Representing key phytoplankton functional groups in ocean carbon cycle models: Coccolithophorids

By M. D. Iglesias-Rodriguez, Christopher W. Brown, S. Doney, J. Kleypas, D. Kolber, Z. Kolber, P. Hayes, Paul G. Falkowski. 2002

341 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/7740099ab9c210eccd5d67ef89932f29073eb5b3

How researchers see this paper

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

In Global and Planetary Change

In Oceanography

Citations in the corpus

Poleward expansion of the coccolithophore Emiliania huxleyi (2014, methodology): “Both maps were generated similarly by grouping pixels of weekly global composites of this imagery into coccolithophore bloom and non-bloom classes using a supervised, multispectral algorithm based upon mean remote sensing reflectances (Brown and Yoder, 1994; Iglesias-Rodrı́guez et al., 2002).”
Pelagic functional group modeling: Progress, challenges and prospects (2006, neutral): “These findings were used to construct an empirical probability model that predicts the occurrence of E. huxleyi blooms based upon these environmental constraints (Iglesias-Rodrı́guez et al., 2002).”
Functional groups in marine phytoplankton assemblages dominated by diatoms in fjords of southern Chile (2008, neutral): “coccolithophorids ( Iglesias-Rodriguez, et al. 2002; Smayda, 2002; de Vargas et al., 2007,”
Ecological niches of open ocean phytoplankton taxa (2015, background): “Two well established concepts are (i) plankton functional types (PFTs) (Iglesias-Rodr ıguez et al. 2002; Le Qu er e et al. 2005; Hood et al. 2006), and the Reynolds’ C-S-R model (Reynolds 1988, 2006), which builds on Margalef’s “mandala” model (Margalef 1978).”
Historical climate change and ocean turbulence as selective agents for two key phytoplankton functional groups (2004, background): “…contrast, coccolithophorids have a higher affinity for nitrogen, which allows them to grow in low-nutrient environments, such as the Sargasso Sea, and to bloom in nutrient-depleted temperate seas (Hulburt 1970, Brown & Yoder 1994, Balch et al. 1996, Henriksson 2000, Iglesias-Rodriguez et al. 2002).”
Novel copper‐binding and nitrogen‐rich thiols produced and exuded by Emiliania huxleyi (2004, background): “huxleyi can be very successful in semioligotrophic regions where nitrogen is low (Iglesias-Rodriguez et al. 2002).”
Zinc availability and alkaline phosphatase activity in Emiliania huxleyi: Implications for Zn‐P co‐limitation in the ocean (2006, neutral): “huxleyi blooms (Iglesias-Rodriguez et al. 2002; Kristiansen et al. 1994; Townsend et al. 1994; Tyrrell and Taylor 1996).”
Empirical models of toxigenic Pseudo-nitzschia blooms: Potential use as a remote detection tool in the Santa Barbara Channel (2009, methodology): “Iglesias-Rodriguez et al. (2002) applied parametric thresholds from field data to constrain a model that uses satellite imagery to detect coccolithophorid blooms.”
The 2008 Emiliania huxleyi bloom along the Patagonian Shelf: Ecology, biogeochemistry, and cellular calcification (2013, background): “Such blooms occur in several oceanic (e.g., Iceland Basin) and coastal (e.g., North Sea, Patagonian Shelf) regions of the world’s ocean [Brown and Yoder, 1994; Iglesias-Rodriguez et al., 2002].”