Time-series variation of diatom valve fluxes at Station K2 in the western Subarctic Pacific

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  • ONODERA Jonaotaro
    Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology
  • OHASHI Atsushi
    Graduate School of Earth and Planetary Sciences, Faculty of Sciences, Kyushu University
  • TAKAHASHI Kozo
    Graduate School of Earth and Planetary Sciences, Faculty of Sciences, Kyushu University Hokusei Gakuen University
  • C. HONDA Makio
    Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology

Bibliographic Information

Other Title
  • 北西北太平洋定点観測点Station K2における珪藻殻フラックスの時系列変動
  • キタセイホク タイヘイヨウ テイテン カンソクテン Station K2 ニ オケル ケイソウカクフラックス ノ ジケイレツ ヘンドウ

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Description

Time-series variation of diatom sidocoenosis and sinking flux was studied at Station K2 (47°N, 167°E, 5,280 m in water depth) in the western Subarctic Pacific during two study periods (March 2005–June 2006, and November 2009–June 2010).During the first period, the level of diatom flux was similar to those previously observed on the pelagic side of the study area, and the dominant species was Neodenticula seminae, a representative pelagic diatom in the Subarctic Pacific. In the second period, the diatom flux often became much higher than that in the first period, which was due to high dominance of coastal diatoms such as Chaetoceros spp., Thalassiosira nordenskioeldii, and Fragilariopsis spp. Ocean color remote sensing detected a broad water area with high chlorophyll concentration along the east coast of the Kamchatka Peninsula reaching close to Station K2 in May 2009 and 2010. Accordingly, the maximum diatom flux was detected in mid-June 2009. A similar correspondence was previously observed at Station KNOT in 1999.

Journal

  • Diatom

    Diatom 30 (0), 104-121, 2014

    The Japanese Society of Diatomology

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