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東シナ海陸棚斜面域における古環境変化
https://doi.org/10.18999/10.19999/sumrua.9.55
91585942-1762-4e15-9dc6-9c7045cfedf8
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 | 2010-05-19 | |||||
タイトル | ||||||
タイトル | 東シナ海陸棚斜面域における古環境変化 | |||||
その他のタイトル | ||||||
その他のタイトル | Paleoenvironmental changes in the continental slope area of the East China Sea | |||||
著者 |
小栗, 一将
× 小栗, 一将× Oguri, Kazumasa× 松本, 英二× Matsumoto, Eiji× 斎藤, 文紀× Saito, Yoshiki |
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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 | One piston core was collected from the East China Sea continental slope during MASFLEX K96-09 cruise. According to the profile of ^<14>C age of planktonic foraminifera, sediment accumulation rate of this core was 40.9 cm/kyr during 15000 to 11400y.B.P., and decreased to be 16.8cm/kyr after 11400y.B.P.. Organic carbon productivity showed maximum at 13500 y.B.P., and stable carbon isotope ratio (δ^<13>C) of organic carbon showed minimum at the time. These phenomena seem to be related to the sea level rise by deglaciation. | |||||
内容記述タイプ | Abstract | |||||
内容記述 | ||||||
内容記述 | 第10回名古屋大学タンデトロン加速器質量分析計シンポジウム(平成9 (1997)年度)報告 「最新型タンデトロン加速器質量分析計(加速器年代測定システム)による高精度・高分解能14C年代測定の利用分野・方法の開拓(II)」 | |||||
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 | 10.18999/10.19999/sumrua.9.55 | |||||
ID登録タイプ | JaLC | |||||
関連情報 | ||||||
関連タイプ | isVersionOf | |||||
関連識別子 | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://ci.nii.ac.jp/naid/110001136043/ | |||||
書誌情報 |
名古屋大学加速器質量分析計業績報告書 巻 9, p. 55-63, 発行日 1998-03 |
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フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher |