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南大洋におけるアルケノン古水温の変動
https://doi.org/10.18999/sumrua.8.81
https://doi.org/10.18999/sumrua.8.8148ee1d0f-5852-470f-8bb4-420c66d4b14c
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 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2010-05-18 | |||||
タイトル | ||||||
タイトル | 南大洋におけるアルケノン古水温の変動 | |||||
その他のタイトル | ||||||
その他のタイトル | Alkenone sea surface temperatures in the Southern Ocean | |||||
著者 |
池原, 実
× 池原, 実× Ikehara, minoru× 河村, 公隆× Kawamura, Kimitaka× 大河内, 直彦× Ohkouchi, Naohiko× 木元, 克典× Kimoto, Katsunori× 村山, 雅史× Murayama, M.× 中村, 俊夫× Nakamura, T.× 大場, 忠道× Oba, T.× 平, 朝彦× Taira, A. |
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権利 | ||||||
権利情報 | 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会 | |||||
権利 | ||||||
権利情報 | 本文データは学協会の許諾に基づきCiNiiから複製したものである | |||||
抄録 | ||||||
内容記述 | A piston core taken from the Tasman Plateau in the Southern Ocean has been studied for organic compounds to reconstruct the late Pleistocene marine environments. Here we report paleo sea surface temperature (SST) for the last two deglaciations using the unsaturation degree of alkenones (U^k_<37'>) preserved in the marine sediments. The U^k_<37'> record indicates that the SST was at least 4℃ lower than the present SST at the last glacial maximum (LGM), and the amplitude of paleo-SST is at most 5.2℃ from the penultimate glacial (MIS-6) to the last interglacial warm period (the Eemian). These results indicate that the amplitude of Southern Ocean SST fluctuation was twice greater than that reported by the CLIMAP projects. This larger amplitude of glacial/interglacial SST change agrees with the SST changes reconstructed from diatom assemblages in the sediments from the Indian sector Southern Ocean, which showed 5-6℃ difference for the glacial/integlacial periods [Pichon et al., 1992]. The SST decrease in the glacial Southern Ocean may be caused by northward shift of the Antarctic Polar Front (APF) at that time. Our results also demonstrate that the Eemian warm period in the Southern Ocean lasted only 3,000 years followed by a sharp cooling at around 120kyrBP. The sharp cooling in the Southern Ocean seemed to occur a few millennia (2-3kyrs) before the beginning of continental ice-sheet growth | |||||
内容記述タイプ | Abstract | |||||
内容記述 | ||||||
内容記述 | タンデトロン加速器質量分析計業績報告 Summaries of Researches Using AMS 1996 (平成8)年度 | |||||
内容記述タイプ | Other | |||||
出版者 | ||||||
出版者 | 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.18999/sumrua.8.81 | |||||
ID登録タイプ | JaLC | |||||
関連情報 | ||||||
関連タイプ | isVersionOf | |||||
識別子タイプ | URI | |||||
関連識別子 | http://ci.nii.ac.jp/naid/110000476020/ | |||||
書誌情報 |
名古屋大学加速器質量分析計業績報告書 巻 8, p. 81-90, 発行日 1997-03 |
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フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher |