Phytoplankton and Their Role in Primary, New, and Export Production

By Paul G. Falkowski, E. Laws, R. Barber, J. Murray. 2003

218 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/94bfafbf94cb60a35108ea142604ad842a1117d5

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In Oceanography

Citations in the corpus

Pelagic functional group modeling: Progress, challenges and prospects (2006, unknown): “We have defined the term ‘‘biogeochemical functional group’’ following Totterdell et al. (1993) and Falkowski et al. (2003) to refer to ‘‘biogeochemical guilds’’, i.e., groups of organisms that mediate a suite of specific chemical reactions that drive biogeochemical cycles in the ocean (though we…”
Mesopelagic fish biomass in the southern California current ecosystem (2015, background): “Similarly, carbon export models have generally ignored the role of mesopelagic fishes in active transport of carbon from near-surface waters to the deep ocean (Buesseler et al., 2007; Falkowski et al., 2003; Longhurst et al., 1990).”
Carbon export mediated by mesopelagic fishes in the northeast Pacific Ocean (2013, background): “Satellite measurements of surface ocean color can be poor predictor of integrated NPP in the NPSG (Letelier and Karl, 1996; Falkowski et al., 2003).”
The Marine Nitrogen Cycle: Overview and Challenges (2008, methodology): “Due to need to spike the phytoplankton sample with NO 3 , the method is problematic to use in oligotrophic gyres (Falkowski et al., 2003).”
Biological overprint of the geological carbon cycle (2005, background): “The radiation of large eucaryotic marine phyto- plankton in the Mesozoic (Grantham and Wakefield, 1988; Moldowan and Jacobson, 2000) that efficiently exported organic matter contributed to an overall increase in export production through time (Bambach, 1993; Falkowski et al., 2003).”