The influence of phytoplankton assemblage composition on biogeochemical characteristics and cycles in the southern Ross Sea, Antarctica

By W. Smith, V. Asper. 2001

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In Oceanography

Citations in the corpus

ENVIRONMENTAL FACTORS CONTROLLING PHYTOPLANKTON PROCESSES IN THE SOUTHERN OCEAN1 (2002, background): “Furthermore, in contrast to the PF, in the Ross Sea diatoms are reported to bloom later in the season and in waters characterized by shallower mixed layers (Arrigo et al. 1999, but see Smith and Asper 2001).”
Inorganic carbon uptake by Southern Ocean phytoplankton (2008, background): “In addition, diatoms and the colonial haptophyte Phaeocystis antarctica form extensive blooms in coastal and marginal regions such as the Ross Sea (Smith and Asper 2001).”
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).”
Using HPLC pigment analysis to investigate phytoplankton taxonomy: the importance of knowing your species (2004, background): “Casotti et al. 2000; Belviso et al. 2001; Smith and Asper 2001 ) or in combination with CHEMTAX (e.g.”
Chemical and Biological Studies of Particulate Organic Matter in the Ocean (2002, background): “The plankton is thus the initial source of detrital POM (e.g., Boyd and Newton, 1995, 1999; Smith and Asper, 2001; Bury et al., 2001) and its community structure plays a key role in controlling the recycling and export of organic materials into and out of the euphotic zone.”