書誌事項
- タイトル別名
-
- Transportation of foraminifers in the East China Sea. Sediment trap results from the shelf edge to the slope.
- セジメント トラップ ジッケン ニ モトヅク ヒガシシナカイ リクダナ エンペンイキ ニ オケル ユウコウチュウ ノ ユソウ カテイ
この論文をさがす
抄録
The foraminiferal flux from the shelf edge to the slope of the East China Sea was studied through conventional and time series sediment trap experiments during 27 October to 4 November, 1995. Well preserved planktic foraminifers, poorly preserved planktic foraminifers and benthic foraminifers were observed in both types of sediment traps. Such fact indicates that these foraminifers were suspended from the surface sediments. We also found that the benthic foraminiferal species in the surface sediments at the shelf edge and the uppermost slope site were captured by the sediment trap moored at the shelf edge station, and those in the surface sediment sites from the uppermost slope to the Okinawa Trough were captured by the traps at the uppermost slope station and the upper slope station. Furthermore, based on the foraminiferal flux observation by time series sediment traps at the continental slope, we infer that a great number of foraminifers from the surface sediments were suspended by internal tides, and then some of these foraminifers reached the sediment traps through lateral transportation.
収録刊行物
-
- 地質学雑誌
-
地質学雑誌 107 (1), 15-25, 2001
一般社団法人 日本地質学会
- Tweet
キーワード
詳細情報 詳細情報について
-
- CRID
- 1390001206235541632
-
- NII論文ID
- 110003013144
-
- NII書誌ID
- AN00141768
-
- ISSN
- 13499963
- 00167630
-
- NDL書誌ID
- 5655286
-
- 本文言語コード
- ja
-
- データソース種別
-
- JaLC
- NDL
- Crossref
- CiNii Articles
-
- 抄録ライセンスフラグ
- 使用不可