Picophytoplankton : Bottom-up and top-down controls on ecology and evolution
By J. Raven, Z. Finkel, A. Irwin, Dundee Dd. 2005
105 citations recorded by the source corpus.
View Paper: https://www.semanticscholar.org/paper/26e0181b1380d225531148564ef77f6b47469c66
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Citations in the corpus
- Phytoplankton niches estimated from field data (2012, background): “The absence of diatoms and dinoflagellates with niches low in both macronutrients and irradiance is a consequence of the fact that many of these species are relatively resource intensive compared to many of the lowresource species not observed by the CPR (Raven et al. 2006).”
- The C:N:P stoichiometry of organisms and ecosystems in a changing world: A review and perspectives (2012, background): “More than 30% of the CO2 emitted into the atmosphere over the last 200 year because of the burning of fossil fuels and changes in land use is stored in the oceans (Raven and Falkowski, 1999; Raven et al., 2005).”
- Scaling-up from nutrient physiology to the size-structure of phytoplankton communities (2006, unknown): “…rates for a number of ecologically important taxonomic groups at a reference volume of 1 mm3 (Table II) indicates that except for dinoflagellates, many of which are mixotrophs, larger phytoplankton taxa generally have inherently larger maximum growth rates per unit volume (Raven et al., 2006).”
- Spatio-temporal behaviour of the deep chlorophyll maximum in Mediterranean Sea: Development of a stochastic model for picophytoplankton dynamics (2012, background): “Picoeukaryotes, which belong to the smaller size class, present peculiar eco-physiological properties (Raven et al., 2005; Dimier et al., 2007; Worden and Not, 2008), such as low sinking, high growth rate and low nutrient uptake.”
- Optimal phytoplankton cell size in an allometric model (2009, methodology): “Images: Anne W. Thompson (left); Jim Ehrman, Zoe Finkel, Mount Allison Digital Microscopy Lab (right) Mar Ecol Prog Ser 379: 1–12, 2009 2005) and reduce sinking losses (Raven et al. 2005).”