, Nara Women's University/National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | At sites where glacio-isostatic rebound has occurred, the record of sea-level change can be used to infer the former ice thickness and its melting history At Mt Riiser-Larsen, former sea-levels higher than present are indicated by the presence of raised beach deposits and ancient sediments deposited in brackish water Sediment cores from three ice-marginal lakes contained only fresh-water sediment, and a basal radiocarbon age shows that there has been no marine incursion in the last ~10000 years, limiting sea-level during that time to lower than 18 4m above present A well-defined marine limit is present 15 m a s 1, which will be dated using radiocarbon ages on stranded seals and abandoned penguin rookeries We anticipate an age of ~6 ka, because of the interaction between eustatic and isostatic components of sea-level change | |||||
雑誌書誌ID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA1130866X | |||||
書誌情報 |
Polar geoscience 巻 11, p. 249-259, 発行日 1998-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |