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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. 名古屋大学加速器質量分析計業績報告書
  4. 3

海溝域に於ける有機物の水平輸送について

https://doi.org/10.18999/sumrua.3.104
https://doi.org/10.18999/sumrua.3.104
5aeb617f-7de4-4376-b875-28dc2cf8569c
名前 / ファイル ライセンス アクション
KJ00000187536.pdf KJ00000187536.pdf (353.7 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-04-27
タイトル
タイトル 海溝域に於ける有機物の水平輸送について
その他のタイトル
その他のタイトル Horizontal transport of organic matter in the trench environment
著者 半田, 暢彦

× 半田, 暢彦

WEKO 79536

半田, 暢彦

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Handa, Nobuhiko

× Handa, Nobuhiko

WEKO 79537

Handa, Nobuhiko

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原田, 尚実

× 原田, 尚実

WEKO 79538

原田, 尚実

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Harada, Naomi

× Harada, Naomi

WEKO 79539

Harada, Naomi

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中塚, 武

× 中塚, 武

WEKO 79540

中塚, 武

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Nakatsuka, Takeshi

× Nakatsuka, Takeshi

WEKO 79541

Nakatsuka, Takeshi

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杉本, 多津宏

× 杉本, 多津宏

WEKO 79542

杉本, 多津宏

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Sugimoto, T.

× Sugimoto, T.

WEKO 79543

Sugimoto, T.

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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 Collection of sinking particles by sediment trap experiment was conducted in the Japan and Izu-Ogasawara Trenches to assess the significance of the horizontal transport of organic matter across the interface between the coastal and open ocean areas as well as the vertical transport of chemical materials as often observed in the open ocean. Organic materials of the sinking particles collected from these trench areas was analyzed for δ^<14>C and /or ^<14>C to determine their ^<14>C ages. We found that the organic materials of the sinking particles from these trench areas were much older than those of the sinking particles collected from the open ocean of the eastern and central North Pacific, indicating that sediment once settled in the continental shelf and its slope are most likely source materials of the sinking particles in the trench environment as well as the organic materials produced in the surface water by phytoplankton photosynthesis. We also found that ^<14>C age of the surface sediment in the Hidaka Trough tended to become older toward the center of the Japan Trench, however organic matter of the sinking particles was sometimes determined to be much older than that of the sedimentary organic matter from same depth. This clearly indicates that the sinking particle must be much affected by a particle consisting of organic materials with extremely old age.
内容記述タイプ Abstract
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.3.104
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/110000475801/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 3, p. 104-113, 発行日 1992-03
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