Art
J-GLOBAL ID:200902119741555904   Reference number:01A0493120

Silicate to Nitrate Ratio of the Upper Sub-Arctic Pacific and the Bering Sea Basin in Summer: Its Implication for Phytoplankton Dynamics.

夏期の太平洋上部亜北極海域とベーリング海における珪酸塩/硝酸塩比 植物プランクトン動態への意義
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Material:
Volume: 57  Issue:Page: 253-260  Publication year: Jun. 2001 
JST Material Number: G0159B  ISSN: 0916-8370  Document type: Article
Article type: 原著論文  Country of issue: Germany, Federal Republic of (DEU)  Language: ENGLISH (EN)
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Category name(code) classified by JST.
Geochemistry of hydrosphere and biosphere 
Reference (28):
  • ARCHER, D. Upper ocean physics as relevant to ecosystem dynamics: A tutorial. Ecol. Appl. 1995, 5, 724-739
  • BANSE, K. Comparing phytoplankton seasonality in the eastern and western subarctic Pacific and the western Bering Sea. Progr. Oceanogr. 1999, 43, 235-288
  • BOOTH, B. C. Temporal variation in the structure of autrophic and heterotrophic communities in the subarctic Pacific. Progr. Oceanogr. 1993, 32, 57-99
  • BRZEZINSKI, M. A. The Si:C:N ratio of marine diatoms: Interspecific variability and the effect of some environmental variables. J. Phycol. 1985, 21, 347-357
  • DORTCH, Q. The interaction between ammonium and nitrate uptake in phytoplankton. Mar. Ecol. Prog. Ser. 1990, 61, 183-201
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