Phytoplankton growth, microzooplankton herbivory and community structure in the southeast Bering Sea: insight into the formation and temporal persistence of an Emiliania huxleyi bloom

By MB Olson, S. Strom. 2002

158 citations recorded by the source corpus.

Subfields: Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/105f4f30e7bafe7375d33a36fd878c56b94ccad1

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Ecology

1. E. Sherr
2. B. Sherr
3. D. Stoecker
4. A. Poulton
5. C. Daniels
6. R. Sheward
7. Peter Lavrentyev
8. J. Stefels

In Oceanography

1. E. Sherr
2. B. Sherr
3. A. Poulton
4. D. Stoecker
5. R. Sheward
6. C. Daniels
7. Michael Steinke
8. Peter Lavrentyev

Citations in the corpus

• Growth physiology and fate of diatoms in the ocean: a review (2005, background): “In coastal, as well as open ocean environments, 45–110% of the standing stock of diatoms can be removed each day by microzooplankton grazing (Verity et al., 1996a; Nejstgaard et al., 1997; Landry et al., 2000a; Calbet, 2001; Strom et al., 2001; Olson and Strom, 2002; Suzuki et al., 2002).”
• Heterotrophic dinoflagellates: a significant component of microzooplankton biomass and major grazers of diatoms in the sea (2007, background): “…major consumers of bloom-forming diatoms In microzooplankton communities of marine systems where diatom blooms occur, heterotrophic dinoflagellates tend to be abundant (Hansen 1991, Archer et al. 2000, Putland 2000, Olson & Strom 2002, Verity et al. 2002, Horner et al. 2005, Leising et al. 2005a).”
• The Bering Sea—A dynamic food web perspective (2007, background): “However, more recent research has emphasized the importance of microzooplankton, with a considerable density of dinoflagellates and ciliates providing a conduit between primary production and upper trophic levels (Olson and Strom, 2002).”
• Mixotrophic Plankton in the Polar Seas: A Pan-Arctic Review (2018, background): “Recent studies in the Arctic indicate that a major portion of pelagic primary production is channeled to the higher trophic levels through unicellular grazers such as ciliates and dinoflagellates (Olson and Strom, 2002; Verity et al., 2002; Calbet et al., 2011b; Sherr et al., 2013; Stoecker et al., ”
• Modelling phytoplankton succession on the Bering Sea shelf: role of climate influences and trophic interactions in generating Emiliania huxleyi blooms 1997 2000 (2004, background): “huxleyi or other flagellates to diatoms (Olson and Strom, 2002).”
• Increases in jellyfish biomass in the Bering Sea: implications for the ecosystem (2002, background): “Since coccolithophores are smaller than diatoms, herbivores that consume coccolithophores might also be expected to be small (Olson & Strom 2002).”
• Biogeochemical implications of comparative growth rates of Emiliania huxleyi and Coccolithus species (2014, background): “Reduced mortality 391 has also been discussed as a possible factor in the formation and persistence of E. huxleyi 392 blooms in the southeast Bering Sea (Olson and Strom, 2002).”
• Environmental constraints on the production and removal of the climatically active gas dimethylsulphide (DMS) and implications for ecosystem modelling (2007, methodology): “…have combined the determination of microzooplankton grazing rates (the Landry-Hassett dilution technique) with DMS(P) analyses and have shown that DMSP-containing algal species may be proportionally less grazed than total algal biomass (Archer et al. 2001b; Olson and Strom 2002; Wolfe et al. 2000).”