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The δ^\u003c13\u003eC values of algae from Antarctica are relatively higher than global values. The reason for the relatively high δ^\u003c13\u003eC values of Antarctic algae may be sought in the limited CO_2 (aq) supply for algae in lake water. ^\u003c14\u003eC concentrations of algae from ponds in the First Crater and Crater Hill near McMurdo Station on Ross Island, where glacial meltwater does not flow into the ponds, are close to the global level in the same year. On the other hand, the algae from Richardson Lake in the Mt. Riiser-Larsen area in Enderby Land, where glacial meltwater flows into the lake, apparently have low ^\u003c14\u003eC concentration, ca. 90% of the global level. These facts lead us to the conclusion that the ^\u003c14\u003eC anomaly is attributable to a DIC of relatively low ^\u003c14\u003eC concentration derived from glacial meltwater with older carbon. 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14C anomaly of freshwater algae in Antarctic coastal ponds and lakes
https://doi.org/10.15094/00003056
https://doi.org/10.15094/00003056da4022df-98e5-4b5f-966b-89b26fa22c43
名前 / ファイル | ライセンス | アクション |
---|---|---|
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Item type | 紀要論文(ELS) / Departmental Bulletin Paper(1) | |||||
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公開日 | 1999-10-01 | |||||
タイトル | ||||||
タイトル | 14C anomaly of freshwater algae in Antarctic coastal ponds and lakes | |||||
言語 | ||||||
言語 | eng | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | AMS ^<14>C measurement | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | Antarctic algae | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | ^<14>C anomaly | |||||
キーワード | ||||||
言語 | en | |||||
主題Scheme | Other | |||||
主題 | reservoir effect | |||||
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 | 10.15094/00003056 | |||||
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) |
Takahashi, Hiroshi A.
× Takahashi, Hiroshi A.× Wada, Hideki× Nakamura, Toshio× Miura, Hideki |
|||||
著者所属(英) | ||||||
en | ||||||
Earth and Planetary Sciences, Graduate School of Science, Nagoya University/Biology and Geoscience, Faculty of Science, Shizuoka University/Dating and Materials Research Center, Nagoya University/National Institute of Polar Research | ||||||
抄録(英) | ||||||
内容記述タイプ | Other | |||||
内容記述 | In order to clarify the credibility of ^<14>C dating of Antarctic freshwater algae, δ^<13>C values and ^<14>C concentrations of algae collected from some lakes and ponds in Antarctic coastal areas were analyzed. ^<14>C concentration was measured by Tandetron Accelerator Mass Spectrometry. The δ^<13>C values of algae from Antarctica are relatively higher than global values. The reason for the relatively high δ^<13>C values of Antarctic algae may be sought in the limited CO_2 (aq) supply for algae in lake water. ^<14>C concentrations of algae from ponds in the First Crater and Crater Hill near McMurdo Station on Ross Island, where glacial meltwater does not flow into the ponds, are close to the global level in the same year. On the other hand, the algae from Richardson Lake in the Mt. Riiser-Larsen area in Enderby Land, where glacial meltwater flows into the lake, apparently have low ^<14>C concentration, ca. 90% of the global level. These facts lead us to the conclusion that the ^<14>C anomaly is attributable to a DIC of relatively low ^<14>C concentration derived from glacial meltwater with older carbon. If such samples are used for ^<14>C dating, the age determination will be erroneous. | |||||
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 12, p. 248-257, 発行日 1999-10 |
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出版者 | ||||||
出版者 | National Institute of Polar Research |