Modelling phytoplankton succession on the Bering Sea shelf: role of climate influences and trophic interactions in generating Emiliania huxleyi blooms 1997 2000
By Agostino Merico, T. Tyrrell, E. Lessard, Temel Oguz, P. Stabeno, S. Zeeman, T. Whitledge. 2004
89 citations recorded by the source corpus.
Subfields: Oceanography
View Paper: https://www.semanticscholar.org/paper/180b1e1a7f1fb60a52b31aa959dab80b5b7e2ac9
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In Oceanography
- Kevin J. Flynn
- Thomas R. Anderson
- Jorn Bruggeman
- Sebastiaan A. L. M. Kooijman
- T. Tyrrell
- Xabier Irigoien
- R. Harris
- Agostino Merico
Citations in the corpus
- Phytoplankton blooms: a ‘loophole’ in microzooplankton grazing impact? (2005, background): “Such an effect has been shown in field studies where microzooplankton community grazing rates on diatoms and Emiliania huxleyii are usually lower than on the other components of the phytoplankton community (Burkill et al., 1987; Verity et al., 1996; Fileman et al., 2002; Merico et al., 2004).”
- Plankton functional type modelling : running before we can walk? (2005, background): “In similar fashion, Merico et al. (Merico et al., 2004) developed a model of seasonal succession on the Bering Sea shelf that included diatoms, flagellates, dinoflagellates and the coccolithophore Emiliania huxleyi, the timing and duration of E. huxleyi blooms agreeing with remotely sensed data.”
- Nitrate : phosphate ratios and Emiliania huxleyi blooms (2005, background): “…to note as well that E. huxleyi was preferentially grazed in the North Atlantic bloom (Holligan et al. 1993), whereas data (Olson and Strom 2002) and modeling (Merico et al. 2004) of the coastal Bering Sea bloom indicated that reduced grazing was important in bloom initiation and duration.”
- A biodiversity‐inspired approach to aquatic ecosystem modeling (2007, background): “In aquatic ecosystems, biodiversity has historically been extensively studied in terms of phytoplankton competition and succession (Margalef 1978; Tilman 1982; Sommer 1985); to this day, many ecosystem models still aim primarily to resolve and explain the rise and fall of phytoplankton species (Meri”
- Intense stratification leads to phytoplankton nutrient limitation and reduced microzooplankton grazing in the southeastern Bering Sea (2008, unknown): “Chl: chlorophyll in experiment initial samples. development of coccolithophorid blooms that in turn affect higher trophic levels through disruption of microzooplankton grazing and trophic transfer (Stockwell et al., 2001; Olson and Strom, 2002; Merico et al., 2004).”