THE ELEMENTAL COMPOSITION OF SOME MARINE PHYTOPLANKTON 1

By T. Ho, Antonietta Quigg, Z. Finkel, A. Milligan, K. Wyman, Paul G. Falkowski, François M. M. Morel. 2003

724 citations recorded by the source corpus.

Subfields: Health, Toxicology and Mutagenesis, Pollution

View Paper: https://www.semanticscholar.org/paper/17869d6e87330a95a549f98934ab2fe3b2e1e474

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Citations in the corpus

The ciliate-copepod link in marine ecosystems (2005, background): “…in the oceans represents an estimated flux of 1.3 to 1.6 GtN yr–1, of which 0.4 to 0.5 and 0.8 to 1.2 GtN yr–1 would be supplied by ciliate and phytoplankton ingestion, respectively (weight C:Nciliates = 5.0, Stoecker & Capuzzo 1990, Gifford & Caron 2000; and weight C:Nalgae = 6.6, Ho et al. 2003).”
The fate of biogenic iron during a phytoplankton bloom induced by natural fertilisation: Impact of copepod grazing (2008, background): “The same observation holds for laboratory cultures where cells growing under low-Fe conditions exhibit lower percentages of surface-associated Sarthou et al., Deep Sea Research II, 55, 734-751 21/50 Fe (20–30%, Sunda and Huntsman, 1995; Ho et al., 2003).”
The elemental stoichiometry of aquatic and terrestrial ecosystems and its relationships with organismic lifestyle and ecosystem structure and function: a review and perspectives (2011, background): “Redfield ratios in marine phytoplankton (Ho et al. 2003; Klausmeier et al. 2008) and in inorganic dissolved matter in deep oceans have been observed throughout the world (Hecky et al. 1993).”
Effects of iron limitation on intracellular cadmium of cultured phytoplankton: Implications for surface dissolved cadmium to phosphate ratios (2009, methodology): “we multiplied the average phytoplankton Cd:C ratio reported by Ho et al. (2003) (1.43µmol mol−1) by 2.3, to obtain a Cd:C value of 3.3 µmol Cd mol C−1.”
The effects of Cu and Fe availability on the growth and Cu:C ratios of marine diatoms (2008, methodology): “Ho et al. (2003) report values of 0.”
Plankton copper requirements and uptake in the subarctic Northeast Pacific Ocean (2009, background): “Data on the cellular Cu requirements of marine plankton is scarce, and is restricted to a few monospecific phytoplankton cultures (Sunda and Huntsman, 1995; Ho et al., 2003; Annett et al., 2008), particulate Cu:C in surface waters calculated from measured net plankton Cu:P (Martin et al., 1976; Co”
Euglena sp. as a suitable source of lipids for potential use as biofuel and sustainable wastewater treatment (2013, neutral): “Removal of nutrients with a lower N/P ratio of 2:1 is observed compared to the earlier experiments with N/P ratio of 20–11 (Ho et al. 2003; Boelee et al. 2011).”
Element stoichiometries of individual plankton cells collected during the Southern Ocean Iron Experiment (SOFeX) (2004, methodology): “The Mn contents of both diatoms and flagellates were close to the bulk results of Martin and Knauer (1973) and Collier and Edmond (1984) but are almost an order of magnitude below those measured for Southern Ocean plankton (Cullen et al. 2003) or cultured cells (Ho et al. 2003).”
Phytoplankton in a changing world: cell size and elemental stoichiometry (2010, background): “Similarly, commonality in trace element stoichiometry has been interpreted as a reflection of basic biochemical requirements while differences define unique strategies among taxa that determine their environmental niche (Ho et al., 2003; Quigg et al., 2003; Klausmeier et al., 2004; Arrigo, 2005).”
Environmental control of open‐ocean phytoplankton groups: Now and in the future (2010, background): “Although diatoms have physiological Fe require- ments that are lower than most algal groups (Ho et al. 2003), their ability to rapidly outcompete other algae and form blooms following natural or purposeful Fe enrichments results in an influential role in Fe biogeochemistry (Boyd et al. 2007).”
Different reactions of Southern Ocean phytoplankton size classes to iron fertilization (2006, background): “Laboratory experiments have shown that the elemental composition of phytoplankton can differ significantly from the Redfield ratio and that diatoms in general have lower C : P and N : P ratios than other taxonomical phytoplankton groups (Ho et al. 2004; Klausmeier et al. 2004).”
Responses of elemental and biochemical composition of Chaetoceros muelleri to growth under varying light and nitrate : phosphate supply ratios and their influence on critical N: P (2004, background): “To these systematic variations among species (Ho et al. 2003) when cultured under nutrient-replete conditions at one temperature and light level must be added the systematic phenotypic variability within species that arises from growth under nutrient-limiting, light-limiting, or both conditions…”