Tarama Knoll: Geochemical and biological profiles of hydrothermal activity

• 資料種別: 図書
• タイトル: Tarama Knoll: Geochemical and biological profiles of hydrothermal activity
• 著者・編者: Yamanaka, Toshiro; Nagashio, Hiromi; Nishio, Ryu; Kondo, Kazuna; Noguchi, Takuroh; Okamura, Kei; Nunoura, Takuro; Makita, Hiroko; Nakamura, Kentaro; Watanabe, Hiromi; Inoue, Kazuhiro; Toki, Tomohiro; Iguchi, Kouichiro; Tsunogai, Urumu; Nakada, Ryoichi; Ohshima, Shogo; Toyoda, Shin; Kawai, Jun; Yoshida, Naohiro; Ijiri, Akira; Sunamura, Michinari
• 著者標目: Yamanaka, Toshiro; Nagashio, Hiromi; Nishio, Ryu; Kondo, Kazuna; Noguchi, Takuroh; Okamura, Kei; Nunoura, Takuro; Makita, Hiroko; Nakamura, Kentaro; Watanabe, Hiromi; Inoue, Kazuhiro; Toki, Tomohiro; Iguchi, Kouichiro; Tsunogai, Urumu; Nakada, Ryoichi; Ohshima, Shogo; Toyoda, Shin; Kawai, Jun; Yoshida, Naohiro; Ijiri, Akira; Sunamura, Michinari
• 出版事項: Springer Japan
• 出版年月日等: 2015-01-10
• 出版年（W3CDTF）: 2015-01-10
• タイトル（掲載誌）: Subseafloor Biosphere Linked to Global Hydrothermal Systems; TAIGA Concept
• 掲載ページ: 497-
• 本文の言語コード: eng
• 件名標目: Hydrothermal activity; Hydrothermal plume; Southern Okinawa Trough; Tarama Knoll
• 対象利用者: 一般
• 一般注記: Tarama Knoll is located about 60 km north of Tarama Island, Sakishima Islands, southwestern Japan. The knoll has an almost conical shape, with foot and summit depths of 2,000 and 1,490 m (total relief = 510 m) from the sea surface, respectively. This area has been identified as a possible active submerged volcano called “Tarama Knoll” (Otani et al. 2004). However, there are actually two separate knolls in the area. This knoll is located northeast of the other, which is named Tarama Hill. During the KT05-26 cruise on the R/V Tanseimaru, a methane anomaly was detected near the seafloor around the area and was considered to be of possible hydrothermal origin. Based on visual observation of the seafloor and its bathymetry, this knoll is considered a pumice cone. Dense turbid water is often observed around summit of the knoll, and a methane anomaly was detected in the water. These observations suggest that the turbid water is a hydrothermal plume. An iron-rich, red-brown sediment-covered area was discovered at a depth of 1,510–1,540 m on the southwestern slope near the summit. At the red-brown sediment area, a weak shimmering of clear fluid could be observed, and the fluid temperature reached 20 °C. Sampled shimmering fluid showed a high silica concentration (≥1 mM), indicating an interaction between the fluid and the surrounding rock. These chemical data support the occurrence of active hydrothermal circulation at Tarama Knoll.; 図書の１章
• 一次資料へのリンクURL: https://u-ryukyu.repo.nii.ac.jp/record/2008855/files/2015_497.pdf （fulltext）; https://u-ryukyu.repo.nii.ac.jp/record/2008855/files/2015_497.pdf
• オンライン閲覧公開範囲: インターネット公開
• 関連情報（DOI）: 10.1007/978-4-431-54865-2_40
• 連携機関・データベース: 国立情報学研究所 : 学術機関リポジトリデータベース（IRDB）（機関リポジトリ）; https://irdb.nii.ac.jp
• 提供元機関・データベース: 琉球大学 : 琉球大学学術リポジトリ