Nutrient and carbon removal ratios and fluxes in the Ross Sea

By Colm Sweeney, W. Smith, B. Hales, R. Bidigare, C. Carlson, L. Codispoti, L. Gordon, Dennis A. Hansell, F. Millero, Mi-Ok Park and 1 more. 2000

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Phaeocystis blooms in the global ocean and their controlling mechanisms: a review (2005, background): “In most of these deep-water environments, however, the exported Phaeocystis-derived material is largely remineralised in the mesopelagic zone (Von Bodungen et al., 1986; Wassmann, 1994; Sweeney et al., 2000) with little carbon reaching the deep ocean and the sediment.”
The elemental stoichiometry and composition of an iron‐limited diatom (2005, background): “The current view proposes that differences in taxonomic composition of the phytoplankton community are largely responsible for the non-Redfield N : P and C : P drawdown ratios and is strongly supported by observational data (Arrigo et al. 1999; Sweeney et al. 2000; Smith and Asper 2001).”
Global sea-air CO2 flux based on climatological surface ocean pCO2, and seasonal biological and temperature effects (2002, background): “04231C 1 was determined experimentally by Takahashi et al. (1993) for a North Atlantic surface-water sample.”
The seasonal development of the bacterioplankton bloom in the Ross Sea, Antarctica, 1994-1997 (2001, background): “Sweeney et al. (2000) and Carlson et al. (2000) demonstrate that a significant portion (>4 mol C m-2) of the seasonal NCP is exported vertically out of the surface 150 m.”