Top‐down control of phytoplankton biomass and community structure in the monsoonal Arabian Sea

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Contributions of mesozooplankton to vertical carbon export in a coastal upwelling system (2013, background): “At times, mesozooplankton are also able to regulate carbon export rates by exerting top-down grazing pressure on phytoplankton (Goericke 2002, Olli et al. 2007, Landry et al. 2009) or consuming sinking particles (Wilson et al. 2010).”
Response of phytoplankton communities to increased anthropogenic influences (southwestern lagoon, New Caledonia) (2006, background): “Indeed, diatoms and dinoflagellates, which are the major groups of large phytoplankters, exhibit important physiological and ecological differences (Goericke 2002), and, among picophytoplankton cells, Prochlorococcus and Synechococcus may utilize different nitrogen sources (Moore et al. 2002) and…”
Phytoplankton succession and nitrogen utilization during the development of an upwelling bloom (2011, background): “Even when grazing pressure prevents the accumulation of biomass to bloom levels, diatoms have been observed to grow at sufficiently high rates to maintain a major contribution to the biomass (Goericke 2002).”